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Interseismic Strain Accumulation in the Marmara Sea Region

Department of Geodesy
General Command of Mapping
TR-06100, Ankara, Turkey
eayhan{at}hgk.mil.tr(M.E.A., C.D., O.L., A.K.)
Bundesamt für Kartographie und Geodasie
Richard-Strauss-Allee 11
D-60598 Frankfurt am Main, Germany
(Y.A.)
Geology Department
Istanbul Technical University
Istanbul, Turkey
(A.A.B.)
Marmara Research Center
TUBITAK
Gebze, Turkey
(S.E.)
Kandilli Observatory and Earthquake Research Institute
Bogazici University
Istanbul, Turkey
(H.Ö.)

Manuscript received 30 August 2000.

The Marmara Sea region is deforming along the branches of the North Anatolian Fault (NAF), which is the boundary between the Anatolian and the Eurasian plates. We evaluate Global Positioning System (GPS) measurements performed from 1992 to 1999, up to the 17 August 1999 zmit earthquake, to quantify the interseismic strain accumulation pattern in the Marmara Sea region. We compute interseismic velocities in a frame fixed to the Eurasian plate at 136 GPS points. To compute the frame-independent strain rates, we first smooth the north-south and the east-west velocity components separately to obtain the values at grid nodes, and then we compute directional derivatives and strain rates. Shear-strain rates reveal that the Marmara Sea region is within the plate boundary deformation zone having a width of about 110 km. The largest shear-strain rate accumulation is along the northern branch of the NAF, with maximum shear-strain rate reaching 220 nstrain/yr in the Marmara Sea. We calculate clockwise rigid body rotation rates with a maximum of 10 deg/m.y. along the northern branch while the Anatolian plate rotates anticlockwise. Dilatation rates display adjacent local tensional and compressional areas in the east-west direction within the Marmara Sea. Assuming the uniform simple shear, we compute the NAF slip rates vary between 11 and 26 mm/yr, with a minimum around zmit, and increase east and west of zmit.

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