石油与天然气地质 ›› 1987, Vol. 8 ›› Issue (3): 315-319.doi: 10.11743/ogg19870315

• 论文 • 上一篇    下一篇

沙洲地区二叠系长兴组牙形石

丁连生, 包德宪   

  1. 地质矿产部华东石油地质局
  • 收稿日期:1986-08-19 修回日期:1987-02-02 出版日期:1987-09-25 发布日期:2012-01-16

CONODONTS OF THE UPPER PERMIAN CHANGXING FORMATION IN SHAZHOU REGION

Ding Liansheng, Bao Dexian   

  1. The East China Bureau of Petroleum Geology
  • Received:1986-08-19 Revised:1987-02-02 Online:1987-09-25 Published:2012-01-16

PDF (PC)

813

被引次数

20

摘要：

沙洲地区沙1井牙形石可划分为两个化石组合带:(1)Neogondolella subcarinata subcarinata-Neog. subcarinata elongata带,代表长兴组下部;(2)Neog. Subcarinata changxingensis-Neog. Carinata带,代表长兴组上部。

Abstract:

Abundant conodonts were found in the Changxing Formation of the upper Permian at well Sha-1 in Shazhou legion, Jiangsu Province. These conodont fossils they be divided into 2 assemblage zones: 1.Neogondolella subcarinata subcarinata- Neog. subcarinata elongata represente the lower part of the Changxing Formation, and it may be contrasted with Gondolella subcarinata named by H. Kozour in 1978,and Anchignathodus typicalis found by Clark in 1977. 2.Neogondolella subcarinata chongxingensis-Neog. carinata represent the upper part of the Chengxing Formation. The fauna has relatively particular features and local specialities. It may be the youngest stratum of the Permianin the world.