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• W2890178153 endingPage "2151" @default.
• W2890178153 startingPage "2123" @default.
• W2890178153 abstract "The global Precambrian–Cambrian system includes an important series of hydrocarbon-bearing strata. However, because rocks of this age are typically deeply buried, few petroleum exploration breakthroughs have been made, and the presence of source rocks remains somewhat controversial. Recently, commercial condensate and gas were discovered from the deep (∼6900 m [∼22,600 ft]) Zhongshen 1C (ZS1C) exploratory well drilled in the Tazhong uplift of the Tarim Basin, China, leading to renewed interest in the development of Cambrian source rocks in the basin. On the basis of outcrop reconnaissance and sample testing from around the Tarim Basin, we show that a set of high-quality source rocks were developed within the lower Cambrian Yuertusi Formation (J1y), at the base of the lower Cambrian. These rocks are black shales and typically have a total organic carbon content between 2% and 6% but extending as high as 17% in selected regions. This marine sequence is 10–15 m (33–49 ft) thick in some outcrops along the margins of the basin. Seismic data indicate that these high-quality source rocks may cover an area as large as 260,000 km2 (100,000 mi2). Their main organic parent material was benthic multicellular algae. On the basis of high-temperature thermal simulations conducted on these source rocks, we show that the gas composition and carbon isotopes from the ZS1C well are similar to the products generated at a thermal evolution stage corresponding to a vitrinite reflectance of between 2.2% and 2.5%. Late-stage natural gas accumulated within these rocks over time. The δ34S correlation of organic sulfur compounds in the condensate with Cambrian sulfates provides further evidence for a J1y source rock origin of the ZS1C condensate and gas. The Cambrian dolomites in association with a salt seal exhibit favorable geological conditions for large-scale hydrocarbon accumulation. A new set of deep exploration strata can, therefore, be developed, guiding future deep Cambrian hydrocarbon exploration in the Tarim Basin." @default.
• W2890178153 created "2018-09-27" @default.
• W2890178153 creator A5011866909 @default.
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• W2890178153 creator A5061602320 @default.
• W2890178153 creator A5069714324 @default.
• W2890178153 creator A5080361939 @default.
• W2890178153 date "2018-10-01" @default.
• W2890178153 modified "2023-10-09" @default.
• W2890178153 title "Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China" @default.
• W2890178153 cites W1558237779 @default.
• W2890178153 cites W1579082897 @default.
• W2890178153 cites W1615261580 @default.
• W2890178153 cites W1693703638 @default.
• W2890178153 cites W1764649536 @default.
• W2890178153 cites W1804076876 @default.
• W2890178153 cites W1964114055 @default.
• W2890178153 cites W1968499642 @default.
• W2890178153 cites W1968704350 @default.
• W2890178153 cites W1970354646 @default.
• W2890178153 cites W1971173905 @default.
• W2890178153 cites W1973053640 @default.
• W2890178153 cites W1974438203 @default.
• W2890178153 cites W1978263132 @default.
• W2890178153 cites W1979315982 @default.
• W2890178153 cites W1980392563 @default.
• W2890178153 cites W1981173237 @default.
• W2890178153 cites W1981905703 @default.
• W2890178153 cites W1986567322 @default.
• W2890178153 cites W1986843887 @default.
• W2890178153 cites W1986916739 @default.
• W2890178153 cites W1989860834 @default.
• W2890178153 cites W1992762978 @default.
• W2890178153 cites W1994160943 @default.
• W2890178153 cites W1994201136 @default.
• W2890178153 cites W1994510458 @default.
• W2890178153 cites W1995137647 @default.
• W2890178153 cites W1996562355 @default.
• W2890178153 cites W1997325616 @default.
• W2890178153 cites W1998138507 @default.
• W2890178153 cites W2000661450 @default.
• W2890178153 cites W2002371280 @default.
• W2890178153 cites W2002953373 @default.
• W2890178153 cites W2004538472 @default.
• W2890178153 cites W2006593586 @default.
• W2890178153 cites W2009023071 @default.
• W2890178153 cites W2012596346 @default.
• W2890178153 cites W2017143661 @default.
• W2890178153 cites W2017668629 @default.
• W2890178153 cites W2020299821 @default.
• W2890178153 cites W2020610733 @default.
• W2890178153 cites W2023133943 @default.
• W2890178153 cites W2023644427 @default.
• W2890178153 cites W2028864600 @default.
• W2890178153 cites W2029619643 @default.
• W2890178153 cites W2029873401 @default.
• W2890178153 cites W2030711274 @default.
• W2890178153 cites W2031770702 @default.
• W2890178153 cites W2033518493 @default.
• W2890178153 cites W2035690644 @default.
• W2890178153 cites W2037108679 @default.
• W2890178153 cites W2039544921 @default.
• W2890178153 cites W2040269188 @default.
• W2890178153 cites W2042550843 @default.
• W2890178153 cites W2043233032 @default.
• W2890178153 cites W2045149838 @default.
• W2890178153 cites W2048279742 @default.
• W2890178153 cites W2048347763 @default.
• W2890178153 cites W2049811834 @default.
• W2890178153 cites W2052078336 @default.
• W2890178153 cites W2052873114 @default.
• W2890178153 cites W2055862951 @default.
• W2890178153 cites W2056160475 @default.
• W2890178153 cites W2057260077 @default.
• W2890178153 cites W2057391595 @default.
• W2890178153 cites W2058741861 @default.
• W2890178153 cites W2059109340 @default.
• W2890178153 cites W2062978390 @default.
• W2890178153 cites W2064361108 @default.
• W2890178153 cites W2069536345 @default.
• W2890178153 cites W2070336776 @default.
• W2890178153 cites W2070822025 @default.
• W2890178153 cites W2073955916 @default.
• W2890178153 cites W2075619059 @default.
• W2890178153 cites W2078335897 @default.
• W2890178153 cites W2079412336 @default.
• W2890178153 cites W2084141580 @default.
• W2890178153 cites W2084927468 @default.
• W2890178153 cites W2085199314 @default.
• W2890178153 cites W2086671380 @default.
• W2890178153 cites W2091708215 @default.
• W2890178153 cites W2092008995 @default.
• W2890178153 cites W2100744462 @default.
• W2890178153 cites W2104409229 @default.
• W2890178153 cites W2108356947 @default.
• W2890178153 cites W2108538927 @default.
• W2890178153 cites W2111968947 @default.

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