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塔中地区下奥陶统层间不整合岩溶发育特征及其控制因素
引用本文:陈贞万,王振宇,张云峰,孙崇浩. 塔中地区下奥陶统层间不整合岩溶发育特征及其控制因素[J]. 重庆科技学院学报(自然科学版), 2012, 14(2): 28-31
作者姓名:陈贞万  王振宇  张云峰  孙崇浩
作者单位:1. 西南石油大学,成都,610500
2. 中国石油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);四川省重点学科建没项目(SZD0414)
摘    要:塔中地区下奥陶统鹰山组见发育程度不等的多种岩溶现象,存在规模不同、形态各异的岩溶缝洞系统.一个发育完整的层间不整合岩溶通常由表层岩溶带、垂向渗滤岩溶带、径流岩溶带和潜流岩溶带构成.岩溶带发育程度与深度因受到地区、岩性、构造部位、古地貌位置、古水文条件、暴露时长等因素影响而差异较大.

关 键 词:层间不整合  岩溶特征  岩溶带  下奥陶统鹰山组  塔中地区

The Developed Characteristics and Controlling Factors of the Layer Unconformity Karst in the Lower Ordovician of TaZhong Area
CHEN Zhenwan , WANG Zhenyu , ZHANG Yunfeng , SUN Chonghao. The Developed Characteristics and Controlling Factors of the Layer Unconformity Karst in the Lower Ordovician of TaZhong Area[J]. Journal of Chongqing University of Science and Technology:Natural Science Edition, 2012, 14(2): 28-31
Authors:CHEN Zhenwan    WANG Zhenyu    ZHANG Yunfeng    SUN Chonghao
Affiliation:1.Southwest Petroleum University,Chengdu 610500;2.Exploration and Development Research Institute of Petrochina Tarim Oilfield Company,Korla 841000)
Abstract:Various karst phenomenon developed in Lower Ordovician Yingshan Formation of Tazhong area,appears in different scale,different forms of karst fracture cave system.A completely developed the layer unconformity karst can be divided into superfacial karst zone,vertical percolation dissolvedzone,radial flow dissolved zone and groundwater flow zone.Karst development degree and depth vary with the change of region,lithology,tectonics,landform position,ancient hydrological conditions and duration of exposure and other factors.
Keywords:layer unconformity Karst  characteristic of Karst division  karst division area Lower Ordovician Yingshan formation  TaZhong area
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