IGGCAS OpenIR  > 矿产资源研究院重点实验室
Genesis and prospecting significance of the Buziwannan gold-polymetallic ore deposit in the West Kunlun Orogen Belt, China: Constraints from mineral geochemistry and in situ S-Pb isotope analyses of sulfides
Chen, Peiwen1,2,3,7; Zeng, Qingdong3,4,5,8; Zhou, Lingli6; Liu, Bing1,2; Fu, Yong1,2; Sun, Guotao1,2,3; Yu, Bing3,4; Long, Zhen1,2
2023
Source PublicationJOURNAL OF GEOCHEMICAL EXPLORATION
ISSN0375-6742
Volume244Pages:23
AbstractThe Buziwannan gold-polymetallic deposit is located in Northwest China's West Kunlun Orogen Belt (WKOB). There are two metallogenic stages that have been identified: skarn and hydrothermal. In this research study, in situ mineral geochemistry and sulfur-lead isotopes are used to precisely constrain the genesis and ore-forming process. Pyrite is the most dominant sulfide, and four types have been identified. Py0 is a sedimentary euhedral crystal; Py1 is a subhedral grain occurring in skarn ores, and coexists with Po1, Apy1, Ccp1 and Gn1; Py2, which coexists with Apy2, Po2 and Ccp2, is a subhedral to irregular crystal; and Py3 is a colloform crystal. Gn2 is the most recent sulfide. Magnetite and Ccp1 LA-ICMPS analyses indicate a skarn origin. Py0 and Py1 have the highest Co/ Ni ratios and Ni contents, respectively, and Au has positive correlations with Pb, Ag and As, according to the trace element compositions of pyrite (LA-ICPMS). With the exception of four spots, most pyrites have Au (0.01-30.23 ppm) and As (1.47-15,709 ppm) concentrations below the Au saturation line, indicating that the majority of gold is present as lattice bound Au+. Py3 has clearly higher Sb contents indicating that Sb-rich fluids were added. The delta 34S values of sulfides show that the sedimentary Py0 and skarn sulfides have the highest and lowest delta 34S values of +13.30 to +14.67 %o and +4.48 to +7.77 %o, respectively, and other sulfides possess delta 34S values that fall between the two members, indicating a mixed source of magmatic and sedimentary. The lead isotope values also indicate that the sulfides from the hydrothermal stage have a mixed Pb source of magmatic and sedimentary. The skarn ores are spatially and genetically related to the Triassic granodiorite, indicating a Triassic age for ore formation. The Triassic magmatic intrusions hold the potential for future gold deposit exploration in the WKOB.
KeywordIn situ sulfur isotope In situ lead isotope Buziwannan gold-polymetallic deposit WKOB
DOI10.1016/j.gexplo.2022.107125
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province
WOS KeywordPOTASSIC MICROGRANULAR ENCLAVES ; CALC-ALKALINE GRANITOIDS ; PORPHYRY MO DEPOSIT ; TECTONIC EVOLUTION ; NORTHWEST CHINA ; TIBET PLATEAU ; ACCRETIONARY TECTONICS ; METALLOGENIC EVENTS ; ZIRCON SHRIMP ; CARLIN-TYPE
Language英语
Funding ProjectNational Natural Science Foundation of China[42102084] ; Second Tibetan Plateau Scientific Expedition and Research Program[2019QZKK2702] ; Special Research Fund of Natural Science (Special Post) of Guizhou University[[2020 (27)] ; Science and Technology Foundation of Guizhou Province[ZK [2022] 041]
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Second Tibetan Plateau Scientific Expedition and Research Program ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Special Research Fund of Natural Science (Special Post) of Guizhou University ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province ; Science and Technology Foundation of Guizhou Province
WOS Research AreaGeochemistry & Geophysics
WOS SubjectGeochemistry & Geophysics
WOS IDWOS:000893452700001
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/106999
Collection矿产资源研究院重点实验室
Corresponding AuthorChen, Peiwen; Zeng, Qingdong
Affiliation1.Guizhou Univ, Coll Resource & Environm Engn, Guiyang 550012, Peoples R China
2.Minist Educ, Key Lab Karst Georesources & Environm, Guiyang 500025, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
4.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
5.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
6.Univ Coll Dublin, Sch Earth Sci, iCRAG, Dublin, Ireland
7.Jiaxiu South Rd, Guiyang 550012, Peoples R China
8.Beitucheng West Rd, Beijing 100029, Peoples R China
First Author AffilicationKey Laboratory of Mineral Resources, Chinese Academy of Sciences
Corresponding Author AffilicationKey Laboratory of Mineral Resources, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Chen, Peiwen,Zeng, Qingdong,Zhou, Lingli,et al. Genesis and prospecting significance of the Buziwannan gold-polymetallic ore deposit in the West Kunlun Orogen Belt, China: Constraints from mineral geochemistry and in situ S-Pb isotope analyses of sulfides[J]. JOURNAL OF GEOCHEMICAL EXPLORATION,2023,244:23.
APA Chen, Peiwen.,Zeng, Qingdong.,Zhou, Lingli.,Liu, Bing.,Fu, Yong.,...&Long, Zhen.(2023).Genesis and prospecting significance of the Buziwannan gold-polymetallic ore deposit in the West Kunlun Orogen Belt, China: Constraints from mineral geochemistry and in situ S-Pb isotope analyses of sulfides.JOURNAL OF GEOCHEMICAL EXPLORATION,244,23.
MLA Chen, Peiwen,et al."Genesis and prospecting significance of the Buziwannan gold-polymetallic ore deposit in the West Kunlun Orogen Belt, China: Constraints from mineral geochemistry and in situ S-Pb isotope analyses of sulfides".JOURNAL OF GEOCHEMICAL EXPLORATION 244(2023):23.
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