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dc.rights.licenseIn Copyrighten_US
dc.creatorCoppersmith, Ryan Thomas
dc.date.accessioned2023-10-20T15:49:32Z
dc.date.available2023-10-20T15:49:32Z
dc.date.created2006
dc.identifierWLURG038_Coppersmith_thesis_2006
dc.identifier.urihttps://dspace.wlu.edu/handle/11021/36279
dc.description.abstractHigh-resolution remote sensing data and 3D modeling techniques offer new tools for structural analysis that improve on the efficiency, accuracy and precision of geologic mapping, and provide insight into the structure of an area that is difficult to obtain otherwise. I combine conventional remote sensing data and geologic mapping with laser survey data into a complete 3D model that constrains the surface and subsurface geometry of a part of the Catalan Coastal Range at the edge of the Ebro Basin, Spain. For lower relief areas two approaches are used to interpret orthophotos: I interpret on orthophotos in map view and then visualize the interpretation in 3D by draping the interpretation and photos over digital elevation models, secondly I interpret directly on the draped orthophotos. I find the latter approach to be much more accurate in interpreting the surface geology. In areas that are impossible to map in a conventional sense with any precision, such as vertical cliff faces 100' s of meters high, I employ 20 cm resolution ground-based LID AR. These data are of such high fidelity that surfaces generated from the scans allow delineation of individual beds that can be interpreted directly on the surface in 3D, similar to interpreting draped orthophotos as discussed above. To extend the surface interpretation into the subsurface I use a technique exploiting the local 3D information of surface contacts with cross section construction to ultimately build a self-consistent 3D model. For surface contacts that have demonstrable relief change, a shallow subsurface 3D model is created. These provide local structural control for cross-section construction. The cross sections are then used as a framework for building of a 3D model. I found that making use of surface data in a 3D environment such as that described above provides additional understanding of the structure of an area than cannot be obtained by conventional mapping alone.en_US
dc.format.extent51 pagesen_US
dc.language.isoen_USen_US
dc.rightsThis material is made available for use in research, teaching, and private study, pursuant to U.S. Copyright law. The user assumes full responsibility for any use of the materials, including but not limited to, infringement of copyright and publication rights of reproduced materials. Any materials used should be fully credited with the source.en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.subject.otherWashington and Lee University -- Honors in Geologyen_US
dc.title3D Structural Modeling Using Remote Sensing and Ground-Based LIDARen_US
dc.typeTexten_US
dcterms.isPartOfWLURG038 - Student Papersen_US
dc.rights.holderCoppersmith, Ryan Thomasen_US
dc.subject.fastGeology, Structural -- Remote sensing -- Spain -- Cataloniaen_US
dc.subject.fastGeological modelingen_US
dc.subject.fastOptical radar -- Observationsen_US
local.departmentGeologyen_US


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