Can AMS reveal deformation history of serpentinized orogenite peridotite?

Autor: Kusbach, V., Schulmann, K., Ulrich, S., Machek, M., Roxerová, Z.

Publikováno v: XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)

The orogenic peridotite body Mohelno represents an ultramafic igneous rock of asthenospheric origin located in the Moldanubian Zone (the eastern margin of the Bohemian Massif, Czech Republic), which is interpreted as a deep part of the thickened orog

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d87c66f4acd4981422ccc81e9ef229e0

Intrusion of lamprophyre dyke and related deformation effects in the host rock salt: A case study from the Loulé diapir, Portugal

Autor: Machek, M., Roxerová, Z., Závada, P., Silva, P.F., Henry, B., Dědeček, P., Petrovský, E., Marques, F.O.

Publikováno v: In Tectonophysics 26 August 2014 629:165-178

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Evidence for non-coaxiality of ferrimagnetic and paramagnetic fabrics, developed during magma flow and cooling in a thick mafic dyke, Tectonophysics, Volume 629, 26 August 2014, Pages 155-164

Autor: Silva, Pedro, Marques, Fernando, Machek, M., Henry, Bernard, Hirt, Ann, Roxerová, Z., Madureira, Pedro, Vratislav, S.

Publikováno v: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Agência para a Sociedade do Conhecimento (UMIC)-FCT-Sociedade da Informação
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A detailed analysis of fabrics of the chilled margin of a thick dolerite dyke (FoumZguid dyke, SouthernMorocco) was performed in order to better understand the development of sub-fabrics during dyke emplacement and cooling. AMS data were complemented

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::6bde7a988caa6c25140055b38baa9c10
https://hdl.handle.net/10174/13523

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