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宁夏卫宁盆地晚泥盆世中华豆石介族(介形类)的发现
引用本文:王尚启,王成.宁夏卫宁盆地晚泥盆世中华豆石介族(介形类)的发现[J].地层学杂志,1995,19(3):204-207.
作者姓名:王尚启  王成
作者单位:中国科学院南京地质古生物研究所,宁夏回族自治区地质矿产局地质矿产勘察院
摘    要:通过对中华巨石介族的研究,指出宁夏卫宁盆地中宁组下段为法门期滨海相沉积,泥盆纪时属华南生物地理区系。根据生物群和沉积建造的相似性,并结合古地磁资料分析、推测在晚泥盆世期间,包括卫宁盆地在内的河西走廊地体可能还未完全脱离华南地块。

关 键 词:中华豆石介族  晚泥盆世  卫宁盆地  宁夏

Discovery of Late Devonian Sinoleperditiini (Ostracoda) in Zhongwei-Zhongning Basin of Ningxia
Wang Shangqi, Yu Ziye, Wang Cheng.Discovery of Late Devonian Sinoleperditiini (Ostracoda) in Zhongwei-Zhongning Basin of Ningxia[J].Journal of Stratigraphy,1995,19(3):204-207.
Authors:Wang Shangqi  Yu Ziye  Wang Cheng
Abstract:Sinoleperditiini-bearing lower member of Zhongning Formation in the Zhongwei-Zhongning Basin of Ningxia is considered to be Famennian in age and littoral deposits. During the Late Devonian, the Zhongwei-Zhongning Basin may belong to the South China Biogeographical Province because of the presence of Sinoleperditiini there and presumably the Hexi (Gansu) Corridor Terrane including Zhongwei-Zhongning Basin might not yet separated entirely from the South China Block through the analysis of biota (plants,fishes and ostracodes),sedimentary formations and paleomagnetic data from both areas.
Keywords:Sinoleperditiini  Late Devonian  Zhongwei-Zhongning Basin  Ningxia  
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