Results 111 to 120 of about 759 (173)
Large-scale crustal growth driven by LIP magmatism during the Paleoproterozoic. [PDF]
Nat CommunSimões MS +6 more
europepmc +1 more source
Weathering-associated bacteria from the Damma glacier forefield: physiological capabilities and impact on granite dissolution. [PDF]
Appl Environ Microbiol, 2010 Frey B +7 more
europepmc +1 more source
Provenance and Tectonic Evolution of the Kongtongshan Formation Conglomerate in Southwest Ordos Basin, China. [PDF]
ACS OmegaCui L, Nan Q, Zhou W, Song L, Zhang H.
europepmc +1 more source
Magma hybridization in the Western Tatra Mts. granitoid intrusion (S-Poland, Western Carpathians). [PDF]
Mineral Petrol, 2011 Burda J, Gawęda A, Klötzli U.
europepmc +1 more source
Towards a taxonomy of geodiversity. [PDF]
Philos Trans A Math Phys Eng SciHjort J +7 more
europepmc +1 more source
Origin and age of the Eisenkappel gabbro to granite suite (Carinthia, SE Austrian Alps).
Lithos, 2011 Miller C +3 more
europepmc +1 more source
GEOCHEMICAL ASPECTS OF ATMOSPHERIC EVOLUTION [PDF]
Proc Natl Acad Sci U S A, 1965 europepmc +1 more source
Migmatite and Rapakivi Granite in the South Finland
Journal of Geography (Chigaku Zasshi), 2006 openaire +2 more sources
The origin of rapakivi texture by sub-isothermal decompression [PDF]
Precambrian Research, 1999 Abstract The rapakivi texture (plagioclase-mantled K-feldspar ovoids, rounded quartz megacrysts and euhedral plagioclase megacrysts in a more fine-grained granitic matrix) has been studied in five Proterozoic (1.64–1.55 Ga) anorogenic rapakivi granite batholiths in the Fennoscandian Shield with emphasis on mineral stability and inherited cores.
Shebanov, AD,, Eklund, O,
exaly +3 more sources