The Late Carboniferous Fusulinids in the Central Part of Northern <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:City w:st="on">Qiangtang</st1:City>, <st1:country-region w:st="on">Tibet</st1:country-region>, <st1:country-region w:st="on"><st1:place w:st="on">China</st1:place></st1:country-region> <?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p>

The Late Carboniferous Fusulinids in the Central Part of Northern Qiangtang, Tibet, China

详细信息

责任者：Wu Guichun (Institute of Geology ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Yao Jianxin
刊名：Geological Bulletin of China
出版年：2009
卷期：28(9)
关键词：晚石炭世 ; Upper Carboniferous ; 蜓目 ; Fusulinina ; 羌塘盆地 ; Qiangtang Basin
页码：p.1276-1280
图表：1 illus., 1 plate, 7 refs.
分类号：1200
issnNo：ISSN1671-2552
isbnNo：CN11-4648/P

摘要

It has been contentious whether the Late Carboniferous rocks, especially the late Late Carboniferous rocks were deposited in the central part of northern Qiangtang of Tibet mainly because of the lack of irrefutable biological fossils. An important progress was made by the 1:250 000 geological survey, through which the Walongshan Formation was established. Abundant Montiparus and Triticites are newly discovered. These findings inform that the unquestioned late Late Carboniferous rocks were deposited in the central part of the northern Qiangtang, Tibet.

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