Early precambrian A-granitoids in the Aldan Shield and adjacent mobile belts: Sources and geodynamic environments.
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- Petrology, 2012, v. 20, n. 3, p. 218, doi. 10.1134/S0869591112030034
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Works matching IS 08695911 AND DT 2012 AND VI 20 AND IP 3
Results: 6
1
2
Hydrosilicate liquids in the system NaO-SiO-HO with NaF, NaCl and Ta: Evaluation of their role in ore and mineral formation at high T and P.
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- Petrology, 2012, v. 20, n. 3, p. 271, doi. 10.1134/S0869591112020063
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- Article
3
Reactive infiltration instability of a granitization front during the generation and development of granite-gneiss domes.
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- Petrology, 2012, v. 20, n. 3, p. 205, doi. 10.1134/S0869591112030046
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- Article
4
Petrogenesis of variolitic lavas of the Onega structure, Central Karelia.
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- Petrology, 2012, v. 20, n. 3, p. 255, doi. 10.1134/S0869591112030022
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- Article
5
Age and duration of the formation of the Billyakh tectonic melange zone, Anabar shield.
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- Petrology, 2012, v. 20, n. 3, p. 286, doi. 10.1134/S0869591112030058
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- Article
6
Metabasalts of the Bryanta sequence of the Stanovoi complex of the Dzhugdzhur-Stanovoi superterrane, Central Asian fold belt: Age and geodynamic environment of formation.
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- Petrology, 2012, v. 20, n. 3, p. 240, doi. 10.1134/S086959111203006X
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- Article