The Moho Relief Beneath the Zagros Collision Zone Through Modeling of Ground-Based Gravity Data and Utilizing Open-Source Resources in Python

Seismic Moho depth is defined based on a significant seismic velocity change between the crust and the upper mantle. Receiver function studies provide the most reliable estimates of the Moho depth. However, they are limited to some profile strikes to the Zagros collision zone. Here, we present an au...

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Vydané v:	Pure and applied geophysics Ročník 180; číslo 3; s. 909 - 918
Hlavní autori:	Ardestani, Vahid E., Mousavi, Naeim
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Cham Springer International Publishing 01.03.2023 Springer Nature B.V
Predmet:	Density Depth Earth and Environmental Science Earth Sciences Eclogite Geophysics/Geodesy Gravity data Isotopes Methods Modelling Moho S waves Seismic velocities Shear Tomography Upper mantle Wavelength Bouguer gravity anomalies Zagros collision zone Moho relief nonlinear inversion open-source resources
ISSN:	0033-4553, 1420-9136
On-line prístup:	Získať plný text
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