Premium
Tectonic evolution of the High Himalaya in Upper Lahul (NW Himalaya, India)
Author(s) -
Vannay JeanClaude,
Steck Albrecht
Publication year - 1995
Publication title -
tectonics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.465
H-Index - 134
eISSN - 1944-9194
pISSN - 0278-7407
DOI - 10.1029/94tc02455
Subject(s) - geology , nappe , tectonic phase , décollement , sinistral and dextral , fold (higher order function) , paleontology , seismology , shear zone , transpression , tectonics , syncline , orogeny , mechanical engineering , engineering
The Upper Lahul region in the NW Himalaya is located in the transition zone between the High Himalayan Crystalline (HHC) to the SW and the Tethyan Zone sedimentary series to the NE. The tectonic evolution of these domains during the Himalayan Orogeny is the consequence of a succession of five deformation events. An early Dl phase corresponds to synmetamorphic, NE verging folding. This deformation created the Tandi Syncline, which consists of Permian to Jurassic Tethyan metasediments cropping out in the core of a large‐scale synformal fold within the HHC paragneiss. This tectonic event is interpreted as related to a NE directed nappe stacking (Shikar Beh Nappe), probably during the late Eocene to the early Oligocène. A subsequent D2a phase caused SW verging folding in the HHC. This deformation is interpreted as contemporaneous with late Oligocene to early Miocene SW directed thrusting along the Main Central Thrust. In the Tethyan Zone, a D2b phase is marked by a decollement thrust, a system of reverse faults, and gentle folds, associated with SW directed tectonic movements. This deformation is related to an imbricate structure, characteristic of a shallow structural level, and developed in the frontal part of a nappe affecting the Tethyan Zone units of SE Zanskar (Nyimaling‐Tsarap Nappe). A later D3 phase generated the Chandra Dextral Shear Zone (CDSZ), a large‐scale, ductile, dextral strike‐slip shear zone, located in the transition zone between the HHC and the Tethyan Himalaya. The CDSZ most likely represents a part of a system of early Miocene extensional and/or dextral, strike‐slip shear zones observed at the HHC‐Tethyan Zone contact along the entire Himalaya. A final D4 phase induced large‐scale doming and NE verging back folding.