Year-end Sale % OFF 
Abstract
Syndepositional structure is mainly formed under the action of fault activity and sedimentary filling and compaction, and developed in the extensional normal fault descending wall in the tension field environment. In this paper, the concept, formation and development of syngenic structures are described, and the influence and significance of synsedimentary compaction structures on oil and gas are explored.
Published Version (
Free)
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 callMore From: Academic Journal of Environment & Earth Science
Disclaimer: 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.
