Results 171 to 180 of about 8,082 (216)

The distribution of groundwater uranium in Chintamani village, Karnataka, India. [PDF]

open access: yesF1000Res
Rampur S   +11 more
europepmc   +1 more source

Petrographic and geochemical study of Precambrian and Paleozoic rocks in the western Anti-Atlas belt, Morocco: Facies, weathering, provenance and economic exploitation. [PDF]

open access: yesHeliyon
Sebbab MM   +10 more
europepmc   +1 more source

The potential for glacial flour to impact soil fertility, crop yield and nutrition in mountain regions. [PDF]

open access: yesiScience
Tingey S   +14 more
europepmc   +1 more source

Evolução geodinâmica da Faixa Ribeira (SE do Brasil) baseada no estudo de inclusões fluídas e na modelação da fO2 [PDF]

open access: yes, 2007
Bento dos Santos, Telmo   +7 more
core  

Configuration of Migmatite Dome Comparative Tectonics of Migmatite in the Hidaka Metamorphic Belt

open access: yesConfiguration of Migmatite Dome Comparative Tectonics of Migmatite in the Hidaka Metamorphic Belt
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Crystallization processes in migmatites

American Mineralogist, 2001
An 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
openaire   +1 more source

Igneous microstructures in migmatites

Geology, 1988
Clear 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
openaire   +1 more source

Melt segregation in migmatites

Journal of Geophysical Research: Solid Earth, 1995
Anatectic 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
openaire   +1 more source

Schlieren formation in diatexite migmatite: examples from the St Malo migmatite terrane, France

Journal of Metamorphic Geology, 2003
AbstractSchlieren 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
openaire   +1 more source

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