塔里木盆地泥盆-石炭纪转换期层序地层学

新疆石油地质 ›› 1997, Vol. 18 ›› Issue (4): 338-347.

塔里木盆地泥盆-石炭纪转换期层序地层学

陈中强

中国科学院南京地质古生物研究所南京 210008

收稿日期:1995-08-08 出版日期:1997-12-01 发布日期:2021-01-18
作者简介:陈中强, 副研究员地层古生物

SEQUENCE STRATIGRAPHY IN DEVONIAN - CARBONIFEROUS TRANSIT PERIOD IN TARIM BASIN

Chen Zhongqiang

Nanjing Geologic Palaeontologic Institute, Academia Sirica, Nanjing 210008

Received:1995-08-08 Online:1997-12-01 Published:2021-01-18
About author:Chen Zhongqiang, Associate Professor, Stratigraphic Palaeontology

摘要/Abstract

摘要： 对塔里木盆地塔西南、巴楚、满西、和田河、塔中及塔北地区晚泥盆世晚期至早石炭世早期地层进行了层序地层分析,识别出两个层序(相当Vail 等提出的三级层序),认为这一时期塔里木盆地经历了两次较大规模的海平面升降运动。通过层序地层和生物地层研究认为,古塔里木海晚古生代发生的海侵起始于晚泥盆世法门晚期;“东河砂岩”的时代为晚泥盆世法门晚期。

关键词: 塔里木盆地, 层序地层学, 晚泥盆世, 早石炭世, 晚古生代, 海侵

Abstract: This paper makes sequence stratigraphy analysis of Upper Devonian-Lower Carboniferous in southwestern Tarim,Bachu, Manxi, Hotan river, Tazhong and Tabei areas, and two sequences (corresponding to three-order sequences presented by Vail) were identifed. It is considered that Tarim basin have undergone two lange scale sea-level fluctuation. On the basis of sequence stratigraphy and biostratigraphy analyses, it is suggested that Paleozoic transgression of Tarim basin began at the Late Famenian in Late Devonian, and the age of“ Donghe sandstone”should be at the Late Famenian in I ate Devonian.

Key words: Tarim basin, Sequence stratigraphy, Late Devonian, Early Carboniferous, Late Paleozoic, Transgression

陈中强. 塔里木盆地泥盆-石炭纪转换期层序地层学[J]. 新疆石油地质, 1997, 18(4): 338-347.

Chen Zhongqiang. SEQUENCE STRATIGRAPHY IN DEVONIAN - CARBONIFEROUS TRANSIT PERIOD IN TARIM BASIN[J]. Xinjiang Petroleum Geology, 1997, 18(4): 338-347.

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