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四川广元长江沟大隆组的沉积特征及与烃源岩关系的研究
The Dalong Formation section in Changjianggou,Guangyuan,Sichuan:Sedimentary characteristics and their bearings on the source rocks
【摘要】 四川广元长江沟上二叠统大隆组是以灰岩为主夹泥岩的沉积类型,生物群组合面貌十分丰富,沉积特征以还原、低能、低速、缺氧为特点。根据生物群组合面貌和沉积特征,其形成环境应为较深"浅水",而并非"半深海"。本区大隆组由于生物多样性和始终处于特殊的斜坡和缺氧环境,具有优质烃源岩特征,有机碳平均含量达5%,是四川今后寻找油气的有效标志层。
【Abstract】 The Dalong Formation section in Changjianggou,Guangyuan,Sichuan is characterized by limestones intercalated with mudstones,abundant biotic assemblages and deeper shallow-water environments indicated by reduction,low energy,low velocity and oxygen depletion. The bio-diversity and anoxic slope environments made the study area to be favourable for the formation of excellent source rocks,with the average organic carbon contents almost up to 5%,and thus may be potential marker horizons for future petroleum exploration in Sichuan.
【关键词】 生物多样性;
沉积特征;
烃源岩;
大隆组;
四川广元;
【Key words】 bio-diversity; sedimentary characteristics; source rock; Dalong Formation; Guangyuan in Sichuan;
【Key words】 bio-diversity; sedimentary characteristics; source rock; Dalong Formation; Guangyuan in Sichuan;
【基金】 国家自然科学基金(40839903)资助
- 【文献出处】 沉积与特提斯地质 ,Sedimentary Geology and Tethyan Geology , 编辑部邮箱 ,2015年04期
- 【分类号】P618.13
- 【下载频次】251