Pseudomorphic lines of autochthonous granitoids
Для автохтонних ультраметаморфічних гранітоїдів показано існування в природі шести псевдоморфних рядів: лейкогранітоїдного, аляскітоїдного, кінцигітоїдного, плагіогранітоїдного, діоритоїдного й ендербітоїдного та розглянуті їх петрохімічні особливості.
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Recent Advances in the Research and Application of Protective Composites for Stone Surfaces. [PDF]
Shi Q +8 more
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Assessment of the Radioactivity, Metals Content and Mineralogy of Granodiorite from Calabria, Southern Italy: A Case Study. [PDF]
Dattola L +11 more
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Provenance and economic potential of Egyptian black sands: integrated mineralogical and geochemical insights. [PDF]
Khedr MZ +7 more
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Subaerial weathering drove stabilization of continents. [PDF]
Reimink JR, Smye AJ.
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Geochemical and remote sensing insights into the hydrothermal origin of Banded Iron Formations at the Fatira Site, Northern Egyptian Nubian Shield. [PDF]
Saber EA +4 more
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Granitic intrusions enhance strain localization and rapid mantle exhumation along an oceanic detachment fault. [PDF]
Poulaki EM +35 more
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Subcritical cracking and sealing along cleavage planes and subgrain boundaries in plagioclase from the Mado Megamullion oceanic core complex. [PDF]
Nimura K, Okudaira T, Michibayashi K.
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