LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil
Abstract The Jacareacanga Group comprises mafic to ultramafic schists, metacherts, quartzites, pelitic paragneisses, and amphibolites related to siliciclastic-chemical sedimentation and mafic-ultramafic volcanism. These rocks of the Jacareacanga Group correspond to turbidite-related sediments and oc...
Saved in:
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Sociedade Brasileira de Geologia
2025-03-01
|
| Series: | Brazilian Journal of Geology |
| Subjects: | |
| Online Access: | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892025000100302&lng=en&tlng=en |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| _version_ | 1850074760868790272 |
|---|---|
| author | Jenny Alexandra Ortega Cardozo Marcelo Vasquez Marco Antonio Galarza Toro |
| author_facet | Jenny Alexandra Ortega Cardozo Marcelo Vasquez Marco Antonio Galarza Toro |
| author_sort | Jenny Alexandra Ortega Cardozo |
| collection | DOAJ |
| description | Abstract The Jacareacanga Group comprises mafic to ultramafic schists, metacherts, quartzites, pelitic paragneisses, and amphibolites related to siliciclastic-chemical sedimentation and mafic-ultramafic volcanism. These rocks of the Jacareacanga Group correspond to turbidite-related sediments and oceanic crust basalts of a back-arc or trench basin of the early magmatic Cuiú-Cuiú Arc of the Tapajós Domain in the Amazon Craton. Field data and petrographic analysis support the new zircon U-Pb ages obtained through LA-ICP-MS for the rocks of the Jacareacanga Group. A ± 10% concordance criterion applied, along with an exclusion of ages < 2000 Ma to mitigate interference from later events, such as granitic intrusions. Two pelitic paragneisses yielded 207Pb/206Pb ages between 2008 and 2042 Ma and mica schist ages of ca. 2056 Ma, considered to be the maximum sedimentation age of the protoliths of metasedimentary rocks. Zircon populations from the Rhyacian to the Mesoarchean indicate provenance from adjacent cratonic areas. This study shows that the Jacareacanga Basin was formed during the early Orosirian. The oldest detrital zircon ages support provenance from a magmatic arc basin of a continental margin comprising Rhyacian to Mesoarchean crust. |
| format | Article |
| id | doaj-art-89cbc53b720d4f70aa28e8a5a5197f0b |
| institution | DOAJ |
| issn | 2317-4692 |
| language | English |
| publishDate | 2025-03-01 |
| publisher | Sociedade Brasileira de Geologia |
| record_format | Article |
| series | Brazilian Journal of Geology |
| spelling | doaj-art-89cbc53b720d4f70aa28e8a5a5197f0b2025-08-20T02:46:29ZengSociedade Brasileira de GeologiaBrazilian Journal of Geology2317-46922025-03-015510.1590/2317-4889202420240021LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, BrazilJenny Alexandra Ortega Cardozohttps://orcid.org/0009-0000-6633-4159Marcelo Vasquezhttps://orcid.org/0000-0003-2729-9404Marco Antonio Galarza Torohttps://orcid.org/0000-0002-7271-4737Abstract The Jacareacanga Group comprises mafic to ultramafic schists, metacherts, quartzites, pelitic paragneisses, and amphibolites related to siliciclastic-chemical sedimentation and mafic-ultramafic volcanism. These rocks of the Jacareacanga Group correspond to turbidite-related sediments and oceanic crust basalts of a back-arc or trench basin of the early magmatic Cuiú-Cuiú Arc of the Tapajós Domain in the Amazon Craton. Field data and petrographic analysis support the new zircon U-Pb ages obtained through LA-ICP-MS for the rocks of the Jacareacanga Group. A ± 10% concordance criterion applied, along with an exclusion of ages < 2000 Ma to mitigate interference from later events, such as granitic intrusions. Two pelitic paragneisses yielded 207Pb/206Pb ages between 2008 and 2042 Ma and mica schist ages of ca. 2056 Ma, considered to be the maximum sedimentation age of the protoliths of metasedimentary rocks. Zircon populations from the Rhyacian to the Mesoarchean indicate provenance from adjacent cratonic areas. This study shows that the Jacareacanga Basin was formed during the early Orosirian. The oldest detrital zircon ages support provenance from a magmatic arc basin of a continental margin comprising Rhyacian to Mesoarchean crust.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892025000100302&lng=en&tlng=enTapajós DomainJacareacanga GroupCuiú-Cuiú ArcLA-ICP-MS U-Pb zircon dating |
| spellingShingle | Jenny Alexandra Ortega Cardozo Marcelo Vasquez Marco Antonio Galarza Toro LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil Brazilian Journal of Geology Tapajós Domain Jacareacanga Group Cuiú-Cuiú Arc LA-ICP-MS U-Pb zircon dating |
| title | LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil |
| title_full | LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil |
| title_fullStr | LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil |
| title_full_unstemmed | LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil |
| title_short | LA-ICP-MS U-Pb zircon dating of rocks of the Jacareacanga Group, Tapajós Domain, Amazon Craton, Brazil |
| title_sort | la icp ms u pb zircon dating of rocks of the jacareacanga group tapajos domain amazon craton brazil |
| topic | Tapajós Domain Jacareacanga Group Cuiú-Cuiú Arc LA-ICP-MS U-Pb zircon dating |
| url | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892025000100302&lng=en&tlng=en |
| work_keys_str_mv | AT jennyalexandraortegacardozo laicpmsupbzircondatingofrocksofthejacareacangagrouptapajosdomainamazoncratonbrazil AT marcelovasquez laicpmsupbzircondatingofrocksofthejacareacangagrouptapajosdomainamazoncratonbrazil AT marcoantoniogalarzatoro laicpmsupbzircondatingofrocksofthejacareacangagrouptapajosdomainamazoncratonbrazil |