Experimental melts from crustal rocks: a lithochemical constraint on granite petrogenesis
Many studies of experimental petrology have devoted to partial melting of crustal rocks. In
order to provide lithochemical constraints on granite petrogenesis, this paper presents a …
order to provide lithochemical constraints on granite petrogenesis, this paper presents a …
Multistage anatexis during tectonic evolution from oceanic subduction to continental collision: A review of the North Qaidam UHP Belt, NW China
Abstract The North Qaidam ultra-high pressure (UHP) metamorphic belt in the northern
Tibetan Plateau is considered as a typical Alpine-type UHP metamorphic belt due to the …
Tibetan Plateau is considered as a typical Alpine-type UHP metamorphic belt due to the …
[HTML][HTML] On ultrahigh temperature crustal metamorphism: Phase equilibria, trace element thermometry, bulk composition, heat sources, timescales and tectonic …
DE Kelsey, M Hand - Geoscience Frontiers, 2015 - Elsevier
Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …
Osumilite–melt interactions in ultrahigh temperature granulites: phase equilibria modelling and implications for the P–T–t evolution of the Eastern Ghats Province …
The exposed residual crust in the Eastern Ghats Province records ultrahigh temperature
(UHT) metamorphic conditions involving extensive crustal anatexis and melt loss. However …
(UHT) metamorphic conditions involving extensive crustal anatexis and melt loss. However …
Crustal melting and suprasolidus phase equilibria: From first principles to the state-of-the-art
Partial melting is the fundamental process by which juvenile crust was produced from the
mantle and subsequently reworked to become the stable, compositionally-differentiated …
mantle and subsequently reworked to become the stable, compositionally-differentiated …
Consequences of open-system melting in tectonics
Partial melting and melt drainage from deep suprasolidus crust in orogens has important
consequences for tectonics. Melt extraction along prograde segments of clockwise P–T …
consequences for tectonics. Melt extraction along prograde segments of clockwise P–T …
Mechanisms of melt extraction during lower crustal partial melting
Progressive 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 …
due to an expansion in the volume of the mineral plus melt assemblage. For a locally closed …
TTG‐adakitic‐like (Tonalitic‐Trondhjemitic) magmas resulting from partial melting of metagabbro under high‐pressure condition during continental collision in the …
The tectonic regime and melting conditions of adakitic tonalitic‐trondhjemitic leucosomes
and tonalite plutons from the North Qaidam terrane are evaluated through petrology, whole …
and tonalite plutons from the North Qaidam terrane are evaluated through petrology, whole …
Recognition of melferite–A rock formed in syn-deformational high-strain melt-transfer zones through sub-solidus rocks: A review and synthesis of microstructural …
Melt transfer and migration occurs through both supra-and sub-solidus rocks. Mechanisms
of melt transfer include dyking, mobile hydrofracturing and diffuse porous melt flow where …
of melt transfer include dyking, mobile hydrofracturing and diffuse porous melt flow where …
Subduction initiation at the Solomon back‐arc basin: Contributions from both island arc rheological strength and oceanic plateau collision
It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …