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SIMS U-Pb zircon geochronological and geochemical study of the Sn deposits in Tengchong, north of the Southeast Asian metallogenic belt: Implications for the timing of mineralization and ore genesis
Wu, Huaying1,2,3; Deng, Jun2; Wang, Qingfei2; Zhang, Lianchang3; Cui, Xiaolin2; Shu, Qihai2; Zhang, Qiwei2; Zhou, Shumin2
2019-08-01
Source PublicationORE GEOLOGY REVIEWS
ISSN0169-1368
Volume111Pages:21
AbstractThe Tengchong-Lianghe Sn polymetallic metallogenic zone is located in the northern segment of the Southeast Asian tectonic region. It is an important part of the Southeast Asian giant Sn metallogenic belt and contains two large Sn deposits: the Xiaolonghe deposit in the north and the Lailishan deposit in the central region. The Sn mineralization is closely spatiotemporally related to Mesozoic and Cenozoic granitic magmatic activity. In the Xiaolonghe and Lailishan Sn deposits, the Sn mineralization is closely related to biotite granites. The SIMS U-Pb zircon dating analysis of the host biotite granites, integrated with the LA-ICP-MS U-Pb data from cassiterite, precisely constrain the formation of mineralization at Xiaolonghe and Lailishan Sn deposits to 75-76 Ma, the Late Cretaceous, and 50-51 Ma, the Early Eocene, respectively. Major and trace element analyses show that the host granites from the Xiaolonghe and Lailishan deposits have high silicon contents and are rich in potassium, somewhat alkali and metaluminous to weakly peraluminous, and highly differentiated (DI = 91-93). The granites belong to the ilmenite series, which formed under reducing conditions. Zircon delta O-18 of 6.82-7.99 parts per thousand and 5.54-7.30 parts per thousand for the granites from Xiaolonghe and Lailishan deposits, along with the results of previous zircon Hf isotope studies and regional data, indicates that the Xiaolonghe granitic magma mainly originated from the ancient lower crust, whereas the Lailishan granitic magma is mainly dominated by a crustal source with a small contribution of mantle material. Combined with the regional geology, we propose, for the first time, the tectonically genetic model for the two episodes of Sn mineralization present in the Xiaolonghe and Lailishan deposits. During the amalgamation of the West Burma block and the Tengchong-Moulmein block in Late Cretaceous to Early Eocene, a series of high silicic, high-potassium calc-alkaline, metaluminous to weakly peraluminous and collision-related granitic magma, including the crustal source for the Xiaolonghe deposit and the crustal source plus a small amount of mantle material for the Lailishan deposit, experienced a strong differentiation during which abundant ore minerals precipitated and intruded into the country rocks along deep faults and associated fractures, resulting in the development of the Xiaolonghe and Lailishan Sn deposits.
KeywordSIMS U-Pb zircon dates Zircon O isotope Collision-related granites Sn deposits in Tengchong North of the Southeast Asian metallogenic belt
DOI10.1016/j.oregeorev.2019.102954
Funding OrganizationMajor Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China
WOS KeywordA-TYPE GRANITES ; LIANGHE TIN BELT ; TECTONIC EVOLUTION ; WESTERN YUNNAN ; FRACTIONATED GRANITES ; SANJIANG REGION ; TRACE-ELEMENT ; FRAMEWORK ; CHINA ; HF
Language英语
Funding ProjectMajor Research Project of the National Natural Science foundation of China[91855217] ; Major State Basic Research Program of the Peoples Republic of China[2015CB452606] ; Major State Basic Research Program of the Peoples Republic of China[2015CB452602]
Funding OrganizationMajor Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major Research Project of the National Natural Science foundation of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China ; Major State Basic Research Program of the Peoples Republic of China
WOS Research AreaGeology ; Mineralogy ; Mining & Mineral Processing
WOS SubjectGeology ; Mineralogy ; Mining & Mineral Processing
WOS IDWOS:000484869200058
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/93580
Collection矿产资源研究院重点实验室
Corresponding AuthorDeng, Jun
Affiliation1.China Met Geol Bur, Inst Mineral Resources Res, Beijing 100025, Peoples R China
2.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, POB 9825, Beijing 100029, Peoples R China
First Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Wu, Huaying,Deng, Jun,Wang, Qingfei,et al. SIMS U-Pb zircon geochronological and geochemical study of the Sn deposits in Tengchong, north of the Southeast Asian metallogenic belt: Implications for the timing of mineralization and ore genesis[J]. ORE GEOLOGY REVIEWS,2019,111:21.
APA Wu, Huaying.,Deng, Jun.,Wang, Qingfei.,Zhang, Lianchang.,Cui, Xiaolin.,...&Zhou, Shumin.(2019).SIMS U-Pb zircon geochronological and geochemical study of the Sn deposits in Tengchong, north of the Southeast Asian metallogenic belt: Implications for the timing of mineralization and ore genesis.ORE GEOLOGY REVIEWS,111,21.
MLA Wu, Huaying,et al."SIMS U-Pb zircon geochronological and geochemical study of the Sn deposits in Tengchong, north of the Southeast Asian metallogenic belt: Implications for the timing of mineralization and ore genesis".ORE GEOLOGY REVIEWS 111(2019):21.
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