about
Primitive layered gabbros from fast-spreading lower oceanic crust.Tectonic structure, lithology, and hydrothermal signature of the Rainbow massif (Mid-Atlantic Ridge 36°14′N)Tectonic structure, evolution, and the nature of oceanic core complexes and their detachment fault zones (13°20′N and 13°30′N, Mid Atlantic Ridge)First direct observation of coseismic slip and seafloor rupture along a submarine normal fault and implications for fault slip historyDrilling constraints on lithospheric accretion and evolution at Atlantis Massif, Mid-Atlantic Ridge 30°NFrom mantle peridotites to hybrid troctolites: Textural and chemical evolution during melt-rock interaction history (Mt. Maggiore, Corsica, France)Melt/rock reaction at oceanic peridotite/gabbro transition as revealed by trace element chemistry of olivineOrigin and emplacement of ultramafic–mafic intrusions in the Erro-Tobbio mantle peridotite (Ligurian Alps, Italy)Geochemical and petrographic evidence for magmatic impregnation in the oceanic lithosphere at Atlantis Massif, Mid-Atlantic Ridge (IODP Hole U1309D, 30°N)Migration and accumulation of ultra-depleted subduction-related melts in the Massif du Sud ophiolite (New Caledonia)Petrogenesis of highly depleted peridotites and gabbroic rocks from the Mayarí-Baracoa Ophiolitic Belt (eastern Cuba)Enrichment of HFSE in chlorite-harzburgite produced by high-pressure dehydration of antigorite-serpentinite: Implications for subduction magmatismPervasive reactive melt migration through fast-spreading lower oceanic crust (Hess Deep, equatorial Pacific Ocean)Developing community-based scientific priorities and new drilling proposals in the southern Indian and southwestern Pacific oceansBehavior of fluid-mobile elements in serpentines from abyssal to subduction environments: Examples from Cuba and Dominican RepublicSerpentinites act as sponges for fluid-mobile elements in abyssal and subduction zone environmentsIn situ characterization of serpentinites from forearc mantle wedges: Timing of serpentinization and behavior of fluid-mobile elements in subduction zonesScientific DrillingCarbonate mineralization in percolated olivine aggregates: Linking effects of crystallographic orientation and fluid flowPreface: Serpentinites from mid-oceanic ridges to subductionFormation and Evolution of Oceanic Lithosphere: New Insights on Crustal Structure and Igneous Geochemistry from ODP/IODP Sites 1256, U1309, and U1415B, Sr and Pb isotope geochemistry of high-pressure Alpine metaperidotites monitors fluid-mediated element recycling during serpentinite dehydration in subduction mélange (Cima di Gagnone, Swiss Central Alps)Petrology and Trace Element Budgets of High-pressure Peridotites Indicate Subduction Dehydration of Serpentinized Mantle (Cima di Gagnone, Central Alps, Switzerland)Phreatomagmatic eruptions on the Ontong Java Plateau: chemical and isotopic relationship to Ontong Java Plateau basaltsSubduction initiation and ophiolite crust: new insights from IODP drillingTrace element evidence for anatexis at oceanic magma chamber roofs and the role of partial melts for contamination of fresh MORBAnatexis at the roof of an oceanic magma chamber at IODP Site 1256 (equatorial Pacific): an experimental studyGeochemistry of a long in-situ section of intrusive slow-spread oceanic lithosphere: Results from IODP Site U1309 (Atlantis Massif, 30°N Mid-Atlantic-Ridge)Magmatic Response to Subduction Initiation: Part 1. Fore-arc Basalts of the Izu-Bonin Arc From IODP Expedition 352
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P50
description
researcher
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հետազոտող
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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Marguerite Godard
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P106
P31
P496
0000-0003-3097-5135