Abstract
The Semri and Kaimur Series in the Son valley region have undergone two phases of deformation. The first phase structures are penetrative recumbent folds, minor puckers and kinks. The second phase structures are open folds of varying wave lengths. The deformation is a post-Kaimur event. Markundi fault seems to have existed before folding.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
