Normal fault growth in layered rocks with contrasting lithologies: a case study from the upper tip of the Argence Fault (Charente, France)

Author:

Constantin Joël,Saint-Bezar Bertrand

Publisher

Cellule MathDoc/CEDRAM

Subject

Marketing,Organizational Behavior and Human Resource Management,Strategy and Management,Drug Discovery,Pharmaceutical Science,Pharmacology

Reference46 articles.

1. Layer thickness and the shape of faults;Benedicto, A.;Geophys. Res. Lett.,2003

2. [Bourgueil and Moreau, 1970] Bourgueil, M.; Moreau, P. Carte Géologique de la France à 1/50000, Notice explicative de la feuille 709, BRGM, Angoulême, Orléans, 1970

3. Fault zone architecture and permeability structure;Caine, J. S.;Geology,1996

4. The three-dimensional geometry of relay zones within segmented normal faults;Camanni, G.;J. Struct. Geol.,2019

5. Influence of mechanical stratigraphy and initial stress state on the formation of two fault-propagation folds;Cardozo, N.;J. Struct. Geol.,2005

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