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| 新疆喀什凹陷乌拉根铅锌矿床有机质特征及其地质意义 | |
| 引用本文： | 董新丰,薛春纪,李志丹,刘增仁.新疆喀什凹陷乌拉根铅锌矿床有机质特征及其地质意义[J].地学前缘,2013,20(1):129-145. |
| 作者姓名： | 董新丰 薛春纪 李志丹 刘增仁 |
| 作者单位： | 1. 中国国土资源航空物探遥感中心,北京100083;地质过程与矿产资源国家重点实验室;中国地质大学(北京)地球科学与资源学院,北京100083 2. 地质过程与矿产资源国家重点实验室;中国地质大学(北京)地球科学与资源学院,北京100083 3. 中国地质调查局天津地质调查中心,天津,300170 4. 新疆鑫汇矿业有限责任公司,新疆乌鲁木齐,830000 |
| 基金项目： | 国家科技支撑计划项目(2011BAB06B02);国家自然科学基金项目(41072069,40930423) |
| 摘 要： | 乌拉根铅锌矿床位于新疆喀什凹陷北部,矿区及外围发育大量有机物质,有机质与铅锌成矿的关系备受关注。文中采用有机质抽提、族组分分离、定量及饱和烃色谱-质谱等实验分析方法对铅锌矿区有机物质及外围油砂中氯仿沥青"A"和生物标志物进行分析,研究铅锌矿区及外围有机质特征及其地质意义,并对有机质与铅锌矿化的关系进行了探讨。结果表明,近矿围岩和外围油砂中氯仿沥青"A"族组成及其饱和烃的主要生物标志物特征均较相似,CPI=1.11～1.17,Pr/Ph=0.68～1.08,C27、C28、C29规则甾烷具有C27>C28 |
| 关 键 词： | 生物标志物 氯仿沥青“A” 有机质 乌拉根铅锌矿床 喀什凹陷 新疆 |
Characteristics and geological significances of the organic matter in the Wulagen Zn-Pb deposit,Kashi sag,Xinjiang |
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| DONG Xinfeng,XUE Chunji,LI Zhidan,LIU Zengren.Characteristics and geological significances of the organic matter in the Wulagen Zn-Pb deposit,Kashi sag,Xinjiang[J].Earth Science Frontiers,2013,20(1):129-145. | |
| Authors: | DONG Xinfeng XUE Chunji LI Zhidan LIU Zengren |
| Institution: | 1.China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China 2.State Key Laboratory of Geological Processes and Mineral Resources;School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China 3.Tianjin Center,China Geological Survey,Tianjin 300170,China 4.Xinjiang Xinhui Mineral Corporation,rümqi 830000,China |
| Abstract: | Wulagen zinc-lead deposit in Xinjiang Province is located in north margin of Kashi sag.Large quantity of organic matter exists in the mining area and the periphery of Wulagen zinc-lead deposit,and the relationship between organic matter and zinc-lead mineralization has attracted the attention.By the organic extraction,family components separation and quantitative,saturated hydrocarbons chromatogram-mass spectrum,the chloroform bitumen "A" and biomarkers were analyzed,and the characteristics of the organic matter and its geological significances and the relationship between organic matter and zinc-lead mineralization were discussed.The chloroform bitumen"A" family components and main eigenvalues of biomarkers in the wall-rocks and the periphery of Wulagen zinc-lead deposit have a similar and smaller variational range(CPI=1.11-1.17;Pr/Ph=0.68-1.08;C27,C28 and C29 sterane has a pattern of C27>C28 |
| Keywords: | biomarkers chloroform bitumen "A" organic matter Wulagen zinc-lead deposit Kashi sag Xinjiang |
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