Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey

ABSTRACT: A ground magnetic survey in a Central-East area of the Santa Catarina Island tested the continuity of the Cretaceous mafic dykes beneath the aeolic sediments of the Joaquina plain. Vertical gradient measurements taken in 1880 stations did not detect any magnetic anomaly related to subsurfa...

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Main Authors: George Caminha-Maciel, Marcia Ernesto, Welitom R. Borges, Junior Bresolin, Reginaldo Lemos
Format: Article
Language:English
Published: Sociedade Brasileira de Geologia 2017-06-01
Series:Brazilian Journal of Geology
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000200237&lng=en&tlng=en
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author George Caminha-Maciel
Marcia Ernesto
Welitom R. Borges
Junior Bresolin
Reginaldo Lemos
author_facet George Caminha-Maciel
Marcia Ernesto
Welitom R. Borges
Junior Bresolin
Reginaldo Lemos
author_sort George Caminha-Maciel
collection DOAJ
description ABSTRACT: A ground magnetic survey in a Central-East area of the Santa Catarina Island tested the continuity of the Cretaceous mafic dykes beneath the aeolic sediments of the Joaquina plain. Vertical gradient measurements taken in 1880 stations did not detect any magnetic anomaly related to subsurface dykes. Four magnetic profiles located to the north and south of the main area showed the magnetic signature of various dykes some of them already mapped (north profiles), but also some in subsurface (south profiles). These results suggest that the dykes probably were shallow and truncated, and were already eroded along with the crystalline basement.
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spelling doaj.art-5c7b320c22554d7c968aadb321eaa08d2022-12-21T17:45:12ZengSociedade Brasileira de GeologiaBrazilian Journal of Geology2317-46922017-06-0147223724710.1590/2317-4889201720170009S2317-48892017000200237Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic surveyGeorge Caminha-MacielMarcia ErnestoWelitom R. BorgesJunior BresolinReginaldo LemosABSTRACT: A ground magnetic survey in a Central-East area of the Santa Catarina Island tested the continuity of the Cretaceous mafic dykes beneath the aeolic sediments of the Joaquina plain. Vertical gradient measurements taken in 1880 stations did not detect any magnetic anomaly related to subsurface dykes. Four magnetic profiles located to the north and south of the main area showed the magnetic signature of various dykes some of them already mapped (north profiles), but also some in subsurface (south profiles). These results suggest that the dykes probably were shallow and truncated, and were already eroded along with the crystalline basement.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000200237&lng=en&tlng=enDyke swarmSanta Catarina IslandGeophysical mappingGround surveysMagnetic methods
spellingShingle George Caminha-Maciel
Marcia Ernesto
Welitom R. Borges
Junior Bresolin
Reginaldo Lemos
Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey
Brazilian Journal of Geology
Dyke swarm
Santa Catarina Island
Geophysical mapping
Ground surveys
Magnetic methods
title Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey
title_full Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey
title_fullStr Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey
title_full_unstemmed Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey
title_short Evaluation of mafic dyke swarm continuity under the Joaquina dune field with ground magnetic survey
title_sort evaluation of mafic dyke swarm continuity under the joaquina dune field with ground magnetic survey
topic Dyke swarm
Santa Catarina Island
Geophysical mapping
Ground surveys
Magnetic methods
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000200237&lng=en&tlng=en
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