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1. Full Text Melting of Peridotite to 140 Gigapascals
by G. Fiquet and A. L. Auzende and J. Siebert and A. Corgne and H. Bureau and H. Ozawa and G. Garbarino
Science, ISSN 0036-8075, 9/2010, Volume 329, Issue 5998, pp. 1516 - 1518
Interrogating physical processes that occur within the lowermost mantle is a key to understanding Earth's evolution and present-day inner composition. Among... 
Cosmic microwave background radiation | Earth | Liquids | Melting | Peridotite | REPORTS | Liquidus | Core mantle boundary | Perovskites | Solidus | Mantle | EARTHS LOWER MANTLE | CORE-MANTLE BOUNDARY | TEMPERATURE | MULTIDISCIPLINARY SCIENCES | DEEP MANTLE | PHASE-TRANSITION | HIGH-PRESSURE EXPERIMENTS | MAGMA OCEAN | CONSTRAINTS | DIFFERENTIATION | BASE | Thermal properties | Partial melting (Geology) | Research | Natural history | Geomorphology | Igneous rock | Geophysics | Core-mantle boundary | Evolution | Diamond anvil cells | Earth Sciences | Mineralogy | Sciences of the Universe
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2. Full Text The deep carbon cycle and melting in Earth's interior
by Dasgupta, Rajdeep and Hirschmann, Marc M
Earth and Planetary Science Letters, ISSN 0012-821X, 2010, Volume 298, Issue 1, pp. 1 - 13
Carbon geochemistry of mantle-derived samples suggests that the fluxes and reservoir sizes associated with deep cycle are in the order of 10 g C/yr and 10 g C,... 
early Earth | CO 2 | subduction | carbonated silicate melt | iron carbide | carbonate | partial melting | carbonatite | deep carbon cycle | Partial melting | Carbonated silicate melt | Carbonate | Deep carbon cycle | Early Earth | Carbonatite | Iron carbide | Subduction | BEARING ECLOGITE | HIGH-PRESSURE | SUBDUCTION ZONES | CO2 | GARNET LHERZOLITE | MANTLE | GEOCHEMISTRY & GEOPHYSICS | MID-ATLANTIC RIDGE | 3 GPA | METAMORPHIC DEVOLATILIZATION | PHASE-RELATIONS | Lithosphere | Alloys | Atmosphere, Upper | Silicates | Magnesium compounds | Earth | Subduction zones (Geology) | Boron steel | Steel alloys | Carbonates | Mantle | Carbides | Carbon cycle (Biogeochemistry) | Melting | Carbonation | Carbon | Melts
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3. Full Text Melting of MORB at core–mantle boundary
by Pradhan, Gopal K and Fiquet, Guillaume and Siebert, Julien and Auzende, Anne-Line and Morard, Guillaume and Antonangeli, Daniele and Garbarino, Gaston
Earth and Planetary Science Letters, ISSN 0012-821X, 12/2015, Volume 431, pp. 247 - 255
We investigated the melting properties of natural mid-ocean ridge basalt (MORB) up to core–mantle boundary (CMB) pressures using laser-heated diamond anvil... 
experimental mineralogy | high-pressure melting | core–mantle boundary | ULVZ | partial melting | laser heating | Core-mantle boundary | High-pressure melting | Experimental mineralogy | Partial melting | Laser heating | SEISMIC EVIDENCE | HIGH-PRESSURE | DEEP MANTLE | HIGH-TEMPERATURE | X-RAY-DIFFRACTION | LOWERMOST MANTLE | core-mantle boundary | GEOCHEMISTRY & GEOPHYSICS | EARTHS LOWER MANTLE | SUBDUCTED BASALTIC CRUST | OCEANIC-CRUST | POST-PEROVSKITE PHASE | Earth | Perovskite | Analysis | Basalt | Iron oxides | Mantle | Mid-ocean ridges | Melting | Liquidus | Surface layer | Solidus | Texture | Quenching (cooling) | Melts | Sciences of the Universe
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4. Full Text Partial melting in the higher Himalayan crystallines of Eastern Nepal: The effect of decompression and implications for the 'channel flow' model
by Groppo, Chiara and Rolfo, Franco and Indares, Aphrodite
Journal of Petrology, ISSN 0022-3530, 05/2012, Volume 53, Issue 5, pp. 1057 - 1088
Partial melting of deep continental crust may occur during either prograde heating or decompression. Although the effect of temperature on crustal melting has... 
'Channel flow' model | Decompression melting | Partial melting | Higher Himalayan Crystallines | Himalaya | BOHEMIAN MASSIF | GARNET GROWTH | PHASE-EQUILIBRIA | 'channel flow' model | partial melting | PROGRADE METAMORPHISM | GEOCHEMISTRY & GEOPHYSICS | MAIN CENTRAL THRUST | INVERTED METAMORPHISM | CONTINENTAL COLLISION ZONES | HIGH-PRESSURE GRANULITES | decompression melting | P-T PATH | MINERAL ASSEMBLAGES
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5. Full Text Melting controls on the lutetium–hafnium evolution of Archaean crust
by Gardiner, Nicholas J and Johnson, Tim E and Kirkland, Christopher L and Smithies, R. Hugh
Precambrian Research, ISSN 0301-9268, 02/2018, Volume 305, pp. 479 - 488
The lutetium–hafnium (Lu–Hf) isotope record, typically measured in zircon crystals, provides a major tool for the study of crustal growth and differentiation.... 
Partial melting anatexis | Lu/Hf isotopes | Crustal evolution | TTG | Continental crust | Archaean | ZIRCON | SYSTEM | HF ISOTOPES | MINERAL EQUILIBRIA CALCULATIONS | CONTINENTAL-CRUST | GEOSCIENCES, MULTIDISCIPLINARY | LU-HF | ND ISOTOPIC COMPOSITION | GROWTH | OXYGEN ISOTOPES | CONSTRAINTS | Earth | Basalt | Crust | Mines and mineral resources | Analysis | Hafnium
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6. Full Text Partial melting of lower crust at 10–15 kbar: constraints on adakite and TTG formation
by Qian, Qing and Hermann, Jörg
Contributions to Mineralogy and Petrology, ISSN 0010-7999, 6/2013, Volume 165, Issue 6, pp. 1195 - 1224
The pressure–temperature (P–T) conditions for producing adakite/tonalite–trondhjemite–granodiorite (TTG) magmas from lower crust compositions are still open to... 
Trace element | Earth Sciences | Partial melting experiment | Geology | Mineralogy | TTG | Lower continental crust | Mineral Resources | Adakite | LOWER CONTINENTAL-CRUST | UNDERPLATED BASALTIC CRUST | HIGH-FIELD-STRENGTH | NORTH-CHINA-CRATON | THICKENED LOWER CRUST | LOW-K THOLEIITE | GEOCHEMISTRY & GEOPHYSICS | SUBDUCTING OCEANIC-CRUST | RARE-EARTH-ELEMENTS | TRONDHJEMITE-GRANODIORITE TTG | ARCHEAN TECTONOMAGMATIC PROCESSES | MINERALOGY | Toy industry | Amphiboles | Pyroxene | Temperature effects | Melting | Minerals
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7. Full Text Nb–Ta fractionation by partial melting at the titanite–rutile transition
by John, Timm and Klemd, Reiner and Klemme, Stephan and Pfänder, Jörg A and Elis Hoffmann, J and Gao, Jun
Contributions to Mineralogy and Petrology, ISSN 0010-7999, 1/2011, Volume 161, Issue 1, pp. 35 - 45
During the evolution of the Earth, distinct geochemical reservoirs with different Nb/Ta ratios have developed. Archean granitoids of the... 
Earth Sciences | Partial melting | Titanite | Geology | Rutile | Mineralogy | Crustal evolution | Eclogite | Subduction zone | Mineral Resources | Nb–Ta | Nb-Ta | FLUID-ROCK INTERACTION | HIGH-PRESSURE | EXPERIMENTAL CONSTRAINTS | NW-CHINA | SUBDUCTION ZONES | TRACE-ELEMENT MOBILIZATION | HP-LT ROCKS | GEOCHEMISTRY & GEOPHYSICS | WESTERN TIANSHAN OROGEN | EARLY CONTINENTAL-CRUST | ACCESSORY PHASE SATURATION | MINERALOGY | Earth | Reservoirs | Crust | Analysis | Geochemistry | Fractionation | Melting | Evolutionary biology
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8. Full Text Major element chemistry of ocean island basalts — Conditions of mantle melting and heterogeneity of mantle source
by Dasgupta, Rajdeep and Jackson, Matthew G and Lee, Cin-Ty A
Earth and Planetary Science Letters, ISSN 0012-821X, 2010, Volume 289, Issue 3, pp. 377 - 392
We estimate average compositions of near-primary, ‘reference’ ocean island basalts (OIBs) for 120 volcanic centers from 31 major island groups and constrain... 
ocean island basalts | mantle heterogeneity | lithosphere–asthenosphere boundary | partial melting | major element chemistry | lithosphere-asthenosphere boundary | HAWAIIAN PLUME | SOUTHERN INDIAN-OCEAN | VOLCANIC-ROCKS | EASTERN NORTH-ATLANTIC | FRENCH-POLYNESIA | GEODYNAMIC IMPLICATIONS | CAPE-VERDE-ISLANDS | GEOCHEMISTRY & GEOPHYSICS | POTASSIUM-ARGON AGES | HOT-SPOT | DEPLETED PERIDOTITE | Melting | Peridotite | Lava | Basalt | Mantle | Islands | Silicon dioxide | Melts
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9. Full Text High‐grade metamorphism and partial melting of basic and intermediate rocks
by Palin, R. M and White, R. W and Green, E. C. R and Diener, J. F. A and Powell, R and Holland, T. J. B
Journal of Metamorphic Geology, ISSN 0263-4929, 12/2016, Volume 34, Issue 9, pp. 871 - 892
Rocks of basic and intermediate bulk composition occur in orogenic terranes from all geological time periods and are thought to represent significant... 
intermediate | lower continental crust | thermocalc | basic | partial melting | CONSISTENT THERMODYNAMIC DATASET | CORDIERITE-ANTHOPHYLLITE ROCKS | LOWER CONTINENTAL-CRUST | SYSTEM K2O-FEO-MGO-AL2O3-SIO2-H2O-TIO2-FE2O3 | PHASE-EQUILIBRIA | MINERAL EQUILIBRIA CALCULATIONS | GRANULITE-FACIES METAMORPHISM | BROKEN-HILL | NW SCOTLAND | GEOLOGY | PETROLOGICAL CALCULATIONS | THERMOCALC | Metamorphism (Geology) | Basalt | Rocks, Metamorphic | Analysis | Geology | Metamorphism
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