Paleomagnetic study along the southeastern edge of the Altiplano - Puna Plateau: Neogene tectonic rotations
In northwestern Argentina the transition zone between the Puna and the Sierras Pampeanas was deformed in Late Miocene and Pliocene time. Structural observations suggest that local clockwise block rotations might be observed associated with dextral transpression. This study contributes new paleomagne...
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American Geophysical Union
1996
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| LEADER | 16301caa a22011897a 4500 | ||
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| 001 | PAPER-18809 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205010.0 | ||
| 008 | 190411s1996 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-3743068238 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Aubry, L. | |
| 245 | 1 | 0 | |a Paleomagnetic study along the southeastern edge of the Altiplano - Puna Plateau: Neogene tectonic rotations |
| 260 | |b American Geophysical Union |c 1996 | ||
| 270 | 1 | 0 | |m Aubry, L.; Géosciences Rennes, CNRS (UPR 4661), Campus de Beaulieu, 35042 Rennes, France |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a In northwestern Argentina the transition zone between the Puna and the Sierras Pampeanas was deformed in Late Miocene and Pliocene time. Structural observations suggest that local clockwise block rotations might be observed associated with dextral transpression. This study contributes new paleomagnetic results from four sites in Cretaceous rocks and 19 sites in Neogene sedimentary sequences. When compared with reference paleomagnetic data for stable continental South America, the results show an average inclination shallowing error of 10.5° and a pattern of clockwise rotations up to 29°. Study of the anisotropy of magnetic susceptibility (AMS) on 278 specimens provided, for most sites, AMS tensors with an oblate shape controlled by sedimentation and compaction, explaining the observed inclination shallowing. A slight AMS lineation was measured and we argue that this magnetic lineation reflects Late Miocene-Pliocene compression. A correlation observed between magnetic lineations, deduced from the AMS analysis, and rotation estimates from remanent magnetizations, demonstrates that the inferred shortening directions have also been rotated clockwise. |l eng | |
| 593 | |a Géosciences Rennes, CNRS UPR 4661, Rennes, France | ||
| 593 | |a Inst. Francais Rech. Sci. Devmt. C., ORSTOM, Universidad de Chile, Santiago, Chile | ||
| 593 | |a Consejo Natl. de Invest. Cie. y Tec., Depto. de Ciencias Geológicas, Universidad de Buenos Aires, Argentina | ||
| 593 | |a Géosciences Rennes, CNRS (UPR 4661), Campus de Beaulieu, 35042 Rennes, France | ||
| 593 | |a ORSTOM, Departamento de Geologia y Geofisica, Correo Central, casilla 53390, Santiago 1, Chile | ||
| 593 | |a Depto. de Ciencias Geológicas, Ciudad Universitaria, 1428 Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a MAGNETIC LINEATION |
| 690 | 1 | 0 | |a NEOGENE |
| 690 | 1 | 0 | |a PALAEOMAGNETISM |
| 690 | 1 | 0 | |a TECTONIC ROTATION |
| 651 | 4 | |a ARGENTINA, ANDES | |
| 700 | 1 | |a Roperch, P. | |
| 700 | 1 | |a De Urreiztieta, M. | |
| 700 | 1 | |a Rossello, E. | |
| 700 | 1 | |a Chauvin, A. | |
| 773 | 0 | |d American Geophysical Union, 1996 |g v. 101 |h pp. 17883-17899 |k n. 8 |p J. Geophys. Res. B Solid Earth |x 21699313 |w (AR-BaUEN)CENRE-151 |t Journal of Geophysical Research B: Solid Earth | |
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