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) |
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Pages (from-to) | 1056-1065 |
Number of pages | 10 |
Journal | Leading Edge |
Volume | 28 |
Issue number | 9 |
DOIs | |
State | Published - Sep 1 2009 |
Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geology