Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5782182 | Marine and Petroleum Geology | 2017 | 17 Pages |
Abstract
High permeability shales are associated with specific depositional facies. Massive and pyritic mudstones, rich in TOC and quartz, have comparatively high permeability. Laminated mudstone, bioturbated mudstone and carbonate facies, which are relatively enriched in clay or carbonate, have fairly low permeability.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
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Authors
Tian Dong, Nicholas B. Harris, Korhan Ayranci, Cory E. Twemlow, Brent R. Nassichuk,