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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
AAPG FOUNDATION PRATT CONFERENCE: PETROLEUM PROVINCES,
21st CENTURY
January 12-15, 2000
San Diego, California
Gas hydrates occur in sedimentary deposits under conditions of pressure
and temperature present in permafrost regions and beneath the sea in outer
continental margins. The combined information from Arctic gas-hydrate studies
shows that, in permafrost regions, gas hydrates may exist at subsurface
depths ranging from about 130 to 2,000 m. The presence of gas hydrates
in offshore continental margins has been inferred mainly from anomalous
seismic reflectors known as bottom-simulating reflectors, that have been
mapped at depths below the sea floor ranging from about 100 to 1,100 m.
Current estimates of the amount of gas in the world's marine and permafrost
gas hydrate accumulations are in rough accord at about 20,000 trillion
cubic meters.
Gas hydrate as an energy commodity is often grouped with other unconventional
hydrocarbon resources. In most cases, the evolution of a non-producible
unconventional resource to a producible energy resource has relied on significant
capital investment and technology development. To evaluate the energy resource
potential of gas hydrates, will also require the support of sustained research
and development programs.
Despite the fact that relatively little is known about the ultimate
resource potential of natural gas hydrates, it is certain that gas hydrates
are a vast storehouse of natural gas and significant technical challenges
need to be met before this enormous resource can be considered an economically
producible reserve.