Genesis and Geochemical Characteristics of the Cambrian Carbonaceous  Rock Series in Mianxian-Lüeyang Region, Shanxi Province

Abstract

Abstract:

The formation of phosphorus and manganese ore deposit was closely related to the Cambrian carbonaceous rock series which were important prospecting criteria in Mianxian-Lüeyang region. Samples of carbonaceous rock series collected from the study area were analyzed for major and trace elements that were used to demonstrate the genesis. P、Mn element were relatively enriched in carbonaceous rock series and enrichment coefficients were similar，suggesting that the carbonaceous rock series were related to the genesis of the Mn and P deposit. Low MnO/TiO₂ values, plots in Na-Mg and Sr-Ba diagram indicate sedimentary environment from the land closer to marginal sea of the continental slope. Low Sr/Ba，U/Th values and plots in the Al-Fe-Mn triangle diagram represent a non-hydrothermal sedimentary condition. The high V/(V+Ni) and δU values indicate an anoxic sedimentary environment，so the carbonaceous rock series were deposited in an anoxic oxygen (reduction) sedimentary environment.

Key words: carbonaceous rock series；geochemistry；anoxic environment；non-hydrothermal sediment；Mianxian-Lüeyang region, Shanxi Province

CLC Number:

P588.24

QIAO Geng-Biao,YANG Zhong-Tang,LI Zhi-Ming,YANG Xiao-Yong,LAN Xiang-Hua. Genesis and Geochemical Characteristics of the Cambrian Carbonaceous Rock Series in Mianxian-Lüeyang Region, Shanxi Province[J]. Geoscience, 2011, 25(2): 211-218.

References

［1］范德廉，张焘，叶杰，等. 中国的黑色岩系及其有关矿床［M］. 北京：科学出版社，2004：1-48.
［2］刘国平，艾永富. 含碳岩系与金矿床［J］. 黄金地质，1998，4（2）：62-66.
［3］庄汉平，卢家烂，傅家谟，等. 白果园黑色岩系型银（钒）矿床沉积古环境与银（钒）初始富集［J］. 地质论评，1997，43（4）：373-380.
［4］江永宏. 湘黔地区下寒武统黑色岩系型镍钼矿床中重晶石标型特征研究［J］. 现代地质，2009，23（3）：490-496.
［5］杨钟堂，李智明，乔耿彪，等. 陕西省勉县后沟锰矿成矿特征、成矿模式及找矿标志［J］. 地质与勘探，2008，44（2）：38-44.
［6］王立社. 陕西秦岭黑色岩系及其典型矿床地质地球化学与成矿规律研究［D］. 西安：西北大学，2009：53-65.
［7］吴朝东，杨承运，陈其英. 湘西黑色岩系地球化学特征和成因意义［J］. 岩石矿物学杂志，1999，18（1）：26-38.
［8］叶杰，范德廉. 黑色岩系型矿床的形成作用及其在我国的产出特征［J］. 矿物岩石地球化学通报，2000，19（2）：95-102.
［9］Li Shengrong，Gao Zhenmin. Source tracing of noble metal elements in Lower Cambrian black rock series of GuizhouHunan Provinces, China［J］. Sciencein China (Series D)，2000，43（6）：625-632.
［10］赵百胜，刘家军，王建平，等. 白云鄂博群黑色岩系微量元素地球化学特征及地质意义［J］. 现代地质，2007，21（1）：87-94.
［11］杨钟堂，乔耿彪，李智明，等. 陕西省勉县后沟—大坪山锰矿床地质-地球化学特征及控矿因素［J］. 地质科学，2009，44（1）：88-102.
［12］杨忠堂，乔耿彪，李智明，等. 陕西省勉县后沟—大坪山一带锰矿普查报告［R］. 西安：西安地质矿产研究所，2010：17-30.
［13］李会民，李智明. 扬子地台北缘锰矿成矿地质特征及找矿方向研究［J］. 地质与勘探，2005，41（1）：18-21.
［14］龚迎莉，汪双清，沈斌. 电感耦合等离子体原子发射光谱法同时测定沉积岩中15个元素［J］. 岩矿测试，2007，26（3）：230-232.
［15］黎彤. 中国陆壳及其沉积层和上陆壳的化学元素丰度［J］. 地球化学，1994，23（2）：140-145.
［16］刘英俊，曹励明，李兆麟，等. 元素地球化学［M］. 北京：科学出版社，1986：399-407.
［17］Bhatia M R, Crook K A W. Trace element characteristics of gray wackes and tectonic discrimination of sedimentary basins［J］.Contributions to Mineralogy and Petrology, 1986, 92(2): 181-193.
［18］Bostrm K, Peterson M N A. The origin of A1poor ferromanganoan sediments in areas of high heat flow on the East Pacific Rise ［J］. Marine Geology,1969, 7(5): 427-447.
［19］Yamamoto K. Geochemical characteristics and depositional environments of chert and associated rocks in the Franciscan and Shimanto Terranes ［J］.Sedimentary Geology, 1987, 52(1/2): 65-108.
［20］Adachi M, Yamamoto K, Sugisaki R. Hydrothermal chert and associated siliceous rocks from the Northern Pacific, their geological significance as indication of ocean ridge activity［J］. Sedimentary Geology, 1986, 47(1/2): 125-148.
［21］Zhang Zhengwei，Yang Xiaoyong，Li Shuang，et al. Geochemical characteristics of the Xuanwei Group in West Guizhou: Significance of sedimentary environment and mineralization［J］. Chinese Journal of Geochemistry，2010, 29(4): 355-364.
［22］Nicholson K. Genetic types of manganese oxide deposits in Scotland：Indicators of paleooceanspreading rate and a Devonian geochemical mobility boundary［J］. Economic Geology, 1992, 87(5)：1301-1309.
［23］Murray R W. Chemical criteria to identify the depositional environment of chert: General principles and application［J］. Sedimentary Geology, 1994,90(3/4):213-232.
［24］何俊国，周永章，杨志军，等. 藏南彭错林硅质岩地球化学特征及沉积环境分析［J］. 吉林大学学报：地球科学版，2009，39（6）：1055-1065.
［25］江纳言，贾蓉芬，王子玉. 下扬子区二叠纪古地理和地球化学环境［M］. 北京: 石油工业出版社，1994：65-90.
［26］谢建成，杜建国，许卫，等. 安徽贵池地区含锰岩系地质地球化学特征［J］. 地质论评，2006，52（3）：396-408.
［27］杜小伟，杨晓勇，杨钟堂，等. 印度次大陆中央构造带沉积-变质型锰矿的矿物学和地球化学［J］. 地质科学，2009，44（1）：103-117.
［28］Nicholson K. Contrasting mineralogicalgeochemical signatures of manganese guides to metallogenesis［J］. Economic Geology, 1992, 87(5)：1253-1264.
［29］全国矿产储量委员会办公室. 矿产工业要求参考手册［M］. 北京：地质出版社，1987：193-194.
［30］陈建强，周洪瑞，王训练. 沉积学及古地理学教程［M］. 北京：地质出版社，2004：84-87.
［31］范德廉. 锰矿床地质地球化学研究［M］. 北京: 气象出版社，1994：1-12.
［32］赵振华. 微量元素地球化学原理［M］. 北京: 科学出版社，1997：15-30.
［33］Hatch J R，Leventhal J S. Relationship between inferred redoxpotential of the depositional environment and geochemistry of the Upper Pennsylvanian（Missourian） Stark Shale Member of the Dennis Limestone，Wabaunsee County，Kansas,USA［J］. Chemical Geology，1992，99(1/3)：65-82.
［34］Crowley T J，Berner R A. Palaeoclimate：CO2 and climate change［J］. Science，2001, 292：870-872.
［35］Tucker M E. The PrecambrianCambrian boundary seawater che mistry, ocean circulation and nutrient supply in metazoan，extinction and biomineralization［J］.Journal of Geological Society of London，1992, 149(4)：655-668.
［36］施春华，胡瑞忠，王国芝. 贵州织金磷矿岩元素地球化学特征［J］. 矿物学报，2006，26（2）：169-174.
［37］杨剑，易发成，侯兰杰. 黔北黑色岩系的岩石地球化学特征和成因［J］. 矿物学报，2004，24（3）：285-289.
［38］Wignall P B. Black Shales［M］. Oxford: Clarendon Press, 1994: 1-46.

[1]	HOU Yanming, WANG Yunzhang, XU Yongjing, ZHANG Xuemei. Geophysical and Geochemical Characteristics of Cryptoexplosive Breccias at Tanshang, Daixian, Shanxi Province and Their Geological Significance [J]. Geoscience, 2019, 33(04): 727-737.
[2]	ZHENG Wei1, 2，XING Zhi-feng1, 2. Characteristics and Geological Significance of Microbially Induced Sedimentary Structures (MISS) in Changzhougou Formation of Mesoproterozoic in Licheng County, Shanxi Province [J]. Geoscience, 2015, 29(4): 825-832.
[3]	HOU Hong-bing, CHEN Li, GUO Xiao-jing, MA Lin-na. Migration Simulation Research on Hydro-fracturing Fluid in Coal Bed [J]. Geoscience, 2015, 29(2): 331-336.
[4]	MEI Min-Xiang. SequenceStratigraphic Features and Their Paleogeographical Implications for the Mesoproterozoic of the Southern Margin of Wutai Mountain: A Case Study of the Chenjiazhuang Section in Wutai County of Shanxi Province, North China [J]. Geoscience, 2010, 24(5): 888-899.
[5]	HOU Jing-Xie YANG Zhong-Fang. Study of Factors Controlling on Distribution of Heavy Metals in Loess Profiles, Linfen Basin, Shanxi Province [J]. Geoscience, 2008, 22(6): 922-928.

Genesis and Geochemical Characteristics of the Cambrian Carbonaceous Rock Series in Mianxian-Lüeyang Region, Shanxi Province

PDF (PC)

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 5

Recommended Articles

Metrics

Comments