Results 91 to 100 of about 3,414 (186)
Continental evolution influenced by relamination of deeply subducted continental crust. [PDF]
Gómez-Frutos D +3 more
europepmc +1 more source
A Spreading‐Rate Dependence for Periodic Signals Embedded in Otherwise Aperiodic Abyssal Hills
Abstract I present evidence, through an empirical pre‐whitening analysis, that periodic signals are embedded in otherwise aperiodic abyssal hills across paleo‐spreading rates ranging from 1 to 9 cm/yr (half rate). Data are comprised of archival trackline and multibeam bathymetry profiles in north and south Atlantic Oceans, Pacific‐Antarctic Ridge ...
J. A. Goff
wiley +1 more source
Seismic Evidence for Slab Tearing Beneath the Indo‐Myanmar Subduction Zone
Abstract Slab tearing has been increasingly recognized as a key geodynamic process influencing the evolution of the eastern Himalayan syntaxis. However, whether, where and how the subducted Indian slab beneath the Indo‐Myanmar subduction zone has been torn remains poorly constrained.
Shun Yang +9 more
wiley +1 more source
Crust-mantle interactions during subduction of oceanic & continental crust
Castelli, D. +8 more
openaire +3 more sources
Sulfur-enriched sub-arc fluids drive deep sulfur cycling in subduction zones. [PDF]
Tan DB +10 more
europepmc +1 more source
Abstract The Cenozoic convergence between the Indian and Asian plates has driven large‐scale mantle convection that interacts with both plates. Understanding this convergence benefits from clear imaging of the lithosphere‐asthenosphere boundary (LAB).
Yiming Bai +12 more
wiley +1 more source
Collapse and resurgence of the Iceland mantle plume. [PDF]
Pearman C +8 more
europepmc +1 more source
Abstract The Tangra Yumco Rift (TYR) in central Tibet is a key window for crust–mantle interactions during extension. We performed high‐resolution crust‐mantle imaging using receiver function analysis, 1‐D nonlinear S‐wave velocity inversion, and tomoDD tomography, revealing a vertical Crust–Mantle Degassing System (CMDS) bounded by the Zhala (ZF) and ...
Zongxu Li +8 more
wiley +1 more source
Slab tearing and its surface signals controlled by passive margin strength. [PDF]
Maiti G +4 more
europepmc +1 more source
Abstract As the climate warms, associated changes in ocean dynamics will redistribute sea‐water mass within the ocean, contributing to relative sea‐level change. This mass redistribution will cause additional sea‐level changes due to gravitational self‐attraction, deformation of the solid Earth, and shifts in the Earth's rotation axis (GRD), which are ...
Grace Ertel +3 more
wiley +1 more source

