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Permian Fusuline Fauna from the Lower Part of the Lugu Formation in the Central Qiangtang Block and its Geological Implications期刊论文

作者: ZHANG Yichun SHI Guangrong SHEN Shuzhong YUAN Dongxun
DOI:10.1111/1755-6724.12202

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页码: 365-379
被引频次: 10
出版者: WILEY-BLACKWELL,Wiley Subscription Services, Inc
ISSN: 1000-9515,0001-5717
卷期: Volume:88    Issue:2
语言: English
摘要: A Kubergandian (Kungurian) fusuline fauna from the lower part of the Lugu Formation in the Cuozheqiangma area,central Qiangtang Block is described.This fusuline fauna belongs to the Southern Transitional Zone in palaeobiogeography,and is characterised by the presence of the distinctive bi-temperate genus Monodiexodina and many genera common in lower latitude Tethyan areas such as Parafusulina and Pseudodoliolina.The occurrence of Monodiexodina in the fauna confirms that the seamount-type carbonates of the Lugu Formation did not originate from the Palaeotethys Ocean,but rather from a branch of the Neotethys Ocean after the rifting of the Qiangtang Block from the Tethys Himalaya area in the Artinskian.
相关主题: 羌塘地块, 地质意义, 动物群, 二叠纪, 古特提斯洋, Fusuline, Permian, peri‐Gondwanan blocks, Tibet, Qiangtang Block, Peri-Gondwanan blocks, SOUTHWEST CHINA, GONDWANA-AFFINITY, BREAK-UP, BASALTS, NORTHERN TIBET, WEST YUNNAN, PALEOBIOGEOGRAPHY, GEOSCIENCES, MULTIDISCIPLINARY, CHANGNING-MENGLIAN BELT, PANJAL TRAPS, PALEOGEOGRAPHIC IMPLICATIONS, peri-Gondwanan blocks,

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