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Articles by El Khrepy
Collisional Processes in the Crust of the Northern Tien Shan Inferred From Velocity and Attenuation Tomography Studies
Based on seismic data from existing seismic networks in Kyrgyzstan, we have constructed new crustal models of seismic velocity and attenuation for P and S wave s beneath the Kyrgyz Tien Shan. With data from more than 6,000 events recorded by the international KNET network, the most detailed structures were detected in the central-northern part of the study region, where the Kazakh Shield collides with the northern Tien Shan.
Three different types of plumbing systems beneath the neighboring active volcanoes of Tolbachik, Bezymianny and Klyuchevskoy in Kamchatka
The Klyuchevskoy group of volcanoes (KGV) in Kamchatka includes three presently active volcanoes (Klyuchevskoy, Bezymianny and Tolbachik) located close together in an area of approximately 50?×?80?km. These three volcanoes have completely different compositions and eruption styles from each other.
Possible sources of hydrothermal activity and mud volcanism in southern Sakhalin inferred from local earthquake seismic tomography
Sakhalin is a large island located in the Russian Far East in a zone of strong seismic activity. In Sakhalin, there are several mud volcanoes, two of which are among the largest ones in the world. In the paper, we present the first seismic model of the crust beneath Southern Sakhalin obtained from tomographic inversion of travel times of seismic waves from local earthquakes. The derived tomographic model reveals structures that are similar to those of a subduction complex, but in miniature.
3D density model of the upper mantle of Asia based on inversion of gravity and seismic tomography data
We construct a new-generation 3D density model of the upper mantle of Asia and its surrounding areas based on a joint interpretation of several data sets. A recent model of the crust combining nearly all available seismic data is employed to calculate the impact of the crust on the gravity anomalies and observed topography and to estimate the residual mantle anomalies and residual topography.
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