

{"id":261,"date":"2017-06-30T14:27:36","date_gmt":"2017-06-30T18:27:36","guid":{"rendered":"https:\/\/sites.temple.edu\/ncdavatzes\/?page_id=261"},"modified":"2025-07-24T17:57:59","modified_gmt":"2025-07-24T21:57:59","slug":"student-projects-past","status":"publish","type":"page","link":"https:\/\/sites.temple.edu\/ncdavatzes\/research\/student-projects-past\/","title":{"rendered":"Graduate Student Projects (Past)"},"content":{"rendered":"<h2><em><span style=\"text-decoration: underline\"><strong>Projects of Former Graduate Students<\/strong><\/span><\/em><\/h2>\n<h2><\/h2>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-631\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2024-AB-Portrait-150x150.jpeg\" alt=\"\" width=\"150\" height=\"150\" \/> Rebecca Ayanwunmi (<a href=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/AYANWUNMI-Rebecca-2025.pdf\">thesis<\/a>) (MS TU)<\/h2>\n<p>This project focused on quantifying the alteration of the host volcaniclastic rock and how this transformation impacted heat transfer during propagation, flow, and cooling, then basin tectonics and hydrology.<\/p>\n<table style=\"border-collapse: collapse;width: 100%\">\n<tbody>\n<tr>\n<td style=\"width: 100%\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-large wp-image-647 aligncenter\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-GeoMap-1024x692.png\" alt=\"\" width=\"640\" height=\"433\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-GeoMap-1024x692.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-GeoMap-300x203.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-GeoMap-768x519.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-GeoMap-1536x1038.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-GeoMap-2048x1384.png 2048w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/p>\n<p style=\"text-align: center\">(left) Landsat image and (right) map of alteration.<\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-large wp-image-645 aligncenter\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Dike-Outcrop-1024x740.png\" alt=\"\" width=\"640\" height=\"463\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Dike-Outcrop-1024x740.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Dike-Outcrop-300x217.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Dike-Outcrop-768x555.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Dike-Outcrop.png 1224w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/p>\n<p>(upper left) Landsat image of dike outcrop, (upper right) view of dike from across the wash, (lower) outcrop photo of dike contact with host rock on the west side.<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-646 aligncenter\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Effective-Porosity.png\" alt=\"\" width=\"816\" height=\"636\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Effective-Porosity.png 816w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Effective-Porosity-300x234.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-BA-Effective-Porosity-768x599.png 768w\" sizes=\"auto, (max-width: 816px) 100vw, 816px\" \/><\/p>\n<p>Analysis of effective porosity as a function of (upper row) position and (lower row) contact metamorphic facies.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-639\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2024-CK-Portrait-150x150.jpeg\" alt=\"\" width=\"150\" height=\"150\" \/> Colin Krzystek (<a href=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/KRZYSTEK-Colin-2025.pdf\">thesis<\/a>) (MS TU)<\/h2>\n<p>Study of the subsurface geometry of dikes in Surprise Valley to elucidate the process of injection and interaction with basin tectonics.<\/p>\n<table style=\"border-collapse: collapse;width: 100%;height: 72px\">\n<tbody>\n<tr style=\"height: 24px\">\n<td style=\"width: 100%;height: 24px;text-align: center\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-large wp-image-650\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Mag-Survey-Map-1024x367.png\" alt=\"\" width=\"640\" height=\"229\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Mag-Survey-Map-1024x367.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Mag-Survey-Map-300x108.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Mag-Survey-Map-768x275.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Mag-Survey-Map-1536x551.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Mag-Survey-Map-2048x734.png 2048w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/p>\n<p>(left) map of dike outcrops onto Landsat image in the footwall of the Hays Canyon Fault and (right) magnetic surveys of dikes<\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 100%;height: 24px;text-align: center\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-649\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Fig-17-Site-2-Web-version-235x300.jpg\" alt=\"\" width=\"235\" height=\"300\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Fig-17-Site-2-Web-version-235x300.jpg 235w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Fig-17-Site-2-Web-version-801x1024.jpg 801w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Fig-17-Site-2-Web-version-768x982.jpg 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Fig-17-Site-2-Web-version-1202x1536.jpg 1202w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Fig-17-Site-2-Web-version.jpg 1337w\" sizes=\"auto, (max-width: 235px) 100vw, 235px\" \/><\/p>\n<p>Model of magnetic anomaly.<\/td>\n<\/tr>\n<tr style=\"height: 24px\">\n<td style=\"width: 100%;height: 24px;text-align: center\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-large wp-image-648\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension-913x1024.png\" alt=\"\" width=\"640\" height=\"718\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension-913x1024.png 913w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension-268x300.png 268w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension-768x861.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension-1370x1536.png 1370w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension-1826x2048.png 1826w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Extension.png 1887w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/p>\n<p>(a) map of dikes showing cross-section position; (b) cross section of dike geometry; (c) cumulative extension resulting from dike opening in the footwall of the Hays Canyon Fault.<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%;text-align: center\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-large wp-image-651\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Model-1024x720.png\" alt=\"\" width=\"640\" height=\"450\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Model-1024x720.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Model-300x211.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Model-768x540.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Model-1536x1080.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2025\/07\/2025-CK-Model-2048x1439.png 2048w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/p>\n<p>Conceptual model of the evolution of dikes in the Hays Canyon Range.<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-508 size-thumbnail\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/STOWE-Breeann-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/>\u00a0 Breeann Stowe (<a href=\"http:\/\/hdl.handle.net\/20.500.12613\/7736\">thesis<\/a>; <a href=\"https:\/\/www.geothermal-library.org\/index.php?mode=pubs&amp;action=view&amp;record=1034449\">paper<\/a>; <a href=\"https:\/\/www.osti.gov\/biblio\/1823116\">report<\/a>) (BS, MS TU)<\/h2>\n<p>Analysis of core and image logs from the Mount Baker, WA temperature gradient hole.<\/p>\n<table style=\"border-collapse: collapse;width: 35.190616%;height: 609px\">\n<tbody>\n<tr style=\"height: 322px\">\n<td style=\"width: 100%;height: 322px\">\n<p><div id=\"attachment_507\" style=\"width: 2570px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-507\" class=\"wp-image-507 size-full\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-scaled.jpg\" alt=\"\" width=\"2560\" height=\"1094\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-scaled.jpg 2560w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-300x128.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-1024x437.jpg 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-768x328.jpg 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-1536x656.jpg 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-2-FIG-4-Core-Description-2048x875.jpg 2048w\" sizes=\"auto, (max-width: 2560px) 100vw, 2560px\" \/><p id=\"caption-attachment-507\" class=\"wp-caption-text\">Summary of key structural features identified and mapped in core.<\/p><\/div><\/td>\n<\/tr>\n<tr style=\"height: 287px\">\n<td style=\"width: 100%;height: 287px\">\n<p><div id=\"attachment_505\" style=\"width: 224px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-505\" class=\"wp-image-505 size-medium\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-1-FIG-8-9-Correlated-Map-Examples-214x300.png\" alt=\"\" width=\"214\" height=\"300\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-1-FIG-8-9-Correlated-Map-Examples-214x300.png 214w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-1-FIG-8-9-Correlated-Map-Examples-730x1024.png 730w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-1-FIG-8-9-Correlated-Map-Examples-768x1077.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-1-FIG-8-9-Correlated-Map-Examples-1095x1536.png 1095w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-1-FIG-8-9-Correlated-Map-Examples.png 1292w\" sizes=\"auto, (max-width: 214px) 100vw, 214px\" \/><p id=\"caption-attachment-505\" class=\"wp-caption-text\">Comparison of acoustic borehole image log (left) with mapped core (right).<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%\">\n<p><div id=\"attachment_506\" style=\"width: 410px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-506\" class=\"wp-image-506\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-3-FIG-Tadbpole-2022-v2-300x226.png\" alt=\"\" width=\"400\" height=\"301\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-3-FIG-Tadbpole-2022-v2-300x226.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-3-FIG-Tadbpole-2022-v2-1024x772.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-3-FIG-Tadbpole-2022-v2-768x579.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-3-FIG-Tadbpole-2022-v2-1536x1157.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Stowe-3-FIG-Tadbpole-2022-v2-2048x1543.png 2048w\" sizes=\"auto, (max-width: 400px) 100vw, 400px\" \/><p id=\"caption-attachment-506\" class=\"wp-caption-text\">Summary of fracture population mapped in acoustic borehole televiewer log (left) and in core (right). Modified tadpole plot shows the shows the variation in fracture attitude with depth. Note the core reveals far more fractures than are mapped in the image log and a greater diversity of fracture attitude.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>Stowe, B, D Spake, TT Cladouhos, AN Steely, and <strong>NC Davatzes<\/strong>. (2021) Combined Structural Analysis of Core and Image Log of TGH MB76-31 East of Mt Baker, Washington State. Geothermal Resources Council Transactions. v 45, p. 1235-1259. (Geothermal Rising, San Diego, CA October 03, 2011)<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-494 size-thumbnail\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/SAWYER-Morgan-150x150.jpeg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/SAWYER-Morgan-150x150.jpeg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/SAWYER-Morgan.jpeg 200w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Morgan Sawyer (<a href=\"http:\/\/hdl.handle.net\/20.500.12613\/7708\">thesis<\/a>; abstract) (MS TU)<\/h2>\n<p>Investigation of the mechanics of dikes in Surprise Valley, CA and their potential role in crustal fluid flow and geothermal resource potential.<\/p>\n<table style=\"border-collapse: collapse;width: 100%;height: 74px\">\n<tbody>\n<tr style=\"height: 37px\">\n<td style=\"width: 100%;height: 37px\">\n<p><div id=\"attachment_501\" style=\"width: 410px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-501\" class=\"wp-image-501\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-1-Figure-4_7-Site-2-Vert-Seg-Detail-300x239.png\" alt=\"\" width=\"400\" height=\"319\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-1-Figure-4_7-Site-2-Vert-Seg-Detail-300x239.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-1-Figure-4_7-Site-2-Vert-Seg-Detail-1024x817.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-1-Figure-4_7-Site-2-Vert-Seg-Detail-768x613.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-1-Figure-4_7-Site-2-Vert-Seg-Detail-1536x1225.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-1-Figure-4_7-Site-2-Vert-Seg-Detail-2048x1634.png 2048w\" sizes=\"auto, (max-width: 400px) 100vw, 400px\" \/><p id=\"caption-attachment-501\" class=\"wp-caption-text\">A series of washes reveal serial cross sections of a thin frozen dike showing its upper tip and vertical, en echelon segmentation indicating later propagation.<\/p><\/div><\/td>\n<\/tr>\n<tr style=\"height: 37px\">\n<td style=\"width: 100%;height: 37px\">\n<p><div id=\"attachment_502\" style=\"width: 410px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-502\" class=\"wp-image-502\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-2-Figure-6_3-Summary-1024x765.png\" alt=\"\" width=\"400\" height=\"299\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-2-Figure-6_3-Summary-1024x765.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-2-Figure-6_3-Summary-300x224.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-2-Figure-6_3-Summary-768x574.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-2-Figure-6_3-Summary-1536x1147.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Sawyer-2-Figure-6_3-Summary-2048x1530.png 2048w\" sizes=\"auto, (max-width: 400px) 100vw, 400px\" \/><p id=\"caption-attachment-502\" class=\"wp-caption-text\">Model of dike opening in a stratigraphy of variable density. Resulting variation in buoyancy pressure produces variable opening. At the upper tip, insufficient buoyancy pressure is available to open and invade the upper tip of the dike model. Top row depicts a map view, whereas bottom row indicates a cross section through the center of the dike. First column is the tractions imposed on the dike walls due to buoyancy pressure. Middle column is the resulting opening. Right column is the horizontal stress component normal to the dike.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>Sawyer, M, J Glen, <strong>NC Davatzes <\/strong>(2021) Potential role of dikes in damaging rock to support hydrothermal fluid flow, Surprise. <em>AAPG Eastern Section Meeting, October 2-5, 2021, Pittsburg, PA<\/em><\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-495 size-thumbnail\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/SPAKE-Drew-2017-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" \/>\u00a0P Drew Spake (<a href=\"http:\/\/Geothermal Exploration North of Mount Saint Helens, Washington State, USA\" data-wplink-url-error=\"true\">thesis<\/a>; <a href=\"https:\/\/www.osti.gov\/servlets\/purl\/1839984\">paper<\/a>; <a href=\"https:\/\/www.osti.gov\/biblio\/1823116\">report<\/a>) (MS TU)<\/h2>\n<p>Investigation of the geomechanical factors including fracture evolution and stress on the geothermal resource potential of Mount Saint Helens, WA.<\/p>\n<table style=\"border-collapse: collapse;width: 100%\">\n<tbody>\n<tr>\n<td style=\"width: 100%\">\n<p><div id=\"attachment_510\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-510\" class=\"wp-image-510 size-large\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-1-MSH-Map-1024x469.jpg\" alt=\"\" width=\"640\" height=\"293\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-1-MSH-Map-1024x469.jpg 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-1-MSH-Map-300x137.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-1-MSH-Map-768x352.jpg 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-1-MSH-Map-1536x703.jpg 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-1-MSH-Map-2048x938.jpg 2048w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><p id=\"caption-attachment-510\" class=\"wp-caption-text\">Left: Topographic map of Mount Saint Helens and immediate surroundings with earthquakes hypocenters and magnitude from the Pacific Northwest Seismic Network. Right: Cross-section through Mount Saint Helens aligned with the Saint Helens Seismic Zone illustrating the distribution and timing of earthquakes.<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%\">\n<p><div id=\"attachment_503\" style=\"width: 310px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-503\" class=\"wp-image-503 size-medium\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-Overview-300x213.png\" alt=\"\" width=\"300\" height=\"213\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-Overview-300x213.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-Overview-1024x726.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-Overview-768x544.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-Overview.png 1305w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-503\" class=\"wp-caption-text\">Position of detailed structural maps illustrating the fracture and fault patterns in the contact metamorphic aureole around intrusive igneous rock.<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%\">\n<p><div id=\"attachment_509\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-509\" class=\"wp-image-509 size-large\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-1024x663.jpg\" alt=\"\" width=\"640\" height=\"414\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-1024x663.jpg 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-300x194.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-768x497.jpg 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-1536x995.jpg 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-2-Outcrop-Map-2048x1326.jpg 2048w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><p id=\"caption-attachment-509\" class=\"wp-caption-text\">Detailed maps of the contact metamorphic facies and fracture patterns around the intrusion.<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 100%\">\n<p><div id=\"attachment_504\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-504\" class=\"wp-image-504 size-large\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-3-Borhole-Result-1024x701.png\" alt=\"\" width=\"640\" height=\"438\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-3-Borhole-Result-1024x701.png 1024w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-3-Borhole-Result-300x205.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-3-Borhole-Result-768x526.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-3-Borhole-Result-1536x1052.png 1536w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2022\/12\/Spake-3-Borhole-Result-2048x1402.png 2048w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><p id=\"caption-attachment-504\" class=\"wp-caption-text\">Modified tadpole plot, fracture density, static temperature, and stereogram of fracture attitude in a borehole near Mount Saint Helens.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>D. Spake, AN Steely, TT Cladouhos, MW Swyer, C Forson, <strong>NC Davatzes<\/strong>, 2019, Geothermal Exploration North of Mount St. Helens: Washington State Play-Fairway Project, Workshop on Geothermal Reservoir Engineering 44, 19 p.<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-301\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAr0AAAAJGRiNzhmYjgyLTE0YzYtNDVkZS05NTU1LTliZjBmM2UyMTg2OQ-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAr0AAAAJGRiNzhmYjgyLTE0YzYtNDVkZS05NTU1LTliZjBmM2UyMTg2OQ-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAr0AAAAJGRiNzhmYjgyLTE0YzYtNDVkZS05NTU1LTliZjBmM2UyMTg2OQ.jpg 300w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Roselyne Laboso (<a href=\"https:\/\/search-proquest-com.libproxy.temple.edu\/docview\/1858814864?accountid=14270\">thesis<\/a>; <a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2016\/Laboso.pdf\">paper<\/a>; <a href=\"https:\/\/www.osti.gov\/servlets\/purl\/1642469\">report<\/a>) (MS TU)<\/h2>\n<p>Geomechanical analysis of the role of faulting in localizing fracture-hosted geothermal reservoirs at the Bradys Geothermal field, NV.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_280\" style=\"width: 1964px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-280\" class=\"wp-image-280 size-full\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoCartoon.jpg\" alt=\"\" width=\"1954\" height=\"759\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoCartoon.jpg 1954w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoCartoon-300x117.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoCartoon-768x298.jpg 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoCartoon-1024x398.jpg 1024w\" sizes=\"auto, (max-width: 1954px) 100vw, 1954px\" \/><p id=\"caption-attachment-280\" class=\"wp-caption-text\">Tectonic map of surface elevation change in at the Brady Geothermal Field. The impact on the local stress state and fracture potential is explored for idealized geometries of faults in the geothermal field and compared with the distribution of subsidence, subsurface temperature, earthquake hypocenters, and well permeability.<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td>\n<p><div id=\"attachment_282\" style=\"width: 1968px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-282\" class=\"wp-image-282 size-full\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoResult.png\" alt=\"\" width=\"1958\" height=\"810\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoResult.png 1958w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoResult-300x124.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoResult-768x318.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/LabosoResult-1024x424.png 1024w\" sizes=\"auto, (max-width: 1958px) 100vw, 1958px\" \/><p id=\"caption-attachment-282\" class=\"wp-caption-text\">Summary of local stress state in the overlap between two en echelon faults for various spacing configurations. Left: Idealized overlap geometry. Middle: Summary of max coulomb stress in the region between the two simulated faults. Right: stress induced by slip on an example fault model.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>Laboso, R. C. (2016). <i>Fault-controlled damage and permeability at the brady geothermal system, Nevada, U.S.A <\/i>(Order No. 10193609). Available from ProQuest Dissertations &amp; Theses A&amp;I. (1858814864).<\/li>\n<li>\n<div class=\"page\" title=\"Page 3\">\n<div class=\"layoutArea\">\n<div class=\"column\">\n<p>Laboso, R.C., N.C. Davatzes (2016), Fault-Controlled Damage and Permeability at the Brady Geothermal System,Nevada, USA, Proceedings, 41st Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, California, February 22-24, 16p.<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-302\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAX8AAAAJDFiOWQ5N2U5LTI3OTctNGE1ZC05OWE0LTUxMDIwOGZmNmQyYQ-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAX8AAAAJDFiOWQ5N2U5LTI3OTctNGE1ZC05OWE0LTUxMDIwOGZmNmQyYQ-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAX8AAAAJDFiOWQ5N2U5LTI3OTctNGE1ZC05OWE0LTUxMDIwOGZmNmQyYQ-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAX8AAAAJDFiOWQ5N2U5LTI3OTctNGE1ZC05OWE0LTUxMDIwOGZmNmQyYQ.jpg 400w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Olivia Wells (<a href=\"https:\/\/search-proquest-com.libproxy.temple.edu\/docview\/1710061932?accountid=14270\">thesis<\/a>; <a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2015\/Wells.pdf\">paper<\/a>) (MS TU)<\/h2>\n<p>Investigation of the evolution of fracture roughness and dilation accompanying repeated slip with implications for developing an enhanced geothermal system (EGS) at Newberry Volcano, OR.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_284\" style=\"width: 430px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-284\" class=\"wp-image-284\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Wells-Data.png\" alt=\"\" width=\"420\" height=\"221\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Wells-Data.png 900w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Wells-Data-300x158.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Wells-Data-768x404.png 768w\" sizes=\"auto, (max-width: 420px) 100vw, 420px\" \/><p id=\"caption-attachment-284\" class=\"wp-caption-text\">Analysis of dilation history associated with repeated slip on natural fractures in core from well GEO N-2 in the flank of the Newberry Volcano. The pattern reveals two stages of dilation: (1) In the first stage, dilation correlates with primary grain size; (2) In the second stage, dilation is dictated by the linkage of early fractures and natural flaws. The first phase results in significant overall gain in small pores and potential storage for reservoir fluids whereas the second phase results in the largest pore sizes and thus potential increases in permeability.<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td>\n<p><div id=\"attachment_126\" style=\"width: 310px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-126\" class=\"wp-image-126\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2016\/12\/Roughness-263x300.png\" alt=\"\" width=\"300\" height=\"342\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2016\/12\/Roughness-263x300.png 263w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2016\/12\/Roughness.png 662w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-126\" class=\"wp-caption-text\">Conceptual model of the non-linear evolution of secondary porosity as slip increases. Both the grain size of the rock and initial distribution of flaws (small fractures, vugs or vesicles, etc.) control porosity production at small slip. As slip progresses past a critical distance, asperity destruction, gouge production, and fluid-assisted re-mineralization govern a transition to porosity loss.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>\n<div class=\"row\">\n<div class=\"col-md-12\">\n<div class=\"abstract_container \">\n<div id=\"selectable\" class=\"citeThis_background\">\n<p>Wells, O. L. (2015). <i>The evolution of fracture surface roughness and its dependence on slip <\/i>(Order No. 1597133). Available from ProQuest Dissertations &amp; Theses A&amp;I. (1710061932).Wells, O.L. and Davatzes, N.C. (2015) The history of dilation across natural fractures due to evolving surface roughness, Proceedings, Fortieth Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, California, January 28-28, 2015, 12 p.<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-303\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAoAAAAAJGY3MWEzOTllLWI1YzAtNDYzMi05M2Y1LTY1YjdiNjNhZjg1MA-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAoAAAAAJGY3MWEzOTllLWI1YzAtNDYzMi05M2Y1LTY1YjdiNjNhZjg1MA-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAoAAAAAJGY3MWEzOTllLWI1YzAtNDYzMi05M2Y1LTY1YjdiNjNhZjg1MA-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAoAAAAAJGY3MWEzOTllLWI1YzAtNDYzMi05M2Y1LTY1YjdiNjNhZjg1MA.jpg 400w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Justin Roth (<a href=\"https:\/\/search-proquest-com.libproxy.temple.edu\/docview\/1501655565?accountid=14270\">thesis<\/a>;\u00a0<a href=\"http:\/\/pubs.geothermal-library.org\/lib\/grc\/1030571.pdf\">paper<\/a>) (MS TU)<\/h2>\n<p>Investigation of two- and three-dimensional porosity structure in fractured volcanic rocks at Newberry Volcano, OR with implications for geothermal resource potential.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_286\" style=\"width: 554px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-286\" class=\"wp-image-286\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Roth-Data.png\" alt=\"\" width=\"544\" height=\"344\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Roth-Data.png 935w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Roth-Data-300x190.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Roth-Data-768x485.png 768w\" sizes=\"auto, (max-width: 544px) 100vw, 544px\" \/><p id=\"caption-attachment-286\" class=\"wp-caption-text\">Detailed mapping of porosity structure in a multiply reactivated natural fracture from GEO N-2 core in the flank of the Newberry Volcano.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<div class=\"row\">\n<div class=\"col-md-12\">\n<div class=\"abstract_container \">\n<div id=\"selectable\" class=\"citeThis_background\">\n<ul>\n<li>Roth, J. M. (2014). <i>Investigating the volume and structure of porosity in fractured and unfractured rocks from the newberry volcano, oregon: An evaluation and comparison of two- and three-dimensional methods <\/i>(Order No. 1552297). Available from ProQuest Dissertations &amp; Theses A&amp;I. (1501655565).<\/li>\n<li>Roth, J., Davatzes, N.C., Davatzes, A.E.K. (2013) Investigating the volume and structure of porosity in fractured and unfractured rock from the Newberry volcano, Oregon, USA: Evaluation of two- and three-dimensional methods. Geothermal Resources Council Annual Meeting, Las Vegas, NV, September 29-October 2, 2013. 10 p.<\/li>\n<\/ul>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<div class=\"row\">\n<hr \/>\n<\/div>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-304\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/179c49c-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/179c49c-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/179c49c.jpg 227w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Michael Swyer (<a href=\"https:\/\/search-proquest-com.libproxy.temple.edu\/docview\/1294851926?accountid=14270\">thesis<\/a>:\u00a0<a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2012\/Swyer.pdf\">paper\u00a01<\/a>, <a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2013\/Swyer.pdf\">paper 2<\/a>) (MS TU)<\/h2>\n<p>Impact of rock mechanical properties and potential slip on the rhyolite ridge fault in the Desert Peak geothermal field, NV on the potential to expand the resource into hot impermeable rock.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_291\" style=\"width: 620px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-291\" class=\"wp-image-291\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Swyer-2.png\" alt=\"\" width=\"610\" height=\"339\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Swyer-2.png 1977w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Swyer-2-300x167.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Swyer-2-768x427.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Swyer-2-1024x570.png 1024w\" sizes=\"auto, (max-width: 610px) 100vw, 610px\" \/><p id=\"caption-attachment-291\" class=\"wp-caption-text\">(a) Tracer analysis shows pre-stimulation isolation of well 27-15 and post-stimulation connection. (b) Simulated direction of SHmax due to slip on the Rhyolite Ridge fault to remote loading by Basin and Range Extension. In normal fault stress regimes it is assumed this coincides with the preferred strike of normal faults and joints. (c) Slip and (d) slip tendency (ration of shear to effective normal tractions) simulated on the Rhyolite Ridge fault. (e) Seismicity in the vicinity of the geothermal field (re-injection wells are blue, production wells are red, and the study site is a gray square).<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_283\" style=\"width: 324px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-283\" class=\"wp-image-283\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/ClayFrictionPerm.png\" alt=\"\" width=\"314\" height=\"298\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/ClayFrictionPerm.png 896w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/ClayFrictionPerm-300x285.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/ClayFrictionPerm-768x730.png 768w\" sizes=\"auto, (max-width: 314px) 100vw, 314px\" \/><p id=\"caption-attachment-283\" class=\"wp-caption-text\">Analysis of how clay in fault rock controls key fault properties. Increasing clay content reduces both the friction and permeability of fault rock. The relationship is non -linear; a clay fraction beyond a critical threshold is associated with a transition to the clay-end member properties. The properties and critical clay-fraction are mineral dependent. (This analysis was performed at the USGS rock mechanics laboratory as a summer research project by Mike separate from the main focus of his thesis work.)<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<div class=\"row\">\n<div class=\"col-md-12\">\n<div class=\"abstract_container \">\n<div id=\"selectable\" class=\"citeThis_background\">\n<ul>\n<li>Swyer, M. W. (2013). <i>Evaluating the role of the rhyolite ridge fault system in the desert peak geothermal field, NV: Boundary element modeling of fracture potential in proximity of fault slip <\/i>(Order No. 1533315). Available from ProQuest Dissertations &amp; Theses A&amp;I. (1294851926).<\/li>\n<li>Swyer, M.W. and Davatzes, N.C. (2013) Evaluating the role of the Rhyolite Ridge fault system in the Desert Peak Geothermal Field with robust sensitivity testing through boundary element modeling and likelihood analysis, PROCEEDINGS, Thirty-Eight Workshop on Geothermal Reservoir Engineering, Stanford, California, February 11-February 13, SGP-TR-194, 16 p.<\/li>\n<li class=\"page\" title=\"Page 4\">\n<div class=\"layoutArea\">\n<div class=\"column\">\n<div class=\"page\" title=\"Page 4\">\n<div class=\"layoutArea\">\n<div class=\"column\">\n<p>Swyer, M.W. and Davatzes, N.C. (2012) Using Boundary Element Modeling of Fault Slip to Predict Patterns of stress Perturbation and Related Fractures in Geothermal Reservoirs and Explore Parameter Uncertainty, Proceedings, Thirty-Seventh Workshop on Geothermal Reservoir Engineering, Stanford, California, January 30-February 1, SGP-TR-194, 14 p.<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<div class=\"row\">\n<hr \/>\n<\/div>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-305\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAiSAAAAJDQxMTM0YmJkLTI1MDUtNGE0Yi1iMWFmLTkwMTkxYTQwYTA2Nw-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAiSAAAAJDQxMTM0YmJkLTI1MDUtNGE0Yi1iMWFmLTkwMTkxYTQwYTA2Nw-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAiSAAAAJDQxMTM0YmJkLTI1MDUtNGE0Yi1iMWFmLTkwMTkxYTQwYTA2Nw-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAiSAAAAJDQxMTM0YmJkLTI1MDUtNGE0Yi1iMWFmLTkwMTkxYTQwYTA2Nw.jpg 398w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Kelly Blake (<a href=\"https:\/\/search-proquest-com.libproxy.temple.edu\/docview\/900865609?accountid=14270\">thesis<\/a>; <a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2011\/blake.pdf\">paper\u00a01<\/a>, <a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2012\/Blake.pdf\">paper 2<\/a>) (MS TU)<\/h2>\n<p>Analysis of stress heterogeneity in the vicinity of the Coso Geothermal field, CA.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_295\" style=\"width: 489px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-295\" class=\"wp-image-295\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Picture1.png\" alt=\"\" width=\"479\" height=\"278\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Picture1.png 1553w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Picture1-300x174.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Picture1-768x446.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Picture1-1024x594.png 1024w\" sizes=\"auto, (max-width: 479px) 100vw, 479px\" \/><p id=\"caption-attachment-295\" class=\"wp-caption-text\">(left) Visualization of stress concentration around a borehole can (middle left)) induce tensile or compressive failure of the borehole wall evident in acoustic (resistivity, and optical) image logs. (middle right) The shape and position of these structures same the stress state resolved on the borehole wall and is used to infer the local stress tensor. (right) In Coso and other sites we observe that the directions in which the principal stresses acts varies along the borehole relative to an overall mean. This variation occurs within a family of wavelengths and amplitudes whose relative contribution is assessed as a power spectral density.<\/p><\/div><\/td>\n<\/tr>\n<tr>\n<td>\n<p><div id=\"attachment_290\" style=\"width: 549px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-290\" class=\"wp-image-290\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Blake-2.png\" alt=\"\" width=\"539\" height=\"392\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Blake-2.png 1299w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Blake-2-300x218.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Blake-2-768x559.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Blake-2-1024x745.png 1024w\" sizes=\"auto, (max-width: 539px) 100vw, 539px\" \/><p id=\"caption-attachment-290\" class=\"wp-caption-text\">Map of the preferred direction of SHmax +\/- one standard deviation in geothermal fields in the west-central Basin and Range of Nevada. In normal faulting terrains, SHmax is generally expected to align with the strike of active normal faults that define the ranges and will be orthogonal to the overall extension direction expressed by the gradient in the GPS velocity vector field.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>Blake, K. (2011). <i>Crustal stress heterogeneity in the vicinity of a geothermal field: Coso geothermal field, CA <\/i>(Order No. 1500799). Available from ProQuest Dissertations &amp; Theses A&amp;I. (900865609).<\/li>\n<li>Blake, K. and Davatzes, N.C. (2012) Borehole Image Log and Statistical Analysis of FOH-3D, Fallon Naval Air Station, NV, Proceedings, Thirty-Seventh Workshop on Geothermal Reservoir Engineering, Stanford, California, January 30-February 1, SGP-TR-194, 14 p.<\/li>\n<li>Blake, K. and Davatzes, N.C. (2011) Stress Heterogeneity in the Vicinity of the Coso Geothermal Field. Proceedings Thirty-Fifth Workshop on Geothermal Reservoir Engineering, Stanford University, Stanford, California. 11 p.<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-306\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAs8AAAAJDA5YjNlZjhjLWM3YzYtNGNhZi05ZTdmLTc5NzA1ZmQwY2Q5Yg-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAs8AAAAJDA5YjNlZjhjLWM3YzYtNGNhZi05ZTdmLTc5NzA1ZmQwY2Q5Yg-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAs8AAAAJDA5YjNlZjhjLWM3YzYtNGNhZi05ZTdmLTc5NzA1ZmQwY2Q5Yg-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAs8AAAAJDA5YjNlZjhjLWM3YzYtNGNhZi05ZTdmLTc5NzA1ZmQwY2Q5Yg.jpg 400w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Nwachukwu Anyamele (<a href=\"http:\/\/dx.doi.org\/10.34944\/dspace\/8199\">thesis<\/a>; <a href=\"http:\/\/www.searchanddiscovery.com\/abstracts\/html\/2009\/annual\/abstracts\/anyamele.htm\">abstract<\/a>) (MS TU)<\/h2>\n<p>Investigation of the source of clay in the Moab Fault, UT.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_347\" style=\"width: 516px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-347\" class=\"wp-image-347\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-1-copy.png\" alt=\"\" width=\"506\" height=\"342\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-1-copy.png 980w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-1-copy-300x202.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-1-copy-768x518.png 768w\" sizes=\"auto, (max-width: 506px) 100vw, 506px\" \/><p id=\"caption-attachment-347\" class=\"wp-caption-text\">Conceptual model of how faults can incorporate clay-rich material into a fault zone crossing layered sandstone and shale.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_299\" style=\"width: 394px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-299\" class=\"wp-image-299\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-2.png\" alt=\"\" width=\"384\" height=\"422\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-2.png 730w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Anyamele-2-273x300.png 273w\" sizes=\"auto, (max-width: 384px) 100vw, 384px\" \/><p id=\"caption-attachment-299\" class=\"wp-caption-text\">A key issue in fault zone development is the source of fault rock, which can be a combination of mechanically incorporated host rock or authigenically precipitated minerals. Formation of new minerals is promoted by mechanical fracture and grain size reduction exposing new, larger surface area to reaction and simultaneously facilitating fluid flow. In the fault zone we can explore the relative contribution of these two mechanisms by comparing the mineralogy and chemistry of a sample of fault rock to the host rocks dragged past the sample location.<\/p><\/div><\/td>\n<td><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>\n<div class=\"page\" title=\"Page 6\">\n<div class=\"layoutArea\">\n<div class=\"column\">\n<p>Anyamele, N., Davatzes, N.C., and Solum, J. G. (2009). Sources of clay in fault rock of the Moab Fault, Utah. American Association of Petrolem Geologists\/Society for Sedimentary Geology joint annual meeting, Denver, Colorado.<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-307\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAaiAAAAJGJlM2ZmYzRmLTIwNTYtNGRhZS1hZGE5LTc4ZDEwNTM4Zjg1Zg-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAaiAAAAJGJlM2ZmYzRmLTIwNTYtNGRhZS1hZGE5LTc4ZDEwNTM4Zjg1Zg-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAaiAAAAJGJlM2ZmYzRmLTIwNTYtNGRhZS1hZGE5LTc4ZDEwNTM4Zjg1Zg-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAaiAAAAJGJlM2ZmYzRmLTIwNTYtNGRhZS1hZGE5LTc4ZDEwNTM4Zjg1Zg.jpg 400w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Joseph Batir (<a href=\"http:\/\/skemman.is\/en\/item\/view\/1946\/7758\">thesis<\/a>; <a href=\"https:\/\/www.geothermal-energy.org\/pdf\/IGAstandard\/SGW\/2012\/Batir.pdf\">paper<\/a>) (MS RES)<\/h2>\n<p>Investigating the stress state of the Hellisheidi geothermal field, IS.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_296\" style=\"width: 1497px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-296\" class=\"wp-image-296 size-full\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/BATIR-1.png\" alt=\"\" width=\"1487\" height=\"906\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/BATIR-1.png 1487w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/BATIR-1-300x183.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/BATIR-1-768x468.png 768w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/BATIR-1-1024x624.png 1024w\" sizes=\"auto, (max-width: 1487px) 100vw, 1487px\" \/><p id=\"caption-attachment-296\" class=\"wp-caption-text\">Observations of stress in Iceland from the world stress map.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<table>\n<tbody>\n<tr>\n<td style=\"text-align: center\">\n<p><div id=\"attachment_297\" style=\"width: 455px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-297\" class=\"wp-image-297\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Batir-3.png\" alt=\"\" width=\"445\" height=\"380\" \/><p id=\"caption-attachment-297\" class=\"wp-caption-text\">Resolution of the stress tensor onto an arbitrarily oriented borehole surface. The cavity introduced by the borehole concentrates the stress which can cause the borehole wall to fail. The position and shape of these failure structures is used to infer the stress state (direction of principal stresses and their magnitudes) in the rock where they occur. (left) Illustration of the relationship between the borehole and stress tensor. (middle) Position of induced borehole failure structures on the deviated borehole surface as well as deviation data. (right) Model of SHmax azimuth as constrained by a vertical stress calculated from a model of rock density and a model of the unconfined compressive rock strength.<\/p><\/div><\/td>\n<td><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>\n<div class=\"page\" title=\"Page 4\">\n<div class=\"layoutArea\">\n<p class=\"column\">Batir, J., Davatzes, N.C., and Asmundsson, R. (2012) Preliminary State of Stress of the Hellisheidi Geothermal Field, Hengill Volcanic Zone, Iceland, Proceedings, Thirty-Seventh Workshop on Geothermal Reservoir Engineering, Stanford, California, January 30-February 1, SGP-TR-194, 17 p.<\/p>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-308\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAupAAAAJGU2NTYxOTczLWUyMjctNDY0MC05MDZlLTI3ZDE1YzQ5YTZkMQ-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAupAAAAJGU2NTYxOTczLWUyMjctNDY0MC05MDZlLTI3ZDE1YzQ5YTZkMQ-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAupAAAAJGU2NTYxOTczLWUyMjctNDY0MC05MDZlLTI3ZDE1YzQ5YTZkMQ-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/AAEAAQAAAAAAAAupAAAAJGU2NTYxOTczLWUyMjctNDY0MC05MDZlLTI3ZDE1YzQ5YTZkMQ.jpg 400w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Drew Fetterman\u00a0(<a href=\"http:\/\/hdl.handle.net\/1946\/7748\">thesis<\/a>; <a href=\"http:\/\/pubs.geothermal-library.org\/lib\/grc\/1029261.pdf\">paper<\/a>) (MS RES)<\/h2>\n<p>Investigation of the porosity history of natural fractures in volcanic rock of the Newberry Volcano, OR.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_287\" style=\"width: 184px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-287\" class=\"wp-image-287\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Fetterman-Example-295x300.png\" alt=\"\" width=\"174\" height=\"177\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Fetterman-Example-295x300.png 295w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Fetterman-Example.png 478w\" sizes=\"auto, (max-width: 174px) 100vw, 174px\" \/><p id=\"caption-attachment-287\" class=\"wp-caption-text\">Porosity mapped in GEO N-2 core from the flank of the Newberry Volcano.<\/p><\/div><\/td>\n<td>\n<p><div id=\"attachment_288\" style=\"width: 354px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-288\" class=\"wp-image-288\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/FettermanConcept-300x153.png\" alt=\"\" width=\"344\" height=\"175\" \/><p id=\"caption-attachment-288\" class=\"wp-caption-text\">Fracture thickness and porosity observed in core from GEO N-2 in the flank of the Newberry Volcano, OR. Mapping of component structures is used to infer the relative accumulated slip and maturity of the fractures. Red indicates fractures with abundant quartz and calcite relative to phyllosilicates. Blue indicates fractures relatively enriched in phyllosilicates.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>\n<div class=\"page\" title=\"Page 4\">\n<div class=\"layoutArea\">\n<div class=\"column\">Fetterman, J.D. and Davatzes, N.C. (2011) Evolution of Fracture Porosity in the Newberry Volcano Geothermal System, Oregon, USA: Feedback between deformation and alteration. Geothermal Resources Council Annual Meeting, San Diego, CA. 7 p.<\/div>\n<div class=\"column\">\n<hr style=\"font-size: 12px\" \/>\n<\/div>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-thumbnail wp-image-309\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/342dba3-150x150.jpg\" alt=\"\" width=\"150\" height=\"150\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/342dba3-150x150.jpg 150w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/342dba3-300x300.jpg 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/342dba3.jpg 400w\" sizes=\"auto, (max-width: 150px) 100vw, 150px\" \/>\u00a0 Amelia Letvin (thesis) (MS RES)<\/h2>\n<p>Mineralogy and alteration history along the Enhanced Geothermal Systems (EGS) test well 55-29, Newberry Volcano, OR.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_289\" style=\"width: 975px\" class=\"wp-caption alignnone\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-289\" class=\"wp-image-289 size-full\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Letvin-Figure.png\" alt=\"\" width=\"965\" height=\"691\" srcset=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Letvin-Figure.png 965w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Letvin-Figure-300x215.png 300w, https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/Letvin-Figure-768x550.png 768w\" sizes=\"auto, (max-width: 965px) 100vw, 965px\" \/><p id=\"caption-attachment-289\" class=\"wp-caption-text\">Summary of characteristics along EGS test well NWG 55-29. (panel 1) Relative abundance of cuttings minerals. (panel 2) Natural gamma radiation. (panel 3) Density log and estimated density from cuttings mineralogy weight percentage. (panel 4) Porosity log. (panel 5) Mud losses encountered during drilling.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<h2><\/h2>\n<hr \/>\n<h2><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-310\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/06\/03a0425.jpg\" alt=\"\" width=\"138\" height=\"134\" \/>\u00a0 Tryana Garza-Cruz\u00a0(thesis; <a href=\"http:\/\/pubs.geothermal-library.org\/lib\/grc\/1028701.pdf\">paper<\/a>) (MS RES)<\/h2>\n<p>Investigation of the stress concentration at the bottom of a borehole, its potential to induce tensile failure, and the implication for interpreting stress from induced borehole failure from image logs.<\/p>\n<table>\n<tbody>\n<tr>\n<td>\n<p><div id=\"attachment_265\" style=\"width: 264px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-265\" class=\"wp-image-265\" src=\"https:\/\/sites.temple.edu\/ncdavatzes\/files\/2017\/05\/Borehole-Cartoon-and-Stress-224x300.png\" alt=\"\" width=\"254\" height=\"345\" \/><p id=\"caption-attachment-265\" class=\"wp-caption-text\">Visualization of the stress concentration along the sides and below the bottom of a borehole. Analysis performed in Poly3D in collaboration with IGEOSS.<\/p><\/div><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<ul>\n<li>\n<div class=\"page\" title=\"Page 4\">\n<div class=\"layoutArea\">\n<div class=\"column\">\n<p>Garza-Cruz, T. &amp; Davatzes, N.C. (2010): Numerical Modeling of the nucleation conditions of drilling-induced Petal Centerline Fracture. Geothermal Resources Council.\u00a0<em>Best Paper Award!<\/em><\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/li>\n<\/ul>\n<h3>For a perspective on the Department of Earth and Environmental Sciences, please visit the <a href=\"http:\/\/ees.cst.temple.edu\">department website<\/a>.<\/h3>\n<p>v2022-12-12, \u00a9 Nicholas C. Davatzes, 2022<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Projects of Former Graduate Students Rebecca Ayanwunmi (thesis) (MS TU) This project focused on quantifying the alteration of the host volcaniclastic rock and how this transformation impacted heat transfer during propagation, flow, and cooling, then basin tectonics and hydrology. (left) &hellip; <a href=\"https:\/\/sites.temple.edu\/ncdavatzes\/research\/student-projects-past\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":8825,"featured_media":0,"parent":32,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-261","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/pages\/261","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/users\/8825"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/comments?post=261"}],"version-history":[{"count":3,"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/pages\/261\/revisions"}],"predecessor-version":[{"id":660,"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/pages\/261\/revisions\/660"}],"up":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/pages\/32"}],"wp:attachment":[{"href":"https:\/\/sites.temple.edu\/ncdavatzes\/wp-json\/wp\/v2\/media?parent=261"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}