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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 |
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| 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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