Development of planar and linear fabrics in Dauphinois shales and slates (French Alps) studied by magnetic anisotropy and its mineralogical control
Authors:
- P. RochetteP. Rochette
- P. VialonPVP. Vialon
- 1 January 1984
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 6 (1-2) , 33-38
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- Grain-size dependence of initial susceptibility and saturation magnetization-related parameters of four natural magnetites in the PSD--MD rangeGeophysical Journal International, 1982
- Magnetic properties of sheet silicates; 2:1 layer mineralsPhysics and Chemistry of Minerals, 1982
- The 57Fe Mössbauer parameters of pyrite and marcasite with different provenancesGeochimica et Cosmochimica Acta, 1982
- Magnetic anisotropy of rocks and its application in geology and geophysicsSurveys in Geophysics, 1982
- The use of m ssbauer spectroscopy of iron in clay mineralogyPhysics and Chemistry of Minerals, 1981
- Characterization of the magnetic fabric of rocksTectonophysics, 1981
- Magnetic susceptibility anisotropy, strain, and progressive deformation in Permian sediments from the Maritime Alps (France)Earth and Planetary Science Letters, 1981
- The influence of deformation mechanisms on magnetic fabrics in weakly deformed rocksTectonophysics, 1981
- Deformation pattern in a heterogeneous material: Folded and cleaved sedimentary cover immediately overlying a crystalline basement (Oisans, French Alps)Tectonophysics, 1980
- Texture and fabric studies across the Kishorn Nappe, near Kyle of Lochalsh, Western ScotlandJournal of Structural Geology, 1979