Results 21 to 30 of about 376 (117)
Crustal and uppermost mantle shear wave velocity structure beneath the Middle East from surface wave tomography [PDF]
SUMMARY We have constructed a 3-D shear wave velocity (Vs) model for the crust and uppermost mantle beneath the Middle East using Rayleigh wave records obtained from ambient-noise cross-correlations and regional earthquakes.
Boschi, Lapo +9 more
core +6 more sources
Abstract We propose a new model for the crust and upper mantle in Iran by joint inversion of gravity and magnetic fields, constrained with a seismic tomography model. We then calculate shear modulus from the Vs velocities and densities. The crust and mantle tomography model is first converted to a density cube through empirical and petrological ...
G. Maurizio +3 more
wiley +1 more source
Six distinct climate zones are identified in Iran: mild and humid, cool and sub‐humid, cold and temperate semi‐arid, warm and semi‐arid, cool and arid, and warm and hyperarid. The maximum precipitation occurs in the southern coastal plains of the Caspian Sea in autumn. The minimum precipitation occurs in southwestern Iran in summer.
Mohammad Saeed Najafi, Omid Alizadeh
wiley +1 more source
Rheological Heterogeneities Control the Non‐Progressive Uplift of the Young Iranian Plateau
Abstract The Iranian plateau is at the early stage of plateau development and intracontinental deformation in response to the Arabia‐Eurasia collision. Its compressive deformation is concentrated in the northern plateau but skips the central counterpart, challenging the common views envisaging the progressive uplift from the collisional front to the ...
Yifan Gao +3 more
wiley +1 more source
Abstract The interpretation of low‐temperature thermochronology (LTT) data in magmatic and metallogenic provinces requires a knowledge of the geothermal field through time. There, the challenge is differentiating rapid cooling following transient perturbations of the geotherms (reheating) from exhumational cooling induced by erosion during tectonic ...
Masoud Biralvand +9 more
wiley +1 more source
The controls on the thermal evolution of continental mountain ranges
Abstract This paper examines the controls on the thermal evolution of continental mountain ranges and investigates how pressure (P) and temperature (T) estimates from metamorphic rocks can be used to reconstruct the thermal histories of orogenic belts.
Alex Copley, Owen Weller
wiley +1 more source
Morph Tectonic Interpretation of Soluklu Basin (Northern Khorasan) Using Geomorphic Indices [PDF]
By recognizing the tectonic effects on fluvial systems , the value and importance of rivers in the study of tech tonic activities were recognized. The Study of stream channels and their displaced deposits by faulting at earthquake time, indicates the ...
Maryam. Ezati, Dr. Maryam. Agh Atabai
doaj +1 more source
Fold growth in the South Caspian Sea Basin: mechanisms and interaction with deep-water lacustrine sediments [PDF]
Growth strata analysis, finite element modelling and mapping of a lacustrine turbidite channel network utilizing a high-quality 3D seismic reflection dataset have been used to explore the Plio-Pleistocene growth history of the Shafag – Asiman fold ...
Procter, Andrew Liam
core +1 more source
Post-Eocene coupled oroclines in the Talesh (NW Iran): paleomagnetic constraints [PDF]
The Talesh Mountains (NW Iran) witnessed a long deformation history from the Triassic Cimmerian orogeny to the ongoing Arabia-Eurasia collision. This protracted multi-stage deformation has generated a remarkably curved orogen with a puzzling kinematic ...
Cotton, L. J. +8 more
core +1 more source
Spatio-temporal evolution of intraplate strike-slip faulting: the Neogene-Quaternary Kuh-e-Faghan Fault, Central Iran [PDF]
Central Iran provides an ideal region to study the long-term morphotectonic response to the nucleation and propagation of intraplate faulting. In this study, a multidisciplinary approach that integrates structural and stratigraphic field investigations ...
Berberian +24 more
core +3 more sources

