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 …
Timescales of crustal melting in the Higher Himalayan Crystallines (Sikkim, Eastern Himalaya) inferred from trace element-constrained monazite and zircon …
The petrology and timing of crustal melting has been investigated in the migmatites of the
Higher Himalayan Crystalline (HHC) exposed in Sikkim, India. The metapelites underwent …
Higher Himalayan Crystalline (HHC) exposed in Sikkim, India. The metapelites underwent …
Partial melting in the Higher Himalayan Crystallines of Eastern Nepal: the effect of decompression and implications for the 'Channel Flow'model
Partial melting of deep continental crust may occur during either prograde heating or
decompression. Although the effect of temperature on crustal melting has been widely …
decompression. Although the effect of temperature on crustal melting has been widely …
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 …
Two-stage partial melting and contrasting cooling history within the Higher Himalayan Crystalline Sequence in the far-eastern Nepal Himalaya
The timing of partial melting and the pressure–temperature (P–T) paths in the High
Himalayan Crystalline Sequence (HHCS) in far-eastern Nepal has been investigated using …
Himalayan Crystalline Sequence (HHCS) in far-eastern Nepal has been investigated using …
Petrology and geochronology of the Namche Barwa Complex in the eastern Himalayan syntaxis, Tibet: constraints on the origin and evolution of the north-eastern …
The Namche Barwa Complex (NBC) in the eastern Himalayan syntaxis, south Tibet, is
generally interpreted as the north-eastern extremity of the exposed Greater Himalayan …
generally interpreted as the north-eastern extremity of the exposed Greater Himalayan …
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 …
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 …