The November 12, 1999 Duzce earthquake ruptured a similar to 40-km-long fau
lt segment of the North Anatolian fault system immediately to the east of t
he August 17, 1999 Izmit rupture. We use displacements of 32 sites derived
from GPS measurements immediately before and after the Duzce earthquake to
estimate the geometry and slip distribution of the coseismic rupture. The s
imilar to 51 degrees northward dipping rupture plane, the rake of the slip
vector (average 3.76 +/- 0.04 m right-lateral, 0.76 +/- 0.04 m normal slip)
, and the slip distribution inferred from the GPS data are consistent with
seismic observations and the distribution of surface offsets measured in th
e field. The geodetically determined moment magnitude is M-w = 7.2. The Duz
ce earthquake had the highest slip-to-rupture-length ratio of any historic
earthquake along the North Anatolian fault. This is consistent with the Duz
ce earthquake being a part of a composite rupture with the preceding Izmit
event.