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Geoscience ›› 2017, Vol. 31 ›› Issue (04): 697-704.

• Petrology • Previous Articles     Next Articles

Formation Time of the Northeastern Jiangxi Ophiolite in the Eastern Jiangnan Orogenic Belt:Evidence from LA-ICP-MS Zircon U-Pb Dating of the Gabbro

JIANG Xingfu1,2(), PENG Songbai2,3(), KUSKY Timothy3,4, WANG Lu3,4, DENG Hao2, WANG Junpeng2   

  1. 1. School of Earth Sciences, East China University of Technology, Nanchang, Jiangxi 330013, China
    2. School of Earth Sciences, China University of Geosciences, Wuhan, Hubei 430074, China
    3. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei 430074, China
    4. Three Gorges Center for Geohazard, Ministry of Education, China University of Geosciences, Wuhan, Hubei 430074, China
  • Received:2016-09-07 Revised:2016-11-24 Online:2017-08-10 Published:2017-09-15

Abstract:

Proterozoic Ophiolite of the eastern Jiangnan orogenic belt in Northeastern Jiangxi was mainly composed of serpentinized ultramafic rock, cumulated rock, isotropic gabbro and diabase, low-temperature and high-pressure blueschist and plagiogranite. LA-ICP-MS zircon U-Pb dating for one gabbro sample from the Northeastern Jiangxi Ophiolite yielded a 207Pb/206Pb age of (992±25) Ma (MSWD=1.19), which represented the intrusion time of the gabbro. The geochronological result suggests the existence of Early Proterozoic palaeo-oceanic basin in the southeastern Yangtze block, which is younger than the late Meso-Proterozoic oceanic basin in the northern margin of the Yangtze block. Therefore, it is proposed that the Meso-Neoproterozoic crystallization basement rocks in the Yangtze craton were formed in a gradually aggregated process with characteristics of trending from northwest to southeast direction.

Key words: Jiangnan orogenic belt, Northeastern Jiangxi Ophiolite, gabbro, zircon U-Pb dating, Early Neoproterozoic

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