Geochemical constraints on the distribution of gas hydrates in the Gulf of Mexico
Links
- More information: Publisher Index Page (via DOI)
- Download citation as: RIS | Dublin Core
Abstract
Gas hydrates are common within near-seafloor sediments immediately surrounding fluid and gas venting sites on the continental slope of the northern Gulf of Mexico. However, the distribution of gas hydrates within sediments away from the vents is poorly documented, yet critical for gas hydrate assessments. Porewater chloride and sulfate concentrations, hydrocarbon gas compositions, and geothermal gradients obtained during a porewater geochemical survey of the northern Gulf of Mexico suggest that the lack of bottom simulating reflectors in gas-rich areas of the gulf may be the consequence of elevated porewater salinity, geothermal gradients, and microbial gas compositions in sediments away from fault conduits.
Study Area
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | Geochemical constraints on the distribution of gas hydrates in the Gulf of Mexico |
Series title | Geo-Marine Letters |
DOI | 10.1007/s00367-005-0001-3 |
Volume | 25 |
Issue | 5 |
Year Published | 2005 |
Language | English |
Publisher | Springer |
Contributing office(s) | Woods Hole Coastal and Marine Science Center |
Description | 8 p. |
First page | 273 |
Last page | 280 |
Other Geospatial | Gulf of Mexico |
Google Analytic Metrics | Metrics page |