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Detachment folding of partially molten crust in accretionary orogens: A new magma-enhanced vertical mass and heat transfer mechanism
- 1.0483167 - GFÚ 2018 RIV US eng J - Journal Article
Lehmann, J. - Schulmann, K. - Lexa, O. - Závada, Prokop - Štípská, P. - Hasalová, Pavlína - Belyanin, G. - Corsini, M.
Detachment folding of partially molten crust in accretionary orogens: A new magma-enhanced vertical mass and heat transfer mechanism.
Lithosphere. Roč. 9, č. 6 (2017), s. 889-909. ISSN 1941-8264. E-ISSN 1947-4253
Institutional support: RVO:67985530
Keywords : continental crust * shear-zone * gneiss domes
OECD category: Geology
Impact factor: 2.766, year: 2017 ; AIS: 1.385, rok: 2017
DOI: https://doi.org/10.1130/L670.1
Permanent Link: http://hdl.handle.net/11104/0278564File Download Size Commentary Version Access Lehmann2017Lithosphere.pdf 4 27.8 MB Publisher’s postprint open-access
Number of the records: 1