Application of Slope Maps as a Complement of Bathymetry: Example from the SW Atlantic
Topographic and bathymetric maps are commonly used to represent the morphology of the Earth's surface at different scales. However, there are specific geological aspects or features that may be masked or not sufficiently highlighted by solely those data. This article shows how the slope maps (o...
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2017
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| 008 | 190410s2017 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85011903588 | |
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| 100 | 1 | |a Esteban, F.D. | |
| 245 | 1 | 0 | |a Application of Slope Maps as a Complement of Bathymetry: Example from the SW Atlantic |
| 260 | |b Taylor and Francis Inc. |c 2017 | ||
| 270 | 1 | 0 | |m Esteban, F.D.; CONICET-Instituto de Geociencias Básicas, Ambientales y Aplicadas (IGEBA), Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad UniversitariaArgentina; email: esteban@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Topographic and bathymetric maps are commonly used to represent the morphology of the Earth's surface at different scales. However, there are specific geological aspects or features that may be masked or not sufficiently highlighted by solely those data. This article shows how the slope maps (or clinometrics), elaborated from the same bathymetric data, are a useful tool to overcome these limitations. To this purpose, we analysed an example of the South-Western Atlantic area where a slope map was produced from the General Bathymetric Chart of the Oceans (GEBCO) bathymetric grid. We show how the slope maps can significantly improve the morpho-bathymetric (or topographical) descriptions and allow extrapolation of interpretations or observations from analysis of seismic sections, identification or highlighting of small morpho-structures, and inference and the distinguishing of areas of diverse morphologies in relation with the sedimentary processes. We propose and discuss the use of slope maps as a complement to bathymetric maps for specific geological studies at macro- and meso-scales. © 2017 Taylor & Francis Group, LLC. |l eng | |
| 536 | |a Detalles de la financiación: PICT 2013 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, 112201101 00618 | ||
| 536 | |a Detalles de la financiación: The authors thank the two anonymous reviewers for constructive comments and suggestions that improved the paper. This work was partially funded by the Agencia Nacional para la Promoci?n de la Ciencia y Tecnolog?a (ANPCyT-FONCyT) with grant PICT 2013 No. 2236 Tipo I (A) and by CONICET through PIP-CONICET No. 112201101 00618. | ||
| 593 | |a CONICET-Instituto de Geociencias Básicas, Ambientales y Aplicadas (IGEBA), Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Dipartimento di Scienze della Terra, Vita e dell'Ambiente dell'Universita di Urbino, Urbino, Italy | ||
| 593 | |a Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Trieste, Italy | ||
| 690 | 1 | 0 | |a BATHYMETRY |
| 690 | 1 | 0 | |a GEOMORPHOMETRY |
| 690 | 1 | 0 | |a SLOPE |
| 690 | 1 | 0 | |a SOUTHWESTERN ATLANTIC |
| 690 | 1 | 0 | |a TERRAIN ANALYSIS |
| 690 | 1 | 0 | |a BATHYMETRY |
| 690 | 1 | 0 | |a MAP |
| 690 | 1 | 0 | |a MORPHOMETRY |
| 690 | 1 | 0 | |a MORPHOSTRUCTURE |
| 690 | 1 | 0 | |a SLOPE |
| 690 | 1 | 0 | |a TERRAIN |
| 690 | 1 | 0 | |a TOPOGRAPHY |
| 690 | 1 | 0 | |a ATLANTIC OCEAN |
| 690 | 1 | 0 | |a ATLANTIC OCEAN (SOUTHWEST) |
| 700 | 1 | |a Tassone, A. | |
| 700 | 1 | |a Menichetti, M. | |
| 700 | 1 | |a Lodolo, E. | |
| 773 | 0 | |d Taylor and Francis Inc., 2017 |g v. 40 |h pp. 57-71 |k n. 1 |p Mar. Geod. |x 01490419 |w (AR-BaUEN)CENRE-6018 |t Marine Geodesy | |
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