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Geoscience ›› 2014, Vol. 28 ›› Issue (3): 472-477.

• Petrology and Study of Ore Deposits • Previous Articles     Next Articles

Discovery of Carboniferous Diorite from Moheertu in Dongwuqi Area, Inner Mongolia: Evidence from Zircon U-Pb Geochronology

YANG Jun-quan1,2, ZHANG Su-rong2, LIU Yong-shun2, CHENG Yin-hang2, TENG Xue-jian2, LI Yan-feng2, PENG Li-na2   

  1. (1School of Earth Sciences and Resources, China University of Geosciences, Beijing100083,China; 2Tianjin Institute of Geology and Mineral Resources, Tianjin300170, China)
  • Online:2014-06-12 Published:2014-06-15

Abstract:

Dongwuqi area in Inner Mongolia, which lies in Uliastai active continental margin, is a part of Central Asian orogenic belt. Numerous magmatites are exposed in this area. The intrusive rocks mainly formed in Permian and Late Mesozoic, and seldom formed in the other period according to report. Diorite was discovered in Moheertu of this area during the 1∶50,000 regional geological surveys. By LA-MC-ICP-MS U-Pb isotopic dating for 24 zircons, weighted mean age of (337.1±1.9) Ma (MSWD=1.3) was obtained from the diorite. The characteristics of these zircons accord with magmatic zircon, and the results can represent the diagenetic age of diorite. Combined with regional geology, we concluded that a tectonothermal event occurred during 337-310 Ma in Dongwuqi area.

Key words: zircon U-Pb dating, Carboniferous, diorite, Dongwuqi, Inner Mongolia, Central Asian orogenic belt

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