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Conodont and ammonite biostratigraphy and age of the Lower-Middle Triassic boundary in southern part of Guizhou Province, China
Middle Triassic boundary is a disputed issue in the world. Lower Middle Triassic strata of different types are well developed in Southwest China. According to the research on conodonts in Ganheqiao Section of Wangmo County and Qingyan Section of Guiyang City, Guizhou Province, six conodont zones, co...
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Published in: | Journal of earth science (Wuhan, China) China), 2010-06, Vol.21 (Suppl 1), p.176-178 |
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container_title | Journal of earth science (Wuhan, China) |
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creator | Yao, Jianxin Ji, Zhansheng Wang, Yanbin Liu, Dunyi Wu, Guichun Wu, Zhenjie Zhang, Jianwei Wang, Liting |
description | Middle Triassic boundary is a disputed issue in the world. Lower Middle Triassic strata of different types are well developed in Southwest China. According to the research on conodonts in Ganheqiao Section of Wangmo County and Qingyan Section of Guiyang City, Guizhou Province, six conodont zones, correlative with those in other regions, can be recognized. |
doi_str_mv | 10.1007/s12583-010-0204-z |
format | article |
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subjects | Biogeosciences Boundaries Earth and Environmental Science Earth science Earth Sciences Geochemistry Geological time Geology Geotechnical Engineering & Applied Earth Sciences Stratigraphy Triassic |
title | Conodont and ammonite biostratigraphy and age of the Lower-Middle Triassic boundary in southern part of Guizhou Province, China |
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