J
Jeremy P. Richards
Researcher at Laurentian University
Publications - 127
Citations - 9844
Jeremy P. Richards is an academic researcher from Laurentian University. The author has contributed to research in topics: Volcanic rock & Igneous rock. The author has an hindex of 42, co-authored 126 publications receiving 8311 citations. Previous affiliations of Jeremy P. Richards include National Institute for Nanotechnology & University of Leicester.
Papers
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Journal ArticleDOI
Tectono-Magmatic Precursors for Porphyry Cu-(Mo-Au) Deposit Formation
TL;DR: In this paper, the authors reviewed various contributing processes for the formation of porphyry Cu-(Mo-Au) deposits, from partial melting in the mantle wedge overlying the subducting plate, through processes of magma interaction with the lithosphere, to mechanisms for magma emplacement and volatile exsolution in the upper crust.
Journal ArticleDOI
Special Paper: Adakite-Like Rocks: Their Diverse Origins and Questionable Role in Metallogenesis
TL;DR: The case for these petrogenetic models for adakites and high Mg andesites is best made in the Archean, when higher mantle geotherms resulted in subducting slabs potentially reaching partial melting temperatures at shallow depths before dehydration rendered the slab infusible as mentioned in this paper.
Book ChapterDOI
Porphyry Deposits: Characteristics and Origin of Hypogene Features
Eric Seedorff,John H. Dilles,John M. Proffett,Marco T. Einaudi,Lukas Zurcher,William J. A. Stavast,David A. Johnson,Mark D. Barton,Jeffrey W. Hedenquist,John F. Thompson,Richard J. Goldfarb,Jeremy P. Richards +11 more
Journal ArticleDOI
Postsubduction porphyry Cu-Au and epithermal Au deposits: Products of remelting of subduction-modified lithosphere
TL;DR: Porphyry Cu ± Mo ± Au and some epithermal Au deposits are formed from hydrothermal fluids exsolved from cooling, water-rich, calc-alkaline magmas emplaced in volcanoplutonic arcs above subduction zones.
Journal ArticleDOI
Magmatic to hydrothermal metal fluxes in convergent and collided margins
TL;DR: In this article, the authors examined the source of normal arc magmas and concluded that they are predominantly derived from partial melting of the metasomatized mantle wedge, with possible minor contributions from subducted sediments.