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dc.date.accessioned 2021-09-14T17:22:46Z
dc.date.available 2021-09-14T17:22:46Z
dc.identifier.uri http://sedici.unlp.edu.ar/handle/10915/124802
dc.description.abstract Structure from Motion–Multi-View Stereo (SfM-MVS) is a relatively new technique that is being adopted in the analysis of sedimentary systems. The technique is especially applicable to studies which focus on the distribution, geometry and quantification of geological bodies including the analysis of sedimentary forms and tectonic structures. This photogrammetric method allows for generating virtual outcrops (VO) and high-resolution digital terrain models (DTMs). In comparison with more sophisticated and expensive techniques such as airborne LiDAR scanning or terrestrial laser scanning, SfM-MVS is a fast low-cost method which with careful use of ground control points, can produce models which are comparable to other digital survey methods for spatial accuracy. In this study, the effectiveness of SfM-MVS in a series of quantitative case studies in sedimentary and basin analyses is discussed. Focus is placed on how the research questions define the workflow strategy to know the limitations, sources of error and potential utility that the SFM-MVS technique has when a virtual sedimentary system is interpreted. Three case studies of different sedimentary environments, previously analyzed with traditional fieldwork techniques, were selected and re-analyzed. For each case study the objective was to resolve quantitative questions that were not possible to determine without the use of VO or DTMs. Questions include: (i) geometrical restoration of a growth strata succession associated with thrust systems; (ii) stacking patterns of littoral ridges during a relative sea-level fall after the Holocene climatic optimum; and (iii) quantification of lake level fall during the past 44 years of a closed lake basin. The results of the work show that the technique has significant application in the analysis of sedimentary systems. However, since geological interpretations depend on the quality of the models that are generated, planning and construction of the VO or DEMs along with their validation are essential to ensure reliable results. en
dc.format El conjunto de datos se compone de las siguiente información: Table 1. Control points RMSE (Case study 1) Table 2. Control points of Case study 1 Table 3. Control points RMSE (Case study 2) Table 4. Check points RMSE (Case study 2) Table 5. Control points of case study 2 Table 6. Check points of case study 2 Table 7. Control points RMSE (Case Study 3) Table 8. Control points of Case Study 3 es
dc.language en es
dc.subject Virtual outcrops es
dc.subject High-resolution digital terrain models es
dc.subject Acquisition es
dc.subject Validation es
dc.subject Virtual analysis es
dc.title Data for: Digital outcrop modelling using “structure-from- motion” photogrammetry: acquisition strategies, validation and interpretations to different sedimentary environments en
dc.type Conjunto de datos es
sedici.identifier.other https://doi.org/10.17632/p2gwkfgm3n.1 es
sedici.creator.person Bilmes, Andrés es
sedici.creator.person D'Elia, Leandro es
sedici.creator.person Varela, Augusto Nicolás es
sedici.creator.person Álvarez, María del Pilar es
sedici.creator.person Eymard, Inès Pauline Marie es
sedici.creator.person Richiano, Sebastián Miguel es
sedici.creator.person Franzese, Juan Rafael es
sedici.creator.person Muravchick, Martín es
sedici.creator.person Bucher, Joaquín es
sedici.creator.person Ariztegui, Daniel es
sedici.creator.person López, Luciano es
sedici.subject.materias Geología es
sedici.description.fulltext true es
mods.originInfo.place Centro de Investigaciones Geológicas es
sedici.subtype Conjunto de datos es
sedici.rights.license Creative Commons Attribution 4.0 International (CC BY 4.0)
sedici.rights.uri http://creativecommons.org/licenses/by/4.0/
sedici.relation.isRelatedWith http://sedici.unlp.edu.ar/handle/10915/124602 es
dc.date.created 2019-08-31
sedici.subject.ford Ciencias de la tierra y ambientales es
dc.description.filiation Fil: Álvarez, María del Pilar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico. Instituto Patagónico para el Estudio de los Ecosistemas Continentales; Argentina.
dc.description.filiation Fil: Bilmes, Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Nacional Patagónico. Instituto de Geología y Paleontología; Argentina.
dc.description.filiation Fil: Bucher, Joaquín. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
dc.description.filiation Fil: D'Elia, Leandro. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina.
dc.description.filiation Fil: Franzese, Juan Rafael. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina.
dc.description.filiation Fil: López, Luciano. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina.
dc.description.filiation Fil: López, Luciano. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
dc.description.filiation Fil: Richiano, Sebastián Miguel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Instituto Patagónico de Geología y Paleontología; Argentina
dc.description.filiation Fil: Varela, Augusto Nicolás. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Cátedra de Micromorfología de Suelos; Argentina. YPF - Tecnología; Argentina.
dc.description.filiation Fil: Varela, Augusto Nicolás. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina


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Creative Commons Attribution 4.0 International (CC BY 4.0) Excepto donde se diga explícitamente, este item se publica bajo la siguiente licencia Creative Commons Attribution 4.0 International (CC BY 4.0)