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黔南坳陷下寒武统烃源岩地球化学特征及成因

贺训云 姚根顺 蔡春芳 沈安江 吴敬武 黄羚 陈子炓

沉积学报2012,Vol.30Issue(4):761-769,9.
沉积学报2012,Vol.30Issue(4):761-769,9.

黔南坳陷下寒武统烃源岩地球化学特征及成因

Geochemical Characteristics and Origins of the Lower Cambrian Source Rocks from the Southern Guizhou Depression,SW China

贺训云 1姚根顺 2蔡春芳 3沈安江 2吴敬武 2黄羚 2陈子炓2

作者信息

  • 1. 中国科学院地质与地球物理研究所,北京100029 中国科学院研究生院,北京100049 中国石油杭州地质研究院,杭州310023 中国石油天然气集团公司碳酸盐岩储层重点实验室,杭州310023
  • 2. 中国石油杭州地质研究院,杭州310023 中国石油天然气集团公司碳酸盐岩储层重点实验室,杭州310023
  • 3. 中国科学院地质与地球物理研究所,北京100029
  • 折叠

摘要

Abstract

The Lower Cambrian source rock samples from three typical profiles in the southern Guizhou Depression were analyzed for TOC values,δ13C values,Tmax temperatures,potential generation,and biomarkers using Rock-Eval,GC,GC-MS to elucidate the geochemical characteristics and its origin.The results show that the Lower Cambrian black shales in the southern Guizhou Depression are regional marine excellent source rocks with depth of 50-150m,and have the TOC values of 0.13%-15.40%,average 3.31%(n=169);the kerogens of the source rocks have the δ13C values of-35.79‰——29.88‰,average-32.85‰(n=35),and the kerogen macerals are mainly sapropelinites;the values of the marine vitrinite reflectance of the kerogens are 1.95%-3.96%,and the values of the equivalent vitrinite reflectance are 2.02%-3.47%;the distribution shapes of the n-alkanes are mainly single peak,and the maximum peak carbon are mainly C22,the C30 hopane and C27ααα20R regular sterane are abundant,the regular steranes are mainly C27C29C28,the Pr/Ph values are 0.27-0.62,the source rocks have relative high abundance of gammacerane and dibenzothiophene,the OEP values are 0.82-1.11,C31 homohopane 22S/(22S+22R) have values of 0.56-0.63,average 0.59;the source rocks are generally characterized by enrichment in light REE,Ba,Mo,V and U element,relative strong negative anomaly of Ce element,relative strong positive anomaly of Eu element and relative high ratio of U/Th.In summary,the Lower Cambrian marine source rocks in the southern Guizhou Depression have a wide distribution with a thickness of from tens of meters to hundreds of meters,the source rocks have high TOC values,are excellent for organic matter type,and have a post-maturity.It is the product which is jointly controlled by high paleo-productivity and anoxic environment.It can provide abundant organic matter for hydrocarbon generation in the southern Guizhou Depression.

关键词

烃源岩评价/海相烃源岩/生物标志化合物/生产力/缺氧环境/牛蹄塘组/黔南坳陷

Key words

source rock evaluation/marine source rock/biomarker/productivity/anoxic environment/Niutitang Formation/southern Guizhou Depression

分类

能源科技

引用本文复制引用

贺训云,姚根顺,蔡春芳,沈安江,吴敬武,黄羚,陈子炓..黔南坳陷下寒武统烃源岩地球化学特征及成因[J].沉积学报,2012,30(4):761-769,9.

基金项目

全国油气资源战略选区调查与评价项目 ()

国家科技重大专项(编号:2008ZX05004-002)资助 ()

沉积学报

OA北大核心CSCDCSTPCD

1000-0550

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