MULTIPLE REFLECTIONS IN A WATER LAYER AND THEIR EFFECT ON THE RELIABILITY OF DATA INTERPRETATION IN SEISMIC MARINE SURVEYING

Marine seismic investigations by the reflection method have been widely used in the USSR and abroad in recent years. The entry of marine seismic surveying into deep-sea water areas permitted conducting regional investigations of regions covered by a thick layer of water. A real possibility has appea...

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Bibliographic Details
Main Author: Kogan,L. I.
Other Authors: MICHIGAN UNIV ANN ARBOR INST OF SCIENCE AND TECHNOLOGY
Format: Text
Language:English
Published: 1970
Subjects:
Physical and Dynamic Oceanography
Geology
Geochemistry and Mineralogy
(*MARINE GEOLOGY
OCEAN BOTTOM TOPOGRAPHY)
(*ECHO RANGING
REFLECTION)
HYDROGRAPHIC SURVEYING
UNDERWATER SOUND
TNT
SEISMOMETERS
PIEZOELECTRIC GAGES
DEPOSITS
BALTIC SEA
ARCTIC OCEAN
BLACK SEA
KARA SEA
USSR
BARENTS SEA
CASPIAN SEA
TRANSLATIONS
Arctic
Arctic Ocean
Barents Sea
Kara Sea
Gulf of Ob
Online Access:http://www.dtic.mil/docs/citations/AD0713721
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0713721
Description
Summary:Marine seismic investigations by the reflection method have been widely used in the USSR and abroad in recent years. The entry of marine seismic surveying into deep-sea water areas permitted conducting regional investigations of regions covered by a thick layer of water. A real possibility has appeared of solving complex geological problems under the conditions of the deep marine basins. Regional seismic investigations began to be conducted regularly in the USSR in 1956 and are being conducted at the present time in the Barents, Baltic Azov, Black, Caspian and Kara (in the Gulf of Ob and Yenisei Bay) Seas. (Author) Trans. of unidentified Russian language article.

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