Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Samira Rebaï"'
Autor:
Arkadi Karakhanian, Samira Rebaï, Yann Rolland, Marc Sosson, Hervé Philip, Vahan Davtyan, Rafael Melkonyan, Ara Avagyan
Publikováno v:
Geological Society, London, Special Publications. 340:393-408
The stress indicators describing the recent (provided by active tectonics framework) and palaeo-stress (provided by micro-fault kinematics and volcanic cluster) patterns show the scale and temporal changes in stress states since the beginning of Arab
Autor:
Hervé Philip, Yann Rolland, Rafael Melkonyan, Marc Sosson, Vahan Davtyan, Samira Rebaï, Ara Avagyan, Arkadi Karakhanian
Publikováno v:
Geodinamica Acta
Geodinamica Acta, Taylor & Francis, 2005, 18 (6), pp.401-416. ⟨10.3166/ga.18.401-416⟩
Geodinamica Acta, 2005, 18 (6), pp.401-416. ⟨10.3166/ga.18.401-416⟩
Geodinamica Acta, Taylor & Francis, 2005, 18 (6), pp.401-416. ⟨10.3166/ga.18.401-416⟩
Geodinamica Acta, 2005, 18 (6), pp.401-416. ⟨10.3166/ga.18.401-416⟩
In the Great Caucasus, the Lesser Caucasus and Eastern Turkey, the distribution of Neogene to Quaternary volcanic cluster geometries, paleo-stress field data of the Lesser Caucasus area (Republic of Armenia) and the P axes of earthquakes focal mechan
Publikováno v:
Tectonophysics. 343:205-232
North of the Arabian plate, active tectonics is characterised by both N–S compression and E–W extension associated with strike-slip faults. The Pambak–Sevan–Sunik fault (PSSF) zone in Armenia is one of the major active structures of the regio
Publikováno v:
Geophysical Journal International. 129:330-346
Summary The rapid opening, since 10 Ma, of the Tyrrhenian Sea in a context of convergence between Eurasia and Africa remains a puzzling geodynamic problem. One of the most plausible scenarios, proposed by Malinverno & Ryan (1986) attributes extension
Publikováno v:
Geophysical Journal International. 110:106-140
SUMMARY A compilation of more than one thousand stress indicators (which include in situ stress measurements, focal mechanisms, microtectonic and other geological data) allowed us to reconstruct the modern stress field in the Mediterranean region and