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dc.contributor.author
Lopez, Monica Graciela
dc.contributor.author
Siegesmund, Siegfried
dc.contributor.author
Wemmer, Klaus
dc.contributor.author
Nolte, Nicole
dc.date.available
2018-04-26T18:56:01Z
dc.date.issued
2017-06
dc.identifier.citation
Lopez, Monica Graciela; Siegesmund, Siegfried; Wemmer, Klaus; Nolte, Nicole; Petrogenesis of the postcollisional Middle Devonian monzonitic to granitic magmatism of the Sierra de San Luis, Argentina; Elsevier Science; Lithos; 288-289; 6-2017; 191-213
dc.identifier.issn
0024-4937
dc.identifier.uri
http://hdl.handle.net/11336/43577
dc.description.abstract
Middle Devonian granitoids intruded the Eastern Sierras Pampeanas basement ca. 600 km east of the inferred proto-Pacific margin of Gondwana along which a ca. 390 Ma collisional event developed. In the Sierra de San Luis, voluminous Middle Devonian (393-382 Ma) batholiths are composed of I-to A-type hybrid Monzonite and Granite suites. Shoshonite and subordinated high-K series, stocks, synplutonic dikes and enclaves make up the Monzonite Suite; rocks are metaluminous alkali-calcic magnesian porphyritic or equigranular monzonite, quartz monzonite, monzodiorite and scarce monzogabbro. High-K and subordinated shoshonite series metaluminous to mildly peraluminous magnesian alkali-calcic to calc-alkalic porphyritic or equigranular quartz monzonite, granodiorite, monzogranite and equigranular leucomonzogranites make up the Granite Suite plutons and batholiths. Only a small group of highly evolved granites are ferroan. SiO2 (46–62%), Cr, Ni, V, Sc, LILE, LREE, Th, Zr and variable, Sr/Y, (La/Yb) N and (Tb/Yb)N, smooth Eu/Eu*, moderate Na2O (ca 3.5), and troughs at Nb and Ta for Monzonite Suite rocks suggest an subduction-related enriched lithospheric mantle source. Sm-Nd data (TDM 0.98 -1.08 Ga, εNd(380Ma) 0.66-1.47) and 87Sr/86Sri (0.703520-0.704203) are compatible with an enriched mantle source. The metaluminous porphyritic quartz monzonite-monzogranite and the mildly peraluminous equigranular biotite monzogranites of the Granite Suite are characterized by relatively moderate Al2O3, CaO, and 87Sr/86Sri, high LILE, Cr, variable Sr/Y, (La/Yb)N and Eu/Eu* and low Rb/Sr (<1.2) suggest a mafic source. The porphyritic monzogranite (TDM 1.20-1.28 Ga , εNd(380Ma) -3.02 to -3.3, 87Sr/86Sri 0.706578–0.707027) and the biotite monzogranites (TDM 1.31 Ga, εNd(380Ma) -3.3, 87Sr/86Sri 0.707782) would share a common source. The equigranular alkali-calcic leucomonzogranites are characterized by Rb/Sr >1.5, ASI 1.05-1.18, and Ga/Al 2.6-3.9, εNd(380Ma) -3.74 to-3.95 and (87Sr/86Sr)i 0.710743-0.712955 which would point to metasedimentary or felsic igneous crustal sources. Nevertheless their TDM 1.36-1.38 Ga is considerably younger than the mean 1.8-1.6 Ga Eastern Sierras Pampeanas crustal residence age and less radiogenic. Middle Devonian magmatism would record an episode of crustal growth by enriched mantle derived magma input and variable degrees of partial melting of a lower crustal source at the wanning stages of the Achalian orogeny.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier Science
dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
Petrogenesis Monzonite And Granite Suites
dc.subject
Postcollisional Magmatism
dc.subject
Middle Devonian
dc.subject
Sierra de San Luis-Sierras Pampeanas-Argentina
dc.subject.classification
Meteorología y Ciencias Atmosféricas
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS
dc.title
Petrogenesis of the postcollisional Middle Devonian monzonitic to granitic magmatism of the Sierra de San Luis, Argentina
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2018-04-13T18:11:59Z
dc.identifier.eissn
1872-6143
dc.journal.volume
288-289
dc.journal.pagination
191-213
dc.journal.pais
Países Bajos
dc.journal.ciudad
Amsterdam
dc.description.fil
Fil: Lopez, Monica Graciela. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotopica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina
dc.description.fil
Fil: Siegesmund, Siegfried. Geoscience Centre of the Georg-August University; Alemania
dc.description.fil
Fil: Wemmer, Klaus. Geoscience Centre of the Georg-August University; Alemania
dc.description.fil
Fil: Nolte, Nicole. Geoscience Centre of the Georg-August University; Alemania
dc.journal.title
Lithos
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/http://linkinghub.elsevier.com/retrieve/pii/S0024493717301925
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.lithos.2017.05.018
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