Earth crustal model 1 (ECM1): A 1 x 1 global seismic and density model

WD Mooney, C Barrera-Lopez, MG Suárez… - Earth-Science …, 2023 - Elsevier
Abstract Earth Crustal Model 1 (ECM1) is a 1° x 1° global crustal model that describes the
thickness of the crust, including the overlying sediments, and the corresponding seismic …

Planned products of the Mars structure service for the InSight mission to Mars

MP Panning, P Lognonné, W Bruce Banerdt… - Space Science …, 2017 - Springer
The InSight lander will deliver geophysical instruments to Mars in 2018, including
seismometers installed directly on the surface (Seismic Experiment for Interior Structure …

Intracontinental deformation of the Tianshan Orogen in response to India-Asia collision

W Li, Y Chen, X Yuan, W Xiao, BF Windley - Nature Communications, 2022 - nature.com
How the continental lithosphere deforms far away from plate boundaries has been long
debated. The Tianshan is a type-example of ongoing lithospheric deformation in an …

Crustal and uppermost mantle structure beneath the United States

W Shen, MH Ritzwoller - Journal of Geophysical Research …, 2016 - Wiley Online Library
This paper presents a new model of the shear velocity structure of the crust and uppermost
mantle beneath the contiguous US The model is based on more than a decade of USArray …

Eastward expansion of the Tibetan Plateau by crustal flow and strain partitioning across faults

QY Liu, RD Van Der Hilst, Y Li, HJ Yao, JH Chen… - Nature …, 2014 - nature.com
The lateral expansion of the southeastern Tibetan Plateau causes devastating earthquakes,
but is poorly understood. In particular, the links between regional variations in surface …

Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions

X Bao, X Sun, M Xu, DW Eaton, X Song, L Wang… - Earth and Planetary …, 2015 - Elsevier
Competing geodynamic models, such as rigid-block extrusion, continuous deformation, and
the mid-lower crustal flow, have been proposed to describe the growth and expansion of …

[HTML][HTML] 利用面波频散与接收函数联合反演青藏高原东南缘地壳上地幔速度结构

郑晨, 丁志峰, 宋晓东 - 地球物理学报, 2016 - html.rhhz.net
青藏高原东南缘对于青藏高原的隆升, 增厚和物质逃逸等问题有着重要的研究价值.
本文对研究区内布设的大型流动地震台阵的观测记录进行处理, 联合反演面波频散与接收函数 …

Transdimensional inversion of receiver functions and surface wave dispersion

T Bodin, M Sambridge, H Tkalčić… - … research: solid earth, 2012 - Wiley Online Library
We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …

Seismic imaging of the magmatic underpinnings beneath the Altiplano-Puna volcanic complex from the joint inversion of surface wave dispersion and receiver …

KM Ward, G Zandt, SL Beck, DH Christensen… - Earth and Planetary …, 2014 - Elsevier
Located in the central Andes, the Altiplano-Puna Volcanic Complex (APVC) is the location of
an 11–1 Ma silicic volcanic field, one of the largest and youngest on Earth. Yet its …

A framework for 3-D joint inversion of MT, gravity and seismic refraction data

M Moorkamp, B Heincke, M Jegen… - Geophysical Journal …, 2011 - academic.oup.com
We present a 3-D joint inversion framework for seismic, magnetotelluric (MT) and scalar and
tensorial gravity data. Using large-scale optimization methods, parallel forward solvers and …