Results 201 to 210 of about 31,172 (296)
Extrapolating rock physicochemical properties from discrete sample data using computer vision. [PDF]
Grant LJC +5 more
europepmc +1 more source
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 +2 more
wiley +1 more source
Abstract The South Asian summer monsoon has exhibited a pronounced Northwest India‐Indo‐Gangetic Plains rainfall dipole since 1999, with northwest India experiencing a 24.6% increase, while rainfall in the Indo‐Gangetic Plain has decreased by 4.4%.
Nimmakanti Mahendra +5 more
wiley +1 more source
Abstract This study evaluates the performance of different WRF model configurations in simulating all 19 heavy precipitation events over Bushehr Province, Iran, over two decades (2000–2019). For the first time, the sensitivity of combinations of three physical parameterization options—seven cumulus (Cu) schemes, three planetary boundary layer (PBL ...
N. Pegahfar, Y. Shao
wiley +1 more source
Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago. [PDF]
Hoernle K +13 more
europepmc +1 more source
Abstract Seafloor basalt samples recovered from the Caroline Basin (CB), the Parece Vela Basin (PVB), and the Western Philippine Sea Plate (WPSP) are analyzed for whole‐rock major and trace elements (including H2O), Sr‐Nd‐Pb‐Hf isotopes and 40Ar‐39Ar age‐dating.
Guo‐Liang Zhang +3 more
wiley +1 more source
Three Cases Revealing Remarkable Genetic Similarity Between Vent-Endemic Rimicaris Shrimps Across Distant Geographic Regions. [PDF]
Lee WK, Cho SY, Ju SJ, Kim SJ.
europepmc +1 more source
Abstract The seismic behavior of subduction megathrusts varies spatially and is influenced by the properties of subducting plates, including their sedimentary cover. Characterizing these subduction inputs is essential for understanding the mechanisms behind fault slip variability.
Philip M. Barnes +12 more
wiley +1 more source
Warming waters herald a submarine eruption. [PDF]
Chadwick WW.
europepmc +1 more source
Abstract Rifting is a tectonic process that leads to extensive magmatic activity, continental breakup, and the formation of new oceanic crust. The interplay between rifting and dynamic mantle flow driven by thermal heterogeneity in the mantle along the rift‐axis can influence magmatism and deformation beyond the rift zone.
Min‐Seok Jang, Byung‐Dal So
wiley +1 more source

