Geochemical modeling and hydrothermal experiments used to constrain the conditions of illite diagenesis in sedimentary basins
<p> Two hydrothermal experiments were performed using sandstone core material from the Norwegian North Sea with synthetic brines reacted at approximately 150°C and 450 bars, temperature and pressure calculated to simulate a depth of burial of approximately 4 km. The results of the expe...
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| Language: | EN |
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San Jose State University
2017
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| Online Access: | http://pqdtopen.proquest.com/#viewpdf?dispub=10253450 |