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塔中北斜坡下奥陶统鹰山组热液岩溶特征及发育模式
引用本文:罗亚男,罗新生,张云峰,孙崇浩.塔中北斜坡下奥陶统鹰山组热液岩溶特征及发育模式[J].重庆科技学院学报(自然科学版),2012,14(3):19-22.
作者姓名:罗亚男  罗新生  张云峰  孙崇浩
作者单位:1. 西南石油大学,成都,610500
2. 塔里木油田分公司勘探开发研究院,库尔勒,841000
基金项目:国家科技重大专项(2008ZX05004-004);四川省重点学科建设项目(SZD0414)
摘    要:塔中北斜坡下奥陶统鹰山组受热液改造强烈,来源于地壳深部富含CO2和H2S的热液流体沿断裂、不整合面等发生运移,并对其流经的碳酸盐岩围岩发生溶蚀及白云岩化,形成孔洞缝组合,极大地改善了储层的物性.热液岩溶识别标志为岩石热褪色、非选择性溶蚀、缝洞充填典型热液矿物、“树状扩散”、“层状叠合”的地震反射等特征.

关 键 词:热液岩溶  识别标志  模式  鹰山组  塔中北斜坡

The Hydrothermal Karst Characteristics and Developmental Mode of Yingshan Formation of Lower-Ordovician of North Slope of Tazhong
LUO Yanan , LUO Xinsheng , ZHANG Yunfeng , SUN Chonghao.The Hydrothermal Karst Characteristics and Developmental Mode of Yingshan Formation of Lower-Ordovician of North Slope of Tazhong[J].Journal of Chongqing University of Science and Technology:Natural Science Edition,2012,14(3):19-22.
Authors:LUO Yanan  LUO Xinsheng  ZHANG Yunfeng  SUN Chonghao
Affiliation:1.Southwest Petroleum University,Chengdu 610500;2.Research Institute of Exploration and Development,Tarim Oilfield Company,Korla 841000)
Abstract:The Yingshan formation,Lower-Ordovician of North Slope of Tazhong is strongly reformed by hydrothermal solution.Hydrothermal fluids from the deep crust,containing much CO2and H2S migrates along the fault and unconformity plane,corrodes and dolomizes the Carbonate rock flowing by.As a result,the assemblage of pores,holes and fractures is formed and the reservoir is greatly improved.Identification marks of hydrothermal karst are the rock heat bleaching,non-selective corrosion,fracture caves infilling of typical hydrothermal mineral and seismic reflection features of "tree-proliferation","layered composite",etc.
Keywords:hydrothermal karst  identification mark  mode  Yingshan formation  north slope of Tazhong
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