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Assessment of radioactivity and radiological hazards associated with bricks in eastern Nepal. [PDF]
Shrestha AK +3 more
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Crystallization Pathways of Iron Formations: Insights From Magnetic Properties and High-Resolution Imaging of the 2.7 Ga Carajás Formation, Brazil. [PDF]
Teixeira L +4 more
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The method of radiation risk assessment based on physico-geographical regionalisation: a case study of Carpathians, Poland. [PDF]
Jędrzejek F +2 more
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Configuration of Migmatite Dome Comparative Tectonics of Migmatite in the Hidaka Metamorphic Belt
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Analysis of Variance of the Composition of a Migmatite
Science, 1963To determine the variation of composition in a Front Range migmatite, an analysis of variance (nested design) was run on field measurements. The regional variation is too small to be considered significant, but the areal variation (between outcrops) is large enough to warrant comparison with some other measurable variable such as country rock ...
R F, Ward, S L, Werner
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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 ...
Berger, Alfons, Roselle, Gregory
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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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General Characteristics of Migmatites and Migmatite Terranes
1999Structures and structural relationships resulting from superimposed deformation have long been recognized by geologists, and references to this perception can be found in the literature at least as far back as the late nineteenth century (Clough, The Geology of Cowal (Gunn et al, 1897, pp. 23, 24), and here, under ‘Fold (Structure) sets’, section 5.3),
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