Esquema de tres interfaces con compensación isostática local en el margen continental Argentino
In the present paper, we investigate the Airy type isostatic compensation scheme for three interfaces:water-sediments, sediments-crust and crust-mantle, using forward modelling to calculate the isostaticanomaly with different approximations of Parkers expression in the Argentine continentalmargin. T...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2016 |
| País: | Argentina |
| Institución: | Consejo Nacional de Investigaciones Científicas y Técnicas |
| Repositorio: | CONICET Digital (CONICET) |
| Idioma: | español |
| OAI Identifier: | oai:ri.conicet.gov.ar:11336/112766 |
| Acceso en línea: | http://hdl.handle.net/11336/112766 |
| Access Level: | acceso abierto |
| Palabra clave: | ISOSTASIA ANOMALÍAS DE GRAVEDAD MARGEN CONTINENTAL ARGENTINO DESARROLLO DE PARKER https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| Sumario: | In the present paper, we investigate the Airy type isostatic compensation scheme for three interfaces:water-sediments, sediments-crust and crust-mantle, using forward modelling to calculate the isostaticanomaly with different approximations of Parkers expression in the Argentine continentalmargin. The isostatic anomaly is estimated as the residue between the observed free air anomaly andthe calculated free air anomaly through the sum of the contributions from the tree interfaces.After that, we perform the inversion of the isostatic anomaly in order to find the deflection of theMoho necessary to compensate it (or minimize it) using one term of Parkers expression in the inversion,as an experiment to test the numerical methods. The Moho here considered is obtained fromknowing the depth of the basement and crustal thickness. Another way to estimate the crust-mantleinterface (Moho) is by the inversion with the iterative method of Parker-Oldenburg (Parker, 1973;Oldenburg, 1974), which allows inverting the Bouguer anomaly with more than one term. With theMoho thus obtained, a free-air gravity anomaly can be calculated, which reproduces the observedanomaly quite well. Even considering that the experiment constitutes a schematic model just to testthe numerical methods involved, from the comparison with the only available digitized refractionprofile in the study area, we find that the large wavelength of the inverted Moho is reproduced fairlywell by the modeled Moho for both methods. However, the iterative method yields smoother surfaces,possibly more realistic surfaces given the roughness that the other estimates present. |
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