MUD VOLCANOES AND SHEAR-WAVE IMAGING - AN EXAMPLE 4C TEST LINE IN THE CASPIAN SEA

dc.contributor.author	Probert T.
dc.contributor.author	Bryan R.
dc.contributor.author	Ronen S.
dc.contributor.author	Engelmark F.
dc.contributor.author	Akenteiva E.
dc.contributor.author	Browning G.
dc.contributor.author	Rowson C.
dc.contributor.author	Bakhshiev F.
dc.contributor.author	Kawai N.
dc.contributor.author	Nazarov A.
dc.date.accessioned	2021-03-03T03:56:29Z
dc.date.available	2021-03-03T03:56:29Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=27945250
dc.identifier.citation	SEG Technical Program Expanded Abstracts, 2001, 20, 1, 787-790
dc.identifier.issn	1052-3812
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26174
dc.description.abstract	The general description of a mud volcano is an injection or eruption of mud fluids from a highly pressurized zone to a shallower, lower-pressure zone or eruption to the surface. These features are often associated with gas and fluidized sediments forming complex structures. They are poorly resolved using conventional P-wave seismic imaging and they present a number of challenges for hydrocarbon exploration and development. The benefits from converted-wave methods include imaging through the gas, improved resolution, pore-pressure prediction, and better imaging of complex structures with wide-azimuth geometry.
dc.title	MUD VOLCANOES AND SHEAR-WAVE IMAGING - AN EXAMPLE 4C TEST LINE IN THE CASPIAN SEA
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.