Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau
The Maurice Ewing Bank is located east of the Falkland/Malvinas Islands and is one of the most intriguing regions of southern Gondwana. The interaction of several microplates with major cratonic areas resulted in complex displacements between Paleozoic and Cretaceous times. Here, we present combined...
Guardado en:
| Autores principales: | , , , , |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_03019268_v314_n_p28_Chemale |
| Aporte de: |
| id |
todo:paper_03019268_v314_n_p28_Chemale |
|---|---|
| record_format |
dspace |
| spelling |
todo:paper_03019268_v314_n_p28_Chemale2023-10-03T15:18:38Z Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau Chemale, F., Jr. Ramos, V.A. Naipauer, M. Girelli, T.J. Vargas, M. Falkland-Malvinas Islands Maurice Ewing Bank Mesoproterozoic Mesozoic Paleogeographic reconstruction basement rock deformation detrital deposit hafnium isotopic analysis lutetium Mesozoic paleogeography Proterozoic tectonic reconstruction uranium-lead dating zircon Atlantic Ocean Falkland Islands (Malvinas) Stenia The Maurice Ewing Bank is located east of the Falkland/Malvinas Islands and is one of the most intriguing regions of southern Gondwana. The interaction of several microplates with major cratonic areas resulted in complex displacements between Paleozoic and Cretaceous times. Here, we present combined U-Pb and Lu-Hf zircon isotopic analyses of the Maurice Ewing Bank basement to constrain the age and tectonic setting to aid in paleogeographic reconstruction. The high-grade paragneisses in the bank present dominant Late Mesoproterozoic detrital zircon age distributions with populations at 1032 ± 12 Ma, 1068 ± 16 Ma and 1233 ± 8 Ma and juvenile signature (positive εHf[t] values). The gneisses are cutting by anatectic pink granite crystallized at 1006 ± 13 Ma which formed after syn-collisional high-grade metamorphism and shows juvenile and some crustal component (εHf[t] = +1.6 to −3). The Maurice Ewing Bank basement rocks have same Stenian age and dominant juvenile signature as the arc-related basement rocks from the Falkland/Malvinas Islands and are probably part of the same continental plateau of the South America continent. This new finding enables future reconstructions in paleogeographic models where the basement of the Falkland/Malvinas Islands and the Maurice Ewing Bank formed a single block during the Mesoproterozoic and were partly separated by crustal stretching during the opening of the Atlantic Ocean in the Late Jurassic-Cretaceous. The block played a major role in the deformation of the Cape Fold Belt from the Late Paleozoic through the Mesozoic. © 2018 Elsevier B.V. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_03019268_v314_n_p28_Chemale |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
Falkland-Malvinas Islands Maurice Ewing Bank Mesoproterozoic Mesozoic Paleogeographic reconstruction basement rock deformation detrital deposit hafnium isotopic analysis lutetium Mesozoic paleogeography Proterozoic tectonic reconstruction uranium-lead dating zircon Atlantic Ocean Falkland Islands (Malvinas) Stenia |
| spellingShingle |
Falkland-Malvinas Islands Maurice Ewing Bank Mesoproterozoic Mesozoic Paleogeographic reconstruction basement rock deformation detrital deposit hafnium isotopic analysis lutetium Mesozoic paleogeography Proterozoic tectonic reconstruction uranium-lead dating zircon Atlantic Ocean Falkland Islands (Malvinas) Stenia Chemale, F., Jr. Ramos, V.A. Naipauer, M. Girelli, T.J. Vargas, M. Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau |
| topic_facet |
Falkland-Malvinas Islands Maurice Ewing Bank Mesoproterozoic Mesozoic Paleogeographic reconstruction basement rock deformation detrital deposit hafnium isotopic analysis lutetium Mesozoic paleogeography Proterozoic tectonic reconstruction uranium-lead dating zircon Atlantic Ocean Falkland Islands (Malvinas) Stenia |
| description |
The Maurice Ewing Bank is located east of the Falkland/Malvinas Islands and is one of the most intriguing regions of southern Gondwana. The interaction of several microplates with major cratonic areas resulted in complex displacements between Paleozoic and Cretaceous times. Here, we present combined U-Pb and Lu-Hf zircon isotopic analyses of the Maurice Ewing Bank basement to constrain the age and tectonic setting to aid in paleogeographic reconstruction. The high-grade paragneisses in the bank present dominant Late Mesoproterozoic detrital zircon age distributions with populations at 1032 ± 12 Ma, 1068 ± 16 Ma and 1233 ± 8 Ma and juvenile signature (positive εHf[t] values). The gneisses are cutting by anatectic pink granite crystallized at 1006 ± 13 Ma which formed after syn-collisional high-grade metamorphism and shows juvenile and some crustal component (εHf[t] = +1.6 to −3). The Maurice Ewing Bank basement rocks have same Stenian age and dominant juvenile signature as the arc-related basement rocks from the Falkland/Malvinas Islands and are probably part of the same continental plateau of the South America continent. This new finding enables future reconstructions in paleogeographic models where the basement of the Falkland/Malvinas Islands and the Maurice Ewing Bank formed a single block during the Mesoproterozoic and were partly separated by crustal stretching during the opening of the Atlantic Ocean in the Late Jurassic-Cretaceous. The block played a major role in the deformation of the Cape Fold Belt from the Late Paleozoic through the Mesozoic. © 2018 Elsevier B.V. |
| format |
JOUR |
| author |
Chemale, F., Jr. Ramos, V.A. Naipauer, M. Girelli, T.J. Vargas, M. |
| author_facet |
Chemale, F., Jr. Ramos, V.A. Naipauer, M. Girelli, T.J. Vargas, M. |
| author_sort |
Chemale, F., Jr. |
| title |
Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau |
| title_short |
Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau |
| title_full |
Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau |
| title_fullStr |
Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau |
| title_full_unstemmed |
Age of basement rocks from the Maurice Ewing Bank and the Falkland/Malvinas Plateau |
| title_sort |
age of basement rocks from the maurice ewing bank and the falkland/malvinas plateau |
| url |
http://hdl.handle.net/20.500.12110/paper_03019268_v314_n_p28_Chemale |
| work_keys_str_mv |
AT chemalefjr ageofbasementrocksfromthemauriceewingbankandthefalklandmalvinasplateau AT ramosva ageofbasementrocksfromthemauriceewingbankandthefalklandmalvinasplateau AT naipauerm ageofbasementrocksfromthemauriceewingbankandthefalklandmalvinasplateau AT girellitj ageofbasementrocksfromthemauriceewingbankandthefalklandmalvinasplateau AT vargasm ageofbasementrocksfromthemauriceewingbankandthefalklandmalvinasplateau |
| _version_ |
1782027481764593664 |