Xiaozhong Ding, Liu Xun, FU De-rong, Yao Jian-xin, Yong Wang, WU Shao-zu, Yi Yan
Abstract
塔里木板块西北缘石炭纪时期为一典型的被动大陆边缘,通过对本区石炭纪沉积层序及相对海平面变化研究,识别出不同类型的层序界面(SB1,SB2),并据此划分了4个二级沉积层序-超层序(Super-sequence)和8个三级沉积层序(Sequence),且在区域上或全球范围内基本上可以对比.但由于所在大地构造位置不同,其沉积背景条件差异很大,因而在不同地区可以形成不同样式、不同数量的沉积层序,海平面变化表现形式也存在差别.
OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
塔里木板块西北缘石炭纪时期为一典型的被动大陆边缘,通过对本区石炭纪沉积层序及相对海平面变化研究,识别出不同类型的层序界面(SB1,SB2),并据此划分了4个二级沉积层序-超层序(Super-sequence)和8个三级沉积层序(Sequence),且在区域上或全球范围内基本上可以对比.但由于所在大地构造位置不同,其沉积背景条件差异很大,因而在不同地区可以形成不同样式、不同数量的沉积层序,海平面变化表现形式也存在差别.
Key concepts: Geology, Carboniferous, Margin (machine learning), Paleontology, Sequence stratigraphy, Sequence (biology), Tarim basin, China