Deep‐slab fluids fuel extremophilic Archaea on a Mariana forearc serpentinite mud volcano: Ocean Drilling Program Leg 195
- 14 November 2003
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 4 (11)
- https://doi.org/10.1029/2003gc000588
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Paleogeographic reconstruction and origin of the Philippine SeaPublished by Elsevier ,2003
- A hydrogen-based subsurface microbial community dominated by methanogensNature, 2002
- Metamorphic devolatilization of subducted oceanic metabasalts: implications for seismicity, arc magmatism and volatile recyclingPublished by Elsevier ,2001
- Comparative Analysis of Methane-Oxidizing Archaea and Sulfate-Reducing Bacteria in Anoxic Marine SedimentsApplied and Environmental Microbiology, 2001
- Significance of serpentine mud volcanism in convergent marginsPublished by Geological Society of America ,2000
- Thermal and dynamical evolution of the upper mantle in subduction zonesJournal of Geophysical Research, 1997
- Blueschist metamorphism in an active subduction zoneNature, 1993
- Fluid Processes in Subduction ZonesScience, 1990
- Origin and emplacement of Mariana forearc seamountsGeology, 1985
- Structure and Tectonics of the Mariana Arc and Fore-Arc: Drillsite Selection SurveysPublished by International Ocean Discovery Program (IODP) ,1982