Results 181 to 190 of about 3,355 (205)

Late Cretaceous and Cenozoic dynamics of the Bohemian Massif inferred from the paleostress history of the Lusatian Fault Belt

Journal of Geodynamics, 2015
Miroslav Coubal, Jiri Malek, Jiří Adamovič   +2 more
exaly  

Tectonic evolution of the northern African margin in Tunisia from paleostress data and sedimentary record

Tectonophysics, 2002
samir Bouaziz, Mohamed Soussi, Hedi Zouari   +2 more
exaly  

Maximum Paleostress Orientation from Joint Shape: ABSTRACT

AAPG Bulletin, 1994
openaire   +1 more source

Brittle tectonic evolution and paleostress field reconstruction in the southwestern part of the Fennoscandian Shield, Forsmark, Sweden

Tectonics, 2011
Giulio Viola
exaly  

One step beyond: Full determination of paleostress tensors

2022
openaire   +1 more source

Finite-element modelling of Tertiary paleostress fields in the eastern part of the Tajo Basin (central Spain)

Tectonophysics, 1998
Sierd Apl Cloetingh, Gerardo de Vicente
exaly  

Paleostress regimes from brittle structures of the Karakoram–Kohistan Suture Zone and surrounding areas of NW Pakistan

Journal of Asian Earth Sciences, 2010
Stefan Heuberger, Bernard Célérier, Jean-Pierre Burg   +2 more
exaly  

Changes in paleostress and its magnitude related to seismic cycles in the Chelung‐pu Fault, Taiwan

Tectonics, 2015
Yoshitaka Hashimoto, En-Chao Yeh, Weiren Lin   +2 more
exaly  

Paleostress analysis of the Cretaceous rocks in the eastern margin of the Dead Sea transform, Jordan

Journal of African Earth Sciences, 2004
Mohammad Atallah
exaly  

PALEOSTRESS TRAJECTORIES AND POLYPHASE RIFTING IN ARC-BACKARC OF EASTERNPONTIDES

1985
In the modernconvergent plate margins geological and geophysical evidences imply thatmaximum horizontal stresses (sHmax) over the overriding plate are transmittedfrom plate boundry to the backarc  region.  This causes compressive regime in the plateboundry and extensive regime in the backarc or inner part of overriding plate.
openaire   +1 more source