首页 | 官方网站   微博 | 高级检索  
     

鄂尔多斯盆地奥陶系风化壳岩溶储层研究
引用本文:王雪莲,王长陆,陈振林,田继军.鄂尔多斯盆地奥陶系风化壳岩溶储层研究[J].特种油气藏,2005,12(3):32-35,108.
作者姓名:王雪莲  王长陆  陈振林  田继军
作者单位:中国地质大学,湖北,武汉,430074
摘    要:鄂尔多斯盆地在奥陶系顶部发育大面积的风化壳岩溶储层.不整合面、溶蚀孔洞缝、岩溶地貌是其区别于其它储层的特殊标志.复杂多变的溶蚀孔、洞、缝及其组合,构成了风化壳岩溶储层的储集空间.该类储层受岩性、沉积相带、古地貌形态、成岩作用改造等因素控制.

关 键 词:风化壳  岩溶型储层  识别标志  影响因素  鄂尔多斯盆地
文章编号:1006-6535(2005)03-0032-04

Study of Ordovician weathering crust karst reservoirs in Ordos Basin
WANG Xue-Lian,WANG Chang-lu,CHEN Zhen-lin,TIAN Ji-jun.Study of Ordovician weathering crust karst reservoirs in Ordos Basin[J].Special Oil & Gas Reservoirs,2005,12(3):32-35,108.
Authors:WANG Xue-Lian  WANG Chang-lu  CHEN Zhen-lin  TIAN Ji-jun
Abstract:There developed a vast area of weathering crust karst reservoirs on top Ordovician in Ordos Basin. Unconformity surface, karst cave and karst landform are signs distinguishing from other reservoirs. The complex association of karst cave and fissures constitutes the reservoir space of weathering crust karst reservoirs. Such reservoirs subjected to lithology, sedimentary facies belt, palaeogeomorphology, and diagenesis.
Keywords:weathering crust  karst reservoir  distinguish sign  influence factor  Ordos Basin
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号