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- W3088854531 abstract "The use of mineral diagenetic indices and organic matter maturity is useful for reconstructing the evolution of sedimentary basins and critical assessments for potential source rocks for petroleum exploration. In this study, the relationship of clay mineral diagenesis and organic matter thermal indices (Rock-Eval Tmax) and calculated vitrinite reflectance (%Ro) were used to constrain the maximum burial depths and temperatures of three distinct intervals within the northern Permian Basin, USA. X-ray diffraction of clay fractions (<2 µm) consists of illite, chlorite, and illite-smectite intermediates. Primary clay mineral diagenetic changes progressively increase in ordering from R0 to R1 I-S between 2359.5 and 2485.9 m and the appearance of chlorite at 2338.7 m. Rock-Eval pyrolysis data show 0 to 14 wt% TOC, HI values of 40 to 520 mgHC/g TOC, and S2 values of 0 to 62 mg HC/g, with primarily type II kerogen with calculated %Ro within the early to peak oil maturation window. Evaluation of the potential for oil generation is relatively good throughout the Tonya 401 and JP Chilton wells. Organic maturation indices (Tmax, %Ro) and peak burial temperatures correlate well with clay mineral diagenesis (R0–R1 I-S), indicating that maximum burial depths and temperatures were between 2.5 and 4 km and <100 °C and 140 °C, respectively. Additionally, the use of clay mineral-derived temperatures provides insight into discrepancies between several calculated %Ro equations and thus should be further investigated for use in the Permian Basin. Accordingly, these findings show that clay mineral diagenesis, combined with other paleothermal proxies, can considerably improve the understanding of the complex burial history of the Permian Basin in the context of the evolution of the southern margin of Laurentia." @default.
- W3088854531 created "2020-10-01" @default.
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- W3088854531 date "2020-09-23" @default.
- W3088854531 modified "2023-10-17" @default.
- W3088854531 title "Evaluation of Shale Source Rocks and Clay Mineral Diagenesis in the Permian Basin, USA: Inferences on Basin Thermal Maturity and Source Rock Potential" @default.
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- W3088854531 cites W1980255788 @default.
- W3088854531 cites W1980966289 @default.
- W3088854531 cites W1993547842 @default.
- W3088854531 cites W2008647814 @default.
- W3088854531 cites W2010379567 @default.
- W3088854531 cites W2013368477 @default.
- W3088854531 cites W2013591344 @default.
- W3088854531 cites W2025878233 @default.
- W3088854531 cites W2031255046 @default.
- W3088854531 cites W2041198162 @default.
- W3088854531 cites W2044364877 @default.
- W3088854531 cites W2051599684 @default.
- W3088854531 cites W2052694638 @default.
- W3088854531 cites W2054832820 @default.
- W3088854531 cites W2056626204 @default.
- W3088854531 cites W2066626423 @default.
- W3088854531 cites W2070412097 @default.
- W3088854531 cites W2078942094 @default.
- W3088854531 cites W2080659964 @default.
- W3088854531 cites W2082784403 @default.
- W3088854531 cites W2088765570 @default.
- W3088854531 cites W2092273609 @default.
- W3088854531 cites W2094285609 @default.
- W3088854531 cites W2102845953 @default.
- W3088854531 cites W2106177527 @default.
- W3088854531 cites W2107163286 @default.
- W3088854531 cites W2114327345 @default.
- W3088854531 cites W2114984018 @default.
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- W3088854531 cites W2122338764 @default.
- W3088854531 cites W2123499574 @default.
- W3088854531 cites W2131014399 @default.
- W3088854531 cites W2132286220 @default.
- W3088854531 cites W2133165788 @default.
- W3088854531 cites W2136310936 @default.
- W3088854531 cites W2140106632 @default.
- W3088854531 cites W2146034720 @default.
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- W3088854531 cites W2170995602 @default.
- W3088854531 cites W2171779737 @default.
- W3088854531 cites W2193949973 @default.
- W3088854531 cites W2303042025 @default.
- W3088854531 cites W2337587504 @default.
- W3088854531 cites W2338080953 @default.
- W3088854531 cites W2442588307 @default.
- W3088854531 cites W2528834079 @default.
- W3088854531 cites W2568919292 @default.
- W3088854531 cites W2582959074 @default.
- W3088854531 cites W2590202419 @default.
- W3088854531 cites W2727163156 @default.
- W3088854531 cites W2734144208 @default.
- W3088854531 cites W2765134301 @default.
- W3088854531 cites W2766334242 @default.
- W3088854531 cites W2771000646 @default.
- W3088854531 cites W2784125801 @default.
- W3088854531 cites W2790047115 @default.
- W3088854531 cites W2795169152 @default.
- W3088854531 cites W2796844541 @default.
- W3088854531 cites W2895437714 @default.
- W3088854531 cites W2921393817 @default.
- W3088854531 cites W2961727775 @default.
- W3088854531 cites W2964744526 @default.
- W3088854531 cites W2971110065 @default.
- W3088854531 cites W2981235883 @default.
- W3088854531 cites W3003921492 @default.
- W3088854531 cites W3012737208 @default.
- W3088854531 cites W4245131553 @default.
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- W3088854531 doi "https://doi.org/10.3390/geosciences10100381" @default.
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