Results 171 to 180 of about 6,578 (212)
Seismic imaging of a basaltic Lesser Antilles slab from ancient tectonics. [PDF]
Yang X +7 more
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Microbial metabolic potential of hydrothermal vent chimneys along the submarine ring of fire. [PDF]
Murray L, Fullerton H, Moyer CL.
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Source mechanism of impulsive seafloor events that track submarine lava flows. [PDF]
Wang P +7 more
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Enigmatic H<sub>2</sub>- and CH<sub>4</sub>-rich hydrothermal plumes at the ultramafic-hosted Lucky B site, 81°N on Lena Trough, Arctic Ocean. [PDF]
Albers E +14 more
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Re-Os dating of the Makimine and Shimokawa VMS deposits for new age constraints on ridge subduction beneath Japanese Islands. [PDF]
Nozaki T, Takaya Y, Nakayama K, Kato Y.
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Tectonic structures on the Juan de Fuca Ridge
Geological Society of America Bulletin, 1977The northern Juan de Fuca Ridge is an actively spreading part of the East Pacific Rise system that is flooded with young turbidite sediments from the nearby continental margin. A detailed geophysical survey was completed at the intersection of the ridge with the Sovanco Fracture Zone.
E. E. DAVIS, C.R.B. LISTER
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Hydrothermal effects west of the Juan de Fuca Ridge
Deep Sea Research Part I: Oceanographic Research Papers, 1993The Juan de Fuca Ridge in the northeast Pacific Ocean is a region of extensive hydrothermal activity, and plumes emanating from the ridge can be dispersed by the oceanic circulation at about 2000 m. Off-axis temperature-salinity characteristics and water-property maps suggest a history of variability in hydrothermal activity on the ridge.
Glenn A. Cannon +2 more
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Introduction to Juan de Fuca Ridge Special Section
Journal of Geophysical Research: Solid Earth, 1987The U.S. Geological Survey and several other institutions have been studying the southernmost segment of the Juan de Fuca Ridge for several years by almost every means available to marine geologists and geophysicists [e.g., Normark et al., this issue].
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