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Paleomagnetic data from the Precordillera of northern Chile: A multiphase rotation history related to a multiphase deformational history
| Indexado |
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| DOI | 10.1016/J.TECTO.2020.228569 | ||||
| Año | 2020 | ||||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
Abstract
Current models propose that rotations in CARP were entirely Cenozoic and largely accomplished in a single Paleogene event. Our data indicate that each of the Peruvian, K-T and Incaic deformation events contributed to CARP, with each event generating a non-uniform pattern of rotations which was superimposed on prior rotations in a non-uniform manner.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | Puigdomenech, C. | - |
Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) - Argentina
Consejo Nacional de Investigaciones Científicas y Técnicas - Argentina |
| 2 | Somoza, R. | Hombre |
Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) - Argentina
Consejo Nacional de Investigaciones Científicas y Técnicas - Argentina |
| 3 | Tomlinson, Andrew J. | Hombre |
Servicio Nacional de Geología y Minería - Chile
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| 4 | Renda, E. M. | - |
Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) - Argentina
Consejo Nacional de Investigaciones Científicas y Técnicas - Argentina |
| Fuente |
|---|
| Agencia Nacional de Promoción Científica y Tecnológica |
| ANPCyT |
| Agencia Nacional de Promoción CientÃfica y Tecnológica |
| National Subdirection of Geology, SERNAGEOMIN |
| Agradecimiento |
|---|
| We dedicate this paper to the loving memory of our friend and teacher Ruben Somoza. This research was partially funded by ANPCyT PICT2012-1302 and support for AT was provided by the National Subdirection of Geology, SERNAGEOMIN. We thank S. Geuna, L. Gallo and A. Rapalini for reading and improving the manuscript. Super IAPD software packages by Torsvik (NGU) and Remasoft program (AGICO SA) were used to analyze the data. Carlos A. Vazquez and Matias Naselli kindly collaborated during preparation of samples and running of hysteresis loops. Discussion with them of some rock magnetic results are also acknowledged. Thanks to the two anonymous referees for provided careful and constructive reviews to our manuscript. |
| We dedicate this paper to the loving memory of our friend and teacher Rubén Somoza. This research was partially funded by ANPCyT PICT2012-1302 and support for AT was provided by the National Subdirection of Geology, SERNAGEOMIN. We thank S. Geuna, L. Gallo and A. Rapalini for reading and improving the manuscript. Super IAPD software packages by Torsvik (NGU) and Remasoft program (AGICO SA) were used to analyze the data. Carlos A. Vazquez and Matias Naselli kindly collaborated during preparation of samples and running of hysteresis loops. Discussion with them of some rock magnetic results are also acknowledged. Thanks to the two anonymous referees for provided careful and constructive reviews to our manuscript. |
