Published January 1, 2009 | Version v1
Journal article Open

Moho, crustal architecture and deep deformation under the North Marmara Trough, from the SEISMARMARA Leg 1 offshore-onshore reflection-refraction survey

  • 1. Inst Phys Globe, UMR 7154, Dept Seismol, F-75252 Paris 05, France
  • 2. Univ Pau & Pays Adour, F-64010 Pau, France
  • 3. ITU, Seismol Lab, Istanbul, Turkey
  • 4. Inst Seismol & Volcanol, Sapporo, Hokkaido, Japan
  • 5. TUBITAK MAM, Marmara Res Ctr, Gebze, Turkey

Description

Understanding further the nature and evolution at lithospheric scale of the Sea of Marmara on the North Anatolian Fault needs constraints on the deep crustal and Mono spatial variation. This has been probed here with offshore-onshore and OBS, Ocean Bottom Seismometer refraction seismics, in addition to coincident MCS, marine multichannel reflection seismic profiles over the whole North Marmara Trough.

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