T
Tom Argles
Researcher at Open University
Publications - 49
Citations - 2275
Tom Argles is an academic researcher from Open University. The author has contributed to research in topics: Metamorphism & Metamorphic rock. The author has an hindex of 23, co-authored 46 publications receiving 1965 citations.
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Himalayan architecture constrained by isotopic tracers from clastic sediments
Andy Richards,Tom Argles,Nigel Harris,Randy Parrish,Talat Ahmad,Fiona Darbyshire,Erich Draganits +6 more
TL;DR: In this article, the authors report the first geochemical traverse to integrate U-Pb ages and Hf data on single detrital zircons with bulk-rock Sm-Nd-Rb-Sr isotopic measurements across the breadth of the Himalayan orogen, in northwest India.
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Causes and consequences of protracted melting of the mid-crust exposed in the North Himalayan antiform
Hong-Fei Zhang,Nigel Harris,Randy Parrish,Simon P. Kelley,Li Zhang,Nick Rogers,Tom Argles,Jess King +7 more
TL;DR: In this paper, trace-element and isotopic analyses from 4 two-mica granites that intrude both core and metasedimentary mantle of the North Himalayan antiform in southern Tibet provide evidence for protracted melting of the mid-crust during convergent tectonics.
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Contribution of crustal anatexis to the tectonic evolution of Indian crust beneath southern Tibet
TL;DR: In this article, the Sakya Dome of southern Tibet has been studied and two distinct suites of anatectic granites are identified, which carry contrasting implications for the tectonic evolution of the India-Asia collision zone.
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Developing an inverted Barrovian sequence; insights from monazite petrochronology
Catherine Mottram,Clare J. Warren,Daniele Regis,Nick M.W. Roberts,Nigel Harris,Tom Argles,Randall R. Parrish +6 more
TL;DR: In this article, petrochronologic methods applied here constrain a complex temporal and thermal deformation history, and demonstrate that inverted metamorphic sequences can preserve a rich record of the duration of progressive ductile evolution of the thrust.
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Exhumation of the Ronda peridotite and its crustal envelope: constraints from thermal modelling of a P–T–time array
TL;DR: The Ronda peridotite in the Betic Cordillera of southern Spain is a relic of the sub-orogenic lithospheric mantle that was exhumed during earliest Miocene time from about 66 km depth.