Receiver function images of the Hellenic subduction zone and comparison to microseismicity

Autor: Sodoudi, F., Brüstle, A., Meier, T., Kind, R., Friederich, W., EGELADOS working group

Publikováno v: Solid Earth, Vol 6, Iss 1, Pp 135-151 (2015)
Solid Earth

New combined P receiver functions and seismicity data obtained from the EGELADOS network employing 65 seismological stations within the Aegean constrained new information on the geometry of the Hellenic subduction zone. The dense network and large da

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6f895a4c5a89d8652ce1115f31c56310
https://www.solid-earth.net/6/135/2015/

LAB and other lithospheric discontinuities below Cratons

Autor: Sodoudi, F.

Publikováno v: Geophysical Research Abstracts Vol. 15, EGU2013-4378, 2013
General Assembly European Geosciences Union (Vienna, Austria 2013)#

Cratons are extremely stable continental areas of the Earth’s crust, which have been formed and remained largely unchanged since Precambrian. However, their formation and how they survived destruction over billions of years remains a subject of deb

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::05f88519f713e5e4469259f3896992f4
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:246999

Scandinavia: A former Tibet?

Autor: Kind, R., Sodoudi, F., Yuan, X., Shomali, H., Roberts, R., Gee, D., Eken, T., Bianchi, M., Tilmann, F., Balling, N., Jacobsen, B., Kumar, P., Geissler, W.

Publikováno v: Geochemistry Geophysics Geosystems (G3)
Kind, R, Sodoudi, F, Yuan, X, Shomali, H, Roberts, R, Gee, D, Eken, T, Bianchi, M, Tilmann, F, Balling, N, Jacobsen, B H, Kumar, P & Geissler, W H 2013, ' Scandinavia : A former Tibet? ', Geochemistry, Geophysics, Geosystems, bind 14, nr. 10, s. 4479-4487 . https://doi.org/10.1002/ggge.20251

The Himalaya and the Tibetan Plateau are uplifted by the ongoing northward underthrusting of the Indian continental lithosphere below Tibet resulting in lithospheric stacking. The layered structure of the Tibetan upper mantle is imaged by seismic met

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::10ac04a8ef7d5d9076b2f5606d70c7bd
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:248038

The lithosphere-asthenosphere boundary observed with USArray receiver functions and comparison with other regions

Autor: Kind, R., Kumar, P., Yuan, X., Mechie, J., Sodoudi, F., Heit, B.

Publikováno v: Geophysical Research Abstracts Vol. 14, EGU2012-4996, 2012
General Assembly European Geosciences Union (Vienna, Austria 2012)#

The dense deployment of seismic stations so far in the western half of the United States within the USArray project provides the opportunity to study in greater detail the structure of the lithosphere-asthenosphere system. We use the S receiver funct

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::12d9130f7443a94240bf55497a6e9be6
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:247101

A Receiver Function Study in Kope-Dagh (Iran) Using Short Period Data

Autor: Mohammadi, E., Sodoudi, F., Sadidkhouy, A.

Publikováno v: Geophysical Research Abstracts Vol. 13, EGU2011-3304-1, 2011
General Assembly European Geosciences Union (Vienna, Austria 2011)#

Geographic location of Iran plateau between Arabia and Eurasia plates caused the Iranian plate to be in a high pressure condition. Configuration and tectonic structures procedure in this region is affected by motions of these plates. With respect to

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1821523c9ec633f9aa34201c996245e2
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:247046