首页|Geochronology and Geochemistry of Ore-related Granitoids in the Giant Gariatong Rb Deposit,Tibet and Implications for Rb Metallogeny in China

Geochronology and Geochemistry of Ore-related Granitoids in the Giant Gariatong Rb Deposit,Tibet and Implications for Rb Metallogeny in China

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Rubidium(Rb)deposits mostly occur in the South China and Central Asia orogenic belts and are often closely associated with highly differentiated granites.This study investigates a newly-discovered giant Rb deposit at Gariatong in the Central Lhasa terrane in Tibet.Detailed field studies and logging data revealed that the Rb mineralization mainly occurs in monzogranite and is related to greisenization.LA-ICP-MS U-Pb dating of zircon yielded ages of 19.1±0.2 Ma and 19.0±0.2 Ma for greisenized monzogranite and fresh monzogranite,respectively.The monzogranites are characterized as strongly peraluminous,with high contents of SiO2,Al2O3,K2O and Na2O as well as a high differentiation index.They are enriched in light rare earth and large ion lithophile elements with significant negative Eu anomalies and depleted high field-strength elements.Petrological and geochemical features of these ore-related monzogranites suggest that they are highly fractionated S-type granites,derived from remelting of crustal materials in a post-collisional setting.The geochemistry of zircon and apatite points to a low oxygen fugacity of the ore-related monzogranite during the magma's evolution.The discovery of the Gariatong Rb deposit suggests that the Central Lhasa terrane may be an important region for rare metal mineralization.

LA-ICP-MS U-Pb datinggeochemistryRb metallogenyGariatongTibet

LIN Bin、TANG Juxing、TANG Pan、SUN Yan、QI Jing、M.SANTOSH、XIE Jinling、DENG Shilin、LI Faqiao、XIE Fuwei、ZHOU Aorigele

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MNR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China

SinoProbe Laboratory,Chinese Academy of Geological Sciences,Beijing 100094,China

The Key Laboratory of the Ministry of Education on Solid Waste Treatment and Recycling,School of Environment and Resource,Southwest University of Science and Technology,Mianyang,Sichuan 621010,China

School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China

Department of Earth Sciences,University of Adelaide,Adelaide SA-5005,Australia

Faculty of Geosciences and Environmental Engineering,Southwest Jiaotong University,Chengdu 610031,China

Regional Geological Survey Team of the Tibetan Bureau of Geology and Mineral Exploration and Development,Lhasa 851400,China

College of Earth Science and Key Laboratory of Tectonic Controlled Mineralization and Oil Reservoirs,Chengdu University of Technology,Chengdu 610059,China

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National Key Research and Development Program of ChinaNational Natural Science Foundation of ChinaNational Natural Science Foundation of ChinaBasic Research Fund of the Chinese Academy of Geological SciencesBasic Research Fund of the Chinese Academy of Geological SciencesChina Scholarship Council project and the Geological Survey project

2022YFC29050014227209342230813JKYZD202316KK2116DD20230054

2024

10.1111/1755-6724.15113

地质学报(英文版)
中国地质学会

地质学报(英文版)

CSTPCD
影响因子：1.414
ISSN：1000-9515
年,卷(期)：2024.98(1)
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