Amanote Research
Register
Sign In
Discover open access scientific publications
Search, annotate, share and cite publications
Publications by Alexander V Sobolev
Experimental and Petrological Studies of Melt Inclusions in Phenocrysts From Mantle-Derived Magmas: An Overview of Techniques, Advantages and Complications
Chemical Geology
Petrology
Geochemistry
Geology
Related publications
Mantle-Derived Trace Element Variability in Olivines and Their Melt Inclusions
Earth and Planetary Science Letters
Planetary Sciences
Space
Petrology
Planetary Science
Geochemistry
Geophysics
Earth
Relationships Between Campi Flegrei and Mt. Somma Volcanism: Evidence From Melt Inclusions in Clinopyroxene Phenocrysts From Volcanic Breccia Xenoliths
Mineralogy and Petrology
Petrology
Geochemistry
Geophysics
Peridotite Melting to GPa and Genesis of Primary Mantle-Derived Magmas
Melt, Crystal, and Fluid Inclusions in Olivine and Clinopyroxene Phenocrysts From the Submarine Shield Stage Hyaloclastites of Gran Canaria, Sites 953 and 956
Quantification of the CO2 Budget and H2O–CO2 Systematics in Subduction-Zone Magmas Through the Experimental Hydration of Melt Inclusions in Olivine at High H2O Pressure
Earth and Planetary Science Letters
Planetary Sciences
Space
Petrology
Planetary Science
Geochemistry
Geophysics
Earth
Evidence on Mixing of Mantle and Crustal Derived Magmas in Bodrum (Mugla) Area Volcanic Rocks, Southwest Turkey
Mineralogical Magazine
Petrology
Geochemistry
Deep Pre-Eruptive Storage of Silicic Magmas Feeding Plinian and Dome-Forming Eruptions of Central and Northern Dominica (Lesser Antilles) Inferred From Volatile Contents of Melt Inclusions
Contributions to Mineralogy and Petrology
Petrology
Geochemistry
Geophysics
Sr and Nd Isotopic Compositions of Individual Olivine-Hosted Melt Inclusions From Hawai'i and Samoa: Implications for the Origin of Isotopic Heterogeneity in Melt Inclusions From OIB Lavas
Chemical Geology
Petrology
Geochemistry
Geology
Trace Element Geochemistry of Oceanic Peridotites and Silicate Melt Inclusions : Implications for Mantle Melting and Ocean Ridge Magmagenesis