Shear wave splitting along a nascent plate boundary: the North Anatolian Fault Zone

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Biryol C. B., Zandt G., Beck S. L., ÖZACAR A. A., Adiyaman H. E., Gans C. R.

GEOPHYSICAL JOURNAL INTERNATIONAL, cilt.181, sa.3, ss.1201-1213, 2010 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 181 Sayı: 3
  • Basım Tarihi: 2010
  • Doi Numarası: 10.1111/j.1365-246x.2010.04576.x
  • Dergi Adı: GEOPHYSICAL JOURNAL INTERNATIONAL
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.1201-1213
  • Anahtar Kelimeler: Mantle processes, Seismic anisotropy, Continental tectonics: strike-slip and transform, Dynamics of lithosphere and mantle, SAN-ANDREAS FAULT, SEISMIC ANISOTROPY, UPPER-MANTLE, EASTERN TURKEY, MEDITERRANEAN REGION, CENTRAL CALIFORNIA, RECEIVER FUNCTIONS, SUBDUCTION ZONE, COLLISION ZONE, ISPARTA ANGLE
  • Orta Doğu Teknik Üniversitesi Adresli: Evet

Özet

P>The North Anatolian Fault Zone (NAFZ) is a transform structure that constitutes the boundary between the Anatolian Plate to the south and the Eurasia Plate to the north. We analysed the properties of the upper-mantle strain field and mantle anisotropy in the vicinity of NAFZ via splitting of SKS and SKKS phases. We used data from the North Anatolian Fault (NAF) passive seismic experiment. This is the first study that analyses the upper-mantle anisotropy in this region and our results indicate that the observed upper-mantle strain field is uniform underneath the array with consistent NE-SW polarization directions for fast split waves. The measured lag times between the arrivals of the fast and slow split waves varies from 0.5 to 1.6 s for the study area. Smaller lag times are obtained consistently in the eastern part of the array. However, we do not observe any significant variation in either the polarization directions or the delay times across the plate boundary (NAFZ).