Advanced Search
Volume 37 Issue 3
. 
Turn off MathJax
Article Contents
Abstract
References
Article Navigation >  Acta Sedimentologica Sinica  > 2019  >  37(3): 477-490

CHEN DengHui, SUI QingLin, ZHAO XiaoJian, JING DeLong, TENG JiaXin, GAO YongBao. Geology, Geochemical Characteristics, and Sedimentary Environment of Mn-bearing Carbonate from the Late Carboniferous Muhu Manganese Deposit in West Kunlun[J]. Acta Sedimentologica Sinica, 2019, 37(3): 477-490. doi: 10.14027/j.issn.1000-0550.2018.157
Citation: CHEN DengHui, SUI QingLin, ZHAO XiaoJian, JING DeLong, TENG JiaXin, GAO YongBao. Geology, Geochemical Characteristics, and Sedimentary Environment of Mn-bearing Carbonate from the Late Carboniferous Muhu Manganese Deposit in West Kunlun[J]. Acta Sedimentologica Sinica, 2019, 37(3): 477-490. doi: 10.14027/j.issn.1000-0550.2018.157
shu

Geology, Geochemical Characteristics, and Sedimentary Environment of Mn-bearing Carbonate from the Late Carboniferous Muhu Manganese Deposit in West Kunlun

doi: 10.14027/j.issn.1000-0550.2018.157
  • 1.

    Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an 710054, China;

  • 2.

    Research Centre for Orogenic Geology, China Geological Survey, Xi'an 710054, China;

  • 3.

    Xi'an Center of China Geological Survey, China Geological Survey, Xi'an 710054, China

Funds:  National Natural Science Foundation of China, No. 41503046; Natureal Science Foundation of Shaanxi Province, No. 2017MJ4024; Geological Survey Project of China Geological Survey, No. DD20160015
  • Received Date: 2018-04-12
  • Rev Recd Date: 2018-07-30
  • Publish Date: 2019-06-10
  • A set of clastic-carbonate rocks developed in the Maerkansu of West Kunlun during the Late Carboniferous recently revealed that it has a great potential for rhodochrosite prospecting and has attracted significant attention. The clastic-carbonate lithofacies division and sedimentary environment analyses were carried out by measuring the manganese-bearing rock series profile, thin section identification, electron probe, scanning electron microscope, geochemical analysis, and strontium isotope testing of the carbonate rocks in the Muhu manganese mine. Our study indicates that the manganese-bearing rock series consists of eight clastic-carbonate rock facies:marlite, arenaceous limestone, microcrystalline manganese carbonate, microcrystalline-micrite limestone, gravelly limestone, gravelly arenaceous limestone, calcareous sandstone, calcareous conglomerate, and combinations of three rock facies. Based on the geochemical and strontium isotope characteristics of the ore body and its roof and floor rocks, the ancient seawater temperature averaged 22.68℃, which belongs to the subtropical zone. In all, the manganese-bearing rocks are clastic shore facies and shallow sea-land shelf facies deposits with shallow seawater. The roof and floor rocks of the ore body were in a relatively shallow oxidation-weak reduction environment with seawater, while the rhodochrosite was formed in shallow sea-land shelf sedimentary depressions with relatively deep seawater under a reduced sedimentary environment, which is related to submarine volcanic hydrothermal activity.
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-052024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-0400.511.522.5
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 3.4 %FULLTEXT: 3.4 %META: 82.0 %META: 82.0 %PDF: 14.6 %PDF: 14.6 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 3.2 %其他: 3.2 %其他: 1.6 %其他: 1.6 %China: 1.1 %China: 1.1 %Seattle: 0.5 %Seattle: 0.5 %United States: 0.8 %United States: 0.8 %[]: 0.3 %[]: 0.3 %上海: 4.0 %上海: 4.0 %东莞: 0.3 %东莞: 0.3 %中卫: 0.8 %中卫: 0.8 %临汾: 1.1 %临汾: 1.1 %乌鲁木齐: 0.5 %乌鲁木齐: 0.5 %保山: 0.3 %保山: 0.3 %兰州: 0.3 %兰州: 0.3 %凉山: 0.8 %凉山: 0.8 %北京: 14.3 %北京: 14.3 %南宁: 0.3 %南宁: 0.3 %南昌: 1.1 %南昌: 1.1 %台州: 0.5 %台州: 0.5 %合肥: 0.5 %合肥: 0.5 %和田: 0.3 %和田: 0.3 %哈尔滨: 0.3 %哈尔滨: 0.3 %城南: 0.3 %城南: 0.3 %天津: 0.3 %天津: 0.3 %奥马哈: 0.3 %奥马哈: 0.3 %山景城: 0.3 %山景城: 0.3 %巴音郭楞: 0.3 %巴音郭楞: 0.3 %廊坊: 0.8 %廊坊: 0.8 %张家口: 1.6 %张家口: 1.6 %成都: 0.8 %成都: 0.8 %昆明: 1.1 %昆明: 1.1 %昌吉: 0.5 %昌吉: 0.5 %朝阳: 0.3 %朝阳: 0.3 %杭州: 0.3 %杭州: 0.3 %武汉: 2.6 %武汉: 2.6 %沈阳: 0.3 %沈阳: 0.3 %波茨坦: 0.3 %波茨坦: 0.3 %深圳: 1.1 %深圳: 1.1 %湖州: 0.3 %湖州: 0.3 %漯河: 0.8 %漯河: 0.8 %漳州: 0.3 %漳州: 0.3 %焦作: 0.3 %焦作: 0.3 %牡丹江: 0.3 %牡丹江: 0.3 %盘锦: 0.5 %盘锦: 0.5 %秦皇岛: 0.3 %秦皇岛: 0.3 %芒廷维尤: 14.0 %芒廷维尤: 14.0 %苏州: 0.5 %苏州: 0.5 %荆州: 0.8 %荆州: 0.8 %衢州: 0.5 %衢州: 0.5 %西宁: 29.6 %西宁: 29.6 %西安: 0.3 %西安: 0.3 %贵阳: 0.8 %贵阳: 0.8 %赤峰: 0.5 %赤峰: 0.5 %运城: 3.7 %运城: 3.7 %邯郸: 0.3 %邯郸: 0.3 %郑州: 1.3 %郑州: 1.3 %镇江: 0.3 %镇江: 0.3 %长沙: 0.5 %长沙: 0.5 %长治: 0.5 %长治: 0.5 %青岛: 0.3 %青岛: 0.3 %其他其他ChinaSeattleUnited States[]上海东莞中卫临汾乌鲁木齐保山兰州凉山北京南宁南昌台州合肥和田哈尔滨城南天津奥马哈山景城巴音郭楞廊坊张家口成都昆明昌吉朝阳杭州武汉沈阳波茨坦深圳湖州漯河漳州焦作牡丹江盘锦秦皇岛芒廷维尤苏州荆州衢州西宁西安贵阳赤峰运城邯郸郑州镇江长沙长治青岛

  • Cited by

    Periodical cited type(16)

    1. 张帮禄，吕志成，于晓飞，李永胜，甄世民. 西昆仑玛尔坎苏锰矿带含锰岩系时代厘定及地质意义. 吉林大学学报(地球科学版). 2023(01): 120-139 .
    2. 郭志伟，赵丙刚，李智斌，孙金龙，齐云飞，和越，赵迪. 中亚造山带南缘玉石山锰矿成矿作用及成矿模式研究. 中国锰业. 2023(01): 22-26+31 .
    3. 周亚丽，潘泽，李晓姣，韩姗姗，张盛亚，乔海霞. 北祁连西段黑峡口锰矿地球化学特征及成因研究. 中国锰业. 2023(01): 52-56 .
    4. 陈登辉，隋清霖，郭周平，赵晓健，滕家欣，高永宝. 西昆仑玛尔坎苏地区穆呼锰矿含锰岩系沉积环境——来自■类化石及碳酸盐岩碳、氧、锶同位素证据. 西北地质. 2022(02): 1-13 .
    5. 黄碧云，胡兴旺，曹智鹏，曹成刚，王一点. 青海省都兰县某锰矿成矿地质背景研究. 中国锰业. 2022(02): 37-44 .
    6. 王双，尚凯凯，杨继兵，张素超，李原. 北阿尔金锰矿成矿地质条件特征及成矿规律研究. 中国锰业. 2022(04): 1-5+11 .
    7. 孙丹，刘珊珊，谭和勇，叶萍. 北山裂谷系北缘小独梁地区锰矿地质条件特征及成因分析. 中国锰业. 2022(04): 23-28 .
    8. 张连昌，董志国，张帮禄，李文君，彭自栋，王长乐，朱明田. 西昆仑“玛尔坎苏式”富锰矿主控因素及成矿模式. 地质学报. 2022(09): 3195-3210 .
    9. 杨小三，彭明章. 北山鲤鱼梁锰矿成矿地质条件及矿床成因研究. 中国锰业. 2022(05): 25-30+48 .
    10. 吕志成，陈辉，宓奎峰，张帮禄，谢月桥，庞振山，程志中，薛建玲，公凡影，段彬，吕鑫. 勘查区找矿预测理论与方法及其应用案例. 地质力学学报. 2022(05): 842-865 .
    11. 李文渊，张照伟，高永宝，洪俊，陈博，张志炳. 昆仑古特提斯构造转换与镍钴锰锂关键矿产成矿作用研究. 中国地质. 2022(05): 1385-1407 .
    12. 张帮禄，薛建玲，吕志成，于晓飞，李永胜，甄世民. 西昆仑玛尔坎苏锰矿带晚石炭世岩相古地理特征及其对成矿的控制. 地质通报. 2022(11): 2047-2064 .
    13. 金川，谢月桥，李玉飞，张阳. 西昆仑玛尔坎苏锰矿带含锰岩系沉积相分布特征. 新疆有色金属. 2021(01): 26-27 .
    14. 马登贤，朱海波，王蒙，宋玉亭，张智强，郑成龙，苗秀川，马林. 新疆奥尔托喀讷什锰矿床地质特征及成因. 中国锰业. 2021(02): 11-17 .
    15. 董志国，张连昌，董飞羽，张帮禄，谢月桥，查斌，彭自栋，王长乐. 西昆仑穆呼锰矿床地质特征、控矿因素及成矿模式. 吉林大学学报(地球科学版). 2020(05): 1358-1372 .
    16. 张连昌，张帮禄，董志国，谢月桥，李文君，彭自栋，朱明田，王长乐. 西昆仑玛尔坎苏石炭纪大型锰矿带构造背景与成矿条件. 吉林大学学报(地球科学版). 2020(05): 1340-1357 .

    Other cited types(7)

通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索
Get Citation
PDF
XML

Article Metrics

Article views(438) PDF downloads(241) Cited by(23)

Proportional views
Related
Publishing history
  • Received:  2018-04-12
  • Revised:  2018-07-30
  • Published:  2019-06-10

Geology, Geochemical Characteristics, and Sedimentary Environment of Mn-bearing Carbonate from the Late Carboniferous Muhu Manganese Deposit in West Kunlun

doi: 10.14027/j.issn.1000-0550.2018.157
  • 1. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an 710054, China;
  • 2. Research Centre for Orogenic Geology, China Geological Survey, Xi'an 710054, China;
  • 3. Xi'an Center of China Geological Survey, China Geological Survey, Xi'an 710054, China
Funds:  National Natural Science Foundation of China, No. 41503046; Natureal Science Foundation of Shaanxi Province, No. 2017MJ4024; Geological Survey Project of China Geological Survey, No. DD20160015
  • Received Date: 2018-04-12
  • Rev Recd Date: 2018-07-30
  • Publish Date: 2019-06-10

Abstract: A set of clastic-carbonate rocks developed in the Maerkansu of West Kunlun during the Late Carboniferous recently revealed that it has a great potential for rhodochrosite prospecting and has attracted significant attention. The clastic-carbonate lithofacies division and sedimentary environment analyses were carried out by measuring the manganese-bearing rock series profile, thin section identification, electron probe, scanning electron microscope, geochemical analysis, and strontium isotope testing of the carbonate rocks in the Muhu manganese mine. Our study indicates that the manganese-bearing rock series consists of eight clastic-carbonate rock facies:marlite, arenaceous limestone, microcrystalline manganese carbonate, microcrystalline-micrite limestone, gravelly limestone, gravelly arenaceous limestone, calcareous sandstone, calcareous conglomerate, and combinations of three rock facies. Based on the geochemical and strontium isotope characteristics of the ore body and its roof and floor rocks, the ancient seawater temperature averaged 22.68℃, which belongs to the subtropical zone. In all, the manganese-bearing rocks are clastic shore facies and shallow sea-land shelf facies deposits with shallow seawater. The roof and floor rocks of the ore body were in a relatively shallow oxidation-weak reduction environment with seawater, while the rhodochrosite was formed in shallow sea-land shelf sedimentary depressions with relatively deep seawater under a reduced sedimentary environment, which is related to submarine volcanic hydrothermal activity.

CHEN DengHui, SUI QingLin, ZHAO XiaoJian, JING DeLong, TENG JiaXin, GAO YongBao. Geology, Geochemical Characteristics, and Sedimentary Environment of Mn-bearing Carbonate from the Late Carboniferous Muhu Manganese Deposit in West Kunlun[J]. Acta Sedimentologica Sinica, 2019, 37(3): 477-490. doi: 10.14027/j.issn.1000-0550.2018.157
Citation: CHEN DengHui, SUI QingLin, ZHAO XiaoJian, JING DeLong, TENG JiaXin, GAO YongBao. Geology, Geochemical Characteristics, and Sedimentary Environment of Mn-bearing Carbonate from the Late Carboniferous Muhu Manganese Deposit in West Kunlun[J]. Acta Sedimentologica Sinica, 2019, 37(3): 477-490. doi: 10.14027/j.issn.1000-0550.2018.157
shu

    HTML

Catalog

    Links

    Journal Online

    Contact Us

    • Website Copyright © 2011 Editorial Office of Acta Sedimentologica Sinica
    • Address: 8 Tianshui Middle Road, Lanzhou
    • Post code: 730000   Tel:（0931）8264231
    • 陇ICP备2021001824号-28
    • 甘公网安备 62010202000673号
    Wechat

    Email alert

    RSS

    Supported by: Beijing Renhe Information Technology Co. Ltd  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return