Ore Genesis of the Lower Urgen Porphyry Molybdenum Deposit in the Northern Great Xing'an Range, Northeast China: Constraints from Molybdenite Re-Os Dating, Fluid Inclusions, and H-O-S-Pb Isotopes
文献类型：期刊论文
| 作者 | Zhang, Guangliang6; Xie, Wei1,2; Wen, Shouqin6; Zeng, Qingdong1; Zhou, Lingli5; Wang, Hui6; Zhang, Kailun6; Tang, Tieqiao4; Ma, Pengcheng3 |
| 刊名 | MINERALS
 |
| 出版日期 | 2023-09-01 |
| 卷号 | 13期号:9页码:32 |
| 关键词 | molybdenite Re-Os dating fluid inclusions H-O-S-Pb isotopes lower urgen molybdenum deposit NE China |
| DOI | 10.3390/min13091189 |
| 英文摘要 | The Lower Urgen molybdenum deposit (44,856 t Mo @ 0.141%), situated in the northern Great Xing'an Range, is a newly discovered porphyry molybdenum deposit. Mineralization is characterized by veinlet-disseminated- and vein-type quartz-sulfide orebodies primarily occurring in the cupola of the Early Cretaceous granite porphyry stock. In this study, we present a detailed description of the ore geology, molybdenite Re-Os dating, H-O-S-Pb isotopic compositions, and fluid inclusion (FI) analyses including petrography, laser Raman, and microthermometry to precisely constrain the timing of ore formation, the origin of ore-forming fluids and materials, as well as the metal precipitation mechanism. Molybdenite Re-Os dating yielded two model ages of 141.2 +/- 1.5 and 147.7 +/- 1.7 Ma, coeval with the regional Late Jurassic-Early Cretaceous molybdenum metallogenesis. The hydrothermal process can be divided into three stages: the quartz-molybdenite(-pyrite) stage, quartz-polymetallic sulfide stage, and quartz-carbonate stage. Four types of FIs were distinguished for quartz, including two-phase liquid-rich (L-type), saline (S-type), CO2-rich (C1-type), and CO2-bearing (C2-type) FIs. Microthermometric data showed that the homogenization temperatures and salinities from the early to late stages were 240-430 degrees C, 5.0-11.9, and 30.1-50.8 wt% NaCl equiv.; 180-280 degrees C and 3.0-9.1 wt% NaCl equiv.; and 120-220 degrees C and 0.2-7.9 wt% NaCl equiv., respectively, suggesting a decreasing trend. H-O isotopic compositions indicate that the ore-forming fluids were initially of magmatic origin with the increasing incorporation of meteoric water. S-Pb isotopic compositions indicate that the ore-forming materials originated from granitic magmas, and the mineralization is genetically related to the ore-bearing granite porphyry stock in the deposit. Fluid immiscibility and fluid-rock interaction are collectively responsible for the massive deposition of molybdenite in stage 1, whereas fluid mixing and immiscibility played a critical role in the deposition of polymetallic sulfide in stage 2. |
| WOS关键词 | CU-MO DEPOSIT ; ZIRCON U-PB ; ASIAN OROGENIC BELT ; CENTRAL JILIN PROVINCE ; LA-ICP-MS ; MAGMATIC-HYDROTHERMAL FLUIDS ; MESOZOIC IGNEOUS ROCKS ; NE CHINA ; INNER-MONGOLIA ; VOLCANIC-ROCKS |
| 资助项目 | We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy ; Mining & Mineral Processing |
| 语种 | 英语 |
| WOS记录号 | WOS:001072595400001 |
| 出版者 | MDPI |
| 资助机构 | We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. ; We are grateful to three anonymous reviewers for their constructive comments, which greatly help in improving our paper. We would like to thank the managers of the Baojin Mining Group Co., Ltd. for their support of our fieldwork. |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/110802]  |
| 专题 | 地质与地球物理研究所_中国科学院矿产资源研究重点实验室 |
| 通讯作者 | Xie, Wei |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Peoples R China 3.China Railway Design Corp, Tianjin 300308, Peoples R China 4.Design & Res Co Ltd, China Water Resources Bei Fang Invest, Tianjin 300222, Peoples R China 5.Vrije Univ Amsterdam, Dept Earth Sci, Boelelaan 1105, NL-1081 HV Amsterdam, Netherlands 6.Northeastern Univ, Dept Geol, Key Lab Minist Educ Safe Min Deep Met Mines, Shenyang 110819, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Guangliang,Xie, Wei,Wen, Shouqin,et al. Ore Genesis of the Lower Urgen Porphyry Molybdenum Deposit in the Northern Great Xing'an Range, Northeast China: Constraints from Molybdenite Re-Os Dating, Fluid Inclusions, and H-O-S-Pb Isotopes[J]. MINERALS,2023,13(9):32. |
| APA | Zhang, Guangliang.,Xie, Wei.,Wen, Shouqin.,Zeng, Qingdong.,Zhou, Lingli.,...&Ma, Pengcheng.(2023).Ore Genesis of the Lower Urgen Porphyry Molybdenum Deposit in the Northern Great Xing'an Range, Northeast China: Constraints from Molybdenite Re-Os Dating, Fluid Inclusions, and H-O-S-Pb Isotopes.MINERALS,13(9),32. |
| MLA | Zhang, Guangliang,et al."Ore Genesis of the Lower Urgen Porphyry Molybdenum Deposit in the Northern Great Xing'an Range, Northeast China: Constraints from Molybdenite Re-Os Dating, Fluid Inclusions, and H-O-S-Pb Isotopes".MINERALS 13.9(2023):32. |
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来源：地质与地球物理研究所
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