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浙江八面山萤石矿床流体包裹体地球化学研究
引用本文:闫飞,夏学惠,徐少康,吴颖慧,逄思宇.浙江八面山萤石矿床流体包裹体地球化学研究[J].化工矿产地质,2010,32(4):215-220.
作者姓名:闫飞  夏学惠  徐少康  吴颖慧  逄思宇
作者单位:中化地质矿山总局地质研究院,河北涿州,072754
摘    要:八面山萤石矿床流体包裹体可分为三大类型:Ⅰ气液包裹体,Ⅱ气体包裹体,Ⅲ含子矿物的多相包裹体;矿床成矿温度变化不大,主要集中在120~240°C之间。细粒条带状萤石矿石包裹体温度变化在115~250℃之间;巨晶块状萤石矿石和石英脉型萤石矿石包裹体温度集中在135~170℃之间。萤石矿床流体包裹体以低盐度成矿流体为主。成矿过程中起作用的成矿流体为KCl-H2O体系和CO2-CaF2-H2O体系,成矿溶液的离子类型属K+-Ca2+-HCO--F-型,KCl-H2O体系反映岩浆期后热液作用的结果,而CO2-CaF2-H2O体系可能反映了寒武纪矿源层成矿体系。通过包裹体研究,认为八面山萤石矿床是受地层-岩体-层间断裂共同控制"三位一体"的热液成因矿床。

关 键 词:流体包裹体  地球化学  八面山萤石矿床

STUDY ON FLUID INCLUSION GEOCHEMISTRY OF BA-MIANSHAN FLUORITE DEPOSITS OF ZHEJIANG PROVINCE
Yan Fei,Xia Xuehui,Xu Shaokang,Wu Yinghui,Pang Siyu.STUDY ON FLUID INCLUSION GEOCHEMISTRY OF BA-MIANSHAN FLUORITE DEPOSITS OF ZHEJIANG PROVINCE[J].Geology of Chemical Minerals,2010,32(4):215-220.
Authors:Yan Fei  Xia Xuehui  Xu Shaokang  Wu Yinghui  Pang Siyu
Institution:Yan Fei Xia Xuehui Xu Shaokang Wu Yinghui Pang Siyu Geological Institute of China Chemical Geology and Mine Bureau,Zhuozhou,Hebei,072754,China
Abstract:There are three types of fluid inclusions in Bamianshan fluorite deposits,vapor-liquid inclusion,vapor inclusion and polyphase inclusions with daughter minerals.The ore-forming temperature varies slightly,mostly in 120~240°C.The inclusion temperature changes at a range of 115~250℃ in fine banded fluorite,while in megacryst massive fluorite and quartz vein fluorite at a range of 135~170℃.The fluid inclusion of fluorite deposits mainly are low salinity ore-forming fluid,and the ionic type of ore-forming fluid is K+-Ca2+-HCO--F-,there are two ore-forming fluid system in the hydrothermal process,the KCl-H2O system represents the results of later magmatic period and CO2-CaF2-H2O system may represents ore-forming system of the Cambrian source bed.According to the study on fluid inclusions,the Bamianshan fluorite deposit is a hydrothermal deposit controlled by strata,rock mass and interlayer fracture.
Keywords:fluid inclusion  geochemistry  Bamianshan fluorite deposit
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