Enhanced buckling due to river incision:

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Enhanced buckling due to river incision:. the Oxaya Antiform, northern Chile. Gerold Zeilinger, Fritz Schlunegger, Univ. Bern Guy Simpson, ETH Zurich. Outline. Introduction. Examples of transverse rivers intersecting anticlines in compressional belts - PowerPoint PPT Presentation

Transcript of Enhanced buckling due to river incision:

  • Enhanced buckling due to river incision:the Oxaya Antiform, northern ChileGerold Zeilinger, Fritz Schlunegger, Univ. BernGuy Simpson, ETH Zurich

  • OutlineIntroductionExamples of transverse rivers intersecting anticlines in compressional beltsCan incision amplify buckling also in active continental margins?

  • OutlineIntroductionStudy areaGeographical positionTectonic frameStratigraphy of important units Geological overview

  • OutlineIntroductionStudy areaAnticline structureOxaya Anticline geometry Basement Tertiary units unconformityTertiary units fold geometry Spatial distribution of structures

  • OutlineIntroductionStudy areaAnticline structureInterpretationTiming of anticline growth (River incision history)(Regional compression)

  • OutlineIntroductionStudy areaAnticline structureInterpretationConclusion Does the incision of the studied valleys influence the deformation of the surrounding Oxaya Anticline?

  • Worldwide examplesIntroduction

  • Worldwide examplesPyrenees: Segre River at Oliana AnticlineIntroduction

  • Worldwide examplesPyrenees: Segre River at Oliana AnticlineSwiss Alps: Reuss above Lake LucerneIntroduction

  • Worldwide examplesPyrenees: Segre River at Oliana AnticlineSwiss Alps: Reuss above Lake LucerneFrench Alps: Fier river at Val du FierIntroduction

  • Worldwide examplesPyrenees: Segre River at Oliana AnticlineSwiss Alps: Reuss above Lake LucerneFrench Alps: Fier river at Val du FierHimalaya: Arun riverIntroduction

  • Worldwide examplesPyrenees: Segre River at Oliana AnticlineSwiss Alps: Reuss above Lake LucerneFrench Alps: Fier river at Val du FierHimalaya: Arun riverApennine: Fold-thrust belt of the UmbriaMarche ApenninesIntroduction

  • LocationStudy area

  • LocationStudy area

  • LocationStudy area

  • LocationStudy area

  • StratigraphyStudy area

  • StratigraphyStudy area

  • Study area

  • StratigraphyStudy area

  • Study area

  • StratigraphyStudy area

  • Study area

  • StratigraphyStudy area

  • Study area

  • StratigraphyStudy area

  • Study area

  • StratigraphyStudy area

  • Study area

  • StratigraphyStudy area

  • Study area

  • Simplified Geological Map (after Uhlig, 1999 and Garcia, 2003 unpublished)Study area

  • Simplified Geological Map (after Uhlig, 1999 and Garcia, 2003 unpublished)Study area

  • Schematic ProfilesStudy area

  • Oxaya Anticline GeometryAnticline structure

  • Oxaya Anticline GeometryAnticline structure

  • Basement Tertiary units unconformityAnticline structureEW

  • Basement Tertiary units unconformityAnticline structureImage by Michi StrasserWE

  • Tertiary units fold geometryAnticline structureEWEWAzapa ValleyLluta Valley

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Spatial distribution of structuresAnticline structure

  • Timing of anticline growth Interpretation

  • Timing of anticline growth Interpretation

  • Timing of anticline growth Interpretation

  • Timing of anticline growth Interpretation

  • Conclusion

    The Formation of the Oxaya Anticline was enhanced by the incision of the studied valleys.Incision amplified buckling occurs also in regions not representing fold and thrust belts.The Oxaya Anticline is coherent with the results of numerical modelling of transverse rivers.Existing deformation can be substantially enhanced by surface processes

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    Geographical position of the area Tectonic frameStratigraphic of important units Geological OverviewTopographic geometry Basement Tertiary strata unconformityTertiary stratas fold geometry Spatial distribution of structuresGeographical position of the area Tectonic frameStratigraphic of important units Geological OverviewTopographic geometry Basement Tertiary strata unconformityTertiary stratas fold geometry Spatial distribution of structuresGeographical position of the area Tectonic frameStratigraphic of important units Geological OverviewTopographic geometry Basement Tertiary strata unconformityTertiary stratas fold geometry Spatial distribution of structuresGeographical position of the area Tectonic frameStratigraphic of important units Geological OverviewTopographic geometry Basement Tertiary strata unconformityTertiary stratas fold geometry Spatial distribution of structuresGeographical position of the area Tectonic frameStratigraphic of important units Geological OverviewTopographic geometry Basement Tertiary strata unconformityTertiary stratas fold geometry Spatial distribution of structures