A deformed alkaline igneous rock-carbonatite complex from the Western Sierras Pampeanas, Argentina: Evidence for late Neoproterozoic opening of the Clymene Ocean?
dc.contributor.author | Casquet, Cesar | |
dc.contributor.author | Pankhurst, Robert J | |
dc.contributor.author | Galindo, Carmen | |
dc.contributor.author | Rapela, Carlos W | |
dc.contributor.author | Fanning, Christopher | |
dc.contributor.author | Baldo, Edgardo | |
dc.contributor.author | Dahlquist, Juan A. | |
dc.contributor.author | Gonzalez-Casado, Jose M | |
dc.contributor.author | Colombo, Fernando | |
dc.date.accessioned | 2015-12-08T22:40:02Z | |
dc.date.issued | 2008 | |
dc.date.updated | 2015-12-08T10:20:13Z | |
dc.description.abstract | A deformed ca. 570 Ma syenite-carbonatite body is reported from a Grenville-age (1.0-1.2 Ga) terrane in the Sierra de Maz, one of the Western Sierras Pampeanas of Argentina. This is the first recognition of such a rock assemblage in the basement of the Central Andes. The two main lithologies are coarse-grained syenite (often nepheline-bearing) and enclave-rich fine-grained foliated biotite-calcite carbonatite. Samples of carbonatite and syenite yield an imprecise whole rock Rb-Sr isochron age of 582 ± 60 Ma (MSWD = 1.8; Sri = 0.7029); SHRIMP U-Pb spot analysis of syenite zircons shows a total range of 206Pb-238U ages between 433 and 612 Ma, with a prominent peak at 560-580 Ma defined by homogeneous zircon areas. Textural interpretation of the zircon data, combined with the constraint of the Rb-Sr data suggest that the carbonatite complex formed at ca. 570 Ma. Further disturbance of the U-Pb system took place at 525 ± 7 Ma (Pampean orogeny) and at ca. 430-440 Ma (Famatinian orogeny) and it is concluded that the Western Sierras Pampeanas basement was joined to Gondwana during both events. Highly unradiogenic 87Sr/86Sr values in calcites (0.70275-0.70305) provide a close estimate for the initial Sr isotope composition of the carbonatite magma. Sm-Nd data yield εNd570 values of +3.3 to +4.8. The complex was probably formed during early opening of the Clymene Ocean from depleted mantle with a component from Meso/Neo-proterozoic lower continental crust. | |
dc.identifier.issn | 0301-9268 | |
dc.identifier.uri | http://hdl.handle.net/1885/36327 | |
dc.publisher | Elsevier | |
dc.source | Precambrian Research | |
dc.subject | Keywords: calcite; carbonatite; deformation; Gondwana; Grenvillian orogeny; igneous rock; isotope; lithology; mantle; Proterozoic; syenite; uranium-lead dating; zircon; Argentina; Sierras Pampeanas; South America DARCs; Gondwana; Rodinia; Syenite; U-Pb SHRIMP zircon dating | |
dc.title | A deformed alkaline igneous rock-carbonatite complex from the Western Sierras Pampeanas, Argentina: Evidence for late Neoproterozoic opening of the Clymene Ocean? | |
dc.type | Journal article | |
local.bibliographicCitation.lastpage | 220 | |
local.bibliographicCitation.startpage | 205 | |
local.contributor.affiliation | Casquet, Cesar, Universidad Complutense de Madrid | |
local.contributor.affiliation | Pankhurst, Robert J, British Geological Survey | |
local.contributor.affiliation | Galindo, Carmen, Universidad Complutense de Madrid | |
local.contributor.affiliation | Rapela, Carlos W, Universidad Nacional de La Plata | |
local.contributor.affiliation | Fanning, Christopher, College of Physical and Mathematical Sciences, ANU | |
local.contributor.affiliation | Baldo, Edgardo, Universidad Nacional de Cordoba | |
local.contributor.affiliation | Dahlquist, Juan A., CRILAR-CONICET | |
local.contributor.affiliation | Gonzalez-Casado, Jose M, Universidad Autonoma de Madrid | |
local.contributor.affiliation | Colombo, Fernando, Universidad Nacional de Cordoba | |
local.contributor.authoremail | u4029993@anu.edu.au | |
local.contributor.authoruid | Fanning, Christopher, u4029993 | |
local.description.embargo | 2037-12-31 | |
local.description.notes | Imported from ARIES | |
local.identifier.absfor | 040304 - Igneous and Metamorphic Petrology | |
local.identifier.absfor | 040313 - Tectonics | |
local.identifier.absfor | 040203 - Isotope Geochemistry | |
local.identifier.ariespublication | u4027924xPUB135 | |
local.identifier.citationvolume | 165 | |
local.identifier.doi | 10.1016/j.precamres.2008.06.011 | |
local.identifier.scopusID | 2-s2.0-51449119851 | |
local.identifier.thomsonID | 000259794500006 | |
local.identifier.uidSubmittedBy | u4027924 | |
local.type.status | Published Version |
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