Rôle des hétérogénéités mantelliques dans la genèse des MORB : étude expérimentale de la fusion partielle des pyroxénites et des interactions magma/roche à haute pression
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- Published
- 2010-01-01
- Cited by
- 2
- References
- 345
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:127156476
References
- Fusion partielle d'un manteau métasomatisé par un liquide adakitique : approches géochimique et expérimentale de la genèse et de l'évolution des magmas de l'arrière-arc équatorien
- Ultramafic inclusions and host alkali olivine basalts of the southern coastal plain of the Red Sea, Kingdom of Saudi Arabia
- Petrologic and microstructural constraints on focused melt transport in dunites and the rheology of the shallow mantle
- Petrology and geochemistry of composite ultramafic xenoliths in alkalic basalts and implications for magmatic processes within the mantle
- Thermometrie et origine des eclogites peralumineuses : cas des pyroxenites a grenat-corindon des beni bousera (nord du maroc)
- Generation of basaltic magma
- Mantle solidus: Experimental constraints and the effects of peridotite composition
- Library of Experimental Phase Relations (LEPR): A database and Web portal for experimental magmatic phase equilibria data
- Adiabat_1ph: A new public front‐end to the MELTS, pMELTS, and pHMELTS models
- Origin of MORB enrichment and relative trace element compatibilities along the Mid‐Atlantic Ridge between 10° and 24°N
- New experimental observations on the anhydrous solidus for peridotite KLB‐1
- Oceanic spreading rate and crustal thickness
- Abyssal tholeiites from the Oceanographer Fracture Zone
- Significance of large, refractory dunite bodies in the upper mantle of the Bay of Islands Ophiolite
- Dunite distribution in the Oman Ophiolite: Implications for melt flux through porous dunite conduits
- New insights into the origin and distribution of the DUPAL isotope anomaly in the Indian Ocean mantle from MORB of the Southwest Indian Ridge
- Compositional variations of coexisting phases with degree of melting of peridotite in the upper mantle
- Mantle heterogeneity and flow from seismic and geodynamic constraints
- Geochemical distinctions between “crustal” and mantle-derived peridotites/pyroxenites in high/ultrahigh pressure metamorphic complexes
- Primitive mantle magmas recorded as silicate melt inclusions in igneous minerals
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