Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Tsvetomila Mateeva"'
Autor:
Karel Schulmann, Geoffroy Mohn, Etienne Skrzypek, Benoît Petri, Philippe Robion, Tsvetomila Mateeva, Gianreto Manatschal, Othmar Müntener
Publikováno v:
Geological Society of America Bulletin
Geological Society of America Bulletin, Geological Society of America, 2018, 130 (1-2), pp.331-352. ⟨10.1130/B31693.1⟩
Geological Society of America Bulletin, Geological Society of America, 2018, 130 (1-2), pp.331-352. ⟨10.1130/B31693.1⟩
International audience; Magma transfer between lower and upper continental crust is a fundamental process linking the dominantly mafic composition of the lower crust with the more felsic composition of the upper crust. We explore the mechanisms of ma
Autor:
Tsvetomila Mateeva, G. Mohn, Benoît Petri, Gianreto Manatschal, Etienne Skrzypek, Federico Galster
Publikováno v:
International Journal of Earth Sciences
International Journal of Earth Sciences, Springer Verlag, 2017, 106 (8), pp.2873-2893. ⟨10.1007/s00531-017-1465-x⟩
International Journal of Earth Sciences, Springer Verlag, 2017, 106 (8), pp.2873-2893. ⟨10.1007/s00531-017-1465-x⟩
International audience; The end of an orogenic cycle is commonly associated with a general extensional regime, widespread magmatism and complex metamorphic overprints. The Austroalpine domain in SE Switzerland and N Italy preserves a polyphase tecton
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::92b5002370083a59e51655500e3557c1
https://hal.archives-ouvertes.fr/hal-01670449/document
https://hal.archives-ouvertes.fr/hal-01670449/document
Autor:
John Wheeler, Gianreto Manatschal, Tsvetomila Mateeva, George A. Wolff, Nick Kusznir, Suzanne Picazo
Publikováno v:
SWISS JOURNAL OF GEOSCIENCES
Swiss Journal of Geosciences
Swiss Journal of Geosciences, Springer, 2017, 110 (2), pp.457-478. ⟨10.1007/s00015-017-0266-3⟩
Swiss Journal of Geosciences
Swiss Journal of Geosciences, Springer, 2017, 110 (2), pp.457-478. ⟨10.1007/s00015-017-0266-3⟩
Evidence from ultraslow spreading mid-ocean ridges and both fossil and present-day Ocean–Continent Transitions (OCT) demonstrates that mantle serpentinization resulting from the interaction of mantle rock and water during tectonic exhumation is wid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f4846a0ef04194935d6413ccde4a1259
http://livrepository.liverpool.ac.uk/3006402/1/SJGS-D-16-00058_R2.pdf
http://livrepository.liverpool.ac.uk/3006402/1/SJGS-D-16-00058_R2.pdf