Tectonic rotations and internal structure of Eocene plutons in Chuquicamata, northern Chile
A paleomagnetic and AMS study on Eocene plutonic complexes in the Calama area, northern Chile, reveals high-temperature, high-coercivity magnetizations of dominantly thermoremanent origin and magnetic fabrics controlled by magnetite. The paleomagnetic results indicate that ~. 43. Ma plutons underwen...
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Elsevier
2015
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| LEADER | 19983caa a22016937a 4500 | ||
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| 003 | AR-BaUEN | ||
| 005 | 20230518205646.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84937515032 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Somoza, R. | |
| 245 | 1 | 0 | |a Tectonic rotations and internal structure of Eocene plutons in Chuquicamata, northern Chile |
| 260 | |b Elsevier |c 2015 | ||
| 270 | 1 | 0 | |m Somoza, R.; Departamento de Ciencias Geológicas, Pabellón 2, Ciudad Universitaria, Argentina |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Tomlinson, A.J., Blanco, N., Dilles, J.H., Carta Calama, Región de Antofagasta. Servicio Nacional de Geología y Minería, Carta Geológica de Chile, Serie Preliminar (2010), p. 42. , 8: 3 anexos, escala 1:50.000. Santiago, Chile; Vernon, R.H., Questions about myrmekite in deformed rocks (1991) J. Struct. Geol., 13, pp. 979-985 | ||
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| 520 | 3 | |a A paleomagnetic and AMS study on Eocene plutonic complexes in the Calama area, northern Chile, reveals high-temperature, high-coercivity magnetizations of dominantly thermoremanent origin and magnetic fabrics controlled by magnetite. The paleomagnetic results indicate that ~. 43. Ma plutons underwent clockwise tectonic rotation, whereas adjacent ~. 39. Ma plutons did not undergo discernible rotation. This points to a middle Eocene age for the younger tectonic rotations associated with the Central Andean Rotation Pattern in the Chuquicamata-Calama area.The petrofabric in these rocks formed under conditions ranging from purely magmatic (i.e. before full crystallization) to low-temperature solid-state deformation. AMS and paleomagnetism suggest that the plutonic bodies were formed by progressive amalgamation of subvertical magma sheets spanning multiple magnetic polarity chrons. The parallelism between magmatic and tectonic foliations suggests that regional tectonic stress controlled ascent, emplacement and rock deformation during cooling. In this context, we suggest that magma ascent and emplacement in the upper crust likely exploited Mesozoic structures which were locally reactivated in the Eocene. © 2015 Elsevier B.V. |l eng | |
| 593 | |a IGEBA, CONICET-Universidad de Buenos Aires, Argentina | ||
| 593 | |a Servicio Nacional de Geología y Minería, Santiago, Chile | ||
| 593 | |a Instituto de Geociências, Universidade de São Paulo, Brazil | ||
| 593 | |a Department of Geosciences, Oregon State University, Corvallis, OR, United States | ||
| 690 | 1 | 0 | |a CENTRAL ANDES |
| 690 | 1 | 0 | |a CHUQUICAMATA |
| 690 | 1 | 0 | |a MAGNETIC FABRIC |
| 690 | 1 | 0 | |a TECTONIC ROTATIONS |
| 690 | 1 | 0 | |a COERCIVE FORCE |
| 690 | 1 | 0 | |a DEFORMATION |
| 690 | 1 | 0 | |a GEOMAGNETISM |
| 690 | 1 | 0 | |a MAGNETIC POLARITY |
| 690 | 1 | 0 | |a MAGNETISM |
| 690 | 1 | 0 | |a METALS |
| 690 | 1 | 0 | |a ROTATION |
| 690 | 1 | 0 | |a CENTRAL ANDES |
| 690 | 1 | 0 | |a CHUQUICAMATA |
| 690 | 1 | 0 | |a INTERNAL STRUCTURE |
| 690 | 1 | 0 | |a LOW TEMPERATURES |
| 690 | 1 | 0 | |a MAGNETIC FABRICS |
| 690 | 1 | 0 | |a REGIONAL TECTONICS |
| 690 | 1 | 0 | |a SOLID STATE DEFORMATION |
| 690 | 1 | 0 | |a TECTONIC ROTATIONS |
| 690 | 1 | 0 | |a TECTONICS |
| 690 | 1 | 0 | |a DEFORMATION |
| 690 | 1 | 0 | |a EMPLACEMENT |
| 690 | 1 | 0 | |a EOCENE |
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| 690 | 1 | 0 | |a HIGH TEMPERATURE |
| 690 | 1 | 0 | |a MAGNETIC FABRIC |
| 690 | 1 | 0 | |a PALEOMAGNETISM |
| 690 | 1 | 0 | |a TECTONIC ROTATION |
| 690 | 1 | 0 | |a THERMOREMANENT MAGNETIZATION |
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a ANTOFAGASTA |
| 690 | 1 | 0 | |a CALAMA |
| 650 | 1 | 7 | |2 spines |a PLUTON |
| 651 | 4 | |a CHILE | |
| 700 | 1 | |a Tomlinson, A.J. | |
| 700 | 1 | |a Zaffarana, C.B. | |
| 700 | 1 | |a Singer, S.E. | |
| 700 | 1 | |a Puigdomenech Negre, C.G. | |
| 700 | 1 | |a Raposo, M.I.B. | |
| 700 | 1 | |a Dilles, J.H. | |
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