Fluid seepage at the continental margin offshore Costa Rica and southern Nicaragua

Online Access: Get full text
doi: 10.1029/2008GC001978
Author(s): Sahling, Heiko; Masson, Douglas G.; Ranero, César R.; Hühnerbach, Veit; Weinrebe, Wilhelm; Klaucke, Ingo; Bürk, Dietmar; Brückmann, Warner; Suess, Erwin
Author Affiliation(s): Primary:
University of Bremen, Research Centre Ocean Margins, Bremen, Federal Republic of Germany
Other:
National Oceanography Centre Southampton, United Kingdom
CSIC, Instituto de Ciencias del Mar, Spain
University of Kiel, Federal Republic of Germany
GEOMAR, Federal Republic of Germany
Volume Title: Geochemistry, Geophysics, Geosystems - G<sup>3</sup>
Source: Geochemistry, Geophysics, Geosystems - G>3`, 9(5). Publisher: American Geophysical Union and The Geochemical Society, United States. ISSN: 1525-2027
Note: In English. 57 refs.; illus., incl. 1 table, sketch map
Summary: A systematic search for methane-rich fluid seeps at the seafloor was conducted at the Pacific continental margin offshore southern Nicaragua and northern central Costa Rica, a convergent margin characterized by subduction erosion. More than 100 fluid seeps were discovered using a combination of multibeam bathymetry, side-scan sonar imagery, TV-sled observations, and sampling. This corresponds, on average, to a seep site every 4 km along the continental slope. In the northwestern part of the study area, subduction of oceanic crust formed at the East Pacific Rise is characterized by pervasive bending-induced faulting of the oceanic plate and a relatively uniform morphology of the overriding continental margin. Seepage at this part of the margin typically occurs at approximately cone-shaped mounds 50-100 m high and up to 1 km wide at the base. Over 60 such mounds were identified on the 240 km long margin segment. Some normal faults also host localized seepage. In contrast, in the southeast, the 220 km long margin segment overriding the oceanic crust formed at the Cocos-Nazca Spreading Centre has a comparatively more irregular morphology caused mainly by the subduction of ridges and seamounts sitting on the oceanic plate. Over 40 seeps were located on this part of the margin. This margin segment with irregular morphology exhibits diverse seep structures. Seeps are related to landslide scars, seamount-subduction related fractures, mounds, and faults. Several backscatter anomalies in side-scan images are without apparent relief and are probably related to carbonate precipitation. Detected fluid seeps are not evenly distributed across the margin but occur in a roughly margin parallel band centered 28±7 km landward of the trench. This distribution suggests that seeps are possibly fed to fluids rising from the plate boundary along deep-penetrating faults through the upper plate.
Year of Publication: 2008
Research Program: ODP Ocean Drilling Program
Key Words: 07 Marine Geology and Oceanography; 20 Geophysics, Applied; Acoustical methods; Alvin; Bathymetry; Central America; Continental margin; Costa Rica; East Pacific; Fluid phase; Gas seeps; Geophysical methods; Geophysical profiles; Geophysical surveys; Leg 170; Leg 205; Marine methods; Nicaragua; Nicoya Peninsula; North Pacific; Northeast Pacific; Ocean Drilling Program; Ocean floors; Offshore; Pacific Ocean; Reflection methods; Seepage; Seismic methods; Seismic profiles; Sonar methods; Southern Nicaragua; Subduction zones; Submersibles; Surveys; Three-dimensional models
Coordinates: N080000 N110000 W0830000 W0880000
Record ID: 2010006047
Copyright Information: GeoRef, Copyright 2017 American Geosciences Institute. Reference includes data supplied by, and/or abstract, Copyright, American Geophysical Union, Washington, DC, United States