Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Balanced Structural Models of Mohand and Santaurgarh Ramp Anticlines, Himalayan foreland Fold-Thrust Belt, Dehra Dun Re-Entrant, Uttaranchal


Affiliations
1 HOEC, Vadodara, India
2 Department of Earth Sciences, Indian Institute of Technology, Roorkee - 247 667, Uttaranchal
     

   Subscribe/Renew Journal


Two anticlines, viz., Mohand and Santaurgarh, are present in the Dehra Dun re-entrant of the Himalayan foreland fold-thrust belt. We describe balanced fault-related folding models that adequately reproduce the fold geometry of these two anticlines as deduced from the surface orientation data. The Mohand anticline can be modelled as a multibend fault-bend fold related to the Main Frontal Thrust. A multi-bend fault-propagation folding model with about 47% forelimb thinning is appropriate for the Santaurgarh anticline. The Santaurgarh anticline is related to a blind thrust with anticlinal breakthrough structure (Santaurgarh thrust). Uniformly tapering layers are required in both the models. We also present balanced and restored cross sections across the foreland belt and calculate a shortening of 6.4 km or 17.2% within the Tertiary sedimentary belt.

Keywords

Mohand Anticline, Santaurgarh Anticline, Balanced Structural Models, Northwestern Himalayas, Dehra Dun, Uttaranchal.
Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 220

PDF Views: 2




  • Balanced Structural Models of Mohand and Santaurgarh Ramp Anticlines, Himalayan foreland Fold-Thrust Belt, Dehra Dun Re-Entrant, Uttaranchal

Abstract Views: 220  |  PDF Views: 2

Authors

Premanand Mishra
HOEC, Vadodara, India
Dilip K. Mukhopadhyay
Department of Earth Sciences, Indian Institute of Technology, Roorkee - 247 667, Uttaranchal

Abstract


Two anticlines, viz., Mohand and Santaurgarh, are present in the Dehra Dun re-entrant of the Himalayan foreland fold-thrust belt. We describe balanced fault-related folding models that adequately reproduce the fold geometry of these two anticlines as deduced from the surface orientation data. The Mohand anticline can be modelled as a multibend fault-bend fold related to the Main Frontal Thrust. A multi-bend fault-propagation folding model with about 47% forelimb thinning is appropriate for the Santaurgarh anticline. The Santaurgarh anticline is related to a blind thrust with anticlinal breakthrough structure (Santaurgarh thrust). Uniformly tapering layers are required in both the models. We also present balanced and restored cross sections across the foreland belt and calculate a shortening of 6.4 km or 17.2% within the Tertiary sedimentary belt.

Keywords


Mohand Anticline, Santaurgarh Anticline, Balanced Structural Models, Northwestern Himalayas, Dehra Dun, Uttaranchal.