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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Contributions of gamma-ray spectrometry to terrestrial impact crater studies: The example of Serra da Cangalha, northeastern Brazil

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Author(s):
Vasconcelos, Marcos Alberto R. [1] ; Leite, Emilson P. [1] ; Crosta, Alvaro P. [1]
Total Authors: 3
Affiliation:
[1] Univ Estadual Campinas, Inst Geosci, BR-13083870 Campinas, SP - Brazil
Total Affiliations: 1
Document type: Journal article
Source: Geophysical Research Letters; v. 39, FEB 25 2012.
Web of Science Citations: 3
Abstract

Several geophysical methods have been used for decades for the identification and exploration of impact craters. Most of them are based on seismic, potential fields and electrical data, focusing on exploration of anomalies caused by changes in physical properties or by structures associated with the formation of the crater. Gamma-ray spectrometry is usually not mentioned among the geophysical methods employed in crater studies, although it is known that impact cratering processes cause a number of physical/chemical changes in the country rocks. These changes include the remobilization of hydrothermal fluids which directly modify the composition of target rocks and, subsidiarily, of soils related to these rocks. Therefore, the distribution of radioactive elements K, Th and U has the potential to map such modifications. We present the analysis of gamma-ray signatures at the Serra da Cangalha impact structure, located in northeastern Brazil, using methods for enhancing K anomalies and also the overall gamma-ray signatures. These results provide valuable information on the distinct zones within the crater and might contribute to the understanding of hydrothermal enrichment processes produced as a result of the impact event. Citation: Vasconcelos, M. A. R., E. P. Leite, and A. P. Crosta (2012), Contributions of gamma-ray spectrometry to terrestrial impact crater studies: The example of Serra da Cangalha, northeastern Brazil, Geophys. Res. Lett., 39, L04306, doi: 10.1029/2011GL050525. (AU)