Himalayan leucogranites: A review of geochemical and isotopic characteristics, timing of formation, genesis, and rare metal mineralization

HW Cao, QM Pei, M Santosh, GM Li, LK Zhang… - Earth-Science …, 2022 - Elsevier
As prototypes of crust-derived remelted S-type granite, Himalayan leucogranites have
considerable relevance in crustal evolution and associated metallogeny. However, given …

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 …

[HTML][HTML] On ultrahigh temperature crustal metamorphism: Phase equilibria, trace element thermometry, bulk composition, heat sources, timescales and tectonic …

DE Kelsey, M Hand - Geoscience Frontiers, 2015 - Elsevier
Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …

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 Xiang, H Mu… - Earth and Planetary …, 2016 - Elsevier
Despite several decades of investigations, the nature and timing of the India–Asia collision
remain debated. In the western Himalaya, the leading edge of the Indian continent was …

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 …

Insight into zircon REE oxy-barometers: A lattice strain model perspective

X Zou, K Qin, X Han, G Li, NJ Evans, Z Li… - Earth and Planetary …, 2019 - Elsevier
Zircon rare earth element (REE) oxy-barometers have been widely used to calculate magma
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …

How does the mid-crust accommodate deformation in large, hot collisional orogens? A review of recent research in the Himalayan orogen

JM Cottle, KP Larson, DA Kellett - Journal of Structural Geology, 2015 - Elsevier
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 …

Pressure–temperature–time–deformation path of kyanite-bearing migmatitic paragneiss in the Kali Gandaki valley (Central Nepal): Investigation of Late Eocene–Early …

S Iaccarino, C Montomoli, R Carosi, HJ Massonne… - Lithos, 2015 - Elsevier
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 …

[HTML][HTML] What can we learn from melt inclusions in migmatites and granulites?

B Cesare, A Acosta-Vigil, O Bartoli, S Ferrero - Lithos, 2015 - Elsevier
With less than two decades of activity, research on melt inclusions (MI) in crystals from rocks
that have undergone crustal anatexis–migmatites and granulites–is a recent addition to …

Long-lived high-temperature granulite-facies metamorphism in the Eastern Himalayan orogen, south Tibet

Z Zhang, H Xiang, X Dong, H Ding, Z He - Lithos, 2015 - Elsevier
Abstract The Namche Barwa Complex exposed in the Eastern Himalayan Syntaxis, south
Tibet, underwent high-pressure (HP) and high-temperature (HT) granulite-facies …