V.A. Viginsky (
Turbidities in late
Miocene-Pliocene sediments of
Seismic studies viewing have allowed
revealing in a stratas above Maycop of a Tuapse trough (
Lateral correlation of seismic
records anomalies has allowed mapping position of Meotitian-Pontian turbidity
tongues. There are correspondence of late Miocene turbidity channels with
canyons existing in a modern contour of
Detected bodies of Meotitian-Pontian
turbidity currents are characterized in following arguments: channels length
(including fan complexes) - ~ 40 miles, channels length to a bifurcation zone -
~ 23 miles. Near parameters has a Miocene deepwater turbidity sand body of
basin
The morphological similarity of
Black Sea Meotitian-Pontian turbidity tongue bodies with Cingoz formation
deepwater turbidity sand body of south
Lithological composition of turbidity channels fan parts
("tongue" facies) and "lobes" facies can be described as
largely sand, according to the available data of field researchings.
2003 AAPG
International Conference and Exhibition (