Can Fractures in Soft Sediments Host Significant Quantities of Gas Hydrates?
Thomas McGee, Carol Lutken, J. Robert Woolsey, Rudy Rogers, Jennifer Dearman, Charlotte Brunner, F. Leo Lynch, 2009. "Can Fractures in Soft Sediments Host Significant Quantities of Gas Hydrates?", Natural Gas Hydrates—Energy Resource Potential and Associated Geologic Hazards, T. Collett, A. Johnson, C. Knapp, R. Boswell
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The Gulf of Mexico Hydrate Research Consortium has collected several types of data in and around Mississippi Canyon Lease Block 798 (MC798), anarea of the northern Gulf of Mexico where fine-grained sediment occurs at the sea floor and where hydrates have been sampled. Swath bathymetry, heat-flow measurements, core samples, and subbottom profiles were collected. Hydrate was grown in the laboratory in sediments subsampled from the cores to demonstrate that the surficial sedimentsinMC798 are conducive to hydrate formation. Herein, data are presented and results discussed.
It is postulated that significant quantities of hydrate could form in fine-grained sediments by filling fracture porosity produced by polygonal faulting. Analyses of cores combined with laboratory experiments indicate that conditions in MC798 are conducive to the formation of polygonal faults. Heat-flow measurements indicate that the hydrate stability zone is about 400 m (1312 ft) thick. Its upper 100 ms or so appears on two-dimensional (2-D) subbottom profiles to be fine grained.Small, near-vertical fractures indicated by features called brooms are common there. Thus, it is possible that a polygonal fault system exists in the upper 100 ms (75 m [246 ft] at 1500 m/s [4921 ft/s]). It is acknowledged that 2-D profiles cannot demonstrate this conclusively. Conclusive proof would require a three-dimensional (3-D) data set with sufficient resolution to demonstrate intercon-nectivity among the small faults.
If polygonal faulting exists, gas and water could circulate through the fractures and be exposed to smectite-rich clays, a situation favorable to hydrate formation. X-ray images of pressure cores have documented hydrate accumulation within small, nearly vertical fractures in fine-grained sediments. Thus, it is possible that polygonal fault systems could host significant accumulations of hydrate in the Gulf of Mexico.
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Natural Gas Hydrates—Energy Resource Potential and Associated Geologic Hazards
In September 2004, the American Association of Petroleum Geologists (AAPG) convened a Hedberg Research Conference in Vancouver, British Columbia, Canada titled "Natural Gas Hydrates: Energy Resource Potential and Associated Geologic Hazards." As a continuation of the Hedberg Research Conference in Vancouver, the conveners of the conference and the editors of this Memoir have worked with more than 150 authors and coauthors to prepare this Memoir on gas hydrates. This publication follows the goals of the Hedberg conference; however, the contents of this Memoir were expanded to include all aspects of gas hydrates in nature. This Memoir contains 39 individual contributions, ranging from long topical summaries to shorter focused research papers. This Memoir has been published in two parts, with digital versions of all the complete research papers included on the enclosed CD. The hardcopy portion of the Memoir includes abstracts and several key figures for each of the contributions along with a complete copy of a gas hydrate technical review. The digital portion of this Memoir has been organized into a series of topical sections consisting of review articles, marine gas hydrate papers, and gas hydrate laboratory and modeling studies. Because of the rapidly emerging worldwide interest in gas hydrates, this comprehensive treatise on the geology of gas hydrates will be valuable to both the gas hydrate research community and exploration/development geologists working in arctic and deep marine environments.