New insights into the heterogeneity of the lithosphere‐asthenosphere system beneath South China from teleseismic body‐wave attenuation
Teleseismic body‐wave attenuation provides an independent constraint on the architecture
of the lithosphere‐asthenosphere system. We obtain the first map of teleseismic attenuation …
of the lithosphere‐asthenosphere system. We obtain the first map of teleseismic attenuation …
Thin lithosphere beneath the central Appalachian Mountains: Constraints from seismic attenuation beneath the MAGIC array
The passive margin of the eastern coast of the United States is known to be geologically
active, with recently rejuvenated topography, intraplate seismicity, and volcanism of Eocene …
active, with recently rejuvenated topography, intraplate seismicity, and volcanism of Eocene …
Evaluating models for lithospheric loss and intraplate volcanism beneath the Central Appalachian Mountains
The eastern margin of North America has been shaped by a series of tectonic events
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …
Variable Depths of Magma Genesis in the North China Craton and Central Asian Orogenic Belt Inferred From Teleseismic P Wave Attenuation
Eastern Asia is a prime location for the study of intracontinental tectono‐magmatic activity.
For instance, the origin of widespread intraplate volcanism has been one of the most …
For instance, the origin of widespread intraplate volcanism has been one of the most …
Teleseismic attenuation, temperature, and melt of the upper mantle in the Alaska subduction zone
Seismic deployments in the Alaska subduction zone provide dense sampling of the seismic
wavefield that constrains thermal structure and subduction geometry. We measure P and S …
wavefield that constrains thermal structure and subduction geometry. We measure P and S …
Joint analysis of seismic and electrical observables beneath the Central Appalachians requires partial melt in the upper mantle
Abstract The Central Appalachian Anomaly (CAA) is a region of the upper mantle beneath
eastern North America that exhibits pronounced anomalies in its seismic velocity, seismic …
eastern North America that exhibits pronounced anomalies in its seismic velocity, seismic …
Crustal and upper mantle attenuation structure beneath the southeastern Tibetan Plateau and its implications on plateau outgrowth
H Liu, S Pei, W Liu, X Xue, J Li… - Journal of Geophysical …, 2024 - Wiley Online Library
Abstract The eastern Tibetan Plateau (TP) is crucial to the exploration of plateau outgrowth
mechanisms. Teleseismic attenuation may provide constraints on anelasticity in the …
mechanisms. Teleseismic attenuation may provide constraints on anelasticity in the …
Dynamic upwelling beneath the Salton Trough imaged with teleseismic attenuation tomography
Abstract The Salton Trough is one of the few regions on Earth where rifting is subaerial
instead of submarine. We use the relative attenuation of teleseismic P phases recorded by …
instead of submarine. We use the relative attenuation of teleseismic P phases recorded by …
Lateral variations in teleseismic attenuation of the conterminous US and new insights derived from its relationship to Mantle seismic velocity
Much of our knowledge of the North American lithosphere comes from imaging seismic
velocities. Additional constraints on the subsurface can be gained by studying seismic …
velocities. Additional constraints on the subsurface can be gained by studying seismic …
Evidence for stress localization caused by lithospheric heterogeneity from seismic attenuation
Abstract The Wyoming Craton underwent tectonic modifications during the Laramide
Orogeny, which resulted in a series of basement‐cored uplifts that built the modern‐day …
Orogeny, which resulted in a series of basement‐cored uplifts that built the modern‐day …