Get 20M+ Full-Text Papers For Less Than $1.50/day. Start a 14-Day Trial for You or Your Team.

Learn More →

Some Recognitions on the Sedimentary‐Tectonic Development of the Meso‐Cenozoie Basins in Eastern China

Some Recognitions on the Sedimentary‐Tectonic Development of the Meso‐Cenozoie Basins in Eastern... Abstract Since Jurassic, intense and repeated tectonic movements have taken place in eastern China, of which the Yanshanian movement is the most important. Thereby the development of the basins between the Jurassic and Eogene in the studied areas may by divided into two different stages, i.e. the Yanshanian subcycle (J‐K11) and the North China subcycle (K21‐E). The basement and tectonic stress field of the basins played an obvious role in controlling the sedimentary‐tectonic development of the basins, and down‐faulted basins might form under different stress states. Besides, the shearing stress also played an important part while the basins were forming in the noted areas. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Some Recognitions on the Sedimentary‐Tectonic Development of the Meso‐Cenozoie Basins in Eastern China

Acta Geologica Sinica (English Edition) , Volume 1 (4) – Dec 1, 1988

Loading next page...
 
/lp/wiley/some-recognitions-on-the-sedimentary-tectonic-development-of-the-meso-ehGoIWuvPB

References (9)

Publisher
Wiley
Copyright
© 1988 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.1988.mp1004002.x
Publisher site
See Article on Publisher Site

Abstract

Abstract Since Jurassic, intense and repeated tectonic movements have taken place in eastern China, of which the Yanshanian movement is the most important. Thereby the development of the basins between the Jurassic and Eogene in the studied areas may by divided into two different stages, i.e. the Yanshanian subcycle (J‐K11) and the North China subcycle (K21‐E). The basement and tectonic stress field of the basins played an obvious role in controlling the sedimentary‐tectonic development of the basins, and down‐faulted basins might form under different stress states. Besides, the shearing stress also played an important part while the basins were forming in the noted areas.

Journal

Acta Geologica Sinica (English Edition)Wiley

Published: Dec 1, 1988

There are no references for this article.