Vicente López Sánchez‐Vizcaíno

Universidad de Jaén

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Carlos J. Garrido

Instituto Andaluz de Ciencias de la Tierra

María Teresa Gómez‐Pugnaire

Universidad de Granada

José Alberto Padrón‐Navarta

Instituto Andaluz de Ciencias de la Tierra

Claudio Marchesi

Universidad de Granada

A. Jabaloy

Universidad de Granada

Károly Hidas

Instituto Geológico y Minero de España

Manuel D. Menzel

Instituto Andaluz de Ciencias de la Tierra

Casto Laborda‐López

Institut Català de Paleoecologia Humana i Evolució Social

Volkmar Trommsdorff

ETH Zurich

Nicole Dilissen

Vrije Universiteit Brussel

Cooperative Institutions

Universidad de Granada

Instituto Andaluz de Ciencias de la Tierra

Consejo Superior de Investigaciones Científicas

Centre National de la Recherche Scientifique

Géosciences Montpellier

Université de Montpellier

ETH Zurich

Universidad de Jaén

Durham University

Instituto Andaluz de Tecnología

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Tschermak's substitution in antigorite and consequences for phase relations and water liberation in high-grade serpentinites

Lithos (2013)

José Alberto Padrón‐Navarta Vicente López Sánchez‐Vizcaíno Jörg Hermann J. A. D. Connolly Carlos J. Garrido

Diopside

Greenschist

Tremolite

10.1016/j.lithos.2013.02.001

Cite

Citations (177)

High pressure breakdown of antigorite to spinifex-textured olivine and orthopyroxene, SE Spain

Contributions to Mineralogy and Petrology (1998)

Volkmar Trommsdorff Vicente López Sánchez‐Vizcaíno María Teresa Gómez‐Pugnaire Othmar Müntener

Enstatite

Diopside

Pyrope

Pyroxene

10.1007/s004100050412

Cite

Citations (177)

Carbonation of mantle peridotite by CO2-rich fluids: the formation of listvenites in the Advocate ophiolite complex (Newfoundland, Canada)

Lithos (2018)

Manuel D. Menzel Carlos J. Garrido Vicente López Sánchez‐Vizcaíno Claudio Marchesi Károly Hidas

Magnesite

Peridotite

Brucite

Ultramafic rock

10.1016/j.lithos.2018.06.001

Cite

Citations (83)

Incompatible element-rich fluids released by antigorite breakdown in deeply subducted mantle

Earth and Planetary Science Letters (2001)

Marco Scambelluri P. Bottazzi Volkmar Trommsdorff R. Vannucci Jörg Hermann

Trace element

Lithophile

Incompatible element

10.1016/s0012-821x(01)00457-5

Cite

Citations (166)

Olivine-rich veins in high-pressure serpentinites: A far-field paleo-stress snapshot during subduction

Journal of Structural Geology (2022)

A. Jabaloy Vicente López Sánchez‐Vizcaíno José Alberto Padrón‐Navarta Károly Hidas María Teresa Gómez‐Pugnaire

Field observations within the Atg-serpentinite domain of the subducted ultramafic massif from Cerro del Almirez (SE Spain) reveal the existence of two generations of abundant olivine-rich veins formed as open, mixed mode and shear fractures during prograde metamorphism. Type I veins were synchronous with the development of the serpentinite main foliation (S1) and shearing, whereas Type II veins post-date the S1 surfaces. These structural relationships indicate that, while the Atg-serpentinites underwent ductile plastic deformation at temperatures of 450°-600 °C and pressures of 0.7–1.7 GPa, they also experienced punctuated brittle behaviour events. The brittle fractures were most likely due to fluid overpressures formed by release of H2O during the brucite breakdown reaction for the case of Type I veins (2 vol % H2O) and due to a combination of minor dehydration reactions related to continuous compositional and structural changes in antigorite (0.3 vol % H2O) for Type II veins. Type II olivine-rich veins were formed by brittle failure in a well-defined paleo-stress field and were not significantly deformed after their formation. Comparison of the principal paleo-stress orientation inferred from Type II veins with those formed at peak metamorphic conditions in the ultramafic rocks at Cerro del Almirez shows a relative switch in the orientation of the maximum and minimum principal paleo-stress axes. These relative changes can be attributed to the cyclic evolution of shear stress, fluid pressure and fault-fracture permeability allowing for stress reversal.

Ultramafic rock

Massif

Differential stress

Stress field

10.1016/j.jsg.2022.104721

Cite

Citations (6)

Late Variscan magmatism in the Nevado-Filábride Complex: U-Pb geochronologic evidence for the pre-Mesozoic nature of the deepest Betic complex (SE Spain)

Lithos (2012)

María Teresa Gómez‐Pugnaire Daniela Rubatto J. M. Fernández-Soler A. Jabaloy Vicente López Sánchez‐Vizcaíno

Leucogranite

Protolith