3D structural modeling approach by discretization of a basic structural map associated with magnetic data-Reference-Cited by-同舟云学术

3D structural modeling approach by discretization of a basic structural map associated with magnetic data

Published:2024-07-18 Issue: Volume: Page:1-14
ISSN:1226-9328
Container-title:Geosystem Engineering
language:en
Short-container-title:Geosystem Engineering

Author:

Ndam Njikam Mohamed Moustapha¹^ORCID,Meying Arsène¹,Ribodetti Alessandra²,Amougou Alain Zanga³,Lionel Ebengué Atéga Philippe⁴,Afzal Butt Nabeel⁵,Téthys-Authie Chiewo Ceukou⁶,Constant Djomagueu¹,Songo Majura A. M.⁷

Affiliation:

1. School of Geology and Mining Engineering, University of Ngaoundere, Meiganga, Cameroon

2. Université Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Valbonne, France

3. Department of Physics, Faculty of Science, University of Douala, Douala, Cameroon

4. Mines Alès Institute, Alès, France

5. National Centre of Excellence in Geology (NCEG), University of Peshawar, Peshawar, Pakistan

6. Department of Physics, University of Yaounde I, Yaounde, Cameroon

7. School of Mines and Geosciences, University of Dar es Salaam, Dar es Salaam, Tanzania

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/12269328.2024.2377315

Reference39 articles.

1. Anderson, E., Zhou, W., & Santi, P. (2013). Aeromagnetic signature of the geology and mineral resources near the pebble porphyry CU-AU-MO deposit, Southwest Alaska. ProQuest LLC.

2. A NEW METHOD FOR INTERPRETATION OF AEROMAGNETIC MAPS: PSEUDO‐GRAVIMETRIC ANOMALIES

3. Barbosa, R. D., & Pereira, J. G. (2013). Invers?o 3D de dados Magnéticos na Regi?o de Mara Rosa - Goiás, Brasil, utilizando Geosoft VOXI. 13th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 26?29 August 2013, SEG Global Meeting Abstracts. Brazilian Geophysical Society (pp. 520–525). https://doi.org/10.1190/sbgf2013-109

4. Approximating edges of source bodies from magnetic or gravity anomalies

5. Growth of vertically segmented normal faults