Article ID Journal Published Year Pages File Type
8909341 Marine and Petroleum Geology 2017 41 Pages PDF
Abstract
The range of δ13C values (−5.8-3.6‰ VPDB) suggests that the main source of carbon in the calcite cements was primarily marine mixed with isotopically more negative carbon from atmospheric/soil-derived CO2.
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Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
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Diagenetic history and reservoir properties of the Cenomanian-Turonian carbonates in southwestern Iran and the Persian Gulf
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