石油与天然气地质 ›› 1992, Vol. 13 ›› Issue (1): 47-56.doi: 10.11743/ogg19920105

• 论文 • 上一篇    下一篇

中国西北地区板块构造与盆地类型

杨克明, 熊永旭, 李晋光, 先蓉有   

  1. 地质矿产部石油地质综合大队 湖北 江陵 434100
  • 收稿日期:1991-09-09 修回日期:1991-10-05 出版日期:1992-03-25 发布日期:2012-01-16

PLATE TECTONICS AND BASIN TYPES IN NORTHWESTERN CHINA

Yang Keming, Xiong Yongxu, Li Jinguang, Xian Rongyou   

  1. Comprehensive Research Institute of Petroleum Geology, MGMR, Jiangling, Hubei
  • Received:1991-09-09 Revised:1991-10-05 Online:1992-03-25 Published:2012-01-16

PDF (PC)

471

被引次数

23

摘要：

自显生宙以来,中国西北地区经历了中元古代至早古生代的板块离散、晚古生代至三叠纪末的板块敛合碰撞、侏罗纪至第四纪的盆山体制三个主要发展阶段,形成了三大类、十一亚类主要类型盆地。盆地在纵向上往往具"先张后压"的双层结构特征。

关键词: 中国西北地区, 板块构造, 地球动力学, 盆地类型, 盆地特征

Abstract:

Northwest China had experienced three major development stages,i.e.plate diver-gence from Middle Proterozoic to Early Paleozoic;plate convergence from Late Paleozoic to the end of Triassic;basin-mountain mechanism from Jurassic to Quaternary.The transformation between the tectonic mechanisms of oceanic and continental lithospheres,together with the influence exerted by the Tethys Plate since Meso-Cenozoicresu lted in three type basins(tensional,compresional and strike-slip.basins)and eleven subtype basins.Multicycle is the basic characteristic of the superimposed basins in this area.The basins extended first and then compressed,thus forming double-layer structure in verti-cle.The extention provided ideal place for the deposition of source rocks and the compres-sion prepared necessary condition for hydrocarbon migration ahd accumulation.