Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Interpretation of marine magnetic anomalies. Part II. Analysis of the new method and algorithm based on the least squares method. / Ivanov, S. A.; Merkur'ev, S. A.
в: Geomagnetism and Aeronomy, Том 54, № 4, 07.2014, стр. 530-536.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Interpretation of marine magnetic anomalies. Part II. Analysis of the new method and algorithm based on the least squares method
AU - Ivanov, S. A.
AU - Merkur'ev, S. A.
PY - 2014/7
Y1 - 2014/7
N2 - In this work, the problem of interpreting linear marine magnetic anomalies in the context of the spreading model is considered. Based on the least squares method, a new algorithm for determining the position of direct and reverse polarity blocks is proposed. The global minimum of the residual is found by a combination of the multistart and Monte Carlo methods. Using an example of a field of three blocks perturbed by a normal noise, it is shown that the method yields an error close to the minimum possible. Using a model constructed by the inversion scale, it is revealed that the proposed algorithm allows one to find positions of block boundaries of the field without noise with a higher accuracy determined in fact by the computation time.
AB - In this work, the problem of interpreting linear marine magnetic anomalies in the context of the spreading model is considered. Based on the least squares method, a new algorithm for determining the position of direct and reverse polarity blocks is proposed. The global minimum of the residual is found by a combination of the multistart and Monte Carlo methods. Using an example of a field of three blocks perturbed by a normal noise, it is shown that the method yields an error close to the minimum possible. Using a model constructed by the inversion scale, it is revealed that the proposed algorithm allows one to find positions of block boundaries of the field without noise with a higher accuracy determined in fact by the computation time.
UR - http://www.scopus.com/inward/record.url?scp=84904722072&partnerID=8YFLogxK
U2 - 10.1134/S0016793214040197
DO - 10.1134/S0016793214040197
M3 - Article
AN - SCOPUS:84904722072
VL - 54
SP - 530
EP - 536
JO - Geomagnetism and Aeronomy
JF - Geomagnetism and Aeronomy
SN - 0016-7932
IS - 4
ER -
ID: 51323601