西昆仑玛尔坎苏地区穆呼锰矿含锰岩系沉积环境——来自(虫筳)类化石及碳酸盐岩碳、氧、锶同位素证据

陈登辉; 隋清霖; 郭周平; 赵晓健; 滕家欣; 高永宝

doi:10.19751/j.cnki.61-1149/p.2022.02.001

西昆仑玛尔坎苏地区穆呼锰矿含锰岩系沉积环境——来自(虫筳)类化石及碳酸盐岩碳、氧、锶同位素证据

陈登辉^1,2,3,
隋清霖⁴,
郭周平^1,2,3,
赵晓健^1,2,3,
滕家欣^1,2,3,
高永宝^1,2,3

1. 自然资源部岩浆作用成矿与找矿重点实验室, 陕西西安 710054;
2. 中国地质调查局造山带地质研究中心, 陕西西安 710054;
3. 中国地质调查局西安地质调查中心, 陕西西安 710054;
4. 南华大学资源环境与安全工程学院, 湖南衡阳 421001

基金项目:

第二次青藏高原综合科学考察研究“西昆仑-祁漫塔格地区锰铁铅锌铜等大宗金属矿产科考”（2021QZKK0303）；国家自然科学基金“西昆仑塔什库尔干地区赞坎铁矿床流体包裹体研究及对膏盐层参与铁矿成矿的启示”（41503046）、陕西省自然科学基金“西昆仑奥尔托喀讷什锰矿优质富锰矿成因”“西昆仑奥尔托卡纳什锰矿上石炭统含锰碳酸盐岩沉积环境研究”（2019JQ-935、2017JM4024）和中国地质调查局“西昆仑大红柳滩-甜水海地区大型矿产资源基地综合调查”（DD20190143）。

详细信息

作者简介:
陈登辉(1980-),男,博士,高级工程师,主要从事矿产地质调查和沉积学研究。E-mail:47134454@qq.com。

中图分类号: P618.32
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出版历程
- 收稿日期: 2021-06-23
- 修回日期: 2021-12-07
- 网络出版日期: 2022-07-28

Sedimentary Environment of Mn-bearing Carbonate from the Muhu Manganese Deposit in Malkansu, West Kunlun: Evidences from Fusulinids and C-O-Sr Isotopes

CHEN Denghui^1,2,3,
SUI Qinglin⁴,
GUO Zhouping^1,2,3,
ZHAO Xiaojian^1,2,3,
TEN Jiaxin^1,2,3,
GAO Yongbao^1,2,3

1. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an 710054, Shaanxi, China;
2. Research Center for Orogenic Geology, China Geological Survey, Xi'an 710054, Shaanxi, China;
3. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, Shaanxi, China;
4. School of Resource & Environment and Safety Engineering, University of South China, Hengyang 421001, Hunan, China

摘要

摘要: 穆呼锰矿是玛尔坎苏锰矿带东部重要的典型锰矿床，锰矿体主要产于一套碎屑岩-碳酸盐岩之中。含锰岩系顶部产出的（虫筳）类化石主要为似纺锤（虫筳）Quasifusulina属，其中包括最揉似纺锤（虫筳）Quasifusulina tennissima（Schellwien）、大豆形似纺锤（虫筳）Quasifusulina phaselus（Lee）和拟紧卷似纺锤（虫筳）Quasifusulina paracompacta（Chang）3个种和2个未定种，指示含锰岩系为晚石炭世地层。锰矿体顶底板围岩δ¹³C_PDB值为-2.06‰~3.99‰，δ¹⁸O_PDB值为-13.35‰~-7.49‰，⁸⁷Sr/⁸⁶Sr值为0.707 70~0.707 97。菱锰矿δ¹³C_PDB值为-16.60‰~-1.95‰，δ¹⁸O_PDB值为-11.51‰~-4.48‰，⁸⁷Sr/⁸⁶Sr值为0.707 64~0.707 90。综合分析，认为穆呼锰矿含锰岩系为温暖、盐度正常、水动力相对较强的浅海陆棚沉积；水体清澈，但相对于碳酸盐岩台地沉积水体要浑浊。碳酸盐岩和锰矿层在沉积过程中受到了陆表水的影响，菱锰矿的形成与有机质还原作用有关。
- 上石炭统 /
- 碎屑岩-碳酸盐岩 /
- 沉积环境 /
- (虫筳)类 /
- 碳、氧、锶同位素 /
- 穆呼锰矿 /
- 西昆仑
Abstract: Muhu Manganese Deposit is an important typical manganese deposit in the eastern part of the Malkansu Manganese Belt. Manganese ore bodies are mainly hosted in a set of clastic-carbonate rocks. Fossils from the top of manganese-bearing rock series are mainly Quasifusulina, include Quasifusulina tennissima (Schellwien), Quasifusulina phaselus (Lee), Quasifusulina paracompacta (Chang), and two unidentified species, indicating that the geological age of the manganese-bearing strata should be the Late Carboniferous. The δ¹³C_PDB values of surrounding rock range from -2.06‰ to 3.99‰; δ¹⁸O_PDBvalues range from -13.35‰ to-7.49‰; and ⁸⁷Sr/⁸⁶Sr values range from 0.707 70 to 0.707 97. In contrast, the δ¹³C_PDB values of rhodochrosite range from -16.60‰ to-1.95‰; δ¹⁸O_PDB values range from -11.51‰ to-4.48‰; and ⁸⁷Sr/⁸⁶Sr values range from 0.707 64 to 0.707 90. Comprehensive analysis reveals that the Mn-bearing rock series in Muhuhu Manganese Deposit developed in a shallow shelf with warm, normal salinity, and relatively strong hydrodynamic force. The water column is clear, but comparatively turbid compared to carbonate platform sedimentary environment. The deposition of carbonate rocks and manganese deposits was affected by surface water, and the formation of rhodochrosite is associated with the reduction of organic matter.
- Late Carboniferous /
- terrigenous clastics-carbonate /
- sedimentary environment /
- fusulinids /
- C, O, Sr isotopes /
- Muhu manganese deposit /
- West Kunlun

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西昆仑玛尔坎苏地区穆呼锰矿含锰岩系沉积环境——来自(虫筳)类化石及碳酸盐岩碳、氧、锶同位素证据

作者简介: 陈登辉(1980-),男,博士,高级工程师,主要从事矿产地质调查和沉积学研究。E-mail:47134454@qq.com。

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Sedimentary Environment of Mn-bearing Carbonate from the Muhu Manganese Deposit in Malkansu, West Kunlun: Evidences from Fusulinids and C-O-Sr Isotopes

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作者简介:
陈登辉(1980-),男,博士,高级工程师,主要从事矿产地质调查和沉积学研究。E-mail:47134454@qq.com。