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塔里木盆地西克尔萤石地球化学特征及成因讨论
引用本文:饶红娟,罗平,阳正熙,周刚,宋金民.塔里木盆地西克尔萤石地球化学特征及成因讨论[J].沉积学报,2010,28(4):821-831.
作者姓名:饶红娟  罗平  阳正熙  周刚  宋金民
作者单位:成都理上大学能源学院,成都,610059;中国石油勘探开发研究院,北京,100083;中国石油勘探开发研究院,北京,100083;成都理上大学能源学院,成都,610059;成都理上大学沉积地质研究院,成都,610059
基金项目:国家重点基础研究发展规划 
摘    要:通过对塔里木盆地西克尔地区萤石矿及赋矿围岩进行地球化学分析,探讨该区萤石矿成因。研究表明,萤石矿物稀土元素配分模式图表现出轻稀土元素相对富集,正铕异常特点;微量元素分析显示Eu、Sr、Ba具有相关性;Sr同位素比值与围岩相近。最终认为萤石矿成矿流体主要来自于加热的盆地卤水,微量(包括稀土)元素来自下伏地层及围岩,Ba、Eu、F等元素可能来自下寒武统硅质岩及磷块岩。

关 键 词:塔里木  萤石  稀土元素  正铕异常  热水沉积
收稿时间:1900-01-01

Geochemistry of Fluorite and Its Genesis in Sickl Area, Tarim Basin
RAO Hong-juan,LUO Ping,YANG Zheng-xi,ZHOU Gang,SONG Jin-min.Geochemistry of Fluorite and Its Genesis in Sickl Area, Tarim Basin[J].Acta Sedimentologica Sinica,2010,28(4):821-831.
Authors:RAO Hong-juan  LUO Ping  YANG Zheng-xi  ZHOU Gang  SONG Jin-min
Institution:Energy School, Chengdu University of Technology, Chengdu 610059
Abstract:Geochemistry of fluorite deposits and its ore rocks in Sickl area, Tarim Basin is applied to investigate the ingenesis. The study shows that: relative LREE concentration and positive Eu anomaly are resulted from REE distribution pattern diagrams of fluorite; Eu, Sr and Ba are related closely in trace element analysis; the isotope ratio of Sr in fluorite is close to that in surrounding rocks. Conclusions are: ore forming fluids of the fluorite mainly are from the infiltration of heated basin brine ; trace elements(including REE) are from underlying strata and surrounding rocks; and elementsF, Ba, Eu are from Lower Cambrian siliceous rocks and phosphorite.
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