The nature of the Palaeozoic oceanic basin at the southwestern margin of Gondwana and implications for the origin of the Chilenia terrane (Pichilemu region, central Chile)

Author(s)

Hyppolito, Thais ^{[1, 2]} ; Juliani, Caetano ^[1] ; Garcia-Casco, Antonio ^[2] ; Meira, Vinicius Tieppo ^[1] ; Bustamante, Andres ^[1] ; Herve, Francisco ^{[3, 4]}

Affiliation

^[1] Univ Sao Paulo, Inst Geociencias, Dept Geoquim & Geotecton, BR-01498 Sao Paulo - Brazil

^[2] Univ Granada, Dept Mineral & Petrol, Granada - Spain

^[3] Univ Chile, Dept Geol, Santiago - Chile

^[4] Univ Andres Bello, Escuela Ciencias Tierra, Santiago - Chile

• Document type: Journal article
• Source: INTERNATIONAL GEOLOGY REVIEW; v. 56, n. 9, p. 1097-1121, 2014.
• Web of Science Citations: 12

Abstract

The Coastal Accretionary Complex of central Chile constitutes the product of early Carboniferous to Late Triassic subduction at the rear of Chilenia, a continental terrane likely derived from Laurentia and accreted to southwestern margin of Gondwana during the Mid to Late Devonian. The complex contains basaltic metavolcanic sequences of the subducted oceanic lithosphere accreted to the active margin. In this paper, we address the tectonic setting of these rocks by means of a geochemical study in the coastal area of Pichilemu region, central Chile. The accreted fragments of oceanic crust occupy different structural levels, exhibit variable metamorphic grade, and have geochemical fingerprints that reveal a compositional heterogeneity of the subducted oceanic crust. The amphibolites have N to E-MORB compositions. Greenschist units include N-MORB and E-MORB transitional to OIB, and blueschists and greenschists interleaved within a single metavolcanosedimentary sequence have OIB signatures. Neodymium isotopic systematics indicate depleted and enriched mantle sources, whereas strontium isotopic systematics indicate seawater/rock interaction. The variety of rocks suggests formation in an oceanic setting characterized by shallow and deep mantle sources, such as plume-influenced ridge. Based on the geological, petrological, geochemical, and isotopic characteristics, we propose that the metavolcanic protoliths of the Pichilemu region formed relatively close to the western margin of the Chilenia terrane during the initial stage (late Cambrian-Early Devonian) of seafloor development and drifting of this continental block. Geochemical similarities with oceanic units accreted to the active margin south of the Pichilemu region indicate a regional pattern of the oceanic crust subducted under the Palaeozoic Chilean margin between, at least, 34 S and 39 S latitude, strongly supporting the activity of a mantle plume. This, in turn, can be correlated with the location of the Pacific plume generation zone in early Palaeozoic era, corroborating a Laurentian origin for the Chilenia terrane. (AU)

• FAPESP's process: 12/01191-1 - Evolution of the paired metamorphic belt in the coastal cordillera of Central Chile: metamorphism and tectonics of the proto-andean margin in South American Continent
• Grantee: Caetano Juliani
• Support Opportunities: Regular Research Grants
• FAPESP's process: 12/17635-6 - Metamorphism and tectonic evolution of paired metamorphic belt of Tanumé and Pichilemu regions, Chilean Coastal Cordillera, VI region
• Grantee: Thaís Nogueira Hyppolito
• Support Opportunities: Scholarships abroad - Research Internship - Doctorate
• FAPESP's process: 10/11954-7 - Metamorphism and tectonic evolution of the paired metamorphic belt at Tanumé and Pichilemu regions, Chilean Coastal Cordillera, VI Region
• Grantee: Thaís Nogueira Hyppolito
• Support Opportunities: Scholarships in Brazil - Doctorate