Deformation thermometry based on quartz c-axis fabrics and recrystallization microstructures: A review
RD Law - Journal of structural Geology, 2014 - Elsevier
For quartz-rich tectonites two types of deformation thermometer are currently commonly
employed: 1) The quartz c-axis fabric opening-angle thermometer that provides an estimate …
employed: 1) The quartz c-axis fabric opening-angle thermometer that provides an estimate …
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 …
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 …
How does the mid-crust accommodate deformation in large, hot collisional orogens? A review of recent research in the Himalayan orogen
The presence of hot, weak crust is a central component of recent hypotheses that seek to
explain the evolution of continent-continent collisions, and in particular may play an …
explain the evolution of continent-continent collisions, and in particular may play an …
[HTML][HTML] Developing an inverted Barrovian sequence; insights from monazite petrochronology
In the Himalayan region of Sikkim, the well-developed inverted metamorphic sequence of
the Main Central Thrust (MCT) zone is folded, thus exposing several transects through the …
the Main Central Thrust (MCT) zone is folded, thus exposing several transects through 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-dipping foreshear planes, occur inside the Sub …
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …
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 …
Long-lived high-temperature granulite-facies metamorphism in the Eastern Himalayan orogen, south Tibet
Abstract The Namche Barwa Complex exposed in the Eastern Himalayan Syntaxis, south
Tibet, underwent high-pressure (HP) and high-temperature (HT) granulite-facies …
Tibet, underwent high-pressure (HP) and high-temperature (HT) granulite-facies …
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 …
Deformation temperatures and flow vorticities near the base of the Greater Himalayan Series, Sutlej Valley and Shimla Klippe, NW India
We report new deformation temperature and flow vorticity data from the base of the Greater
Himalayan Series (GHS) exposed in the Sutlej Valley and Shimla Klippe of NW India. We …
Himalayan Series (GHS) exposed in the Sutlej Valley and Shimla Klippe of NW India. We …