GSTDTAP  > 地球科学
DOI10.1306/03141817183
Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China
Zhu, Guangyou1,2; Chen, Feiran1; Wang, Meng1; Zhang, Zhiyao1; Ren, Rong1; Wu, Lin1
2018-10-01
发表期刊AAPG BULLETIN
ISSN0149-1423
EISSN1558-9153
出版年2018
卷号102期号:10页码:2123-2151
文章类型Article
语种英语
国家Peoples R China
英文摘要

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 (similar to 6900 m [similar to 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 ((sic)(1)y), 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 highquality source rocks may cover an area as large as 260,000 km(2) (100,000 mi(2)). 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 delta S-34 correlation of organic sulfur compounds in the condensate with Cambrian sulfates provides further evidence for a (sic)(1)y 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.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000447260300009
WOS关键词ORGANIC-MATTER PRESERVATION ; SULFUR-ISOTOPIC COMPOSITIONS ; PALEOZOIC MARINE PETROLEUM ; NW CHINA ; TAZHONG AREA ; BLACK SHALES ; SOUTH CHINA ; BIOSTRATIGRAPHIC CORRELATION ; DIAMONDOID HYDROCARBONS ; YANGTZE PLATFORM
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/24409
专题地球科学
作者单位1.PetroChina, Res Inst Petr Explorat & Dev, 20 Xueyuan Rd, Beijing 100083, Peoples R China;
2.PetroChina, Res Inst Petr Explorat & Dev, Geol & Geochem, Beijing, Peoples R China
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GB/T 7714
Zhu, Guangyou,Chen, Feiran,Wang, Meng,et al. Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China[J]. AAPG BULLETIN,2018,102(10):2123-2151.
APA Zhu, Guangyou,Chen, Feiran,Wang, Meng,Zhang, Zhiyao,Ren, Rong,&Wu, Lin.(2018).Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China.AAPG BULLETIN,102(10),2123-2151.
MLA Zhu, Guangyou,et al."Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China".AAPG BULLETIN 102.10(2018):2123-2151.
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