The distribution of groundwater uranium in Chintamani village, Karnataka, India. [PDF]
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Etude des terroirs de Miantso-Mahabo-Ambatoumena-Ambatoumanga-Ambatoulampy et Ambohimiadana : Imerina centrale [PDF]
Lannoy, M. de, Leneuf, Bernard
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Petrographic and geochemical study of Precambrian and Paleozoic rocks in the western Anti-Atlas belt, Morocco: Facies, weathering, provenance and economic exploitation. [PDF]
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Evolução geodinâmica da Faixa Ribeira (SE do Brasil) baseada no estudo de inclusões fluídas e na modelação da fO2 [PDF]
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Configuration of Migmatite Dome Comparative Tectonics of Migmatite in the Hidaka Metamorphic Belt
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Crystallization processes in migmatites
American Mineralogist, 2001An important prerequisite for interpreting microstructures in plutonic and metamorphic rocks is understanding crystallization processes. This study uses crystal size distribution (CSD) and grain shape parameters to investigate mineral-reaction-controlled crystal growth and melt solidification in migmatites of the Bayerische Wald (Variscan Orogeny ...
Alfons Berger, Gregory Roselle
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Igneous microstructures in migmatites
Geology, 1988Clear differences between the microstructures of leucosomes and mesosomes occur in some nebulitic migmatites in the Proterozoic Arunta block, central Australia. The leucosomes show crystal faces of K-feldspar (microcline-microperthite), cordierite, andalusite, and plagio clase against quartz, indicating crystallization of a melt.
R. H. Vernon, W. J. Collins
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Melt segregation in migmatites
Journal of Geophysical Research: Solid Earth, 1995Anatectic stromatic migmatites have a symmetrical layered structure with a low ratio of thickness to length and a periodicity, features that have not been explained satisfactorily but which are related to physical processes of melt segregation. We evaluate the compaction model for segregation as it applies to migmatites and develop models for melt ...
Michael Brown +3 more
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Schlieren formation in diatexite migmatite: examples from the St Malo migmatite terrane, France
Journal of Metamorphic Geology, 2003AbstractSchlieren are trains of platy or blocky minerals, typically the ferromagnesian minerals and accessory phases, that occur in granites and melt‐rich migmatites, such as diatexites. They have been considered as: (1) unmelted residue from xenoliths or the source region; (2) mineral accumulations formed during magma flow; (3) compositional layering;
I. Milord, E. W. Sawyer
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