新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2014年
2期
164-167
,共4页
刘松柏%张占武%张练练%赵文平%李海波
劉鬆柏%張佔武%張練練%趙文平%李海波
류송백%장점무%장련련%조문평%리해파
咱满铁列克提河%铁列克提组%达尔塔斯%新层型
偺滿鐵列剋提河%鐵列剋提組%達爾塔斯%新層型
찰만철렬극제하%철렬극제조%체이탑사%신층형
Zanmantielieketi River%Tielieketi group%Da’ertasl%The new stratotype bisect
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。
通過1∶5萬老裕民、塔斯提等7幅地質調查，錶明新疆裕民縣偺滿鐵列剋提河下遊右岸層型剖麵所劃分的晚泥盆世鐵列剋提組時代為早-中泥盆世。在新疆託裏縣達爾塔斯建立鐵列剋提組層型剖麵，併將該組劃分為兩箇巖性段，時代為晚泥盆世。
통과1∶5만로유민、탑사제등7폭지질조사，표명신강유민현찰만철렬극제하하유우안층형부면소화분적만니분세철렬극제조시대위조-중니분세。재신강탁리현체이탑사건립철렬극제조층형부면，병장해조화분위량개암성단，시대위만니분세。
Through 1∶50000 Laoyumin,Tasiti etc.seven geological survey,the age of Late Devonian Tielieketi forma-tion divided by stratotype bisect located in the right bank of downstream along Zanmantielieketi River in XinJiang Yu-min county,thereby the stratotype bisect of the original Tielieketi formation lose their meaning.Based on the system analy-sis,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.
