西准噶尔上泥盆统铁列克提组层型剖面的重新厘定  

The Redefinition of Stratotype Bisect for the Upper Devonian Tielieketi Formation in West Junggar,Xinjiang

作　　者：刘松柏 张占武 张练练 赵文平 李海波 

机构地区：[1]陕西区域地质矿产研究院,陕西咸阳712000

出　　处：《新疆地质》2014年第2期164-167,共4页Xinjiang Geology

基　　金：新疆1:5万老裕民;塔斯提等7幅区域地质调查(1212011120507)资助

摘　　要：通过1∶5万老裕民、塔斯提等7幅地质调查,表明新疆裕民县咱满铁列克提河下游右岸层型剖面所划分的晚泥盆世铁列克提组时代为早—中泥盆世。在新疆托里县达尔塔斯建立铁列克提组层型剖面,并将该组划分为两个岩性段,时代为晚泥盆世。Through 1∶50000 Laoyumin,Tasiti etc.seven geological survey,the age of Late Devonian Tielieketi formation divided by stratotype bisect located in the right bank of downstream along Zanmantielieketi River in XinJiang Yumin county,thereby the stratotype bisect of the original Tielieketi formation lose their meaning.Based on the system analysis,it has established new stratotype bisect for Tielieketi formation in Da’ertasl of the Xin Jiang Tuoli county,and Tielieketi formation is divided into two lithological section.According to the corresponding paleontological datas,the age of Tielieketi formation is approtioned for the Late Devonian.

关 键 词：咱满铁列克提河 铁列克提组 达尔塔斯 新层型 

分 类 号：P534.44[天文地球—古生物学与地层学]