Results 201 to 210 of about 2,125,195 (285)

Control of slab tears and slab flat wedging on volcanism in the Alaska subduction zone. [PDF]

Sci Rep
Hu Y, Liu C, Wang Z, Zhao F.
europepmc   +1 more source

Lithium loss from pegmatites controlled by country rock temperature. [PDF]

Nat Commun
Neukampf J, Ellis BS.
europepmc   +1 more source

A slab window in the south rim of the Parece-Vela Basin. [PDF]

Sci Rep
Zhen Z, Dong X, Lintao Z.
europepmc   +1 more source

Characterisation and Stabilisation Mechanisms of Azelaic Acid Nanosuspensions: Insights from a Dual Stabiliser System. [PDF]

Pharmaceutics
Miočić S, Torić J, Juretić M, Đoković J, Randjelović D, Savić S, Ferderber K, Čižmek BC, Filipović-Grčić J.   +8 more
europepmc   +1 more source

Isotopic disequilibrium during partial melting

, 2017
Mathias Wolf, R. L. Romer
openaire   +2 more sources

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Mechanisms of melt extraction during lower crustal partial melting

Journal of Metamorphic Geology, 2020
AbstractProgressive vapour‐absent partial melting of a closed rock system increases melt pressure due to an expansion in the volume of the mineral plus melt assemblage. For a locally closed system, we quantify the melt pressure increase per increment of partial melting of a metapelite using phase equilibria modelling and combine it with Mohr–Coulomb ...
Nathan R. Daczko, Nathan R. Daczko, Catherine A. Stuart, Michael A. Etheridge, Timothy Chapman, Timothy Chapman   +5 more
openaire   +3 more sources

Multiple partial melting events in the Sulu UHP terrane: zircon U–Pb dating of granitic leucosomes within amphibolite and gneiss

Journal of Metamorphic Geology, 2012
Thin layers and lenses of granitic leucosome are widely distributed within amphibolites, paragneisses and orthogneisses of the Sulu UHP terrane. They are parallel to, or cross‐cut, foliations in the host rocks at different scales and show evidence of ...
F. Liu, P. Robinson, P. Liu
exaly   +2 more sources

Underplating and Partial Melting: Implications for Melt Generation and Extraction [PDF]

Science, 1989
The quantitative assessment of underplating and concomitant partial melting of continental crust requires the use of geologically reasonable melt fraction distributions as a function of temperature. Conductive modeling indicates that simple underplating of metapelite by basalt can yield magma bodies with melt fractions above the rheological limit of ...
openaire   +2 more sources