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MPN-12 Sederholm symposium on high-grade metamorphism, crustal melting, migmatites and granites - Part 2
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A layered granite: Melt segregation during emplacement or deformation-induced melting?
Mikko Nironen, Matti Kurhila
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Chimney-like porosity waves as a mechanism for fluid expulsion at low temperature environments
Viktoriya Yarushina, Yuri Podladchikov
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Dehydration melting of UHP metamorphic rocks during the initial exhumation in the Dabie-Sulu orogenic belt
Yong-Fei Zheng, Zi-Fu Zhao, Qiong-Xia Xia
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Diatexite-granite connection: The origin of the 1.88 Ga Vaasa granite, Fennoscandian Shield
Hannu Mäkitie, Pekka Sipilä, Matti I Lehtonen, Hannu Kujala, Raimo Lahtinen, Petri Virransalo
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Diffusion-controlled melting in the granitic systems at 800-900°C and 100-200 MPa
Tadao Nishiyama, Takashi Yuguchi, Hiroshi Isobe
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Direct numerical simulation of two-phase flow
Deubelbeiss Yolanda, Kaus Boris, J.P.
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Magma hybridization within an anatectic source region: An example from the Karakoram Shear Zone
Henning Reichardt, Roberto Weinberg
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Mechanisms of crustal anatexis from a LA-ICP-MS study of partially melted metapelitic enclaves and host peraluminous dacite
Antonio Acosta-Vigil, Ian Buick, Joerg Hermann, Bernardo Cesare, Daniela Rubatto
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Microstructures in migmatites derived from leucocratic felsic plutonic rocks: Evidence for aqueous fluids causing anatexis
Edward Sawyer
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Silica and water-undersaturated partial melting progress in metapelites: Anatectic equilibria, P-T calculation and geodynamical implications
Antonio M. Álvarez-Valero, D. J. Waters, L. M. Kriegsman
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