Plume overriding triggers shallow subduction and orogeny in the southern Central Andes
Plate tectonic theory implies that mantle plumes may be eventually overridden by lithosphere during continental drift. These events have particular tectonomagmatic consequences for active margins and hence related orogenic processes. Since the first documentation of plume overriding and the definiti...
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2017
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| LEADER | 21035caa a22012857a 4500 | ||
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| 003 | AR-BaUEN | ||
| 005 | 20230518205728.0 | ||
| 008 | 190410s2017 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85032695643 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Gianni, G.M. | |
| 245 | 1 | 0 | |a Plume overriding triggers shallow subduction and orogeny in the southern Central Andes |
| 260 | |b Elsevier Inc. |c 2017 | ||
| 270 | 1 | 0 | |m Gianni, G.M.; IGSV, Instituto Geofísico Sismológico Ing. Volponi, Universidad Nacional de San Juan, CONICETArgentina; email: guidogianni22@gmail.com |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Plate tectonic theory implies that mantle plumes may be eventually overridden by lithosphere during continental drift. These events have particular tectonomagmatic consequences for active margins and hence related orogenic processes. Since the first documentation of plume overriding and the definition of the plume-modified orogeny concept, only few examples have been recognized in the geologic record. In this study, we analyze the Neogene tectonic evolution of the Southern Central Andes between 35° and 38°S and its potential relation to the subduction of the Payenia plume as a recent analogue of this process. Through a series of tectonic reconstructions we show that progressive Payenia plume overriding correlates with Neogene arc-front migrations linked to slab shallowing, fold belt reactivation in the Main Cordillera and intraplate contraction in the San Rafael block. Additionally, Nazca slab tear determined from tomographic analyses and subsequent diachronous steepening of the subducted plate may also be an aftermath of plume subduction as often described in the final stages of plume-modified orogeny. Finally, we propose a modern analogue for processes previously described, dating back to the Mesoproterozoic, which provides further insights into these complex settings. © 2017 International Association for Gondwana Research |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PICT 2014 1967 | ||
| 536 | |a Detalles de la financiación: This study was supported by the Consejo Nacional de Investigaciones Científicas y Técnicas ( CONICET ) ( PICT 2014 1967 ). This contribution is part of G.M. Gianni postdoctoral studies at the Universidad Nacional de San Juan. We want to dedicate this study to the memory of Dr. Rubén Somoza. We thank editor Dr. Franco Pirajno for manuscript handling and reviewers Dr. Paul Holm and Dr. Brendan Murphy for their constructive suggestions. | ||
| 593 | |a IGSV, Instituto Geofísico Sismológico Ing. Volponi, Universidad Nacional de San Juan, CONICET, Argentina | ||
| 593 | |a IDEAN, Instituto de Estudios Andinos, Universidad de Buenos Aires-CONICET, Argentina | ||
| 690 | 1 | 0 | |a FLAT-SLAB |
| 690 | 1 | 0 | |a FOLD AND THRUST BELT |
| 690 | 1 | 0 | |a PLUME-MODIFIED OROGENESIS |
| 690 | 1 | 0 | |a PLUME-SUBDUCTION ZONE INTERACTION |
| 700 | 1 | |a García, H.P.A. | |
| 700 | 1 | |a Lupari, M. | |
| 700 | 1 | |a Pesce, A. | |
| 700 | 1 | |a Folguera, A. | |
| 773 | 0 | |d Elsevier Inc., 2017 |g v. 49 |h pp. 387-395 |p Gondwana Res. |x 1342937X |t Gondwana Research | |
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