Results 111 to 120 of about 415 (171)

Combined analysis of PS-InSAR and hypsometry integral (HI) for comparing seismic vulnerability and assessment of various regions of Pakistan. [PDF]

Sci Rep, 2022
Ramzan U, Fan H, Aeman H, Ali M, A A Al-Qaness M.   +4 more
europepmc   +1 more source

Accommodation of Arabia-Eurasia convergence in the Zagros-Makran transfer zone, SE Iran: A transition between collision and subduction through a young deforming system

, 2004
International audienceAt Iranian longitude, the Arabian plate is moving northward relative to Eurasia (∼20 mm yr-1 according to GPS). To the east, this relative motion is accommodated by northward subduction under the E-W Makran emerged accretionary ...
Shabanian, E., Regard, V., Feghhi, K., Bellier, O., Thomas, J. -C., Abbassi, M. R., Mercier, J., Soleymani, S.   +7 more
core   +1 more source

Mantle-flow diversion beneath the Iranian plateau induced by Zagros' lithospheric keel. [PDF]

Sci Rep, 2021
Kaviani A, Mahmoodabadi M, Rümpker G, Pilia S, Tatar M, Nilfouroushan F, Yamini-Fard F, Moradi A, Ali MY.   +8 more
europepmc   +1 more source

Effect of Murray ridge on the tsunami propagation from Makran subduction zone [PDF]

Geophysical Journal International, 2014
M. Swapna, Kirti Srivastava
openaire   +1 more source

P- and S-receiver function data in the western part of the Makran Subduction Zone

This dataset consists of the P- and S-receiver functions and the waveforms for seismic stations located in the western part of the Makran Subduction Zone.THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE.
Mokhtarzadeh, R (via Mendeley Data)
core   +1 more source

Petrography, geochemistry and tectonic setting of Salmabad Tertiary volcanic rocks, southeast of Sarbisheh, eastern Iran

Journal of Economic Geology, 2014
Introduction The area reviewed and studied in this paper is located 5 km southeast of Sarbisheh city at eastern border of the Lut block (Jung et al., 1983; Karimpour et al., 2011; Richards et al., 2012) in eastern Iran between 59° 47′ and 59° 53′ E ...
Masoumeh Goodarzi, Seyyed Saeid Mohammadi, Mohammad Hossein Zarrinkoub   +2 more
doaj  

Ongoing formation of felsic lower crustal channel by relamination in Zagros collision zone revealed from regional tomography. [PDF]

Sci Rep, 2020
Talebi A, Koulakov I, Moradi A, Rahimi H, Gerya T.   +4 more
europepmc   +1 more source

Sulfide mineralization in ultramafic rocks of the Faryab ophiolite complex, southern Kerman

Journal of Economic Geology, 2015
Introduction Worldwide, Ni-Cu and PGE magmatic sulfide deposits are confined to the lower parts of stratiform mafic and ultramafic complexes. However, ophiolite mafic and ultramafic complexes have been rarely explored for sulfide deposits despite the ...
Mohammad Ali Rajabzadeh, Fatemeh Al Sadi
doaj  

Crustal Structure of the Collision-Subduction Zone in South of Iran Using Virtual Seismometers. [PDF]

Sci Rep, 2019
Shirzad T, Riahi MA, Assumpção MS.
europepmc   +1 more source

Rupture access to hydrous minerals controls aftershocks in subduction zones. [PDF]

Sci Rep
Gunatilake T, Gerya T, Connolly JAD, Miller SA.   +3 more
europepmc   +1 more source