Deep Sea Research Part A. Oceanographic Research Papers
Hydrothermal vents of Explorer Ridge, northeast Pacific
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Cited by (88)
Chemical characteristics of modern deep-sea metalliferous sediments in closed versus open basins, with emphasis on rare-earth elements and Nd isotopes
2021, Earth-Science ReviewsCitation Excerpt :The Nd-isotope composition of barite-rich sediment at 37°N on the Mid-Atlantic Ridge is close to that of the associated basalts (Dias et al., 2008). On the Southern Explorer Ridge, barite forms a component of massive sulphide-sulphate-silica deposits at the Magic Mountain vent field (Tunnicliffe et al., 1986; Scott et al., 1990). Barite also occurs as residual sandy material within Fe-oxyhydroxide-rich gossanous sediments overlying inactive mounds; this barite has a large positive Eu anomaly, but no Ce anomaly (Barrett et al., 1990).
Radiogenic isotopes in enriched mid-ocean ridge basalts from Explorer Ridge, northeast Pacific Ocean
2017, Geochimica et Cosmochimica ActaCitation Excerpt :If so, then at some point in the future all spreading on Explorer Ridge will cease and most of the Explorer Plate will merge with the North American Plate. Most of the basalt samples from the SER were collected around the Magic Mountain hydrothermal vent field, located on the shallowest section (axial high) of the SER (Fig. 1B) (Tunnicliffe et al., 1986; Embley, 2002; National Oceanic and Atmospheric Administration, 2002a). The Explorer Ridge segments north and south of Magic Mountain have not been investigated by well-navigated submersible or remotely-operated vehicle surveys and remain poorly studied (Cousens et al., 1984; Michael et al., 1989).
The importance of hydrothermal venting to water-column secondary production in the northeast Pacific
2015, Deep-Sea Research Part II: Topical Studies in OceanographyCitation Excerpt :Our estimate for the “distance from the vents” corresponds to the mean lateral distance in kilometers from the up-cast portion of a given tow to the four main vent fields in the axial valley (Thomson et al., 2005). One of the tows was from the Explorer Ridge venting region (Tunnicliffe et al., 1986) located roughly 80 km to the northeast of Endeavour Ridge, and two tows were from the Co-axial Seamount region (Baker et al., 1995; Tunnicliffe et al., 1997) located 125 km to the south of Endeavour Ridge. These distant tows were also considered to be near-vent samples, with distance measured from the nearby venting sources.
Habitat, growth and physiological ecology of a basaltic community of Ridgeia piscesae from the Juan de Fuca Ridge
2003, Deep-Sea Research Part I: Oceanographic Research PapersUnderstanding the biogeography of chemosynthetic ecosystems
2002, Oceanologica ActaTagoro Submarine Volcano as a Natural Source of Significant Dissolved Inorganic Nutrients
2023, Active Volcanoes of the World