石油与天然气地质 ›› 1980, Vol. 1 ›› Issue (1): 26-36.doi: 10.11743/ogg19800104

• 论文 • 上一篇    下一篇

塔里木盆地古生界的含油气前景

易荣龙, 江圣邦   

  1. 地质部石油地质综合大队
  • 出版日期:1980-06-25 发布日期:2012-01-16

THE OIL AND GAS POTENTIAL IN THE PALAEOZOIC OF TARIM BASIN

Yi Ronglong, Jiang Shengbang   

  1. Comprehensive Brigade of Petroleum Geology, Ministry of Geology
  • Online:1980-06-25 Published:2012-01-16

摘要:

新疆塔里木盆地广泛发育着地台型古生界海相碳酸盐岩和碎屑岩,展布面积达六十多万平方公里,其中被掩埋于中、新生界之下者约五十万平方公里。据物探资料估计,在覆盖区内古生界的总厚度大约为4000—6000米,其埋藏深度为1000—10000米。由于在露头区发现了大量的油气显示,因此古生界的含油气前景引起了人们的广泛关注。但是目前古生界的调查研究程度甚低。对这个尚待开拓的找油领域,我们仅依据新疆地质局、新疆石油局和地质部航空物探大队的资料以及我们的实际资料,提出一些粗浅的看法。

Abstract:

The Tarim Basin is an important target area for petroleum prospec-ting in Palaeozoic rocks in China.The platform marine carbonates and clastic rocks of Palaeozoic age are 4000—10000 meters thick and widely spread in Tarim Basin,and lie beneath the Meso-Cenozoic of 1000—10000 meters thick,occupying an area of appoximately 500000 squarekilometers.Frequent oil and gas in dications and commercial amount ofoil flows already found there are possibly derived from the Palaeozoicrocks.In Tarim,the basement is composedof Archaean-Proterozoic crystal-line complexes and metamorphic rocks.The emergence of this platformstarted from Jinning movement.It is suggested that the latitudinal upliftand subsidence formed by this event had controlled the marine regression and transgression and the sediment distribution.The NWW trending,the prototype,both of uplift and subsidence formed in Caledonian mo-vement,were further developed during the period of Hercynian movementand had simultaneously Controlled the distribution of Palaeozoic sedimen-tary zones.Now,eight tectonic units,either NEE and NWW strike,can be subdivided on the basis of the Hercynian tectonic framework.The Yanshanian and,especially,the Himalayan movements exerted an activeeffect on the remigration and accumulation of the Palaeozoic oil and gas.The Palaeozoic oil source rocks are in good abundance.The majoroil source rocks are Carboniferous,Lower Permian and Lower Cambrian,while the less impotant are Middle and Lower Ordovician,Lower Silurian and Upper Sinian.Preliminary study shows that both light oiland gas may occur in the Upper Palaeozoic,but only gas occurs in Lower Palaeozoic rocks.The Carboniferous-Lower Permian carbonates are the most importantoil reservoirs Nevertheless the Upper Sinian dolomites are also of great significance.It is suggested that fractures,planes of unconformity andorganic reefs are probably well developed in these rocks.The data available demonstrate that the marginal zone of the Bachu Uplift and the updip parts of the Maigaiti and northern Tarim PlatformSlopes are promising Palaeozoic belts for oil and gas prospecting.