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Vicente López Sánchez-Vizcaíno

Researcher at University of Jaén

Publications -  35
Citations -  1488

Vicente López Sánchez-Vizcaíno is an academic researcher from University of Jaén. The author has contributed to research in topics: Olivine & Massif. The author has an hindex of 16, co-authored 33 publications receiving 1170 citations. Previous affiliations of Vicente López Sánchez-Vizcaíno include University of Granada & Spanish National Research Council.

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Journal ArticleDOI

Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain

Jeffrey C. Alt, +8 more
- 15 Apr 2012 - 
TL;DR: In this article, the authors use the concentrations and isotope compositions of water, carbon, and sulfur in serpentinites and their dehydration products to trace the cycling of volatiles during subduction.
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Tschermak's substitution in antigorite and consequences for phase relations and water liberation in high-grade serpentinites

José Alberto Padrón-Navarta, +8 more
- 15 Sep 2013 - 
TL;DR: A model for the incorporation of alumina in FeOMgO-Al 2 O 3 -SiO 2 -H 2 O (FMASH) serpentinites has been developed by considering ideal Tschermak (Al 2 Mg − 1 Si − 1 ) solid solution in antigorite as discussed by the authors.
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Metamorphic Record of High-pressure Dehydration of Antigorite Serpentinite to Chlorite Harzburgite in a Subduction Setting (Cerro del Almirez, Nevado–Filábride Complex, Southern Spain)

José Alberto Padrón-Navarta, +5 more
- 01 Oct 2011 - 
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An experimental investigation of antigorite dehydration in natural silica-enriched serpentinite

José Alberto Padrón-Navarta, +4 more
- 01 Jan 2010 - 
TL;DR: In this article, the authors show that antigorite is restricted to high-pressure metamorphism of silica-enriched serpentinite, which is helpful in constraining metamorphic conditions in cold subduction environments.
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Enrichment of HFSE in chlorite‐harzburgite produced by high‐pressure dehydration of antigorite‐serpentinite: Implications for subduction magmatism

Carlos J. Garrido, +6 more
- 01 Jan 2005 - 
TL;DR: In this paper, the authors provide field-based and geochemical evidence showing that high-pressure dehydration of antigorite-serpentinite produces chlorite-harzburgite relatively enriched in HFSE due to the stabilization of F-OH-Ti-clinohumite intergrowths with prograde olivine.