Results 211 to 220 of about 13,224 (265)

Recent advances in Joule‐heating synthesis of functional nanomaterials for photo and electrocatalysis

open access: yesPhotoMat, EarlyView.
This paper presents a comprehensive overview of recent advancements in Joule‐heating synthesis of photo and electrocatalysts, emphasizing its benefits and applications. The objective is to offer an effective strategy for enhancing the diversity and performance of catalytic materials.
Jiaqi Li   +4 more
wiley   +1 more source

Experimental Investigation of Moisture Movement During Freeze–Thaw Cycles and Its Effect on Physical Rock Weathering in Low‐Porosity Alpine Limestone

open access: yesPermafrost and Periglacial Processes, EarlyView.
ABSTRACT The progressive weakening of alpine rockwalls through subcritical cracking, driven by repeated low‐magnitude stress processes, plays a key role in alpine rock weathering. Laboratory studies using acoustic emission (AE) monitoring have shown that thermal stresses from freeze–thaw cycling induce crack propagation, with recent work highlighting ...
Andrew Mitchell, Oliver Sass
wiley   +1 more source

The proto-Gulf of California

Earth and Planetary Science Letters, 1972
Abstract Extensional zones behind trench-arc systems lying along continental edges take the form of volcano-tectonic rift zones. These are characterized by ignimbrite sheets errupted simultaneously with, but behind, the andesite centers. Slightly later, a trough with basin-range structures is formed by crustal extension. The known geology of the Gulf
Daniel E. Karig, Wallace Jensky
openaire   +1 more source

SEDIMENTS OF THE GULF OF CALIFORNIA

Geological Society of America Bulletin, 1960
The Gulf of California is an elongate trough bordered by highlands on the west and mostly by lowlands on the east. Fault scarps divide its floor into a succession of closed basins separated by ridges, some of which are capped by islands. Water flows into the open sea along the east side and leaves along the west side after partial evaporation.
JOHN V. BYRNE, K. O. EMERY
openaire   +1 more source

Origin of the Gulf of California

Geological Society of America Bulletin, 1961
The probable cumulative Late Cretaceous and Cenozoic right-lateral strike-slip displacement along the San Andreas fault in central California is 350 miles. The San Andreas and the allied faults into which it branches southward trend longitudinally into the Gulf of California, and the seismicity of the region indicates that the fault system follows the ...
openaire   +1 more source

The Gulf and Peninsular Province of the Californias

1991
This book is about the Gulf and Peninsular Province of the Californias: Geological and geophysical maps; Regional geophysics and geology; Physical oceanography, primary productivity, and sedimentology, and Hydrothermal processes.
J. Paul Dauphin, Bernd R. T. Simoneit
openaire   +1 more source

Thermohaline circulation in the Gulf of California

Journal of Geophysical Research: Oceans, 1988
The Gulf of California, a narrow, semienclosed sea, is the only evaporative basin of the Pacific Ocean. As a result of evaporative forcing, salinities in the gulf are 1 to 2 ‰ higher than in the adjacent Pacific at the same latitude. This paper examines the thermohaline structure of the gulf and the means by which thermohaline exchange between the ...
openaire   +1 more source

On Tsunami Resonance of the Gulf of California

1993
The influence of the local bathymetry and the shape of the contour in the resonant response of the Gulf of California (Mexico) to incident tsunami waves of various approach directions and frequencies is analyzed.
Francisco J. Sandoval   +1 more
openaire   +1 more source

Macrofaunal Diversity in the Gulf of California

2005
Abstract The Gulf of California (Sea of Cortez) has held a growing fascination for naturalists over the past 150 years (Lindsay 1983). The first serious collectors of marine life in the region were not professional bi-ologists. One was John Xantus (de Vesey), a U.S.
Richard C Brusca   +5 more
openaire   +1 more source

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