Results 111 to 120 of about 311 (158)

Tracing the Neovolcanic zone along the sediment-covered regions of the Red Sea Rift. [PDF]

open access: yesSci Rep
Preine J   +8 more
europepmc   +1 more source

Decoding microbial diversity, biogeochemical functions, and interaction potentials in red sea hydrothermal vents. [PDF]

open access: yesEnviron Microbiome
Altalhi S   +10 more
europepmc   +1 more source

Microbial Communities in and Around the Siboglinid Tubeworms from the South Yungan East Ridge Cold Seep Offshore Southwestern Taiwan at the Northern South China Sea. [PDF]

open access: yesMicroorganisms
Li Y   +20 more
europepmc   +1 more source

Onnamides and a Novel Analogue, Onnamide G, as Potent Leishmanicidal Agents. [PDF]

open access: yesMar Biotechnol (NY)
Jomori T   +15 more
europepmc   +1 more source

Seafloor deformation and forecasts of the April 2011 eruption at Axial Seamount

Nature Geoscience, 2012
The Axial Seamount submarine volcano exhibits an inflation–deflation cycle comparable to similar volcanoes on land. Measurements of ocean bottom pressure document the entire inflation–deflation cycle between eruptions at Axial Seamount in 1998 and 2011, and imply that the timing of submarine eruptions could be more predictable than that of their ...
Marvin Lilley   +2 more
exaly   +2 more sources

Volcanic action at Axial Seamount

Nature, 2000
Axial Seamount is an underwater volcano that lies on a seafloor-spreading centre off the west coast of southern Canada. It is being intensively studied, both through continuous monitoring by instruments at or near the site and through ship-borne ‘event response’ visits by scientists. The most recent burst of volcanic activity at Axial Seamount happened
exaly   +3 more sources

The magnetic structure of Axial Seamount, Juan de Fuca Ridge

Journal of Geophysical Research, 1990
Axial Seamount is a large, volcanically active seamount located in the eastern Pacific on the central Juan de Fuca (JDF) ridge at 46°N, 130′W. Sea surface magnetic anomaly data show that Axial lies completely within crust formed during the Brunhes normal polarity epoch.
Maurice Tivey
exaly   +2 more sources

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