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海南什统萤石矿床地质特征
引用本文:覃海灿,张小文,傅杨荣,纪明秀,古志祥,杨昌松. 海南什统萤石矿床地质特征[J]. 矿产与地质, 2005, 19(4): 398-402
作者姓名:覃海灿  张小文  傅杨荣  纪明秀  古志祥  杨昌松
作者单位:1. 中国地质大学地球科学学院,湖北,武汉,430074;海南省地调院,海南,海口,570206
2. 海南省地调院,海南,海口,570206
摘    要:什统萤石矿床位于海南省白沙拗陷带与五指山隆起的接触部位,是以断裂控矿为主的大型萤石矿床,其容矿构造为NE向张扭性断裂,成矿围岩为二长花岗岩和结晶灰岩.笔者以现场地质事实为依据,细致地研究该区的矿床地质特征,为今后的萤石矿床地质探矿提供了理论依据.

关 键 词:萤石矿床 找矿标志 地质特征 断裂控矿 什统 海南
文章编号:1001-5663(2005)04-0398-05
收稿时间:2004-12-07
修稿时间:2004-12-07

GEOLOGICAL CHARACTERISTICS OF ZHATONG FLUORITE DEPOSIT IN HAINAN ISLAND
QIN Hai-can,ZHANG Xiao-wen,Fu Yang-rong,Ji Ming-xiu,GU Zhi-xiang,YANG Chang-shong. GEOLOGICAL CHARACTERISTICS OF ZHATONG FLUORITE DEPOSIT IN HAINAN ISLAND[J]. Mineral Resources and Geology, 2005, 19(4): 398-402
Authors:QIN Hai-can  ZHANG Xiao-wen  Fu Yang-rong  Ji Ming-xiu  GU Zhi-xiang  YANG Chang-shong
Affiliation:1. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074 ,China ; 2. Hainan Geological Survey, Haikou, 570206,China
Abstract:The Zhatong fluorite deposit is located in contact zone between Baisha depression and Wuzhishan uplift, Hainan Island. It is a large scale deposit with the fracture being the main ore controlling factor. The host structure is a NE striking tenso--shear fracture and the country rocks of the deposit are adamellite and crystalline limestone. Based on the field geological evidences, the characteristics of the mineral geology of the area were studied carefully and provides theoretical basis for further geological prospecting of the fluorite deposit in the area.
Keywords:fluorite deposits   fracture   geological characteristics   Hainan Island
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