scholarly journals Structural relationships between Helminthoid Flysch and Briançonnais Units in the Marguareis Massif: A key for deciphering the finite strain pattern in the external southwestern Alps

2020 ◽  
Author(s):  
Edoardo Sanità ◽  
Jean Marc Lardeaux ◽  
Michele Marroni ◽  
Guido Gosso ◽  
Luca Pandolfi
Keyword(s):  
Finite Strain ◽  
Strain Pattern ◽  
Structural Relationships ◽  
Southwestern Alps

A comparison of geodetic and finite strain pattern in the Aegean, geodynamic implications

2001 ◽  
Vol 187 (1-2) ◽  
pp. 95-104 ◽  
Author(s):  
Laurent Jolivet
Keyword(s):  
Finite Strain ◽  
Strain Pattern

A comparison of mineral grain fabrics and finite strain in amphibolites from eastern Finland

1981 ◽  
Vol 18 (6) ◽  
pp. 995-1003 ◽  
Author(s):  
Denis Gapais ◽  
Jean-Pierre Brun
Keyword(s):  
Finite Strain ◽  
Strain Analysis ◽  
Simple Correlation ◽  
X Ray ◽  
Gneiss Domes ◽  
Strain Pattern ◽  
Strain Ellipsoid ◽  
Eigenvalue Method ◽  
General Strain ◽  
Eastern Finland

Fabrics in amphibolite rocks from the Kuopio area (eastern Finland) are described and compared with results of finite strain analysis. The area consists of mantled gneiss domes, which are deep-seated diapiric structures. Results concern the cover rocks of the domes. Strain ellipsoids range in shape from prolate to oblate (−0.67 ≤ v ≤ 0.52). Strain intensities vary strongly [Formula: see text].Preferred orientations of hornblende have been measured by X-ray texture goniometry and corresponding fabric ellipsoids calculated using an eigenvalue method. The same has been done for biotite where present. Fabric ellipsoids obtained for biotite are all oblate (0.04 ≤ vf ≤ 0.76). Those obtained for hornblende range from prolate to oblate (−0.60 ≤ vf ≤ 0.73). Intensities of hornblende fabric [Formula: see text] are weaker than those of biotite fabric [Formula: see text]. Local variations of results are induced by grain-scale factors, such as grain size, or original fabrics. No simple correlation is found between intensities of fabric and strain. In general, increasing strains are probably accompanied by an increase of the oblateness of biotite fabric ellipsoids. Hornblende fabrics are found to give a good approximation of the prolateness of the finite strain ellipsoid. The resulting L–S tectonite pattern is consistent with the general strain pattern and with the development of domal structures in the Kuopio area.

Finite strain pattern in Andriamena unit (north-central Madagascar): evidence for late Neoproterozoic–Cambrian thrusting during continental convergence

2003 ◽  
Vol 123 (2-4) ◽  
pp. 135-157 ◽  
Author(s):  
Philippe Goncalves ◽  
Christian Nicollet ◽  
Jean-Marc Lardeaux
Keyword(s):  
Finite Strain ◽  
North Central ◽  
Strain Pattern ◽  
Late Neoproterozoic
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