The structure of the crust in TESZ area by kriging interpolation

Czasopismo : Acta Geophysica
Tytuł artykułu : The structure of the crust in TESZ area by kriging interpolation

Autorzy :
Yamasaki, K.
Department of Earth and Planetary Sciences, Faculty of Science, Kobe University, Nada, Kobe, Japan, yk2000@kobe-u.ac.jp,
Teisseyre, R.
Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, rt@igf.edu.pl,
Li, C.
School of Computer Engineering and Science, Shanghai University, Shanghai, China, jyyin@staff.shu.edu.cn,
Majdański, M.
Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, mmajd@igf.edu.pl,
Abstrakty : A precise 3D model of the crust is necessary to start any tectonic or geodynamic interpretation. It is also essential for seismic interpretations of structures lying below as well as for correct analysis of shallow structures using reflection seismics. During the last decades, a number of wide-angle refraction experiments were performed on the territory of central and eastern Europe (POLONAISE’97, CELEBRATION 2000, SUDETES 2003), resulting in many high quality 2D models. It is an interesting and complicated transition zone between Precambrian and Palaeozoic Platforms. This paper presents 3D model of the velocity distribution in the crust and upper mantle interpolated from 2D models of the structure along 33 profiles. The obtained model extends to a depth of 50 km and accurately describes the main features of the crustal structures of Poland and surrounding areas. Different interpolation techniques (Kriging, linear) are compared to assure maximum precision. The final model with estimated uncertainty is an interesting reference of the area for other studies.

Słowa kluczowe : crustal structure, TESZ, interpolation, Kriging,
Wydawnictwo : Instytut Geofizyki PAN
Rocznik : 2012
Numer : Vol. 60, no. 1
Strony : 59 – 75
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DOI :
Cytuj : Yamasaki, K. ,Teisseyre, R. ,Li, C. ,Majdański, M. , The structure of the crust in TESZ area by kriging interpolation. Acta Geophysica Vol. 60, no. 1/2012
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