Results 131 to 140 of about 1,461 (149)

Jolfa Micro-Block in the Late Cretaceous‒Miocene (Azarbaijan Province, NW Iran): Paleostress-Field Analysis Using Inversion Method

Geotectonics, 2022
H. Khodabakhshi, A. Saidi, M. Arian, M. Ghorashi   +3 more
openaire   +1 more source

Tectonic paleostress field and its impact on the geodynamic evolution of Central Iran, case study: the Shotori Mountain

Journal of Mountain Science, 2023
Razieh Abbaspour, Seyed Morteza Mousavi, Ahmad Rashidi, Mohammad Mahdi Khatib, Shahram Shafieibafti   +4 more
openaire   +1 more source

Evolution of paleostress fields and brittle deformation of the Tornquist Zone in Scania (Sweden) during Permo-Mesozoic and Cenozoic times

Tectonophysics, 2007
Francoise Bergerat
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  

Kinematic development and paleostress analysis of the Denizli Basin (Western Turkey): implications of spatial variation of relative paleostress magnitudes and orientations

Journal of Asian Earth Sciences, 2006
Nuretdin Kaymakci
exaly  

Comparison of methods to reconstruct paleostress regimes in the NW-Greater Caucasus fold-and-thrust belt

Comptes Rendus - Geoscience, 2012
Aline Saintot
exaly  

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  

PALEOSTRESS FIELDS OF THE ARABIAN PLATE AND KINEMATIC RECONSTRUCTIONS FROM 80 MA TO PRESENT.

1993
J M Gaulier, L Faure J, Luxey P. ; Allary A, J Angelier, F Bergerat, , De, FAURE, Jean-Luc   +6 more
openaire   +1 more source

Middle Miocene Extension at the Southwestern Corner of the Pannonian Basin: Surface data on faults and paleostress field

1999
Middle Miocene (Badenian-Sarmatian) is a period of broad extension in the Pannonian Basin system when numerous basins opened or widened to accommodate convergence in the outer East Carpathians. Most of the basins were generated along large NE-SW trending strike-slip fault zones or master normal faults and generally acquire elongated, variably deep ...
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Structural analysis of faults and shear joints and reconstruction of Cenozoi paleostress fields on the island of Pag, External Dinarides

2008
This study includes collection, analysis and interpretation of structural data on faults and shear joints observed in Late Cretaceous to Quaternary rocks exposed on the Island of Pag in the External Dinarides. Based on fault kinematic data visualization, processing and analysis it was possible to separate six distinctive fault groups. For each group we
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