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Himalayan metamorphism and its tectonic implications
MJ Kohn - Annual Review of Earth and Planetary Sciences, 2014 - annualreviews.org
The Himalayan range exposes a spectacular assemblage of metamorphic rocks from the
mid-and deep crust that have fostered numerous models of how the crust responds to …
mid-and deep crust that have fostered numerous models of how the crust responds to …
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 …
[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
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 …
Early Eocene (c. 50 Ma) collision of the Indian and Asian continents: Constraints from the North Himalayan metamorphic rocks, southeastern Tibet
H Ding, Z Zhang, X Dong, Z Tian, H ** 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 …
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-dip** foreshear planes, occur inside the Sub …
sequence thrusts, usually north-to NE-dip** foreshear planes, occur inside the Sub …
The South Tibetan Detachment System: history, advances, definition and future directions
Recognition and subsequent study of the syn-convergent low-angle normal faults and shear
zones–the South Tibetan Detachment System (STDS)–that form the upper boundary of the …
zones–the South Tibetan Detachment System (STDS)–that form the upper boundary of the …
Burma Terrane collision and northward indentation in the Eastern Himalayas recorded in the Eocene‐Miocene Chindwin Basin (Myanmar)
Abstract The Burma Terrane (Myanmar) played an important role in the India‐Asia collision
and moved over 2,000 km northward on the Indian Plate during the Cenozoic, before …
and moved over 2,000 km northward on the Indian Plate during the Cenozoic, before …