Woolsey Mound, a 1km-diameter carbonate-gas hydrate complex in the northern Gulf of Mexico, is the site of the Gulf’s only seafloor monitoring station-observatory in its only research reserve, Mississippi Canyon 118. Active venting, outcropping hydrate, and a thriving chemosynthetic community recommend the site for study. Since 2005, the Gulf of Mexico Hydrates Research Consortium has been conducting multidisciplinary studies to 1. Characterize the site, 2. Establish a facility for real-time monitoring-observing of gas hydrates in a natural setting, 3. Study the effects of gas hydrates on seafloor stability, 4. Establish fluid migration routes and estimates of fluid-flux at the site, 5. Establish the interrelationships between the organism...
A deep-sea time-lapse camera and several temperature probes were deployed on the Gulf of Mexico cont...
The main objectives of the project were to monitor, characterize, and quantify in situ the rates of ...
Due to their favorable P-T conditions and organic-rich deposits, sub-seafloor sediments in the north...
A permanent observatory has been installed on the seafloor at Federal Lease Block, Mississippi Canyo...
Woolsey Mound, a carbonate/hydrate complex of cold seeps, vents, and seafloor pockmarks in Mississip...
An active methane vent (Woolsey Mound) in Mississippi Canyon Block 118 (MC118), Gulf of Mexico, has ...
This paper is not subject to U.S. copyright. The definitive version was published in Marine and Pet...
Located on the continental slope in 900m of water, Woolsey Mound dominates seafloor morphology at Mi...
The gas hydrates research Consortium (HRC), established and administered at the University if Missis...
This paper is not subject to U.S. copyright. The definitive version was published in Marine and Pet...
The Gulf of Mexico Hydrates Research Consortium (GOM-HRC) was established in 1999 to assemble leader...
A Consortium, designed to assemble leaders in gas hydrates research, has been established at the Uni...
The Gulf of Mexico Hydrates Research Consortium (GOM-HRC) was established in 1999 to assemble leader...
The Gulf of Mexico Hydrates Research Consortium (GOM-HRC) was established in 1999 to assemble leader...
Cold seeps are areas where methane is transferred from the lithosphere into the hydrosphere, account...
A deep-sea time-lapse camera and several temperature probes were deployed on the Gulf of Mexico cont...
The main objectives of the project were to monitor, characterize, and quantify in situ the rates of ...
Due to their favorable P-T conditions and organic-rich deposits, sub-seafloor sediments in the north...
A permanent observatory has been installed on the seafloor at Federal Lease Block, Mississippi Canyo...
Woolsey Mound, a carbonate/hydrate complex of cold seeps, vents, and seafloor pockmarks in Mississip...
An active methane vent (Woolsey Mound) in Mississippi Canyon Block 118 (MC118), Gulf of Mexico, has ...
This paper is not subject to U.S. copyright. The definitive version was published in Marine and Pet...
Located on the continental slope in 900m of water, Woolsey Mound dominates seafloor morphology at Mi...
The gas hydrates research Consortium (HRC), established and administered at the University if Missis...
This paper is not subject to U.S. copyright. The definitive version was published in Marine and Pet...
The Gulf of Mexico Hydrates Research Consortium (GOM-HRC) was established in 1999 to assemble leader...
A Consortium, designed to assemble leaders in gas hydrates research, has been established at the Uni...
The Gulf of Mexico Hydrates Research Consortium (GOM-HRC) was established in 1999 to assemble leader...
The Gulf of Mexico Hydrates Research Consortium (GOM-HRC) was established in 1999 to assemble leader...
Cold seeps are areas where methane is transferred from the lithosphere into the hydrosphere, account...
A deep-sea time-lapse camera and several temperature probes were deployed on the Gulf of Mexico cont...
The main objectives of the project were to monitor, characterize, and quantify in situ the rates of ...
Due to their favorable P-T conditions and organic-rich deposits, sub-seafloor sediments in the north...