Anisotropy of magnetic susceptibility study in two classical localities of the Gastre Fault System, central Patagonia
The Central Patagonian Batholith is a suite of acid and meso-silicic rocks cropping out in central Patagonia. The emplacement of these rocks has been proposed to be related to the activity of a system of dextral transcurrent faults, the NW-SE Gastre Fault System. This fault system has been ascribed...
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2010
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| 005 | 20250724143129.0 | ||
| 008 | 190411s2010 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-78649850254 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Zaffarana, C.B. | |
| 245 | 1 | 0 | |a Anisotropy of magnetic susceptibility study in two classical localities of the Gastre Fault System, central Patagonia |
| 260 | |c 2010 | ||
| 270 | 1 | 0 | |m Zaffarana, C.B.; Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos AiresArgentina; email: zaffarana@gl.fcen.uba.ar |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a The Central Patagonian Batholith is a suite of acid and meso-silicic rocks cropping out in central Patagonia. The emplacement of these rocks has been proposed to be related to the activity of a system of dextral transcurrent faults, the NW-SE Gastre Fault System. This fault system has been ascribed a transcontinental magnitude and a ∼500 km dextral displacement during Gondwana dismembering in Jurassic times. However, the timing, kinematics and amount of displacement of the Gastre Fault System are still controversial. In this work we have visited two localities which were subject of controversial observations, in order to perform petrographical, microstructural and anisotropy of the magnetic susceptibility studies to contribute to the ongoing discussion. The results mostly agree with the findings von Gosen and Loske (2004) in that rocks spatially and temporally associated to the Gastre Fault System do not show evidence supporting the existence of a major dextral fault system active during Jurassic times. © 2010 Elsevier Ltd. |l eng | |
| 593 | |a Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Argentina | ||
| 593 | |a Consejo Nacional de Investigaciones Científicas, Técnicas (CONICET), Argentina | ||
| 593 | |a Instituto de Geocronología, Geología Isotópica (INGEIS), Argentina | ||
| 593 | |a Departamento de Física, Facultad de Ciencias Exactas, Universidad Nacional de La Plata, Argentina | ||
| 593 | |a Servicio Geológico Minero Argentino (SEGEMAR), Argentina | ||
| 593 | |a Departamento de Geología Básica, Facultad de Ciencias Exactas y Naturales, Universidad de Nacional de Córdoba, Argentina | ||
| 690 | 1 | 0 | |a GASTRE |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a TRANSCONTINENTAL FAULT |
| 690 | 1 | 0 | |a WEST GONDWANA BREAKUP |
| 690 | 1 | 0 | |a BATHOLITH |
| 690 | 1 | 0 | |a CONTINENTAL BREAKUP |
| 690 | 1 | 0 | |a DISPLACEMENT |
| 690 | 1 | 0 | |a FAULTING |
| 690 | 1 | 0 | |a GEOMAGNETISM |
| 690 | 1 | 0 | |a GONDWANA |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a KINEMATICS |
| 690 | 1 | 0 | |a MAGNETIC ANISOTROPY |
| 690 | 1 | 0 | |a PATAGONIA |
| 700 | 1 | |a López de luchi, M.G. | |
| 700 | 1 | |a Somoza, R. | |
| 700 | 1 | |a Mercader, Roberto Carlos | |
| 700 | 1 | |a Giacosa, R. | |
| 700 | 1 | |a Martino, R.D. | |
| 773 | 0 | |d 2010 |g v. 30 |h pp. 151-166 |k n. 3-4 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
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