Crustal structure of Sicily from modelling of gravity and magnetic anomalies

Abstract We aim at modeling the main crustal and thermal interfaces of Sicily (Italy), a key area for understanding the geological complexity at the collisional boundary between the African and European plates. To this end, we analyze the gravity and magnetic fields, integrated with information from...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: M. Milano, Y. Kelemework, M. La Manna, M. Fedi, D. Montanari, M. Iorio
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
Materias:
R
Q
Acceso en línea:https://doaj.org/article/28ef40dccd754d66aba22daa233ebbfc
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:28ef40dccd754d66aba22daa233ebbfc
record_format dspace
spelling oai:doaj.org-article:28ef40dccd754d66aba22daa233ebbfc2021-12-02T18:51:14ZCrustal structure of Sicily from modelling of gravity and magnetic anomalies10.1038/s41598-020-72849-z2045-2322https://doaj.org/article/28ef40dccd754d66aba22daa233ebbfc2020-09-01T00:00:00Zhttps://doi.org/10.1038/s41598-020-72849-zhttps://doaj.org/toc/2045-2322Abstract We aim at modeling the main crustal and thermal interfaces of Sicily (Italy), a key area for understanding the geological complexity at the collisional boundary between the African and European plates. To this end, we analyze the gravity and magnetic fields, integrated with information from well logs, geology, heat flow, and seismic data. In order to make the most accurate description of the crustal structure of the area, we modeled with different methodologies the carbonate and crystalline top surfaces, as well as the Moho and the Curie isotherm surface. The reconstruction of the carbonate platform is achieved using a nonlinear 3D method constrained by the available seismic and borehole data. The crystalline top, the Curie, and the Moho are instead estimated by spectral analysis of both gravity and magnetic data. The results show a complex carbonate basement and a deep crystalline crust in central Sicily, with a prominent uplift beneath the Hyblean Plateau. Maps of the Moho and the Curie isotherm surface define a variable thermal and structural setting of Sicily, with very thin crust in the southern and eastern sectors, where high heat flow is found, and deep and cold crust below the Caltanissetta Basin.M. MilanoY. KelemeworkM. La MannaM. FediD. MontanariM. IorioNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 10, Iss 1, Pp 1-18 (2020)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
M. Milano
Y. Kelemework
M. La Manna
M. Fedi
D. Montanari
M. Iorio
Crustal structure of Sicily from modelling of gravity and magnetic anomalies
description Abstract We aim at modeling the main crustal and thermal interfaces of Sicily (Italy), a key area for understanding the geological complexity at the collisional boundary between the African and European plates. To this end, we analyze the gravity and magnetic fields, integrated with information from well logs, geology, heat flow, and seismic data. In order to make the most accurate description of the crustal structure of the area, we modeled with different methodologies the carbonate and crystalline top surfaces, as well as the Moho and the Curie isotherm surface. The reconstruction of the carbonate platform is achieved using a nonlinear 3D method constrained by the available seismic and borehole data. The crystalline top, the Curie, and the Moho are instead estimated by spectral analysis of both gravity and magnetic data. The results show a complex carbonate basement and a deep crystalline crust in central Sicily, with a prominent uplift beneath the Hyblean Plateau. Maps of the Moho and the Curie isotherm surface define a variable thermal and structural setting of Sicily, with very thin crust in the southern and eastern sectors, where high heat flow is found, and deep and cold crust below the Caltanissetta Basin.
format article
author M. Milano
Y. Kelemework
M. La Manna
M. Fedi
D. Montanari
M. Iorio
author_facet M. Milano
Y. Kelemework
M. La Manna
M. Fedi
D. Montanari
M. Iorio
author_sort M. Milano
title Crustal structure of Sicily from modelling of gravity and magnetic anomalies
title_short Crustal structure of Sicily from modelling of gravity and magnetic anomalies
title_full Crustal structure of Sicily from modelling of gravity and magnetic anomalies
title_fullStr Crustal structure of Sicily from modelling of gravity and magnetic anomalies
title_full_unstemmed Crustal structure of Sicily from modelling of gravity and magnetic anomalies
title_sort crustal structure of sicily from modelling of gravity and magnetic anomalies
publisher Nature Portfolio
publishDate 2020
url https://doaj.org/article/28ef40dccd754d66aba22daa233ebbfc
work_keys_str_mv AT mmilano crustalstructureofsicilyfrommodellingofgravityandmagneticanomalies
AT ykelemework crustalstructureofsicilyfrommodellingofgravityandmagneticanomalies
AT mlamanna crustalstructureofsicilyfrommodellingofgravityandmagneticanomalies
AT mfedi crustalstructureofsicilyfrommodellingofgravityandmagneticanomalies
AT dmontanari crustalstructureofsicilyfrommodellingofgravityandmagneticanomalies
AT miorio crustalstructureofsicilyfrommodellingofgravityandmagneticanomalies
_version_ 1718377435641151488