Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Susanne Grigull"'
Autor:
Dorothea Spaniel-Weise
Publikováno v:
Informationen Deutsch als Fremdsprache. 38:179-180
Autor:
Bjarne Almqvist, Roelant van der Lelij, Karin Högdahl, Rodolphe Lescoutre, Jasmin Schönenberger, Haakon Fossen, Håkan Sjöström, Christopher Juhlin, Stefan Luth, Susanne Grigull, Giulio Viola
This study presents K-Ar geochronology ages of illite from fault gouge in the crystalline basement in central-western Sweden. Samples of fault gouge were taken from two faults localizing brittle deformation along and within mafic dikes that intrude P
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::023e5feffe8460338fa4d9edb32cd61a
https://doi.org/10.31223/x5zh1n
https://doi.org/10.31223/x5zh1n
Autor:
Spaniel-Weise, Dorothea
Publikováno v:
Info DaF: Informationen Deutsch als Fremdsprache; June 2011, Vol. 38 Issue: 2-3 p179-180, 2p
Publikováno v:
International Journal of Rock Mechanics and Mining Sciences. 150:105013
Publikováno v:
GFF. 140:318-322
Postglacial faults in Sweden are generally believed to have ruptured to the surface once either during or shortly after the late Weichselian deglaciation. Stratigraphic data from multiple scarps su...
Publikováno v:
Tectonophysics. :86-101
Many tectonic HP–LT melanges exhibit block-in-matrix structures. In contrast to the pervasively deformed matrix, the blocks of various lithologies and PT-histories usually appear undeformed. If we accept that an HP–LT melange reflects persistent
Autor:
Gernold Zulauf, Henning Reichhardt, Susanne Grigull, Luise Klinger, Georg Wostal, Thomas Klein, Gotthard Kowalczyk
Publikováno v:
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften. 159:375-398
Autor:
Susanne Grigull, Timothy A. Little
Publikováno v:
Journal of Structural Geology. 30:868-875
We present a practical graphical–algebraic method that enables one to achieve the true displacement and shape of deformed geological markers in fault or shear zones as observed on arbitrarily oriented outcrop surfaces. We use as our natural example