Abstract
Sequence of strata with consistent and monotonous repetition of two or more kind alternating lithologies are quite common in geological record through the ages and are interpreted as a product of cyclic sedimentation. Cyclic depositional pattern is extensively found in fluvial deposits. Here a brief model of regional depositional stacking pattern is proposed based on the observations from regional geophysical log correlation as well as core based interpretation from Karanpura field. Subsurface facies study from this marginal Gondwana basin enhanced the understanding of stacking pattern and depositional cyclicity preserved in middle Permian Barakar Formation. Four major fining upward depositional cycles have been established regionally, each consisting of low and high accommodation system tracts at bottom and top of individual cycle respectively. Findings have been correlated with basin evolution process and major geological time events.
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.
