Abstract
The marine sedimentary basin evolution was developed from Jinning movement in the Yangtze and the peripheral region. The continental basin had generated in Middle and Late Triassic. In the Late Proterozoic Early Paleozoic, the tectonic evolution of the phase development and evolution of the basin could be divided into three stages, namely Qingbaikou-Early Sinian, Late Sinian Middle Ordovician, and Late Ordovician Blog Silurian. Three important stages of evolution were Devonian-Early Carboniferous, Late Carboniferous-Early Permian, and Late Permian-Middle Triassic in Late Paleozoic-Mesozoic. Ancient southern continent of Asia had been further proliferation as the Indosinian movement in Middle and Late Triassic.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
