Data report: Stable isotope compositions of dissolved inorganic carbon, methane, sulfate, and sulfide in pore water from the South Chamorro serpentinite mud volcano, Mariana subduction complex

Proceedings of the Ocean Drilling Program: Scientific Results

Volumn 195, Issue , 2006, Pages 1-12

  Komor, Stephen C ^a   Mottl, Michael J ^b  

^a University of Hawaii at Manoa ^*  (United States)

^b UNIVERSITY OF HAWAII   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

DISSOLVED INORGANIC CARBON; ISOTOPIC COMPOSITION; METHANE; OCEAN DRILLING PROGRAM; OXYGEN; SERPENTINITE; SULFATE; SULFIDE; SULFUR; VOLCANO;

MARIANA ARC; PACIFIC OCEAN; SOUTH CHAMORRO SEAMOUNT;

EID: 33747489629     PISSN: 08845891     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (4)

1. Fryer, P., Lockwood, J.P., Becker, N., Phipps, S., and Todd, C.S., 2000. Significance of serpentine mud volcanism in convergent margins. Spec. Pap. - Geol. Soc. Am., 349:35-51.
2. Fryer, P., Wheat, C.G., and Mottl, M.J., 1999. Mariana blueschist mud volcanism: implications for conditions within the subduction zone. Geology, 27:103-106.
3. Mottl, M.J., Komor, S.C., Fryer, P., and Moyer, C.L., 2003. Deep-slab fluids fuel extremophilic Archaea on a Mariana forearc serpentinite mud volcano: Ocean Drilling Program Leg 195. Geochem., Geophys., Geosyst., 4. doi:10.1029/2003GC000588
4. Parkhurst, D.L., and Appelo, C.A.J., 1999. Users guide to PHREEQC (version 2) - Water-Resources Investigations Report 99-4259, Denver.