Citation:

PANGAEA.763225, Supplement to: Bogdanov, YA et al. (2005): Hydrothermal ore deposits of the Snake Pit hydrothermal field (Mid-Atlantic Ridge). Translated from Okeanologiya, 2005, 45(4), 574-591, Oceanology, 45(4), 543-559

Name: Chemical and mineral compositions of sulfide deposits from the Snake Pit hydrothermal field, Mid-Atlantic Ridge rift zone
Published: 2005
License: https://creativecommons.org/licenses/by/3.0/

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Abstract:

The Snake Pit hydrothermal field is located on the top of a neovolcanic rise on the Mid-Atlantic Ridge at sea depths between 3460 and 3510 m. It was surveyed during several oceanological expeditions including DSDP Legs. Additional scientific materials were obtained in 2002 and 2003 during expedition onboard R/V Akademik Mstislav Keldysh with two Mir deep-sea manned submersibles. Three eastern hydrothermal mounds (Moose, Beehive, and Fir Tree) are located on the upper part of the eastern slope of the rise over a common fractured pedestal composed of fragments of massive sulfides. The western group of hydrothermal deposits is encountered on the western slope of the axial graben. Within this mature hydrothermal field, which was formed over the past 4000 years, we studied morphology of the hydrothermal mounds, chemistry and mineralogy of hydrothermal deposits, chemistry of sulfide minerals, and isotope composition of sulfur in them.

Project(s):

Archive of Ocean Data (ARCOD)

Coverage:

Median Latitude: 23.368593 * Median Longitude: -44.951994 * South-bound Latitude: 23.368280 * West-bound Longitude: -44.953450 * North-bound Latitude: 23.368850 * East-bound Longitude: -44.950850

Event(s):

AMK47-4326-1 * Latitude: 23.368380 * Longitude: -44.952170 * Elevation: -3460.0 m * Location: Snake Pit Hydrothermal Field, Beehive mound * Campaign: * Basis: Akademik Mstislav Keldysh * Method/Device: MIR deep-sea manned submersible (MIR)

AMK47-4326-2 * Latitude: 23.368380 * Longitude: -44.952170 * Elevation: -3460.0 m * Location: Snake Pit Hydrothermal Field, Beehive mound * Campaign: * Basis: Akademik Mstislav Keldysh * Method/Device: MIR deep-sea manned submersible (MIR)

AMK47-4327-1 * Latitude: 23.368550 * Longitude: -44.951770 * Elevation: -3492.0 m * Location: Snake Pit Hydrothermal Field, Beehive mound * Campaign: * Basis: Akademik Mstislav Keldysh * Method/Device: MIR deep-sea manned submersible (MIR)

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

5 datasets

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Datasets listed in this publication series

Bogdanov, YA; Lein, AY; Sagalevich, AM et al. (2005): (Table 2) Chemical composition of sulfide deposits from the Beehive hydrothermal edifice, Snake Pit hydrothermal field. https://doi.org/10.1594/PANGAEA.763175
Bogdanov, YA; Lein, AY; Sagalevich, AM et al. (2005): (Table 3) Chemical composition of sulfide deposits from the Moose hydrothermal edifice, Snake Pit hydrothermal field. https://doi.org/10.1594/PANGAEA.763176
Bogdanov, YA; Lein, AY; Sagalevich, AM et al. (2005): (Table 4) Chemical composition of sulfide deposits from the Fir Tree relict hydrothermal edifice and the Nail active hydrothermal edifice, Snake Pit hydrothermal field. https://doi.org/10.1594/PANGAEA.763177
Bogdanov, YA; Lein, AY; Sagalevich, AM et al. (2005): (Table 5) Mineral composition of hydrothermal edifices from the Snake Pit hydrothermal field. https://doi.org/10.1594/PANGAEA.763223
Bogdanov, YA; Lein, AY; Sagalevich, AM et al. (2005): (Table 6) Chemical composition of sulfide minerals from the Snake Pit hydrothermal field. https://doi.org/10.1594/PANGAEA.763224