李胜荣
主要从事金矿床地质学与成因矿物学、环境及生命矿物学、黑色岩系地球化学和成矿系统学研究。
个性化签名
- 姓名:李胜荣
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学术头衔:
博士生导师
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学科领域:
矿物学(包括放射性矿物学)
- 研究兴趣:主要从事金矿床地质学与成因矿物学、环境及生命矿物学、黑色岩系地球化学和成矿系统学研究。
李胜荣,男,汉族,1956年10月出生,1978-1981年在河北地质学院学习,获学士学位。1983-1984年在武汉地质学院北京研究生部学习,1985-1986年在印度地质调查局培训学院学习。1989-1992年在中国地质大学(北京)学习,获矿物学理学博士学位。1993-1994年在中国科学院地球化学研究所作博士后研究。1995年1月被中国科学院地球化学研究所破格评定为研究员,1995年2月至今在中国地质大学(北京)地球科学与资源学院任教,1997年1月被地质矿产部破格评定为教授。现任岩石与矿物教研室主任、博士生导师,兼任中国矿物岩石地球化学学会成因矿物学找矿矿物学专业委员会主任,中国教育家协会理事,中文核心期刊《矿物岩石》 、 《岩石矿物学杂志》 、 《现代地质》编委会委员,国家自然科学基金委员会地球科学部第十届专家评议组成员,国家“973计划”特聘专家组成员。国际地质对比计划IGCP501项目国际执行委员,中国工作组组长。
曾先后任结晶学、矿物学、成因矿物学、现代矿物学、环境与生命矿物学、岩浆岩石学、矿床学和专业英语等9门课程主讲,指导硕士生17人,协助指导博士生7人,指导博士生10人。负责中国博士后基金、国家教委博士点基金、国家自然科学基金、国家攀登计划、国家“973”计划、地质大调查和国际地质对比计划(IGCP501)等项目24项,参加15项。主要从事金矿床地质学与成因矿物学、环境及生命矿物学、黑色岩系地球化学和成矿系统学研究。出版专著5部(含英文版2部),参与编写专著3部(含英文版1部)。在《中国科学》 、《科学通报》 、《自然科学进展》 、《地质论评》 、《矿物学报》 、《岩石学报》、《矿床地质》、《现代地质》 、《矿物岩石》 、《岩石矿物学杂志》、《Chinese Journal of Geochemistry》 、《Journal of China University of Geosciences》、《Sciencein China》、《Progressin Natural Science》、《Chinese Science Bulletin》、《Mineralogical Magazine》、《Clay Science》、《HimalayanJournalofScience》等国内外重要学术刊物发表论文120余篇。SCI和EI刊物论文13篇。获地质矿产部科技成果三等奖2项,其他奖8项。
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【期刊论文】Some typical partition and distributition patterns of platinum group elements
李胜荣, L. Shengrong, G. Zhenmin
GOLDSCHMIDT CONFERENCE EDINBURGH 1994,-0001,():
-1年11月30日
Some typical partition and distributition patterns of platinum group elements (PGEs) are noticed by the authors in the study on geochemical indicator system of PGEs. They can be taken as useful tools in solving diagenetic and metallogenic as well as other more extended geochemical problems.
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【期刊论文】Silicalites of Hydrothermal Origin in the Lower Cambrian Black Rock Series of South China *
李胜荣, LI SHFNGRONG, AND GAO ZHENMIN
Vol. 15 No.2 CHINESE JOURNAL OF GEOCHEMISTRY 1996,-0001,():
-1年11月30日
A silicalite bed was found in the hanging wall and foot wall of the sulfide-rich bed of the Lower Cambrian black rock series in Sourh China. Its origin was not described before. On the oxide (SiO2-Al2O3, SiO2-MgO, SiO2-K2O+Na2O) diagrams for discriminating silicalites of chemical, biological and volcanic origins (Liu Xiufeng, 1991), most of the data points of silicalites fall within the areas representing silicalites of chemical and volcanic origins. On the Al-Fe-Mn diagram for discriminating silicalites of hydrorhermal and biological origins (Yamamoto, 1987), the data points fall within the areas represenring silicalires of hydrothermal and hydrothermal-biological origins. On the SiO2-Al2O3 diagram for discriminating silicalites of hydrorhermal and hydrogenous origins (Bonatti, 1975), the dara points mostly fall within the hydrothermal area. The ratios of SiO/Al2O3, SiO2/(K2O+Na2O), SiO2/MgO, and K2O/Na2O in the silicalites stand between those of volcanic sediments and of seafloor hydrothermal sediments. The total amount of rare-earth elements in the silicalites is low; the North American Shale-normalized REE patterns decline leftward with obvious negative Ce anomaly. The trace elements Mo, Zn, As, Sb, Se, U, and Ba are higher than those in non-hydrothermal sediments and U/Th≥ 1. The present authors think that the silicalites are derived from seafloor hot brines which had artracted elements from igneous rocks.
silicalite, hot brine, black rock series, Lower Cambrian series, South China
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李胜荣, SHENGRONG LI, JUNFENG SHEN, HONG XU
Symposium of the Kanazawa University 21st-Century COE Program Vol. 1 (2003),-0001,():
-1年11月30日
In the Lower Cambrian black shales of south China developed a metal-rich bed with large amounts of Au, Ag and platinum group elements (NME) and many other metals such as Ni, Mo, As, Ba and Se. The concentrations of NME are much higher in Zunyi of Guizhou province (PGE+Au, 1138×10-9; Ag, 91775×10-9) than that in Zhangjiajie of Hunan province (PGE+Au, 605×10-9; Ag, 18 534×10-9). The Romean data are of 2.550 and 2.393 for the metal-rich bed and black shale in Zhangjiajie and the equivalent data are of 3.054 and 3.272 in Zunyi. The δ13C (PDB, %o) values are of-31.008~-31.181 (±0.2) for kerogen from Zhangjiajie and -31.723~-33.854 (±0.2) from Zunyi. Correspondently, the Proterozoic and Cambrian ultramafic magmatism in Guizhou province is much more developed than that in Hunan province. This might be of significance to indicate that the NME in the black shales were originally from ultramafic magma or the igneous rocks.
reflectance and carbon isotopes of kerogen, black shale, noble metal elements, Lower Cambrian, Guizhou-Hunan provinces,, China.,
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李胜荣, 江永宏, 王吉中,
矿物岩石,2003,23(2):22~26,-0001,():
-1年11月30日
黄铁矿在云南墨江金厂金矿床中广泛出现于蛇纹岩、黄铁铬绢英岩、硅质岩和石英脉中。通过对与黄铁矿成因产状密切关联的热液演化阶段的划分、黄铁矿的晶形统计、黄铁矿的热电性研究、黄铁矿的电子探针分析、黄铁矿所赋存的含金岩矿石标本中金品位化学分析,确定了与成矿物质来源金厂蛇纹岩化镁质超基性岩、硅质岩和可能隐伏的酸性侵入岩有关的系列成因标型。在对黄铁矿热电标型的均方差参数的自然对数值(lnMp)与金品位自然对数值(lnTg)的相关性研究基础上,提出当lnMp值接近4.1时,金的品位值接近工业开采标准。金厂金矿体与镍矿体尽管空间上分离,但近镍矿体与富金石英脉中黄铁矿的共生元素组成成分表明金、镍矿体中部分矿质具有同源同期的特征。此外,金厂组硅质岩和可能的隐伏岩体在成矿物源和热源方面的贡献不容忽视。
金厂金矿床, 黄铁矿, 成因标型, 找矿标型
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李胜荣, 别风雷, 侯增谦, 苏文超, 徐九华
岩石学报,2000, 16(4):575~580,-0001,():
-1年11月30日
本文用ICP-MS首次测定了呷村银多金属黑矿型矿床矿石流体包裹体中的稀土元素含量。研究表明,主成矿期流体稀土元素配分模式均为轻稀土富集,Eu具明显正异常。通过初步对比,本区主成矿期流体与东太平洋脊、大西洋脊等现代高温酸性地热系统热液具有相似的稀土模式,反映了它们物化条件的相似性;但前者∑REE高于后者,且两者Eu/Eu*值不同。经过分析,本区成矿流体Eu正异常主要为T、pH、fo2控制,另外,围岩性质和水2岩主反应带压力也可能影响了REE含量及Eu异常的不同。至于(La/Yb)cn>1,可能是由于矿物或微粒表面的吸附作用所致。
VMS矿床, 流体包裹体, 稀土元素, ICP-MS, 川西呷村
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【期刊论文】Genetic Mineralogy of Pyrite from Jindoushan Gold Deposit, Yantai, Shandong Province *
李胜荣, YINGJ IFENG, ZHOU XINHUA, LI SHENGRONG, AND SUN DAISHENG
Vol. 20 No.3 CHINESE JOURNAL OF GEOCHEMISTRY 2001,-0001,():
-1年11月30日
This paper deals with the genetic mineralogy of pyrite from the Jindoushan gold deposit. As a predominant goldbearing mineral, pyrite bears lots of information about mineralization, which can be elucidated through the study of mineralogical characters such as crystal form, chemical composition, thermoelectrical coefficient, etc. In addition, the detailed genetic mineralogy data of pyrite can also help evaluate the prospects of gold deposits.
genetic mineralogy, pyrite, Shandong
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李胜荣, 肖润, , 周肃, 莫宣学, 申俊峰, 闫柏琨, 刘波
矿床地质,2005,24(1):1~14,-0001,():
-1年11月30日
西藏改则地区属班公湖-怒江板块缝合带西段,该区岩金的找矿和理论研究十分薄弱,找矿方向不明确。文章从金的成矿背景、成矿特征和成矿年代学研究入手,探讨了该缝合带演化过程中金的成矿作用,试图为该区金找矿方向的确立提供依据。研究表明,该区金矿主要分布在羌塘板片南缘铁格山一带的侏罗系雁石坪群和缝合带内木嘎岗日地体达查一带的侏罗系木嘎岗日群浅变质火山-沉积建造中。大地构造及地球化学研究反映出雁石坪群和木嘎岗日群是大陆裂谷-边缘海环境中形成的亚稳定的复理石沉积,其形成伴随有较大规模的蛇绿岩和基性火山喷发,同时有较明显的海底热水活动,地层中集中了较丰富的Au、Cu等幔源物质而成为Au的初始矿源层。早白垩世晚期,在冈底斯地块和羌塘地块碰撞拼贴过程中,富含Au、Cu等幔源组分的I型中酸性岩浆上侵,并加热下渗的海水,使之与岩浆混合成为汲取初始矿源层、蛇绿岩和中酸性岩浆岩中Au的有效介质,进而携带Au在各种岩石裂隙中运移沉淀,形成蚀变岩-石英脉过渡型金矿体。在晚白垩世海盆关闭且发生差异隆升造山过程中,原有矿床的顶部被剥蚀,并以砂矿的形式开始了金矿的再生。
地球化学, 金矿, 年代学, 含矿建造, 成矿模式, 西藏
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李胜荣, WANG Jizhong, , **, LI Shengrong, JIANG Yonghong, WEI Ruihua, and NU Huapeng
Vol. 24 No.3 CHINESE JOURNAL OF GEOCHEMISTRY 2005,-0001,():
-1年11月30日
In terms of environmental mineralogy, the environmental properties of metallic minerals, including chemical activation, adsorption, pore effect and nanometer effect, have been analyzed. On the basis of the analysis of environmental properties of metallic minerals, the applications of ironbearing sulfides, iron and manganese oxides in the purification of wastewaters containing heavy metal ions (Cr6+, Hg2+, Pb2+, etc.) have been summarized. Moreover, research on the application of metallic minerals in environmental protection has been anticipated. It should be a piece of dominating work for environmental mineralogic researchers in the future to lucubrate systematically the physical and chemical characteristics of the metallic mineral surfaces, further reveal the reciprocity process between metallic minerals and water surface, perfect the theory and model of the metallic minerals to remove contaminants, intensify study on the facilities and techniques of metallic minerals to remove contaminants, and entail well the extension and propagation of achievements.
metallic mineral, environmental property, environmental protection
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李胜荣, YUAN Wanming, WANG Shicheng, LI Shengrong & YANG Zhiqiang
Chinese Science Bulletin Vol. 47 No.3 February 2002,-0001,():
-1年11月30日
This work makes the quantitative constrain on tectonizations of the Gangdese block, south Qinghai-Tibetan Plateau. Apatite fission track (AFT) dating analyses of 15 samples collected across the Gangdese block show that the Gangdese block went through two periods of tectonizations, during 37.2-18.5Ma and 18.5-8.0Ma in the south Gangdese block, and during 47.6-5.3Ma and 5.3-0Ma in the middle Gangdese block. Different upliftings did not take place in the first period and rapid uplifting occurred in the late period. Meantime, there are some differences between the south and middle Gangdese block. Their uplifting rate is 180m/Ma and 70m/Ma respectively. The rapid uplifting time in the middle Gangdese block lagged behind the time in the south Gangdese block. It is Chala-Jiacuo-Riduo fault zone that is similar to the Yarlung Zangbo fault zone in control of the tectonization.
tectonization, fault zone, fission track, apatite, uplifting and cooling, Gangdese block.,
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