阿根廷圣路易斯省拉瓜达山脉深成岩的岩石学和地球化学特征:与法马提安岩浆弧的成因影响

IF 0.8 4区 地球科学 Q3 GEOLOGY Estudios Geologicos-Madrid Pub Date : 2017-07-06 DOI:10.3989/EGEOL.42711.440
Eber A. Cristofolini, Matías Barzola, J. Otamendi, A. Tibaldi, Augusto Morosini, P. Armas, Giuliano Camilletti
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引用次数: 2

摘要

本研究基于野外关系、岩石学和构造特征以及地球化学特征,对阿根廷圣路易斯省塞拉德拉阿瓜达的结晶复合体进行了地质综合研究。该山脉暴露出以中基性钙碱性火成岩和过铝质长英质花岗岩为主的基底,均位于低角闪岩相稳定的中低变质岩中。所有这些岩性地体被归为El Carrizal-La Aguada杂岩。研究区深成岩与圣路易斯山脉奥陶系法马梯系深成岩的野外对比、岩石学特征和地球化学对比表明,研究区深成岩与法马梯系岩浆弧发育具有成因和时间关系。
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Caracterización petrológica y geoquímica de las rocas plutónicas de la Sierra de La Aguada, Provincia de San Luis, Argentina: Implicaciones genéticas con el arco magmático Famatiniano
This study presents a synthesis on the geology of the crystalline complex that constitute the Sierra de la Aguada, San Luis province, Argentine, from an approach based on field relations, petrologic and structural features and geochemical characteristic. This mountain range exposes a basement dominated by intermediate to mafic calcalkaline igneous rocks and peraluminous felsic granitoids, both emplaced in low to medium grade metamorphic rocks stabilized under low amphibolite facies. All this lithological terrane has been grouped in the El Carrizal-La Aguada Complex. Field relations, petrographic characterization and geochemical comparison of the plutonic rocks from the study area with those belonging to the Ordovician Famatinian suit exposed in the Sierra Grande de San Luis, suggest a genetic and temporal relation linked to the development of the Famatinian magmatic arc.
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来源期刊
CiteScore
1.40
自引率
14.30%
发文量
6
审稿时长
>12 weeks
期刊介绍: Since 1945 Estudios Geologicos publishes original research works, as well as reviews, about any topic on Earth Sciences. Estudios Geologicos is published as one yearly volume, divided into two half-yearly issues. It is edited by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas, CSIC) at the Instituto de Geociencias (CSIC-UCM). Estudios Geologicos provides free access to full-text articles through this electronic edition. Accepted articles appear online as "Forthcoming articles" as soon as the galley proofs have been approved by the authors and the Editor-in-Chief. No changes can be made after online publication.
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