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Volume 24 Issue 4
Aug 2013
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Journal of Earth Science  > 2013  >  24(4): 553-568.
Renyuan Li, Lianfu Mei, Guanghui Zhu, Rumin Zhao, Xiaoming Xu, Houxiang Zhao, Peng Zhang, Yipeng Yin, Yixing Ma. Late Mesozoic to Cenozoic Tectonic Events in Volcanic Arc, West Burma Block: Evidences from U-Pb Zircon Dating and Apatite Fission Ttrack Data of Granitoids. Journal of Earth Science, 2013, 24(4): 553-568. doi: 10.1007/s12583-013-0349-7
Citation: Renyuan Li, Lianfu Mei, Guanghui Zhu, Rumin Zhao, Xiaoming Xu, Houxiang Zhao, Peng Zhang, Yipeng Yin, Yixing Ma. Late Mesozoic to Cenozoic Tectonic Events in Volcanic Arc, West Burma Block: Evidences from U-Pb Zircon Dating and Apatite Fission Ttrack Data of Granitoids. Journal of Earth Science, 2013, 24(4): 553-568. doi: 10.1007/s12583-013-0349-7
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Late Mesozoic to Cenozoic Tectonic Events in Volcanic Arc, West Burma Block: Evidences from U-Pb Zircon Dating and Apatite Fission Ttrack Data of Granitoids

doi: 10.1007/s12583-013-0349-7
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan, 430074, China

  • 2.

    Research Institute of China National Offshore Oil Company Ltd., Beijing, 100027, China

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  • Corresponding author: Renyuan Li, liry@163.com
  • Received Date: 03 Nov 2012
  • Accepted Date: 24 Feb 2013
  • Publish Date: 01 Aug 2013
    Abstract
  • Genetic type of basement granite from volcanic arc in the north of West Burma Block is S-type granites, which developed in volcanic arc of convergent plate margins. The results yield a group of weighted mean 206Pb/238U ages at 102±0.81 Ma (MSWD=0.23), which show similarity to 93.7±3.4 Ma in the northern part of sampling points and 105±2 Ma in the southern part of sampling points, indicating continuous development of volcanic arc in the north of West Burma Block and subsequent granitic intrusion of late Early Cretaceous. The apatite fission track age of the samples is 22.72±3 Ma, thermal history modeling reveals that the volcanic arc in the north of West Burma Block went through two main stages in the process of uplift-cooling since Cenozoic: rapid uplifting and cooling from Late Oligocene to Early Miocene (29±1 to 20±1 Ma) and slow uplifting and cooling since Early Pliocene (4.2±1 Ma).

     

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