S
Stephen J. Edwards
Researcher at University College London
Publications - 39
Citations - 2105
Stephen J. Edwards is an academic researcher from University College London. The author has contributed to research in topics: Mantle (geology) & Ophiolite. The author has an hindex of 15, co-authored 38 publications receiving 1769 citations. Previous affiliations of Stephen J. Edwards include St. John's University & Manchester Metropolitan University.
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Geochemistry and tectonic significance of peridotites from the South Sandwich arc-basin system, South Atlantic
TL;DR: Petrographic and geochemical studies of peridotites from the South Sandwich forearc region provide new evidence for the evolution of the south-sandwich arc-basin system and for the nature of interactions between arc magma and oceanic lithosphere as mentioned in this paper.
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Mine tailings dams: Characteristics, failure, environmental impacts, and remediation
David Kossoff,David Kossoff,William E. Dubbin,Maria Alfredsson,Stephen J. Edwards,Mark G. Macklin,Mark G. Macklin,Karen A. Hudson-Edwards +7 more
TL;DR: In this article, a review of the characteristics, types and magnitudes, environmental impacts, and remediation of mine tailings dam failures is presented, covering the characteristics of the tailings held within these dams, what best safety practice is for these structures, and what adverse effects such accidents might have on the wider environment and how these might be mitigated.
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REE and PGE Geochemical Constraints on the Formation of Dunites in the Luobusa Ophiolite, Southern Tibet
TL;DR: In this article, a chromite-bearing Dunite dyke in the Luobusa ophiolite, Southern Tibet, lies in the Indus-Yarlung Zangbo suture zone that separates Eurasia to the north from the Indian continent to the south.
Journal Article
Harzburgites and refractory melts in the Lewis Hills Massif, Bay of Islands ophiolite complex; the base-metals and precious-metals story
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Whole-rock geochemistry of gabbros from the Southwest Indian Ridge: constraints on geochemical fractionations between the upper and lower oceanic crust and magma chamber processes at (very) slow-spreading ridges
Laurence A. Coogan,Christopher J. MacLeod,H. J. B. Dick,Stephen J. Edwards,AJ Kvassnes,James H. Natland,Paul T. Robinson,G. M. Thompson,Michael J. O'Hara +8 more
TL;DR: In this article, a suite of gabbroic samples formed at the Southwest Indian Ridge with the aim of constraining magmatic processes at ultra slow-spreading centres were collected from a not, vert, similar 700 km2 area around Atlantis Bank, adjacent to the Atlantis II Fracture Zone during cruise JR31 of the RRS James Clark Ross.