Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters

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Standard

Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters. / Xu, Zhengwei; Zou, Guangui; Wei, Qianqian; Tian, Junqi; Yuan, Hemin.

I: Geophysical Journal International, Bind 224, Nr. 2, 01.02.2021, s. 1344-1359.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Xu, Z, Zou, G, Wei, Q, Tian, J & Yuan, H 2021, 'Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters', Geophysical Journal International, bind 224, nr. 2, s. 1344-1359. https://doi.org/10.1093/gji/ggaa518

APA

Xu, Z., Zou, G., Wei, Q., Tian, J., & Yuan, H. (2021). Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters. Geophysical Journal International, 224(2), 1344-1359. https://doi.org/10.1093/gji/ggaa518

Vancouver

Xu Z, Zou G, Wei Q, Tian J, Yuan H. Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters. Geophysical Journal International. 2021 feb. 1;224(2):1344-1359. https://doi.org/10.1093/gji/ggaa518

Author

Xu, Zhengwei ; Zou, Guangui ; Wei, Qianqian ; Tian, Junqi ; Yuan, Hemin. / Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters. I: Geophysical Journal International. 2021 ; Bind 224, Nr. 2. s. 1344-1359.

Bibtex

@article{09e467d071b14116b54dedcc6517b6c3,
title = "Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters",
abstract = "This paper develops a minimum-support focusing stabilizer to perform a joint inversion of the vertical components of gravity and magnetic data using fuzzy c-means clustering (FCM) with the regularized Newton method in a space of weighted parameters. Not only does this joint inversion technology arrive at the conditionally well-posed traditional potential field inversion, but it also increases the structural correlation between multiple inverted models. The FCM and the focusing stabilizer make it possible to balance the convergence of the data space (D) and the model space (M), guiding multimodal geophysical parameters toward assigned petrophysical values, which makes the results more stable and realistic. Two model studies are presented to illustrate the method, a simple synthetic model with two rectangular bodies in a homogenous background and a realistic model of the Volcanogenic Massive Sulfide (VMS) deposits in northeastern New Brunswick, Canada. These models demonstrate that the new focusing joint inversion algorithm produces better images than traditional methods because the FCM function uses the structural correlation of density contrast and magnetic susceptibility as constraints. ",
keywords = "Gravity anomalies and Earth structure, Joint inversion, Magnetic anomalies: modelling and interpretation, Persistence, memory, correlations, clustering",
author = "Zhengwei Xu and Guangui Zou and Qianqian Wei and Junqi Tian and Hemin Yuan",
note = "Publisher Copyright: {\textcopyright} 2021 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society.",
year = "2021",
month = feb,
day = "1",
doi = "10.1093/gji/ggaa518",
language = "English",
volume = "224",
pages = "1344--1359",
journal = "Geophysical Journal International",
issn = "0956-540X",
publisher = "Oxford University Press",
number = "2",

}

RIS

TY - JOUR

T1 - Focusing joint inversion of gravity and magnetic data using a clustering stabilizer in a space of weighted parameters

AU - Xu, Zhengwei

AU - Zou, Guangui

AU - Wei, Qianqian

AU - Tian, Junqi

AU - Yuan, Hemin

N1 - Publisher Copyright: © 2021 The Author(s). Published by Oxford University Press on behalf of The Royal Astronomical Society.

PY - 2021/2/1

Y1 - 2021/2/1

N2 - This paper develops a minimum-support focusing stabilizer to perform a joint inversion of the vertical components of gravity and magnetic data using fuzzy c-means clustering (FCM) with the regularized Newton method in a space of weighted parameters. Not only does this joint inversion technology arrive at the conditionally well-posed traditional potential field inversion, but it also increases the structural correlation between multiple inverted models. The FCM and the focusing stabilizer make it possible to balance the convergence of the data space (D) and the model space (M), guiding multimodal geophysical parameters toward assigned petrophysical values, which makes the results more stable and realistic. Two model studies are presented to illustrate the method, a simple synthetic model with two rectangular bodies in a homogenous background and a realistic model of the Volcanogenic Massive Sulfide (VMS) deposits in northeastern New Brunswick, Canada. These models demonstrate that the new focusing joint inversion algorithm produces better images than traditional methods because the FCM function uses the structural correlation of density contrast and magnetic susceptibility as constraints.

AB - This paper develops a minimum-support focusing stabilizer to perform a joint inversion of the vertical components of gravity and magnetic data using fuzzy c-means clustering (FCM) with the regularized Newton method in a space of weighted parameters. Not only does this joint inversion technology arrive at the conditionally well-posed traditional potential field inversion, but it also increases the structural correlation between multiple inverted models. The FCM and the focusing stabilizer make it possible to balance the convergence of the data space (D) and the model space (M), guiding multimodal geophysical parameters toward assigned petrophysical values, which makes the results more stable and realistic. Two model studies are presented to illustrate the method, a simple synthetic model with two rectangular bodies in a homogenous background and a realistic model of the Volcanogenic Massive Sulfide (VMS) deposits in northeastern New Brunswick, Canada. These models demonstrate that the new focusing joint inversion algorithm produces better images than traditional methods because the FCM function uses the structural correlation of density contrast and magnetic susceptibility as constraints.

KW - Gravity anomalies and Earth structure

KW - Joint inversion

KW - Magnetic anomalies: modelling and interpretation

KW - Persistence, memory, correlations, clustering

U2 - 10.1093/gji/ggaa518

DO - 10.1093/gji/ggaa518

M3 - Journal article

AN - SCOPUS:85099883453

VL - 224

SP - 1344

EP - 1359

JO - Geophysical Journal International

JF - Geophysical Journal International

SN - 0956-540X

IS - 2

ER -

ID: 306971828