Ar and U-Th-Pb age determinations for minerals from ODP Holes of ODP Legs 173 and 210

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Hauptverfasser: Jagoutz, Oliver, Müntener, Othmar, Manatschal, Gianreto, Rubatto, Daniela, Péron-Pinvidic, Gwenn, Turrin, Brent D, Villa, Igor M
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Sprache:en
Veröffentlicht: PANGAEA 2007
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author Jagoutz, Oliver
Müntener, Othmar
Manatschal, Gianreto
Rubatto, Daniela
Péron-Pinvidic, Gwenn
Turrin, Brent D
Villa, Igor M
author_facet Jagoutz, Oliver
Müntener, Othmar
Manatschal, Gianreto
Rubatto, Daniela
Péron-Pinvidic, Gwenn
Turrin, Brent D
Villa, Igor M
collection Datos científicos de ciencias marinas y ambientales
contents We report U-Pb and 39Ar-40Ar measurements on plutonic rocks recovered from the Ocean Drilling Program (ODP) Legs 173 and 210. Drilling revealed continental crust (Sites 1067 and 1069) and exhumed mantle (Sites 1070 and 1068) along the Iberia margin and exhumed mantle (Site 1277) on the conjugate Newfoundland margin. Our data record a complex igneous and thermal history related to the transition from rifting to seafloor spreading. The results show that the rift-to-drift transition is marked by a stuttering start of MORB-type magmatic activity. Subsequent to initial alkaline magmatism, localized mid-oceanic ridge basalts (MORB) magmatism was again replaced by basin-wide alkaline events, caused by a low degree of decompression melting due to tectonic delocalization of deformation. Such "off-axis" magmatism might be a common process in (ultra-) slow oceanic spreading systems, where "magmatic" and "tectonic" spreading varies in both space and time.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_722550
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Ar and U-Th-Pb age determinations for minerals from ODP Holes of ODP Legs 173 and 210
Jagoutz, Oliver
Müntener, Othmar
Manatschal, Gianreto
Rubatto, Daniela
Péron-Pinvidic, Gwenn
Turrin, Brent D
Villa, Igor M
173-1067A; 173-1068A; 173-1069A; 173-1070; 173-1070A; 210-1277; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg173; Leg210; North Atlantic Ocean; Ocean Drilling Program; ODP
We report U-Pb and 39Ar-40Ar measurements on plutonic rocks recovered from the Ocean Drilling Program (ODP) Legs 173 and 210. Drilling revealed continental crust (Sites 1067 and 1069) and exhumed mantle (Sites 1070 and 1068) along the Iberia margin and exhumed mantle (Site 1277) on the conjugate Newfoundland margin. Our data record a complex igneous and thermal history related to the transition from rifting to seafloor spreading. The results show that the rift-to-drift transition is marked by a stuttering start of MORB-type magmatic activity. Subsequent to initial alkaline magmatism, localized mid-oceanic ridge basalts (MORB) magmatism was again replaced by basin-wide alkaline events, caused by a low degree of decompression melting due to tectonic delocalization of deformation. Such "off-axis" magmatism might be a common process in (ultra-) slow oceanic spreading systems, where "magmatic" and "tectonic" spreading varies in both space and time.
title Ar and U-Th-Pb age determinations for minerals from ODP Holes of ODP Legs 173 and 210
topic 173-1067A; 173-1068A; 173-1069A; 173-1070; 173-1070A; 210-1277; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg173; Leg210; North Atlantic Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.722550