Group velocity tomography of the Indo-Eurasian collision zone
نویسندگان
چکیده
منابع مشابه
moho depth and lithospheric thickness of the arabian and eurasian collision zone from potential field data
the targeted area of this research includes e anatoly, nw zagros, and caucasus. these structures are known as a complex and active area and in the early stage of continent-continent collision, which give us unique possibility to monitor such collision in real time. therefore, it is very important to study this active area to have a better knowledge about its tectonic behavior and lithospheric s...
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Geochronologic dating and compilation of existing age data suggest that Cenozoic activities in the eastern Indo^ Asian collision zone of southeast China and Indochina occurred in two episodes, each with distinctive geochemical signatures, at 42^24 Myr and 16^0 Myr. The older rocks are localized along major strike^slip faults such as the Red River fault system and erupted synchronously with tran...
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The Zagros collision zone is known as an active tectonic zone that represents the tectonic boundary between the Eurasian and Arabian plates. A popular strategy for gaining insight into the upper mantle processes is to examine the splitting of seismic shear waves and interpret them in terms of upper mantle anisotropy and deformation. Core phases SK(K)S from over 278 earthquakes (MW ≥ ...
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Mickaël Bonnin,1 Guust Nolet,1 Antonio Villaseñor,2 Josep Gallart2 and Christine Thomas3 1Géoazur, université de Nice/Sophia-Antipolis, CNRS, observatoire de la Côte d’Azur, 250 rue A. Einstein, F-06560 Valbonne, France. E-mail: [email protected] 2Institute of Earth Sciences ‘Jaume Almera’, CSIC, Carrer de Lluı́s Solé i Sabaris, E-08028 Barcelona, Spain 3Westfälische Wilhelms Universität,...
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ژورنال
عنوان ژورنال: Journal of Geophysical Research
سال: 2010
ISSN: 0148-0227
DOI: 10.1029/2009jb007021