Richard E. Bevins
Cardiff University
68 Papers
1K Citations
Richard E. Bevins is an academic researcher from Cardiff University. The author has contributed to research in topics: Metamorphism & Geology. The author has an hindex of 23, co-authored 59 publications. Previous affiliations of Richard E. Bevins include Aberystwyth University.
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Papers
The Ordovician marginal basin of Wales
TL;DR: The lower Palaeozoic Welsh Basin was founded on immature continental crust and volcanic activity was largely influenced by NE-SW-trending faults which defined the NW and SE margins of the basin this paper, with the locus of arc volcanism sited further N, in the Lake District-Leinster Zone of the Caledonides.
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Compositional variations in mafic phyllosilicates from regional low‐grade metabasites and application of the chlorite geothermometer
TL;DR: In this article, the chlorite geothermometer was used to calculate alteration temperatures for metamorphic mafic phyllosilicates in the Los Azufres geothermal system (Mexico).
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Incipient metamorphism in the Lower Palaeozoic marginal basin of Wales
D. Robinson,Richard E. Bevins +1 more
TL;DR: A diagenctic through anchizone to epizone transition is demonstrated in pelitic rocks of the Lower Palaeozoic marginal basin of Wales by examination of variations in phyllo-silicate mineralogy, illite crystallinity and bo parameter of white micas as discussed by the authors.
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Persistent Places in the Mesolithic Landscape: an Example from the Black Mountain Uplands of South Wales.
R.N.E. Barton,P.J. Berridge,Michael Walker,Richard E. Bevins +3 more
- 01 Jan 1995
TL;DR: In this article, the authors report on new work at the upland location of Waun Fignen Felen which consists of discrete Early and later Mesolithic artefact scatters on the edge of a former lake basin.
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Low-grade metamorphism within the Welsh sector of the paratectonic Caledonides
TL;DR: Mineral assemblages within metabasites from the paratectonic Caledonides of Wales show that the grade of metamorphism was predominantly within the prehnite-pumpellyite facies, although green-schist fades occur in the more central parts of the region.
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