Kinematics of the Mw=7.2, 12 November 1999, Duzce, Turkey earthquake

被引:44
作者
Ayhan, ME [1 ]
Bürgmann, R
McClusky, S
Lenk, O
Aktug, B
Herece, E
Reilinger, RE
机构
[1] Gen Command Mapping, Dept Geodesy, Ankara, Turkey
[2] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA
[3] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
[4] Gen Directorate Min Res & Explorat, Dept Geol, Ankara, Turkey
关键词
D O I
10.1029/2000GL011851
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The November 12, 1999 Duzce earthquake ruptured a similar to 40-km-long fault segment of the North Anatolian fault system immediately to the east of the 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 similar 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 the field. The geodetically determined moment magnitude is M-w = 7.2. The Duzce earthquake had the highest slip-to-rupture-length ratio of any historic earthquake along the North Anatolian fault. This is consistent with the Duzce earthquake being a part of a composite rupture with the preceding Izmit event.
引用
收藏
页码:367 / 370
页数:4
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