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Volume 24 Issue 4
Aug 2013
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Journal of Earth Science  > 2013  >  24(4): 619-625.
Limei Tang, Hanlin Chen, Chuanwan Dong, Fengyou Chu. Geochronology, Geochemistry and Its Tectonic Significance of Chahe Granites in Hainan Island. Journal of Earth Science, 2013, 24(4): 619-625. doi: 10.1007/s12583-013-0361-y
Citation: Limei Tang, Hanlin Chen, Chuanwan Dong, Fengyou Chu. Geochronology, Geochemistry and Its Tectonic Significance of Chahe Granites in Hainan Island. Journal of Earth Science, 2013, 24(4): 619-625. doi: 10.1007/s12583-013-0361-y
shu

Geochronology, Geochemistry and Its Tectonic Significance of Chahe Granites in Hainan Island

doi: 10.1007/s12583-013-0361-y
  • 1.

    Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

  • 2.

    Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China

Funds:

the Basic Scientific Research Specific Foundation of Second Institute of Oceanography JT1104

China Postdoctoral Science Foundation 2011M500991

the State Oceanic Administration Foundation of China 2013335

More Information
  • Corresponding author: Hanlin Chen, hlchen@zju.edu.cn
  • Received Date: 13 Jan 2013
  • Accepted Date: 25 Apr 2013
  • Publish Date: 01 Aug 2013
    Abstract
  • There are very few studies on the granites formed in Late Permian in Hainan (海南) Island. Petrology, geochronology and geochemistry research on Late Permian granites in Chahe (叉河) area, Hainan Island will be reported in this article. The results show that, Chahe granites formed in 251 Ma, are riched in SiO2, alkali, Fe2O3 while depleted in MgO and CaO, with low Sr and high Yb, and have all the features consistent with A-type granite. The forming of Chahe granites may suggest that Hainan Island was already in post-orogenic setting in Late Permian.

     

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