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甘肃省肃南县卡瓦铁矿矿区地质特征浅析
引用本文:张春宇,胡小春,黄治化,冯 杰,魏建华. 甘肃省肃南县卡瓦铁矿矿区地质特征浅析[J]. 甘肃地质, 2014, 23(1): 47-51
作者姓名:张春宇  胡小春  黄治化  冯 杰  魏建华
作者单位:[1]兰州大学地质科学与矿产资源学院,甘肃兰州730000 [2]甘肃省地矿局第四地勘院,甘肃酒泉735000
摘    要:甘肃省肃南县卡瓦铁矿位于走廊南山地体与托莱山地体的构造结合部位。地层出露较为简单,主要为长城系桦树沟组以及白垩系下沟组,其中长城系桦树沟组为含矿层位。区内构造较为复杂,主要为加里东期形成的褶皱、断层,也有后期的构造。区内的变质作用程度较低,属于低绿片岩相。区内侵入岩主要为超基性岩,基本沿断层分布。总体上卡瓦铁矿与镜铁山铁矿的地质特征极为相似。

关 键 词:卡瓦  铁矿  矿区地质特征

GEOLOGIC FEATURE OF KAWA IRON DEPOSIT IN SUNAN COUNTY OF GANSU PROVINCE
ZHANG Chun-yu,HU Xiao-chun,HUANG Zhi-hu,FENG Jie and Wei Jian-hua. GEOLOGIC FEATURE OF KAWA IRON DEPOSIT IN SUNAN COUNTY OF GANSU PROVINCE[J]. Acta Geologica Gansu, 2014, 23(1): 47-51
Authors:ZHANG Chun-yu  HU Xiao-chun  HUANG Zhi-hu  FENG Jie  Wei Jian-hua
Affiliation:1.School of Earth Sciences, Lanzhou University, Lanzhou 730000, China; 2. No.4 Geology and Exploration Team, Gansu Provincial Bureau of Geology and Mineral Exploration and Development, Jiuquan 735000, China)
Abstract:Kawa iron mine in Sunan County of Gansu Province is located in structure combining site of Zoulang south mountain terrain and Tuolai mountain terrain. It includes Huashugou Formation of Changcheng System which contains iron mine and Xiagou Formation cretaceous system. It mainly contains fault and fold of Caledonian. It also contains structure behind of Caledonian. It has low degree of metamorphism-Low greenschist facies. Intrusive rocks are mainly uhrabasic rock which distribute along the fault. Overall Kawa Iron Mine Area and Jingtieshan Iron Mine Area have the similar geological characteristics.
Keywords:Kawa  iron mine  geological features
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