Himalayan leucogranites and migmatites: nature, timing and duration of anatexis
RF Weinberg - Journal of Metamorphic Geology, 2016 - Wiley Online Library
Widespread anatexis was a regional response to the evolution of the Himalayan‐Tibetan
Orogen that occurred some 30 Ma after collision between Asia and India. This paper reviews …
Orogen that occurred some 30 Ma after collision between Asia and India. This paper reviews …
20 years of geological mapping of the metamorphic core across Central and Eastern Himalayas
The largest crystalline unit representing the mid-crust in the Himalayan belt is the Greater
Himalayan Sequence (GHS) which stretches all over the 2400 km of length of the belt. The …
Himalayan Sequence (GHS) which stretches all over the 2400 km of length of the belt. The …
[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
P Kapp, PG DeCelles - American Journal of Science, 2019 - ajsonline.org
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …
geological framework and initial growth were fundamentally the result of multiple, previous …
Tectonometamorphic discontinuities within the Greater Himalayan Sequence in Western Nepal (Central Himalaya): Insights on the exhumation of crystalline rocks
The core of the Greater Himalayan Sequence in the Mugu-Karnali area (Western Nepal) is
affected by a thick shear zone with development of nearly 4 km of mylonites (Mangri shear …
affected by a thick shear zone with development of nearly 4 km of mylonites (Mangri shear …
A review on out-of-sequence deformation in the Himalaya
S Mukherjee - Special Publications, 2015 - lyellcollection.org
Out-of-sequence deformation in the Himalaya has been caused mainly by thrusting. Out-of-
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …
Pressure–temperature–time–deformation path of kyanite-bearing migmatitic paragneiss in the Kali Gandaki valley (Central Nepal): Investigation of Late Eocene–Early …
Kyanite-bearing migmatitic paragneiss of the lower Greater Himalayan Sequence (GHS) in
the Kali Gandaki transect (Central Himalaya) was investigated. In spite of the intense …
the Kali Gandaki transect (Central Himalaya) was investigated. In spite of the intense …
Late Oligocene high‐temperature shear zones in the core of the Higher Himalayan Crystallines (Lower Dolpo, western Nepal)
A high‐temperature shear zone, Toijem shear zone, with a top‐to‐the‐SW sense of shear
affects the core of the Higher Himalayan Crystallines (HHC) in western Nepal. The shear …
affects the core of the Higher Himalayan Crystallines (HHC) in western Nepal. The shear …
Tectonometamorphic discontinuities in the Greater Himalayan Sequence: a local or a regional feature?
Abstract The Greater Himalayan Sequence (GHS) is one of the major tectonic units of the
Himalaya running for more than 2400 km along-strike. It has been considered as a coherent …
Himalaya running for more than 2400 km along-strike. It has been considered as a coherent …
Holocene shortening across the Main Frontal Thrust zone in the eastern Himalaya
How plate-boundary processes control intra-continental deformation is a fundamental
question in Earth sciences. Although it is long known that the active India–Asia convergence …
question in Earth sciences. Although it is long known that the active India–Asia convergence …
Reconciling Himalayan midcrustal discontinuities: the Main Central thrust system
The occurrence of thrust-sense tectonometamorphic discontinuities within the exhumed
Himalayan metamorphic core can be explained as part of the Main Central thrust system …
Himalayan metamorphic core can be explained as part of the Main Central thrust system …