石油学报 ›› 1981, Vol. 2 ›› Issue (4): 11-22.DOI: 10.7623/syxb198104002

• 论文 • 上一篇    下一篇

酒泉盆地西部下白垩统沉积相及含油性

朱莲芳, 马宝林   

  1. 中国科学院兰州地质研究所
  • 收稿日期:1980-02-02 出版日期:1981-10-25 发布日期:2013-07-08

SEDIMENTARY FACIES AND OIL POSSIBILITIES OF THE LOWER CRETACEOUS IN THE WESTERN PART OF JIUQUAN BASIN

Zhu Lianfang, Ma Baolin   

  1. Lanzhou Geological Institute of the Academy of Sciences of China
  • Received:1980-02-02 Online:1981-10-25 Published:2013-07-08

摘要: 本文根据砂岩粒度概率累积曲线特征和沉积特征,对酒泉盆地西部下白垩统砂岩体划出13种成因类型,分属五个沉积体系,即洪积扇、河流、三角洲、湖滨及浊流.根据沉积相演化的研究,早白垩世经历了两次水体扩大和缩小的过程.前期水体扩大遍及全盆地,形成良好的生油条件,后期水体规模较小,有利于各种砂岩储集层的形成.

Abstract: On the basis of analyses of the characteristics of the cumulative probability curve of particle size and of the depositional characteristics(including lithology,fabrics and paleontology),the sandstone bodies of Lower Cretaceous in west Jiuquan basin are divided into 13 genetic types in five depositional systems:the diluvial fan deposits,thc fluviatile deposits,the deltaic deposits,the littoral deposits and the turbidites.Differcnces of sandstone bodies deposited under varying environments are described.study of the evolution of the sedimentary facies in early Cretaceous in the basin suggests that it underwent expansion and contraction of the water body twice during the period,resulting in the widespread water encroachment in the early part and the reduced scope of encroachment in the later part.The former was favourable for oil generation and the latter for sandstone reservoir formation.