摘要
探讨鄂西地区下震旦统陡山沱组黑色页岩段有机质富集的差异性。通过鄂西地区陡山沱组野外露头、地质、地球化学综合研究分析,结果表明鄂西地区陡山沱组沉积环境主要为潮坪、台内盆地、台缘浅滩和斜坡。黑色页岩段主要发育于台内盆地,而潮坪主要发育白云岩;鄂西地区陡山沱组黑色页岩发育于B段和D段,其TOC的质量分数大多数>2%,D段TOC的质量分数高于B段,两者相差3%,这种差异与页岩形成的沉积环境密切相关。环境的差异性表现为水体动力条件、古盐度环境和氧化-还原环境的地球化学指标差异。
This paper discusses the differences about the organic matter enrichment in the shale section of the Ediacaran Doushantuo Formation in West Hubei and analyses the outcrops, geology and geochemistry. The results show that the main sedimentary environment includes tidal flats, shelf lagoon, shelf margin and slope. The black shale develops in the shelf lagoon, and the dolomite in the tidal fiats. The black shale of the Doushantuo Formation in West Hubei region develops in Segment B and D, and the TOC value （mass fraction） is mostly higher than 2%, and the TOC value in Segment D higher than segment B. The differences about TOC value depend on different sedimentary environments. The water power, paleosalinity and oxidation reduction environment can reflect the differences of the sedimentary environment. The results can guide the exploration of shale gas.
出处
《成都理工大学学报（自然科学版）》
CAS
CSCD
北大核心
2012年第6期567-574,共8页
Journal of Chengdu University of Technology: Science & Technology Edition
基金
国土资源部油气专项(2009GYXQ15-06)
关键词
陡山沱组
黑色页岩
沉积环境
TOC
地球化学
鄂西
Doushantuo Formation black shale sedimentary environment TOC geochemistry West Hubei
