Results 181 to 190 of about 20,887 (256)
Abstract The ocean beneath ice shelves plays a critical role in their evolution and resilience. Despite this, direct observations of circulation within ice shelf cavities remain scarce. Here, we examine 4.5 years of moored hydrographic data (2018–2022) from the HWD2 borehole, which represent the first multi‐year measurements of currents, temperature ...
Yingpu Xiahou +3 more
wiley +1 more source
Little to no active faulting likely at Europa's seafloor today. [PDF]
Byrne PK +17 more
europepmc +1 more source
Hydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre. [PDF]
Connelly DP +26 more
europepmc +1 more source
Termination of a 6 year ridge‐spreading event observed using a seafloor seismic network on the Endeavour Segment, Juan de Fuca Ridge [PDF]
R. T. Weekly +5 more
openalex +1 more source
Abstract Periodic high‐resolution imagery of Io is essential for understanding its surface evolution, from volcanic eruptions to tectonic deformation to large‐scale mass wasting. Juno flybys in 2023 and 2024 obtained imagery of the surface with the JunoCam imager at 1.8 km/pixel spatial resolution, comparable to global observations from the Galileo ...
C. H. Seeger +5 more
wiley +1 more source
Toward a minimum change model for recent plate motions: calibrating seafloor spreading rates for outward displacement [PDF]
Charles DeMets, Douglas S. Wilson
openalex +1 more source
Abstract During the latest Miocene, the Mediterranean Basin was affected by extreme paleoceanographic and paleoenvironmental changes culminating with evaporite (gypsum and halite) formation during the Messinian Salinity Crisis (MSC: 5.97–5.33 Ma).
F. Lanterna +4 more
wiley +1 more source
Emissions of mantle helium and abiotic methane at newly discovered black smokers along the Central Indian ridge (12°S-16°S). [PDF]
Kim H +8 more
europepmc +1 more source
Abstract Recent observations and drilling campaigns have challenged the typical models for rifted margins by providing evidence for the existence of intermediate cases between the magmatic and amagmatic end‐members. In this contribution, we document the evolution of the Central Campos rifted margin, located in southeast Brazil, based on a combined ...
P. Alvarez +3 more
wiley +1 more source

