首页> 外文会议>International Symposium on the Ordovician System;International Symposium on the Silurian System;IGCP 503 Annual Meeting >MIDDLE AND UPPER ORDOVICIAN CHITINOZOAN ASSEMBLAGES FROM THE KURUKTAG AREA,NORTHEASTERN TARIM BASIN, CHINA
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MIDDLE AND UPPER ORDOVICIAN CHITINOZOAN ASSEMBLAGES FROM THE KURUKTAG AREA,NORTHEASTERN TARIM BASIN, CHINA

机译:塔里木盆地北部库鲁克塔格地区的中上奥陶纪蛇纹石组合

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1 INTRODUCTIONOrdovician strata crop out mainly in the Kalpin area of northwestern Tarim and in the Kuruktag area of northeastern Tarim. In northeastern Tarim, Ordovician chitinozoans were known only from the Tieganlike section and borehole Weima-1, at the border of the Kuruktag Basin (Geng, unpublished data). Detailed biostratigraphical studies have been carried out in the Kuruktag area by Zhong and Hao (1990) and Zhou et al.(1992). However, so far, no chitinozoan investigations have been carried out in this area.
机译:1引言奥陶系地层主要种植在塔里木西北部的Kalpin地区和塔里木东北部的Kuruktag地区。在塔里木东北部,仅在库鲁克塔格盆地边界的铁干样断面和威玛1号井中才知道奥陶纪的甲壳动物(耿,未发表的数据)。 Zhong和Hao(1990)和Zhou等(1992)在Kuruktag地区进行了详细的生物地层学研究。但是,到目前为止,该地区尚未进行过甲壳动物的研究。

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