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STRATI 2013 pp 767-771 | Cite as

Permo–Carboniferous Successions of the Tengchong Block, Western Yunnan, China: Status and Problems

  • Xiaochi JinEmail author
  • Hao Huang
  • Yukun Shi
  • Lipei Zhan
Conference paper
Part of the Springer Geology book series (SPRINGERGEOL)

Abstract

The Permo–Carboniferous of the Tengchong Block is composed of a clastic succession (Menghong Group) and an overlying carbonate succession (Dadongchang Formation). The contents of diamictite and pebbly mudstone, and the presence of Gondwana-affinity faunas, suggest that the Tengchong Block was a Gondwana-derived block. Similar successions have also been reported in many places across Southeast Asia and the Tibetan Plateau. Although a general framework of Permo–Carboniferous successions of the Tengchong Block has been constructed, biostratigraphic studies need to be improved in many aspects.

Keywords

Tengchong Stratigraphy Carboniferous Permian 

Notes

Acknowledgments

This study was financially supported by the National Natural Science Foundation of China (NSFC) (No. 41272043) and the Chinese Geological Survey (No. 2013-02-030-003), for which we are very grateful.

References

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Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  1. 1.Institute of GeologyChinese Academy of Geological SciencesBeijingChina
  2. 2.Department of Earth SciencesNanjing UniversityNanjingChina

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