Plume‐induced sinking of intracontinental lithospheric mantle: An overlooked mechanism of subduction initiation?
Although many different mechanisms for subduction initiation have been proposed, only few
of them are viable in terms of consistency with observations and reproducibility in numerical …
of them are viable in terms of consistency with observations and reproducibility in numerical …
Tomographic images of magma chambers beneath the Avacha and Koryaksky volcanoes in Kamchatka
A new tomographic model (Vp, Vs, and Vp/Vs ratio) was built for two neighboring active
volcanoes, Avacha and Koryaksky, which represent a serious hazard to the population and …
volcanoes, Avacha and Koryaksky, which represent a serious hazard to the population and …
Crustal and upper mantle structure of the Tien Shan orogenic belt from full‐wave ambient noise tomography
Z Lü, H Gao, J Lei, X Yang… - Journal of Geophysical …, 2019 - Wiley Online Library
In order to have a better understanding of the lithosphere formation and modification of the
Tien Shan orogenic belt, we construct a well‐defined shear wave velocity model of the crust …
Tien Shan orogenic belt, we construct a well‐defined shear wave velocity model of the crust …
Lithosphere structure in the collision zone of the NW Himalayas revealed by alocal earthquake tomography
In this study, we obtained new 3D seismic tomography models of the crust and uppermost
mantle beneath the northwestern Himalayas down to a depth of 120 km. The data were …
mantle beneath the northwestern Himalayas down to a depth of 120 km. The data were …
Crustal structure of the Eastern Anatolia Region (Turkey) based on seismic tomography
Here, we investigated the crustal structure beneath eastern Anatolia, an area of high
seismicity and critical significance for earthquake hazards in Turkey. The study was based …
seismicity and critical significance for earthquake hazards in Turkey. The study was based …
Warm versus cold crust in the Tien Shan orogenic belt revealed by seismic Lg attenuation tomography
X Ma, LF Zhao, XB **_structure_in_the_uppermost_mantle_beneath_the_central_Tien_Shan_from_Pn_traveltime_tomography/links/61fc9d5111a1090a79d00271/Opposite-facing-dip**-structure-in-the-uppermost-mantle-beneath-the-central-Tien-Shan-from-Pn-traveltime-tomography.pdf" data-clk="hl=en&sa=T&oi=gga&ct=gga&cd=9&d=9203804132666532638&ei=ySKmZ4KIJoC96rQP5oz8kAU" data-clk-atid="HmPcRRh7un8J" target="_blank">[PDF] researchgate.net
Opposite facing dip** structure in the uppermost mantle beneath the central Tien Shan from Pn traveltime tomography
Abstract The Tien Shan orogenic belt is located in the western region of central Asia, which
has been previously considered to have formed in the Paleozoic and reactivated in the …
has been previously considered to have formed in the Paleozoic and reactivated in the …