新疆巴楚岩关期牙形类化石的发现及泥盆石炭系界线

新疆石油地质 ›› 1991, Vol. 12 ›› Issue (2): 118-127.

新疆巴楚岩关期牙形类化石的发现及泥盆石炭系界线

熊剑飞

西南石油地质局0五项目工程处

收稿日期:1990-11-21 发布日期:2020-05-27

DISCOVERY OF CONODONTS OF YAN GUAN PERIOD AND BOUNDARY BETWEEN DEVONIAN AND CARBONIFEROUS IN BACHU,XINJIANG

Xiong Jianfei

Division of Project No.05,South—west Petroleum Geoiogy Bureau

Received:1990-11-21 Published:2020-05-27

摘要/Abstract

摘要： 本文首次对新疆巴楚小海子岩关期牙形类7属11种进行了研究,分析和论证其生物地层意义,提出泥盆—石炭系界线划在Siphonodella出现稍低位置(巴楚组中段底),并确认原卡拉沙依组亦应为岩关期地层,从而述及岩关阶内部事件在塔北的新发现——巴楚运动。

关键词: 岩关期, 牙形类, 动物群, 新疆巴楚

Abstract: This paper studies conodonts (7 genera with 11 species),analysing and discussing its biostratigraphic significance in Yan Guan period at Xiaohaizi,BaChu of XinJiang. The Devonian-Carboniferous boundary is drawn at the position slightly lower than that where iphonodella occurs (the base of middle member of BaChu formation ).It is aslo determined that the original Kalasay formation is actually Yan Guan period deposite, BaChu movement diseribed as a new discovery of interior events of Yan Guan stage in TaBei.

Key words: Yan Guan period, conodonts, animal group, BaChu of XinJiang

熊剑飞. 新疆巴楚岩关期牙形类化石的发现及泥盆石炭系界线[J]. 新疆石油地质, 1991, 12(2): 118-127.

Xiong Jianfei. DISCOVERY OF CONODONTS OF YAN GUAN PERIOD AND BOUNDARY BETWEEN DEVONIAN AND CARBONIFEROUS IN BACHU,XINJIANG[J]. Xinjiang Petroleum Geology, 1991, 12(2): 118-127.