Research on anisotropic parameters by synthetic seismogram

Based on the extensive-dilatancy anisotropy theory, the method of synthetic seismogram is used to estimate the anisotropic parameters. The advantages of the method lie in that it avoids the singularity resolution and saves calculation time of computer by using the eigenvalue and eigenvector analytic...

Full description

Bibliographic Details
Published in:Earthquake science, Vol. 18, No. 2 (2005), p. 196-205
Main Author: Xiao-ping, Fan
Other Involved Persons: Qing-he, Li ; Yang, Cong-jie
Format: electronic Article
Language:English
ISSN:1867-8777
Item Description:Foundation item: National Natural Science Foundation of China (D4007410) and Joint Seismological Science Foundation of China (603006).
Physical Description:Online-Ressource
DOI:10.1007/s11589-005-0067-z
Subjects:
QR Code: Show QR Code
LEADER 02037nma a2200409 c 4500
001 SPR040241084
003 DE-601
005 20150323184646.0
007 cr uuu---uuuuu
008 150314s2005 000 0 eng d
024 7 |a 10.1007/s11589-005-0067-z  |2 doi 
024 8 |a s11589-005-0067-z 
035 |a s11589-005-0067-z 
040 |b ger  |c GBVCP 
041 0 |a eng 
100 1 |a Xiao-ping, Fan 
245 1 0 |a Research on anisotropic parameters by synthetic seismogram  |h Elektronische Ressource 
300 |a Online-Ressource 
500 |a Foundation item: National Natural Science Foundation of China (D4007410) and Joint Seismological Science Foundation of China (603006). 
520 |a Based on the extensive-dilatancy anisotropy theory, the method of synthetic seismogram is used to estimate the anisotropic parameters. The advantages of the method lie in that it avoids the singularity resolution and saves calculation time of computer by using the eigenvalue and eigenvector analytical expressions of Christoffel equation, at the same time, the result is tested by coherence function. The test result reveals there exists a fine linear relation between original records and synthetic records, indicating the anisotropic parameters estimated by synthetic seismogram can reflect and describe the anisotropic characteristics of the given region medium. 
611 2 7 |a OriginalPaper  |2 gnd 
650 7 |a anisotropy  |2 gnd 
650 7 |a synthetic seismogram  |2 gnd 
650 7 |a anisotropy parameter  |2 gnd 
689 0 0 |A f  |a OriginalPaper 
689 0 |5 DE-601 
689 1 0 |A s  |a anisotropy 
689 1 1 |A s  |a synthetic seismogram 
689 1 2 |A s  |a anisotropy parameter 
689 1 |5 DE-601 
700 1 |a Qing-he, Li 
700 1 |a Yang, Cong-jie 
773 0 8 |i in  |t Earthquake science  |d Berlin : Springer  |g Vol. 18, No. 2 (2005), p. 196-205  |q 18:2<196-205  |w (DE-601)SPR040229165  |x 1867-8777 
856 4 1 |u http://dx.doi.org/10.1007/s11589-005-0067-z  |3 Volltext 
912 |a GBV_SPRINGER 
951 |a AR 
952 |d 18  |j 2005  |e 2  |c 03  |h 196-205