Magnetic fabric of weakly deformed clay-rich sediments in the Italian peninsula: Relationship with compressional and extensional tectonics
- 1 March 1997
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 271 (1-2), 107-122
- https://doi.org/10.1016/s0040-1951(96)00244-2
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Granite emplacement during contemporary shortening and normal faulting: structural and magnetic study of the Veiga Massif (NW Spain)Journal of Structural Geology, 1995
- Magnetic fabric and structural setting of Plio-Pleistocene clayey units in an extensional regime: the Tyrrhenian margin of central ItalyJournal of Structural Geology, 1994
- Dip analysis as a tool for estimating regional kinematics in extensional terranesJournal of Structural Geology, 1994
- Magnetic fabric as a structural indicator of the deformation path within a fold-thrust structure: a test case from the Corbières (NE Pyrenees, France)Journal of Structural Geology, 1992
- The magnetic fabric relationship between sedimentary and basement nappes in the High Tatra Mountains, N. SlovakiaJournal of Structural Geology, 1991
- Chlorite control of correlations between strain and anisotropy of magnetic susceptibilityPhysics of the Earth and Planetary Interiors, 1990
- Magnetic susceptibility of the rock matrix related to magnetic fabric studiesJournal of Structural Geology, 1987
- Development of planar and linear fabrics in Dauphinois shales and slates (French Alps) studied by magnetic anisotropy and its mineralogical controlJournal of Structural Geology, 1984
- The relationship of strain and preferred orientation of phyllosilicate grains in rocks—a reviewTectonophysics, 1983
- The origin of cleavage in the light of magnetic anisotropy investigationsPhysics of the Earth and Planetary Interiors, 1976