Role of basin width variation in tectonic inversion: Insight from analogue modelling and implications for the tectonic inversion of the Abanico Basin, 32°-34°S, Central Andes
We use analogue modelling to investigate the response of compressional deformation superimposed on an extensional basin with along-strike changes in width. Parameters described include extension and shortening distribution and directions, orientation of structures and degree of basin inversion. Two...
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Geological Society of London
2015
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| LEADER | 34429caa a22019337a 4500 | ||
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| 001 | PAPER-24828 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250211090659.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84924897923 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Jara, P. | |
| 245 | 1 | 0 | |a Role of basin width variation in tectonic inversion: Insight from analogue modelling and implications for the tectonic inversion of the Abanico Basin, 32°-34°S, Central Andes |
| 260 | |b Geological Society of London |c 2015 | ||
| 270 | 1 | 0 | |m Jara, P.; Departamento de Ingeniería en Minas, Facultad de Ingeniería, Universidad de SantiagoChile |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a We use analogue modelling to investigate the response of compressional deformation superimposed on an extensional basin with along-strike changes in width. Parameters described include extension and shortening distribution and directions, orientation of structures and degree of basin inversion. Two types of model are presented: in the first (Type I), an extensional basin is constructed with variable width (applying differential extension) and subsequently inverted by homogeneous shortening; in the second (Type II), an extensional basin with constant width is subsequently inverted by inhomogeneous shortening (differential compression). From our observations, we compare both types of model to structural patterns observed in some natural cases from the Central Andes. Both models generate oblique structures, but in the Type II model a significant rotation is characteristic. Our results suggest that in the Central Andes region between 32° and 33°S, the Abanico Basin may correspond to a basin of smaller area compared to the larger basin south of 33°S. Our Type I model further explains some patterns observed there, from which we conclude that the control exercised by the width of a pre-existing basin should be considered when interpreting the geological evolution of that area of the Andes. © 2015 The Geological Society of London. |l eng | |
| 593 | |a Departamento de Ingeniería en Minas, Facultad de Ingeniería, Universidad de Santiago, Chile | ||
| 593 | |a Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Chile | ||
| 593 | |a Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Avda. Rivadavia 1917, Ciudad de Buenos Aires, CP C10AAJ, Argentina | ||
| 593 | |a Laboratorio de Modelado Geológico (LaMoGe), Instituto de Estudios Andinos Don Pablo Groeber, Universidad de Buenos Aires, Ciudad Universitaria, Buenos Aires, C128EHA, Argentina | ||
| 593 | |a Departamento de Ciencias Geológicas, Laboratorio de Tectónica Andina, Instituto de Estudios Andinos Don Pablo Groeber, Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Escuela de Ciencias de la Tierra, Universidad Andres Bello, Santiago, Chile | ||
| 651 | 4 | |a CHILE | |
| 690 | 1 | 0 | |a BASIN EVOLUTION |
| 690 | 1 | 0 | |a COMPRESSION |
| 690 | 1 | 0 | |a DEFORMATION |
| 690 | 1 | 0 | |a EXTENSIONAL TECTONICS |
| 690 | 1 | 0 | |a NUMERICAL MODEL |
| 690 | 1 | 0 | |a STRUCTURAL CONTROL |
| 690 | 1 | 0 | |a TECTONIC EVOLUTION |
| 690 | 1 | 0 | |a ABANICO |
| 690 | 1 | 0 | |a ANDES |
| 690 | 1 | 0 | |a BIO BIO |
| 700 | 1 | |a Likerman, J. | |
| 700 | 1 | |a Winocur, D. | |
| 700 | 1 | |a Ghiglione, M.C. | |
| 700 | 1 | |a Cristallini, Ernesto Osvaldo | |
| 700 | 1 | |a Pinto, L. | |
| 700 | 1 | |a Charrier, R. | |
| 773 | 0 | |d Geological Society of London, 2015 |g v. 399 |h pp. 83-107 |p Geol. Soc. Spec. Publ. |x 03058719 |t Geological Society Special Publication | |
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| 856 | 4 | 0 | |u https://doi.org/10.1144/SP399.7 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_03058719_v399_n_p83_Jara |y Handle |
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| 961 | |a paper_03058719_v399_n_p83_Jara |b paper |c PE | ||
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| 999 | |c 85781 | ||