Results 211 to 220 of about 300,638 (255)

Fluid‐Driven Cohesive Strengthening: Critical Role of Reaction Kinetics as the Determinant for Frictional Stability

AGU Advances, Volume 7, Issue 3, June 2026.
Abstract Following an earthquake, faults lock and regain strength via a combination of healing mechanisms that include pressure solution, contact growth, and cementation. Fault healing dictates strength recovery during the seismic cycle and is therefore a key factor controlling earthquake recurrence intervals, stress drop, and other source properties ...
R. Affinito, G. Volpe, L. Calzolari, T. Mittal, G. Pozzi, C. Marone   +5 more
wiley   +1 more source

The most energetic transients: Tidal disruptions of high-mass stars. [PDF]

Sci Adv
Hinkle JT, Shappee BJ, Auchettl K, Kochanek CS, Neustadt JMM, Polin A, Strader J, Holoien TW, Huber ME, Tucker MA, Ashall C, de Jaeger T, Desai DD, Do A, Hoogendam WB, Payne AV.   +15 more
europepmc   +1 more source

Metamorphic Dehydration, Fluid Pressure, and the Frictional‐Viscous Transition Along Subduction Megathrusts: Case Study in Cascadia and Implications for Slow Earthquakes

AGU Advances, Volume 7, Issue 3, June 2026.
Abstract Relative plate motion in subduction zones transitions from frictional slip to viscous flow with increasing depth and temperature. The frictional‐viscous transition can control the depth extent of megathrust earthquakes and episodic tremor and slip (ETS).
So Ozawa, Eric M. Dunham, Cailey B. Condit   +2 more
wiley   +1 more source

CrossDI: A comprehensive dataset crossing three databases for calculating disruption indexes. [PDF]

Sci Data
Xu S, Wang C, An X, Liu J.
europepmc   +1 more source

Autogenic Shoreline Migration and Its Effect on the Storage of Carbon in Marginal Marine Successions

AGU Advances, Volume 7, Issue 3, June 2026.
Abstract The accumulation of organic matter (OM) near shorelines, known as blue carbon, is a key sink in the global carbon cycle. This accumulation is influenced by elevation relative to sea level of the delta‐top, which changes through the movement of shorelines with time.
Jose R. Silvestre, Kelly M. Sanks, Samuel M. Zapp, Yi Hou, John B. Shaw, Udita Mukherjee, Rhodri M. Jerrett, Robert A. Duller, Kyle M. Straub   +8 more
wiley   +1 more source

A tidal disruption event from an intermediate-mass black hole revealed by comprehensive multi-wavelength observations. [PDF]

Nat Commun
Wang J, Huang M, Xue Y, Jiang N, Huang S, Wang Y, Zhu J, Zhu S, Dai L, Jin C, Luo B, Shu X, Sun M, Wang T, Zou F.   +14 more
europepmc   +1 more source

First Results of a New Inversion Tool for Thermospheric Neutral Mass Density Computations During Severe Geomagnetic Storms

AGU Advances, Volume 7, Issue 3, June 2026.
Abstract In Low Earth Orbit (LEO), atmospheric drag is the dominant source of trajectory prediction error below approximately 700 km altitude, primarily due to inaccuracies in thermospheric density models. This work presents a method for temporally deconvolving Energy Dissipation Rates (EDRs) to produce single‐satellite density estimates, which can be ...
S. Mutschler, M. Pilinski, E. Zesta, D. M. Oliveira, K. Delano, K. Garcia‐Sage, W. K. Tobiska   +6 more
wiley   +1 more source

Anomalous Spin-Optical Helical Effect in Ti-Based Kagome Metal. [PDF]

Adv Mater
Mazzola F, Brzezicki W, Bigi C, Consiglio A, D'Onofrio LJ, Mercaldo MT, Kłosiński A, Bertran F, Le Fèvre P, Clark OJ, Edmonds MT, Tuniz M, De Vita A, Polewczyk V, Jacobsen JB, Jacobsen H, Miwa JA, Wells JW, Jana A, Vobornik I, Fujii J, Mignani N, Samani NT, Crepaldi A, Sangiovanni G, Kataria A, Morresi T, Sanna S, Bonfá P, Ortiz BR, Pokharel G, Wilson SD, Sante DD, Ortix C, Cuoco M.   +34 more
europepmc   +1 more source

Widespread Impact‐Induced Crustal Permeability on the Early Earth

AGU Advances, Volume 7, Issue 3, June 2026.
Abstract The early Earth (i.e., Archean and Hadean Eons, 2.5–4.0 and 4.0–4.5 Ga, respectively) experienced frequent cosmic bombardment. Impacts have been shown to stimulate crustal alteration, for instance via hydrothermal systems active for up to millions of years post‐impact.
A. M. Alexander, S. Marchi, B. C. Johnson   +2 more
wiley   +1 more source