Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (2): 305-343.doi: 10.13278/j.cnki.jjuese.201702101

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Spatial & Temporal Distribution and Tectonic Settings of Magmatic-Hydrothermal Ore Deposits in the Eastern Central Asia Orogen Belt

Lü Bin, Wang Tao, Tong Ying, Zhang Lei, Yang Qidi, Zhang Jianjun   

  1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
  • Received:2016-08-02 Online:2017-03-26 Published:2017-03-26
  • Supported by:
    Supported by the National Key Basic Research Program ("973"Program) of China (2013CB429803), PhD Research Initiation Fund of Guilin University of Technology and Geological Survey Projects of China Geological Survey(DD20160102)

Abstract: The Eastern Central Asian Orogenic Belt (ECAOB) is located in the overlap region among Palo-Asian Ocean tectonic domain, Okhotsk Ocean tectonic domain, and Paleo-Pacific Ocean tectonic domain, and very rich in mineral resources. According to statistics and digital mapping of 201 available isotope ages, out of 1 200 ages, spatial-temporal distribution and tectonic settings of magmatic-hydrothermal ore deposits in the ECAOB are discussed. It's proposed that the mineralization began at Cambrian, and can be identified six distinct metallogenic stages, i.e. 510-473 Ma, 373-330 Ma, 320-253 Ma, 250-210 Ma, 210-167 Ma, 155-100 Ma. From 510 to 473 Ma (peak age at ca. 507 Ma), there developed hydrothermal vein and porphyry Fe/Cu/Au/W ore deposits which are scattered in the Beishan and the Great Xing'an-Lesser Xing'an-Zhangguangcai Ranges, and related to the subduction of Paleo-Asian Ocean and the collision of micro-continents. From the Late Devonian to the Early Carboniferous (373-330), super-large scale porphyry Cu-Au deposits formed in the Oyu Tologi of Southern Mongolia, and related to the subduction of Paleo-Asian Ocean. During the third mineralization stage(320-253 Ma), a small amount of porphyry Cu deposits and orogenic Au deposits developed in the south part of Great Xing'an Ranges. Porphyry Mo poly-metallic deposits formed at 298 Ma firstly appeared in study area, representing an important change of tectonic setting, from the subduction accretion to the collage of plates. During the Triassic (250-210 Ma, peak age at ca. 244 Ma), numerous porphyry Mo deposits were distributed in the Liaoyuan terranes and the South part of Great Xing'an Ranges, whereas some magmatic separation Cu-Ni deposits formed in Zhangguangcai Ranges,which proposed that those deposits are controlled by post-orogenic extension setting involving the closure of the Palo-Asia Ocean Triassic porphyry Cu deposits in the Erguna-South Mongolia are related to the subduction of the Okhotsk Ocean. During the period of 210-167 Ma (peak age at ca. 170 Ma), orogenic-porphyry Au deposits developed in the west to the Mongolia-Okhotsk orogenic belt, while porphyry Cu (Mo) deposits exposed in the Erguna where is located in the east to the Mongolia-Okhotsk orogenic belt. It is likely that those early Jurassic deposits were formed in the tectonic setting of the subduction of the Mongolia-Okhotsk Ocean. Conversely, the mineralization in the eastern part of study area is characterized by porphyry Mo/Cu and skarn Pb-Zn/W/Au ore deposits in the eastern Jilin-Heilongjiang, the Zhangguangcai, the Lesser Xing'an, and the Great Xing'an Ranges, which indicates the westward subduction of the Paleo-Pacific plate. During the last stage of mineralization (155-100 Ma), the mineralization in ECAOB was commonly affected by the extensional tectonic setting. Both epithermal Ag-Pb-Zn and orogenic Au deposits formed in the Erguna massif at 155-120 Ma, while porphyry Mo deposits in this period occurred in the north part of Great Xing'an Ranges. It was considered that most deposits were emplaced under the post-orogenic extensional environment after the collision of the Mongol-Okhotsk Ocean. Whereas synchronous epithermal Au-Mo deposits in the eastern Jilin-Heilongjiang and hydrothermal-skarn Sn deposits in the south part of Great Xing'an Ranges are related to the northward subduction of the Paleo-Pacific plate. Some epithermal and porphyry Au-Mo deposits distributed along the paleo-suture between the North China craton and Jia-Meng massif formed during late Early Cretaceous (120-100 Ma). It can be concluded that the Paleozoic mineralization was controlled by the Palo-Asian Ocean tectonic domain, and continued to the Late Permian (or to Early Triassic), overlapped by the Paleo-Pacific Ocean metallogenic system in the Late Triassic. While, from the Triassic, the mineralization in the Erguna-South Mongolia massif was controlled by the Okhotsk Ocean tectonic domain, and continued to early period of the Early Cretaceous.

Key words: magmatic-hydrothermal ore deposits, isotopic age, spatial and temporal distribution, Eastern Central Asian orogenic belt

CLC Number: 

  • P611.11
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[1] Zhang Zhihui,Zhang Da,Wu Ganguo,Luo Ping,Chen Xihua,Di Yongjun, Lü Liangji. Re-Os Isotopic Age of Molybdenite from the Meizikeng Molybdenite Deposit in Northern Jiangxi Province and Its Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2013, 43(6): 1851-1863.
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