Please use this identifier to cite or link to this item: http://repositorio.unicamp.br/jspui/handle/REPOSIP/2044
Type: Artigo
Title: Magnetic fabric of Araguainha complex impact structure (Central Brazil): Implications for deformation mechanisms and central uplift formation
Author: Yokoyama, E.
Trindade, R. I. F.
Lana, C.
Souza Filho, C. R.
Baratoux, D.
Marangoni, Y. R.
Tohver, E.
Abstract: The weakening mechanisms involved in the collapse of complex impact craters are controversial. The Araguainha impact crater, in Brazil, exposes a complex structure of 40 km in diameter, and is an excellent object to address this issue. Its core is dominated by granite. In addition to microstructural observations, magnetic studies reveal its internal fabric acquired during the collapse phase. All granite samples exhibit impact-related planar deformation features (PDFs) and planar fractures (PFs), which were overprinted by cataclasis. Cataclastic deformation has evolved from incipient brittle fracturing to the development of discrete shear bands in the center of the structure. Fracture planes are systematically decorated by tiny grains (<10 mu m) of magnetite and hematite, and the orientation of magnetic lineation and magnetic foliation obtained by the anisotropies of magnetic susceptibility (AMS) and anhysteretic remanence (AAR) are perfectly coaxial in all studied sites. Therefore, we could track the orientation of deformation features which are decorated by iron oxides using the AMS and AAR. The magnetic fabrics show a regular pattern at the borders of the central peak, with orientations consistent with the fabric of sediments at the crater's inner collar and complex in the center of the structure. Both the cataclastic flow revealed from microstructural observations and the structural pattern of the magnetic anisotropy match the predictions from numerical models of complex impact structures. The widespread occurrence of cataclasis in the central peak, and its orientations revealed by magnetic studies indicate that acoustic fluidization likely operates at all scales, including the mineral scales. The cataclastic flow made possible by acoustic fluidization results in an apparent plastic deformation at the macroscopic scale in the core
Subject: Microestrutura
Cratera de impacto
Anisotropia Magnética
Country: Holanda
Editor: Elsevier Scientific Publishing
Citation: Earth and Planetary Science Letters. Elsevier, v.331, p.347-359, 2012
Rights: fechado
Identifier DOI: 10.1016/j.epsl.2012.01.005
Address: https://www.sciencedirect.com/science/article/pii/S0012821X12000155?via%3Dihub
Date Issue: 2012
Appears in Collections:IG - Artigos e Outros Documentos

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