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Al. I. Cuza University of Iasi, Romania
Faculty of Geography and Geology Department of Geology ![]()
Hydrocarbon potential of the source rock The abundance of organic matter in sediments is usually expressed as the relative percentage of organic carbon on a dry weight basis. Based on its values, the genetic potential of the source rocks can be established, being estimated between poor and excellent (Peters and Cassa, 1994). ![]() ![]() Elemental geochemical analysis for bituminous rocks from Slanic section (Tarcau Nappe) ![]()
van Krevelen diagram (HI vs Tmax), depicting type of kerogen from Lower dysodilic shale Formation, Slanic section.
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