Results 181 to 190 of about 9,710 (277)
Unconventional water and hydrous mineral formation from dry minerals and H<sub>2</sub> fluids. [PDF]
Vitale Brovarone A +10 more
europepmc +1 more source
Photosynthetic primary production in the Mesoproterozoic
Summary The Mesoproterozoic atmosphere had more CO2 and less O2 than at present. While the upper ocean was oxygenated, the deeper ocean was euxinic or ferruginous. Primary production was performed by Chlorobia, Cyanobacteria, Proteobacteria, and Archaeplastida.
Patricia Sánchez‐Baracaldo +1 more
wiley +1 more source
Presence of continental slivers in oceanic transform faults determined by rift inheritance. [PDF]
Balázs A, Gerya T, Tari G.
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
Spreading modes at slow-spreading ridges shifted by mantle heterogeneity of the asthenosphere. [PDF]
Zhang WQ +5 more
europepmc +1 more source
Abstract The Tan‐Lu Fault Zone (TLFZ), the largest lithosphere‐scale strike‐slip fault in eastern China, has experienced multiple tectonic stages and remains high seismic activity, including the 1668 Tancheng earthquake (M 8.5). Here we employ dense‐array receiver functions to resolve crustal thickness, Vp/Vs ratio, and seismic discontinuities in the ...
Yuchen Huang +6 more
wiley +1 more source
A Noachian hydrosphere component in the 4.1-Ga Martian meteorite Teghaza 001. [PDF]
Saper L +5 more
europepmc +1 more source
Abstract Constraining peak temperature during seismic slip is essential for quantifying earthquake energy budgets and fault weakening. Rock magnetic methods provide a sensitive means of estimating shear‐induced coseismic temperature rise; however, the role of fluids in friction‐induced magnetic alterations remains poorly constrained.
Qiang Fu +6 more
wiley +1 more source
Necking of the active Turkana Rift Zone and the priming of eastern Africa for continental breakup. [PDF]
Rowan CM +4 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

