Western Paraná suture/shear zone and the limits of Rio Apa, Rio Tebicuary and Rio de La Plata cratons from gravity data
| Autor: | Federico Lince Klinger, Naomi Ussami, Gabriel Negrucci Dragone, Mario Gimenez, Carlos Alberto Moreno Chaves |
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| Rok vydání: | 2017 |
| Předmět: |
010504 meteorology & atmospheric sciences
010502 geochemistry & geophysics 01 natural sciences SW GONDWANA Ciencias de la Tierra y relacionadas con el Medio Ambiente purl.org/becyt/ford/1 [https] purl.org/becyt/ford/1.5 [https] Paleontology GRAVITY Geochemistry and Petrology GRAVIDADE Suture (geology) SUTURES 0105 earth and related environmental sciences geography geography.geographical_feature_category Geology Crust Sedimentary basin Craton Tectonics Seismic tomography CRATONS Shear zone INTRACONTINENTAL BASINS Meteorología y Ciencias Atmosféricas CIENCIAS NATURALES Y EXACTAS Bouguer anomaly Seismology |
| Zdroj: | Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual) Universidade de São Paulo (USP) instacron:USP CONICET Digital (CONICET) Consejo Nacional de Investigaciones Científicas y Técnicas instacron:CONICET |
| Popis: | We present a new gravity map between 45°?70° W and 5°?40° S integrating open source terrestrial gravity data of Argentina with the South American Gravity Model 2004 (SAGM04), a 5 min-arc resolution gravity model. The Bouguer anomaly map reveals a 2000 km long linear gravity feature from 15° S to 30° S at longitude 55° W, with a steep horizontal gradient separating two gravity domains. The eastern domain is the Paraná basin, with NE-SW trending Bouguer anomalies of −80 mGal in average. The western domain comprises the Chaco-Paraná, Chaco-Tarija and Pantanal basins, with circular positive anomalies of up to 20 mGal in amplitude. Previous seismic studies mapped a thinner crust of less than 35 km in the western domain and the present gravity models indicate a 10?20 kg/m3 denser crust. On the other hand, the eastern domain has a thicker crust of more than 40 km. Seismic tomography models also show P- and S-wave velocity reduction in the western domain whereas high-velocity characterises the Paraná basin. These geophysical data indicate that the gravity gradient marks a transition between two distinct lithospheres. The gravity gradient is associated with a tectonic feature referred to as the Western Paraná suture/shear zone. Granites of 530?570 Ma ages, located parallel or over the gravity gradient, suggest a Neoproterozoic to Early Cambrian age suture/shear zone, thus approximately synchronous and parallel to the Pampean belt. Sediment corrected residual gravity map and its vertical derivative allow us to define the limits of the Rio Apa, Rio de la Plata and Rio Tebicuary cratons. Their eastern and western limits are the Western Paraná suture and the Pampean belt, respectively. This study unravels Precambrian tectonic elements concealed by the Phanerozoic sedimentary basins adding new constraints for the amalgamation history of SW Gondwana. Fil: Dragone, Gabriel Negrucci. Universidade de Sao Paulo; Brasil Fil: Ussami, Naomi. Universidade de Sao Paulo; Brasil Fil: Gimenez, Mario Ernesto. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Lince Klinger, Federico Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Juan. Facultad de Ciencias Exactas, Físicas y Naturales. Instituto Geofísico Sismológico Volponi; Argentina Fil: Chaves, Carlos Alberto Moreno. Universidade de Sao Paulo; Brasil |
| Databáze: | OpenAIRE |
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