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Interpretation of marine magnetic anomalies. Part I. A survey of existing methods and analysis of the analytic signal method. / Ivanov, S. A.; Merkur'ev, S. A.

In: Geomagnetism and Aeronomy, Vol. 54, No. 3, 05.2014, p. 388-396.

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@article{251562caeddf4b12a67f21d59047f8d7,
title = "Interpretation of marine magnetic anomalies. Part I. A survey of existing methods and analysis of the analytic signal method",
abstract = "In this work, the problem of interpreting linear marine magnetic anomalies in the context of the spreading model is considered. Analysis and a comparison of the methods proposed earlier for solving this problem are carried out and the analytic signal method is considered in detail. In terms of a simplest example, it is shown that the AS method has significant restrictions associated primarily with the size and/or occurrence depth of the bodies.",
author = "Ivanov, {S. A.} and Merkur'ev, {S. A.}",
year = "2014",
month = may,
doi = "10.1134/S0016793214030086",
language = "English",
volume = "54",
pages = "388--396",
journal = "Geomagnetism and Aeronomy",
issn = "0016-7932",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Interpretation of marine magnetic anomalies. Part I. A survey of existing methods and analysis of the analytic signal method

AU - Ivanov, S. A.

AU - Merkur'ev, S. A.

PY - 2014/5

Y1 - 2014/5

N2 - In this work, the problem of interpreting linear marine magnetic anomalies in the context of the spreading model is considered. Analysis and a comparison of the methods proposed earlier for solving this problem are carried out and the analytic signal method is considered in detail. In terms of a simplest example, it is shown that the AS method has significant restrictions associated primarily with the size and/or occurrence depth of the bodies.

AB - In this work, the problem of interpreting linear marine magnetic anomalies in the context of the spreading model is considered. Analysis and a comparison of the methods proposed earlier for solving this problem are carried out and the analytic signal method is considered in detail. In terms of a simplest example, it is shown that the AS method has significant restrictions associated primarily with the size and/or occurrence depth of the bodies.

UR - http://www.scopus.com/inward/record.url?scp=84901917251&partnerID=8YFLogxK

U2 - 10.1134/S0016793214030086

DO - 10.1134/S0016793214030086

M3 - Article

AN - SCOPUS:84901917251

VL - 54

SP - 388

EP - 396

JO - Geomagnetism and Aeronomy

JF - Geomagnetism and Aeronomy

SN - 0016-7932

IS - 3

ER -

ID: 51323409