Wide-angle seismic data reveal sedimentary and crustal structure of the Eastern Black Sea

R. A. Edwards; C. L. Scott; D. J. Shillington; T. A. Minshull; P. J. Brown; N. J. White

doi:10.1190/1.3236375

Wide-angle seismic data reveal sedimentary and crustal structure of the Eastern Black Sea

R. A. Edwards
, C. L. Scott
, D. J. Shillington
, T. A. Minshull
, P. J. Brown
, N. J. White

Research output: Contribution to journal › Article › peer-review

8 Scopus citations

Abstract

Wide-angle seismic data from the Eastern Black Sea have been used to determine the geological structure of the sediments, the entire crust, and upper mantle. Data were acquired using a combination of ocean-bottom seismometers (OBS), land seismometers, and a marine air-gun source, providing refracted and reflected energy recorded to offsets in excess of 100 km.

Original language	English (US)
Pages (from-to)	1056-1065
Number of pages	10
Journal	Leading Edge
Volume	28
Issue number	9
DOIs	https://doi.org/10.1190/1.3236375
State	Published - Sep 1 2009
Externally published	Yes

ASJC Scopus subject areas

Geophysics
Geology

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10.1190/1.3236375

Cite this

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abstract = "Wide-angle seismic data from the Eastern Black Sea have been used to determine the geological structure of the sediments, the entire crust, and upper mantle. Data were acquired using a combination of ocean-bottom seismometers (OBS), land seismometers, and a marine air-gun source, providing refracted and reflected energy recorded to offsets in excess of 100 km.",

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AU - Brown, P. J.

AU - White, N. J.

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N2 - Wide-angle seismic data from the Eastern Black Sea have been used to determine the geological structure of the sediments, the entire crust, and upper mantle. Data were acquired using a combination of ocean-bottom seismometers (OBS), land seismometers, and a marine air-gun source, providing refracted and reflected energy recorded to offsets in excess of 100 km.

AB - Wide-angle seismic data from the Eastern Black Sea have been used to determine the geological structure of the sediments, the entire crust, and upper mantle. Data were acquired using a combination of ocean-bottom seismometers (OBS), land seismometers, and a marine air-gun source, providing refracted and reflected energy recorded to offsets in excess of 100 km.

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Wide-angle seismic data reveal sedimentary and crustal structure of the Eastern Black Sea

Abstract

ASJC Scopus subject areas

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