CSCSTI 06.01
BISAC NAT010000
BISAC NAT045050
BISAC NAT025000
BISAC NAT045030
BISAC SCI081000
BISAC SCI092000
BISAC SCI020000
BISAC SCI039000
BISAC SOC053000
BISAC TEC060000
KERCH STRAIT IN KAMYSH-BURUN SPIT AREA: HIGH-RESOLUTION SEISMOACOUSTIC APPROACH
V. N. Zin'ko
Centr arheologicheskih issledovaniy «Demetra»
A. S. Zverev
MGU
(geograficheskiy fakul'tet)
M. Fedin
OOO «Yuzhnoberezhnyy centr izyskaniy
Russian Federation
A. A. Porotov
MGU
(geograficheskiy fakul'tet)
V. Myslivec
MGU
(geograficheskiy fakul'tet)
myslivets@yandex.ru, Russian Federation
V. A. Putans
Institut okeanologii im. P.P. Shirshova RAN
Abstract:
The seismoacoustical investigations was made in the western part of the Kerch strait (Azov sea) near Kamysh-Burun spit. The fracture zone with dislocated sedimentary rocks layers and buried erosional surface was revealed to the west of spit. Three seismofacial units was revealed to the east of spit. The first unit was modern sedimentary cover. The second ones has cross-bedding features and was, probably, the part of early generation of Kamysh-Burun spit, which lied to the east of its modern position. The lower border of the second unit is the erosional surface supposed of phanagorian age. The third unit is screened by acoustic shedows in large part.
The seismoacoustical investigations was made in the western part of the Kerch strait (Azov sea) near Kamysh-Burun spit. The fracture zone with dislocated sedimentary rocks layers and buried erosional surface was revealed to the west of spit. Three seismofacial units was revealed to the east of spit. The first unit was modern sedimentary cover. The second ones has cross-bedding features and was, probably, the part of early generation of Kamysh-Burun spit, which lied to the east of its modern position. The lower border of the second unit is the erosional surface supposed of phanagorian age. The third unit is screened by acoustic shedows in large part.
Keywords:
KERCH STRAIT
KERCH STRAIT
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