Cargando…
A low-temperature ductile shear zone: The gypsum-dominated western extension of the brittle Fella-Sava Fault, Southern Alps
Based on structural and fabric analyses at variable scales we investigate the evaporitic gypsum-dominated Comeglians-Paularo shear zone in the Southern Alps (Friuli). It represents the lateral western termination of the brittle Fella-Sava Fault. Missing dehydration products of gypsum and the lack of...
Autores principales: | Bartel, Esther Maria, Neubauer, Franz, Heberer, Bianca, Genser, Johann |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Elsevier Limited
2014
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4599599/ https://www.ncbi.nlm.nih.gov/pubmed/26523080 http://dx.doi.org/10.1016/j.jsg.2014.09.016 |
Ejemplares similares
-
Displacement–length scaling of brittle faults in ductile shear
por: Grasemann, Bernhard, et al.
Publicado: (2011) -
States of paleostress north and south of the Periadriatic fault: Comparison of the Drau Range and the Friuli Southalpine wedge
por: Bartel, Esther Maria, et al.
Publicado: (2014) -
The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence
por: Petrillo, Giuseppe, et al.
Publicado: (2020) -
FELLA: an R package to enrich metabolomics data
por: Picart-Armada, Sergio, et al.
Publicado: (2018) -
Formation of orogenic gold deposits by progressive movement of a fault-fracture mesh through the upper crustal brittle-ductile transition zone
por: Tavares Nassif, Miguel, et al.
Publicado: (2022)