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- W2385971123 abstract "Hydrocarbon source rocks usually occurred in a marine carbonate environment in Tarim Basin during Ordovician,no effective source rocks have been found in the Middle-Upper Ordovician thick marine clastic.The analysis of pyrolyzed organic carbon in some mudstones systematically sampled from the Queerquek Formation in the eastern Tarim Basin,the detailed observation and description of cores from the Queerquek Formation of Well Yingdong-2,and the comprehensive interpretation of various 2-dimensional seismic sections indicated that a suite of marine hydrocarbon source rocks with a total accumulated thickness of nearly 100m occurs at the middle and lower parts of the Middle-Upper Ordovician thick Queerquek marine clastic.This suite of source rocks,which has TOC as high as 1.23%,is electronically characterized by a higher natural gamma-ray value and lower electric resistivity,indicating a relatively pure mudstone,and is obviously of high amplitude reflection in seismic sections.Widely distributed in the eastern Tarim Basin,these source rocks overlapped and pinched out eastward in the Luoxi platform margin and westward in the Gucheng-Lungudong platform margin,respectively.Meanwhile,the distribution of these source rocks along the south-north strike disappeared at the Che'erchen fault in the south and the Peacock River fault in the north,respectively,while on the northwestern rim they overlapped upon the Peacock River ramp.The marine source rock in the Queerquek Formation is a suite of deep-water shelf–basin facies mudstones deposited during the intermission of extensive development of submarine fans when transgression happened and water body was relatively quiet." @default.
- W2385971123 created "2016-06-24" @default.
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- W2385971123 date "2011-01-01" @default.
- W2385971123 modified "2023-09-25" @default.
- W2385971123 title "Hydrocarbon source rocks in marine clastic of the Middle-Upper Ordovician Queerquek Formation in the eastern Tarim Basin,China" @default.
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