Honnorez, Jose J; Mével, Catherine; Honnorez-Guerstein, B-M; Tomschi, H P (1990): Chemistry of sulfide deposites of ODP Site 106-649 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.745553, Supplement to: Honnorez, JJ et al. (1990): Mineralogy and chemistry of sulfide deposites drilled from hydrothermal mound of the Snake Pit Activity Field, MAR. In: Detrick, R; Honnorez, J; Bryan, WB; Juteau, T; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 106/109, 145-162, https://doi.org/10.2973/odp.proc.sr.106109.137.1990
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Abstract:
The Snake Pit active hydrothermal field was discovered at 23°22'N on the Mid-Atlantic Ridge during ODP Leg 106. Among the ten holes drilled in the mound at the foot of an active chimney, only three (649B, 649F, and 649G) had substantial recovery, and produced cores of unconsolidated hydrothermal deposit made up of porous sulfide fragments with minor talc pellets and biological debris, and a few pieces of brassy massive sulfides.
Eight representative samples from the 6.5-m-long core from Hole 649B were analyzed for bulk chemistry, both by XRF (major elements) and NAA (trace elements). Major elements average compositions show high Fe (36 wt%), S (37 wt%), and Cu (12 wt%) contents, and minor Zn (6.7 wt%), reflecting a mostly high-temperature deposit. Trace elements are characterized by a high Au content (600 ppb) which could express the maturity of the mound.
Mineralogical assemblages show evidence of sequential precipitation, and absence of equilibrium. Major sulfide phases are pyrrhotite, pyrite, Fe, Cu sulfides, marcasite, and sphalerite. Three types of samples are distinguished on the basis of textures and mineral assemblages: type 1, rich in pyrrhotite, with approximately equivalent amounts of Cu, Fe sulfides, and sphalerite and minor pyrite; type 2, rich in Cu, Fe sulfides, which are cubic cubanite with exsolutions and rims of chalcopyrite; and type 3, essentially made up of sphalerite. Type 2 samples likely represent fragments of the inner chimney wall. The presence of talc intergrown with cubic cubanite/chalcopyrite in one big piece from Hole 649G is probably related to mixing of the hydrothermal fluid with seawater.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 23.369117 * Longitude: -44.950900
Date/Time Start: 1985-12-12T00:00:00 * Date/Time End: 1985-12-18T00:00:00
Event(s):
106-649 * Latitude: 23.369117 * Longitude: -44.950900 * Date/Time Start: 1985-12-12T00:00:00 * Date/Time End: 1985-12-18T00:00:00 * Elevation: -3524.0 m * Penetration: 63.9 m * Recovery: 6.7 m * Location: South Atlantic Ocean * Campaign: Leg106 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 10 cores; 63.9 m cored; 0 m drilled; 10.5% recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4 datasets
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Datasets listed in this publication series
- Honnorez, JJ; Mével, C; Honnorez-Guerstein, B-M et al. (1990): (Table 5) Representative analyses of pyrites of ODP Site 106-649. https://doi.org/10.1594/PANGAEA.745549
- Honnorez, JJ; Mével, C; Honnorez-Guerstein, B-M et al. (1990): (Table 4) Representative analyses of pyrrhotite of ODP Site 106-649. https://doi.org/10.1594/PANGAEA.745547
- Honnorez, JJ; Mével, C; Honnorez-Guerstein, B-M et al. (1990): (Table 7) Representative analyses of sphalerites of ODP Site 106-649. https://doi.org/10.1594/PANGAEA.745551
- Honnorez, JJ; Mével, C; Honnorez-Guerstein, B-M et al. (1990): (Table 6) Representative analyses of Fe, Cu sulfides of ODP Site 106-649. https://doi.org/10.1594/PANGAEA.745550