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Organic petrography of Leonardian (Wolfcamp A) mudrocks and carbonates, Midland Basin, Texas: The fate of oil-prone sedimentary organic matter in the oil window
To better understand evolution of oil-prone sedimentary organic matter to petroleum and expulsion from source rock, we evaluated organic petrographic features of Leonardian Wolfcamp A repetitive siliceous and calcareous mudrock and fine-grained carbonate lithofacies cycles occurring in the R. Ricker...
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Published in: | Marine and petroleum geology 2020-02, Vol.112, p.104086, Article 104086 |
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description | To better understand evolution of oil-prone sedimentary organic matter to petroleum and expulsion from source rock, we evaluated organic petrographic features of Leonardian Wolfcamp A repetitive siliceous and calcareous mudrock and fine-grained carbonate lithofacies cycles occurring in the R. Ricker #1 core from Reagan County, Midland Basin, Texas. The objectives of the petrographic investigation were to estimate thermal maturity, identify organic matter types and abundances, and identify the presence or absence of migrated hydrocarbons in organic-lean carbonate layers. An integrated analytical program included geochemical screening [total organic carbon (TOC) content by LECO, programmed pyrolysis by hydrocarbon analyzer with kinetics (HAWK) including analysis of solvent-extracted samples], X-ray diffraction mineralogy, organic petrography, scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS) including correlative light and electron microscopy (CLEM), and micro-Fourier transform infrared spectroscopy (μ-FTIR) analyses of solid bitumen. The data indicate all samples are early to middle oil window thermal maturity with solid bitumen reflectance (BRo) values of 0.55–0.86% and Tmax of 440–455 °C. Organic matter is predominantly solid bitumen (as identified by optical microscopy) in all lithofacies with minor contributions from inertinite. Solid bitumen abundance decreases from siliceous mudrock (TOC >3.0 wt%) to calcareous mudrock (TOC 1.0 to 3.0 wt%) to fine-grained carbonate (TOC |
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•Organic petrography of Wolfcamp A mudrocks and carbonates from Midland Basin was studied.•Thermal maturity is early to middle oil window.•Organic matter is predominantly solid bitumen in all lithofacies with minor contributions from inertinite.•Solid bitumen is residual from thermal conversion of oil-prone sedimentary organic matter.•Mudrocks are source rock lithofacies whereas carbonates are reservoir lithofacies.</description><identifier>ISSN: 0264-8172</identifier><identifier>DOI: 10.1016/j.marpetgeo.2019.104086</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Leonardian ; Organic petrography ; Permian basin ; Solid bitumen ; Thermal maturity ; Wolfcamp A</subject><ispartof>Marine and petroleum geology, 2020-02, Vol.112, p.104086, Article 104086</ispartof><rights>2019</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a387t-bfcd97a1e4c478268b1a7e946b9f6bcf6d3074a1a9182ceb5eec4d11b1ba1b773</citedby><cites>FETCH-LOGICAL-a387t-bfcd97a1e4c478268b1a7e946b9f6bcf6d3074a1a9182ceb5eec4d11b1ba1b773</cites><orcidid>0000-0002-8678-2431 ; 0000-0002-5957-2551</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Hackley, Paul C.</creatorcontrib><creatorcontrib>Zhang, Tongwei</creatorcontrib><creatorcontrib>Jubb, Aaron M.</creatorcontrib><creatorcontrib>Valentine, Brett J.</creatorcontrib><creatorcontrib>Dulong, Frank T.</creatorcontrib><creatorcontrib>Hatcherian, Javin J.</creatorcontrib><title>Organic petrography of Leonardian (Wolfcamp A) mudrocks and carbonates, Midland Basin, Texas: The fate of oil-prone sedimentary organic matter in the oil window</title><title>Marine and petroleum geology</title><description>To better understand evolution of oil-prone sedimentary organic matter to petroleum and expulsion from source rock, we evaluated organic petrographic features of Leonardian Wolfcamp A repetitive siliceous and calcareous mudrock and fine-grained carbonate lithofacies cycles occurring in the R. Ricker #1 core from Reagan County, Midland Basin, Texas. The objectives of the petrographic investigation were to estimate thermal maturity, identify organic matter types and abundances, and identify the presence or absence of migrated hydrocarbons in organic-lean carbonate layers. An integrated analytical program included geochemical screening [total organic carbon (TOC) content by LECO, programmed pyrolysis by hydrocarbon analyzer with kinetics (HAWK) including analysis of solvent-extracted samples], X-ray diffraction mineralogy, organic petrography, scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS) including correlative light and electron microscopy (CLEM), and micro-Fourier transform infrared spectroscopy (μ-FTIR) analyses of solid bitumen. The data indicate all samples are early to middle oil window thermal maturity with solid bitumen reflectance (BRo) values of 0.55–0.86% and Tmax of 440–455 °C. Organic matter is predominantly solid bitumen (as identified by optical microscopy) in all lithofacies with minor contributions from inertinite. Solid bitumen abundance decreases from siliceous mudrock (TOC >3.0 wt%) to calcareous mudrock (TOC 1.0 to 3.0 wt%) to fine-grained carbonate (TOC <1.0 wt%) lithofacies. Interpretations of petrographic data suggest siliceous and calcareous mudrocks are source rock lithofacies and contain solid bitumen (with petroleum generation potential) that is residual (what remains) from conversion of an original Type II sedimentary organic matter. In turn, fine-grained carbonates are interpreted as reservoir lithofacies which contained little or no original oil-prone sedimentary organic matter and at present-day contain only a minor component of migrated solid petroleum sourced from adjacent siliceous and calcareous mudrock lithofacies. This work helps to document petroleum generation and migration processes, improve unconventional reservoir characterization and better define areas of oil window thermal maturity in an area critical to United States hydrocarbon production.
•Organic petrography of Wolfcamp A mudrocks and carbonates from Midland Basin was studied.•Thermal maturity is early to middle oil window.•Organic matter is predominantly solid bitumen in all lithofacies with minor contributions from inertinite.•Solid bitumen is residual from thermal conversion of oil-prone sedimentary organic matter.•Mudrocks are source rock lithofacies whereas carbonates are reservoir lithofacies.</description><subject>Leonardian</subject><subject>Organic petrography</subject><subject>Permian basin</subject><subject>Solid bitumen</subject><subject>Thermal maturity</subject><subject>Wolfcamp A</subject><issn>0264-8172</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNqFkM1OwzAQhHMAiVJ4BnwEqSl2GuKEW0H8SUW9FHG01vamdWnsyA6Uvg2PiqNWXDmtNJqZ3f2S5ILRMaOsuF6PG_Atdkt044yyKqo5LYujZECzIk9LxrOT5DSENaWUV5QNkp-5X4I1isSUd0sP7WpHXE1m6Cx4bcCSy3e3qRU0LZlekeZTe6c-AgGriQIvo63DMCKvRm967Q6CsSOywG8It2SxQlJHQ1_pzCZtvbNIAmrToO3Ax12H_Q10HXpiLOliJnrJ1ljttmfJcQ2bgOeHOUzeHh8W98_pbP70cj-dpTApeZfKWumKA8Nc5bzMilIy4FjlhazqQqq60BPKc2BQsTJTKG8QVa4Zk0wCk5xPhgnf9yrvQvBYi9abSHMnGBU9XLEWf3BFD1fs4cbkdJ_EeN6XQS-CMmhVfNKj6oR25t-OX8KbjP4</recordid><startdate>202002</startdate><enddate>202002</enddate><creator>Hackley, Paul C.</creator><creator>Zhang, Tongwei</creator><creator>Jubb, Aaron M.</creator><creator>Valentine, Brett J.</creator><creator>Dulong, Frank T.</creator><creator>Hatcherian, Javin J.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><orcidid>https://orcid.org/0000-0002-8678-2431</orcidid><orcidid>https://orcid.org/0000-0002-5957-2551</orcidid></search><sort><creationdate>202002</creationdate><title>Organic petrography of Leonardian (Wolfcamp A) mudrocks and carbonates, Midland Basin, Texas: The fate of oil-prone sedimentary organic matter in the oil window</title><author>Hackley, Paul C. ; Zhang, Tongwei ; Jubb, Aaron M. ; Valentine, Brett J. ; Dulong, Frank T. ; Hatcherian, Javin J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a387t-bfcd97a1e4c478268b1a7e946b9f6bcf6d3074a1a9182ceb5eec4d11b1ba1b773</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Leonardian</topic><topic>Organic petrography</topic><topic>Permian basin</topic><topic>Solid bitumen</topic><topic>Thermal maturity</topic><topic>Wolfcamp A</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hackley, Paul C.</creatorcontrib><creatorcontrib>Zhang, Tongwei</creatorcontrib><creatorcontrib>Jubb, Aaron M.</creatorcontrib><creatorcontrib>Valentine, Brett J.</creatorcontrib><creatorcontrib>Dulong, Frank T.</creatorcontrib><creatorcontrib>Hatcherian, Javin J.</creatorcontrib><collection>CrossRef</collection><jtitle>Marine and petroleum geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hackley, Paul C.</au><au>Zhang, Tongwei</au><au>Jubb, Aaron M.</au><au>Valentine, Brett J.</au><au>Dulong, Frank T.</au><au>Hatcherian, Javin J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Organic petrography of Leonardian (Wolfcamp A) mudrocks and carbonates, Midland Basin, Texas: The fate of oil-prone sedimentary organic matter in the oil window</atitle><jtitle>Marine and petroleum geology</jtitle><date>2020-02</date><risdate>2020</risdate><volume>112</volume><spage>104086</spage><pages>104086-</pages><artnum>104086</artnum><issn>0264-8172</issn><abstract>To better understand evolution of oil-prone sedimentary organic matter to petroleum and expulsion from source rock, we evaluated organic petrographic features of Leonardian Wolfcamp A repetitive siliceous and calcareous mudrock and fine-grained carbonate lithofacies cycles occurring in the R. Ricker #1 core from Reagan County, Midland Basin, Texas. The objectives of the petrographic investigation were to estimate thermal maturity, identify organic matter types and abundances, and identify the presence or absence of migrated hydrocarbons in organic-lean carbonate layers. An integrated analytical program included geochemical screening [total organic carbon (TOC) content by LECO, programmed pyrolysis by hydrocarbon analyzer with kinetics (HAWK) including analysis of solvent-extracted samples], X-ray diffraction mineralogy, organic petrography, scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS) including correlative light and electron microscopy (CLEM), and micro-Fourier transform infrared spectroscopy (μ-FTIR) analyses of solid bitumen. The data indicate all samples are early to middle oil window thermal maturity with solid bitumen reflectance (BRo) values of 0.55–0.86% and Tmax of 440–455 °C. Organic matter is predominantly solid bitumen (as identified by optical microscopy) in all lithofacies with minor contributions from inertinite. Solid bitumen abundance decreases from siliceous mudrock (TOC >3.0 wt%) to calcareous mudrock (TOC 1.0 to 3.0 wt%) to fine-grained carbonate (TOC <1.0 wt%) lithofacies. Interpretations of petrographic data suggest siliceous and calcareous mudrocks are source rock lithofacies and contain solid bitumen (with petroleum generation potential) that is residual (what remains) from conversion of an original Type II sedimentary organic matter. In turn, fine-grained carbonates are interpreted as reservoir lithofacies which contained little or no original oil-prone sedimentary organic matter and at present-day contain only a minor component of migrated solid petroleum sourced from adjacent siliceous and calcareous mudrock lithofacies. This work helps to document petroleum generation and migration processes, improve unconventional reservoir characterization and better define areas of oil window thermal maturity in an area critical to United States hydrocarbon production.
•Organic petrography of Wolfcamp A mudrocks and carbonates from Midland Basin was studied.•Thermal maturity is early to middle oil window.•Organic matter is predominantly solid bitumen in all lithofacies with minor contributions from inertinite.•Solid bitumen is residual from thermal conversion of oil-prone sedimentary organic matter.•Mudrocks are source rock lithofacies whereas carbonates are reservoir lithofacies.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.marpetgeo.2019.104086</doi><orcidid>https://orcid.org/0000-0002-8678-2431</orcidid><orcidid>https://orcid.org/0000-0002-5957-2551</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Leonardian Organic petrography Permian basin Solid bitumen Thermal maturity Wolfcamp A |
title | Organic petrography of Leonardian (Wolfcamp A) mudrocks and carbonates, Midland Basin, Texas: The fate of oil-prone sedimentary organic matter in the oil window |
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