石油学报 ›› 1988, Vol. 9 ›› Issue (1): 46-50.DOI: 10.7623/syxb198801006

• 论文 • 上一篇    下一篇

渤海海域下第三系沙河街组陆源硅质碎屑-碳酸盐混合岩

王丽芝   

  1. 渤海石油公司研究院
  • 修回日期:1985-11-30 出版日期:1988-01-25 发布日期:2013-07-08

THE TERRIGENOUS CLASTICS-CARBONATE MIX OF LOWER TERTIARY SHAHEJIE FORMATION OF BOHAI BAY

Wang Lizhi   

  1. The research institute of Boc
  • Revised:1985-11-30 Online:1988-01-25 Published:2013-07-08

摘要: 本文提出渤海地区下第三系沙河街组湖泊成因的碳酸盐岩大都是陆源硅质碎屑和碳酸盐的混合岩。提出陆源硅质碎屑岩和碳酸盐岩之间有一系列过渡岩性,并提出一个初步的定名方案。渤海地区在下第三纪沙河街期大面积的陆源碎屑沉积区包围着小范围的碳酸盐沉积区,和浅海陆架区相比更易于形成这类“混合岩”。据渤海地区所见的三种剖面类型提出了三种混合方式,并推定了陆源碎屑——碳酸盐混合岩沉积模式。

关键词: 碳酸盐沉积物, 碳酸盐岩, 下第三系沙河街组, 陆源碎屑岩, 混合岩, 渤海海域, 硅质碎屑, 渤海地区, 沉积模式, 沉积环境

Abstract: This paper describes that the lacustrine carbonate of lower Tertiary Shahejie Formation in Bohai Bay is mostly terrigenous elastics-carbonate mixture rock. There is a seris of transition rocks between the terrigenous clastic rock and carbonate. The nomenclature of these rocks is tabulated tentatively.In Bohai Bay the small limited areas of lacustrine carbonate deposition are surrounded by large areas of the terrigenous clastic depositions during lower Tertiary. The terrigenous clastic-carbonate mix is more easily formed in lacustrine setting compared with the shelf of shallow sea. Three kinds of this mixture rock profile are discovered in Bohai Bay. According to the profiles three mixing patterns are put forward and the sedimentary model of terrigenous clasticcarbonate mix is illustrated.