Types, characteristics, and time-space distribution of molybdenum deposits in China
Zeng, Qingdong; Liu, Jianming; Qin, Kezhang; Fan, Hongrui; Chu, Shaoxiong; Wang, Yongbin; Zhou, Lingli
刊名INTERNATIONAL GEOLOGY REVIEW
2013-08-01
卷号55期号:11页码:1311-1358
关键词molybdenum deposit six Mo ore-forming stages major metallogenic belt China
ISSN号0020-6814
DOI10.1080/00206814.2013.774195
文献子类Article
英文摘要Molybdenum exploration activity in China has accelerated tremendously during the past decade owing to the continuous, increasing demand for Earth resources. China possesses the largest Mo reserves in the world (exceeding 19.6 Mt). The major ore deposits are of porphyry, porphyry-skarn, skarn, vein, and sedimentary types. Porphyry molybdenum deposits contain 77.5% of the Chinese Mo reserves, with lesser amounts in porphyry-skarns (13%), skarns (5.1%), and veins (4.4%). Exploitation of sedimentary-type molybdenum deposits thus far has been uneconomical. The six Mo provinces are in the Northeast China, Yanliao, Qinling-Dabie, middle-lower Yangtze River Valley, South China, and Sanjiang areas. We recognize six ore-forming periods: (1) Precambrian (>541 Ma), (2) Palaeozoic (541-250 Ma), (3) Triassic (250-200 Ma), (4) Jurassic-Early Cretaceous (190-135 Ma), (5) Cretaceous (135-90 Ma), and (6) Cenozoic (55-12 Ma). The abundance of Mo ore deposits in China reflects the occurrence of multiple periods of tectonism, involving interactions between the Siberian, North China, Yangtze, India, and Palaeo-Pacific plates. Precambrian molybdenum deposits are related to Mesoproterozoic volcanism in an extensional setting. Palaeozoic Cu-Mo deposits are related to calc-alkaline granitic plutons in an island arc or a continental margin setting. Triassic Mo deposits formed in the syn-collision-postcollision tectonic setting between the Siberian and North China plates and between the North China and Yangzi plates. Jurassic-Early Cretaceous molybdenum deposits formed along the eastern margin of Asia and are associated with the palaeo-Pacific plate-subduction tectonic setting. Cretaceous Mo deposits are related to high-K calc-alkaline granitic rocks and formed in a lithospheric thinning setting. Cenozoic molybdenum deposits formed in a collision setting between the Indian and Eurasian continents and the subsequent extensional setting.
WOS关键词PORPHYRY MO DEPOSIT ; ZIRCON U-PB ; CAMBRIAN BLACK SHALES ; RE-OS ISOTOPE ; METAMORPHIC CORE COMPLEX ; CARBONATITE VEIN-TYPE ; YANGTZE-RIVER VALLEY ; DABIE OROGENIC BELT ; CU-AU-MO ; EARTH-ELEMENT GEOCHEMISTRY
WOS研究方向Geology
语种英语
出版者TAYLOR & FRANCIS INC
WOS记录号WOS:000321608100001
资助机构Major State Basic Research Programme of China(2013 CB429804) ; Major State Basic Research Programme of China(2013 CB429804) ; National Natural Science Foundation of China(40972065) ; National Natural Science Foundation of China(40972065) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Major State Basic Research Programme of China(2013 CB429804) ; Major State Basic Research Programme of China(2013 CB429804) ; National Natural Science Foundation of China(40972065) ; National Natural Science Foundation of China(40972065) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Major State Basic Research Programme of China(2013 CB429804) ; Major State Basic Research Programme of China(2013 CB429804) ; National Natural Science Foundation of China(40972065) ; National Natural Science Foundation of China(40972065) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Major State Basic Research Programme of China(2013 CB429804) ; Major State Basic Research Programme of China(2013 CB429804) ; National Natural Science Foundation of China(40972065) ; National Natural Science Foundation of China(40972065) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931) ; Special Study of the Continuous Resources of Crisis Mine of China(20089931)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/87526]  
专题中国科学院地质与地球物理研究所
通讯作者Zeng, Qingdong
作者单位Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
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GB/T 7714
Zeng, Qingdong,Liu, Jianming,Qin, Kezhang,et al. Types, characteristics, and time-space distribution of molybdenum deposits in China[J]. INTERNATIONAL GEOLOGY REVIEW,2013,55(11):1311-1358.
APA Zeng, Qingdong.,Liu, Jianming.,Qin, Kezhang.,Fan, Hongrui.,Chu, Shaoxiong.,...&Zhou, Lingli.(2013).Types, characteristics, and time-space distribution of molybdenum deposits in China.INTERNATIONAL GEOLOGY REVIEW,55(11),1311-1358.
MLA Zeng, Qingdong,et al."Types, characteristics, and time-space distribution of molybdenum deposits in China".INTERNATIONAL GEOLOGY REVIEW 55.11(2013):1311-1358.
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