Titlebook: Evaluation of Shale Source Rocks and Reservoirs; Bodhisatwa Hazra,David A. Wood,Ashok K. Singh Book 2019 Springer Nature Switzerland AG 20

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Einführung in die Theoretische Kinematikalysis and quantification of the various attributes of the complete range of pore sizes dimensions, shapes and connectivity is required. The results of such analysis applied to a suite of samples from a specific province are typically quite revealing about the gas storage potential of the shales and

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Introduction,oth potential source rocks and as potential unconventional petroleum reservoirs. Laboratory analyses and models are now required to assess the extent of petroleum generation, and the quantities of petroleum retained within versus the extent of petroleum expelled from such formations over time. In th

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Matrix Retention of Hydrocarbons,y the shale-matrix. Argillaceous matrices of organic-rich shales generally results in a greater amount of petroleum retention. Under such matrix retention conditions, the best-fit line of a S2 versus total organic carbon (TOC) cross-plot does not pass through the origin but intercepts the TOC-axis.

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,Kerogen’s Potential to Be Converted into Petroleum: Reaction Kinetics and Modelling Thermal Maturitids, thermal maturity and petroleum generation in organic-rich sediments. The roles of biogenic and thermogenic processes are distinguished. The significant roles in thermogenic generation of petroleum of the variables: temperature, time, burial depth and geothermal gradients are established. Therma

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Sedimentary Biomarkers and Their Stable Isotope Proxies in Evaluation of Shale Source and Reservoir. It is represented by the total organic carbon (TOC) content. There exist two important organic fractions, the kerogen, which amounts to the bulk of organic-matter (~80–90%), and the second are the free molecules of lipids ‘the biomarkers’ (10–20%), which include the hydrocarbons and related compou