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Titlebook: Geothermics in Basin Analysis; Andrea Förster,Daniel F. Merriam Book 1999 Kluwer Academic/Plenum Publishers 1999 Sediment.environment.mode

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Erasmus and Nicholas of Cusa on Islaments, burial depths, and heat flow. Because of the complexity of the basin’s thermal history, no previous study has resulted in a single model that predicts the observed thermal maturity for the entire stratigraphic section in the basin. Two hypotheses, however, have resulted from previous studies.
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Geothermics in Basin Analysis978-1-4615-4751-8Series ISSN 1567-8296
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1567-8296 lved. Subject matter includes the measuring oftemperature logs and capturing of industrial temperature data andtheir interpretation to delineate subsurface conditions and processes,the importance of porosity and pore filling for modeling thermalfields, the thermal insulation of shales, geothermal an
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Book 1999itions and processes,the importance of porosity and pore filling for modeling thermalfields, the thermal insulation of shales, geothermal anomaliesassociated with mud diapirs and basin hydrodynamic regimes,temperatures related to magmatic underplating and plate tectonics.
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1567-8296 rface conditions and processes,the importance of porosity and pore filling for modeling thermalfields, the thermal insulation of shales, geothermal anomaliesassociated with mud diapirs and basin hydrodynamic regimes,temperatures related to magmatic underplating and plate tectonics.978-1-4613-7154-0978-1-4615-4751-8Series ISSN 1567-8296
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