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dc.contributor.authorRanero, César R.-
dc.contributor.authorGrevemeyer, Ingo-
dc.contributor.authorSahling, Heiko-
dc.contributor.authorBarckhausen, Udo-
dc.contributor.authorHensen, C.-
dc.contributor.authorWallmann, K.-
dc.contributor.authorWeinrebe, Wilhelm-
dc.contributor.authorVannucchi, P.-
dc.contributor.authorVon Huene, Roland-
dc.contributor.authorMcIntosh, Kirk D.-
dc.date.issued2008-03-11-
dc.identifier.citationGeochemistry, geophysics, geosystems 9(3): Q03S04 (2008)en_US
dc.identifier.issn1525-2027-
dc.identifier.uri10261/25365-
dc.description18 pages, 6 figuresen_US
dc.description.abstractFluid distribution in convergent margins is by most accounts closely related to tectonics. This association has been widely studied at accretionary prisms, but at half of the Earth's convergent margins, tectonic erosion grinds down overriding plates, and here fluid distribution and its relation to tectonics remain speculative. Here we present a new conceptual model for the hydrological system of erosional convergent margins. The model is based largely on new data and recently published observations from along the Middle America Trench offshore Nicaragua and Costa Rica, and it is consistent with observations from other erosional margins. The observations indicate that erosional margins possess previously unrecognized distinct hydrogeological systems: Most fluid contained in the sediment pores and liberated by early dehydration reactions drains from the plate boundary through a fractured upper plate to seep at the seafloor across the slope, rather than migrating along the décollement toward the deformation front as described for accretionary prisms. The observations indicate that the relative fluid abundance across the plate-boundary fault zone and fluid migration influence long-term tectonics and the transition from aseismic to seismogenic behavior. The segment of the plate boundary where fluid appears to be more abundant corresponds to the locus of long-term tectonic erosion, where tectonic thinning of the overriding plate causes subsidence and the formation of the continental slope. This correspondence between observations indicates that tectonic erosion is possibly linked to the migration of overpressured fluids into the overriding plate. The presence of overpressured fluids at the plate boundary is compatible with the highest flow rates estimated at slope seeps. The change from aseismic to seismogenic behavior along the plate boundary of the erosional margin begins where the amount of fluid at the fault declines with depth, indicating a control on interplate earthquakes. A previously described similar observation along accreting plate boundaries strongly indicates that fluid abundance exerts a first-order control on interplate seismogenesis at all types of subduction zones. We hypothesize that fluid depletion with depth increases grain-to-grain contact, increasing effective stress on the fault, and modifies fault zone architecture from a thick fault zone to a narrower zone of localized slipen_US
dc.description.sponsorshipData presented in this work were collected during Sonne cruises 76, 81, 107, 144, 163 and 173 financed by the German BMBF, Meteor cruise 54 financed by the German DFG, BGR99 cruise by the Bundesanstalt für Geowissenschaften and Rohstoffe, and Ewing cruise 0004 financed by NSFen_US
dc.language.isoengen_US
dc.publisherAmerican Geophysical Unionen_US
dc.rightsopenAccessen_US
dc.subjectSubduction zonesen_US
dc.subjectTectonic erosionen_US
dc.subjectSeismogenesisen_US
dc.subjectFluid flowen_US
dc.titleHydrogeological system of erosional convergent margins and its influence on tectonics and interplate seismogenesisen_US
dc.typeartículoen_US
dc.identifier.doi10.1029/2007GC001679.-
dc.description.peerreviewedPeer revieweden_US
dc.relation.publisherversionhttp://dx.doi.org/10.1029/2007GC001679en_US
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