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《Journal of Stratigraphy》 2006-03
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ORDOVICIAN CONODONT ZONES AND SEDIMENTARY SEQUENCES OF THE TARIM BASIN, XINJIANG, NW CHINA

ZHAO Zong-ju~ 1)2), ZHAO Zhi-xin~ 1), and HUANG Zhi-bin~ 1)( 1) Tarim Oil Field, Petrochina, Korla, 841000;2) Hangzhou Institute of Geology, Petrochina, Hangzhou, 310023 )  
On the basis of a large number of conodont samples from outcrop sections of the Keping, Bachu, and Charchaq areas, as well as drilling cores in the Tarim Basin, Xinjiang, the Ordovician conodont zones in the central-western region and eastern region of the Tarim Basin have been established. A total of 22 conodont zones have been recognized in the central-western region of the basin. These are, in ascending order, Variabiloconus aff. bassleri Zone, Rossodus manitouensis-Cordylodus rotundatus-Chosonodina herfurthi Zone, Scolopodus quadraplicatus Zone, Glyptoconus floweri Zone, Tripodus proteus/Paltodus deltifer Zone, Glyptoconus unicostatus Zone, Serratognathus diversus/Paroistodus proteus Zone, Serratognathoides chuxianensis-Scolopodus euspinus-Erraticodon tarimensis Zone, Aurilobodus leptosomatus-Loxodus dissectus Zone, Amorphognathus variabilis Zone, Eoplacognathus suecicus Zone, Pygodus serrus Zone, Pygodus anserinus Zone, Eoplacognathus jianyeensis/Baltoniodus variabilis Zone, Eoplacognathus elongates Zone, Baltoniodus alobatus Zone, Belodina compressa/Periodon grandis Zone, Phragmodus undatus Zone, Belodina confluens Zone, Yaoxianognathus neimengguensis Zone, Yaoxianognathus yaoxianensis Zone, and Aphelognathus pyramidalis Zone. The Lower Ordovician in the eastern region of the basin was deposited in abyssal basin facies, and 5 conodont zones have been recognized. These are, in ascending order, the Cordylodus lindstromi Zone, Cordylodus angulatus Zone, Prioniodus gilberti Zone, Paroistodus proteus Zone, and Prioniodus elegans Zone. In addition, six third-order sequences have been recognized in the Ordovician successions of the Tarim Basin. The relationship between the conodont zones, lithostratigraphic divisions of major structural units, and the six third-order sedimentary sequences, is discussed.
【Fund】: 中国石油塔里木油田分公司博士后科研项目(TLM0401);; 中国石油天然气股份有限公司科技项目(20536)资助
【CateGory Index】: P534.42
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