On the origin of the North Pacific arcs [PDF]
, 2004 We present a new hypothesis that relates global plate tectonics to the formation of marginal basins, island arcs, spreading ridges and arc-shaped mountain belts around the North Pacific Ocean.
Fornós, Joan J. +3 more
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Miocene High-Temperature Magmatism in the Himalayan Orogen [PDF]
Goldschmidt Abstracts, 2020 Peng Gao +4 more
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Thermal Evolution of the Mid-Crust From the Himalayan Orogen [PDF]
, 2008 The Haimanta Group, at the top of the exhumed mid-crust in the western Himalaya (Sutlej valley), underwent prograde metamorphism to depths of 25 to 30 km at c. 30 Ma. Initial exhumation of the Haimanta Group was accompanied by further heating, from 610-620 °C up to 660 °C at c. 23 Ma; further exhumation (at c. 1.3 mm/yr) to a depth of c.
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Dynamic fluvial systems and gravel progradation in the Himalayan foreland [PDF]
, 2000 Although the large-scale stratigraphy of many terrestrial foreland basins is punctuated by major episodes of gravel progradation, the relationships of such facies to hinterland tectonism and climate change are often unclear. Structural reentrants provide
Brozovic, Nicholas, Burbank, Douglas W.
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Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan‐Tibetan orogen [PDF]
, 2004 Christopher Beaumont +3 more
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Active structures of the Himalayan-Tibetan orogen and their relationships to earthquake distribution, contemporary strain field, and Cenozoic volcanism [PDF]
, 2009 Michael H. Taylor, An Yin
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The Main Central thrust and the South Tibetan detachment in the Dadeldhura klippe (West Nepal): New insights for the evolution of the Himalayan metamorphic core [PDF]
, 2013 HKT-ISTP 2013 ...
Antolin, B. +3 more
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Geochemistry and provenance of the Lower Siwaliks from southwestern Kohat, western Himalayan Foreland Basin, NW Pakistan [PDF]
, 2015 Equivalent to the Lower Siwalik Group, the Late Miocene Chinji Formation in Pakistan consists of interbedded in-channel sandstone (SSt) and overbank mudstone (MSt) sequences.
Arif, M., Tahir Shah, M., Ullah, K.
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Metamorphic constraints on the thermal evolution of the central Himalayan Orogen
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1988 Recent studies that integrate conventional thermobarometry of pelitic mineral assemblages with thermodynamic modeling of garnet zoning reveal complex Tertiary P -T paths for the Greater Himalayan metamorphic sequence in the central Himalaya. Viewed in light of our current understanding of the structural evolution of the Himalaya, these data provide ...
Hodges, K. V. +2 more
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