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Bibliographic Details
Main Author: Mario Rebolledo-Vieyra
Format: Artículo científico
Language:es
Published: Universidad Nacional Autónoma de México 2010
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Online Access:https://www.redalyc.org/articulo.oa?id=57214937016
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  • Aeromagnetic anomalies and structural model of the Chicxulub multiring impact crater, Yucatan, Mexico Mario Rebolledo-Vieyra Jaime Urrutia-Fucugauchi Héctor López-Loera Ciencias de la Tierra uplift Mexico Chicxulub crater structural model aeromagnetic anomaly A structural model of the Chicxulub crater is derived from aeromagnetic anomaly modeling, borehole information and magnetic mineral data. Magnetic susceptibility measurements from borehole cores and samples in the crater show that suevite-like breccias have a variable strong magnetic signature, which is related to basement and melt clasts. The crystalline component estimated from clast analyses in the suevite-like breccias has on average higher magnetic susceptibilities (up to 1200×10-5 SI) than that of impact melt (~500×10-5 SI) and crystalline basement (400×10-5 SI). Reduction to the pole and downward analytical continuations show the discrete composite character of the anomaly, with inverse dipolar anomalies. The second-derivative of magnetic anomaly depicts five concentric rings, with the external ring correlating with the cenote ring and marking the surface expression of crater rim. The analytical signal and the radially averaged spectrum yield an estimate of the averaged depth to the magnetic sources, ranging from 1000 to 6000 m. There are three major magnetic sources within the Chicxulub crater: 1) the melt unit, 2) the suevite-like breccia, and 3) the central uplift. Using all these data, including new 2-D magnetic models, a new structural model is proposed. It reveals a system of regional vertical faults that explain the magnetic signal over the southern sector of the crater, whereas a 2.5 km deep central uplift and highly magnetized breccia sequences and melt sheet might be the sources of the main magnetic anomalies. 2010 artículo científico 1026-8774 https://www.redalyc.org/articulo.oa?id=57214937016 es http://www.redalyc.org/revista.oa?id=572 Revista Mexicana de Ciencias Geológicas application/pdf Universidad Nacional Autónoma de México Revista Mexicana de Ciencias Geológicas (México) Num.1 Vol.27