Seeing beyond the outcrop

Paleokarst breccias are a common feature of sedimentary rift basins. The Billefjorden Trough in the High Arctic archipelago of Svalbard is an example of such a rift. Here the Carboniferous stratigraphy exhibits intervals of paleokarst breccias formed by gypsum dissolution. In this study we integrate...

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Published in:Marine and Petroleum Geology
Main Authors: Janocha, Julian, Smyrak-Sikora, Aleksandra, Senger, Kim, Birchall, Thomas
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/63964
https://doi.org/10.1016/j.marpetgeo.2020.104833
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:63964 2024-06-23T07:48:51+00:00 Seeing beyond the outcrop Janocha, Julian Smyrak-Sikora, Aleksandra Senger, Kim Birchall, Thomas 2021-03-01 https://publishup.uni-potsdam.de/frontdoor/index/index/docId/63964 https://doi.org/10.1016/j.marpetgeo.2020.104833 eng eng https://publishup.uni-potsdam.de/frontdoor/index/index/docId/63964 https://doi.org/10.1016/j.marpetgeo.2020.104833 https://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/closedAccess ddc:550 Institut für Geowissenschaften article doc-type:article 2021 ftubpotsdam https://doi.org/10.1016/j.marpetgeo.2020.104833 2024-06-12T00:45:21Z Paleokarst breccias are a common feature of sedimentary rift basins. The Billefjorden Trough in the High Arctic archipelago of Svalbard is an example of such a rift. Here the Carboniferous stratigraphy exhibits intervals of paleokarst breccias formed by gypsum dissolution. In this study we integrate digital outcrop models (DOMs) with a 2D ground penetrating radar (GPR) survey to extrapolate external irregular paleokarst geometries beyond the 2D outcrops. DOMs are obtained through combining a series of overlapping photographs with structure-frommotion photogrammetry, to create mmto dm-resolution georeferenced DOMs. GPR is typically used for surveying the shallow subsurface and relies on detecting the contrasts in electro-magnetic permittivity. We defined three geophysical facies based on their appearance in GPR. By integrating subsurface geophysical data with DOMs we were able to correlate reflection patterns in GPR with outcrop features. The chaotic nature of paleokarst breccias is seen both in outcrop and GPR. Key horizons in outcrop and the GPR profiles allow tying together observations between these methods. Furthermore, we show that this technique expands the twodimensional outcrop surface into a three-dimensional domain, thus complementing, strengthening and extending outcrop interpretations. Article in Journal/Newspaper Arctic Archipelago Arctic Billefjorden Svalbard University of Potsdam: publish.UP Arctic Svalbard Billefjorden ENVELOPE(16.417,16.417,78.563,78.563) Marine and Petroleum Geology 125 104833
institution Open Polar
collection University of Potsdam: publish.UP
op_collection_id ftubpotsdam
language English
topic ddc:550
Institut für Geowissenschaften
spellingShingle ddc:550
Institut für Geowissenschaften
Janocha, Julian
Smyrak-Sikora, Aleksandra
Senger, Kim
Birchall, Thomas
Seeing beyond the outcrop
topic_facet ddc:550
Institut für Geowissenschaften
description Paleokarst breccias are a common feature of sedimentary rift basins. The Billefjorden Trough in the High Arctic archipelago of Svalbard is an example of such a rift. Here the Carboniferous stratigraphy exhibits intervals of paleokarst breccias formed by gypsum dissolution. In this study we integrate digital outcrop models (DOMs) with a 2D ground penetrating radar (GPR) survey to extrapolate external irregular paleokarst geometries beyond the 2D outcrops. DOMs are obtained through combining a series of overlapping photographs with structure-frommotion photogrammetry, to create mmto dm-resolution georeferenced DOMs. GPR is typically used for surveying the shallow subsurface and relies on detecting the contrasts in electro-magnetic permittivity. We defined three geophysical facies based on their appearance in GPR. By integrating subsurface geophysical data with DOMs we were able to correlate reflection patterns in GPR with outcrop features. The chaotic nature of paleokarst breccias is seen both in outcrop and GPR. Key horizons in outcrop and the GPR profiles allow tying together observations between these methods. Furthermore, we show that this technique expands the twodimensional outcrop surface into a three-dimensional domain, thus complementing, strengthening and extending outcrop interpretations.
format Article in Journal/Newspaper
author Janocha, Julian
Smyrak-Sikora, Aleksandra
Senger, Kim
Birchall, Thomas
author_facet Janocha, Julian
Smyrak-Sikora, Aleksandra
Senger, Kim
Birchall, Thomas
author_sort Janocha, Julian
title Seeing beyond the outcrop
title_short Seeing beyond the outcrop
title_full Seeing beyond the outcrop
title_fullStr Seeing beyond the outcrop
title_full_unstemmed Seeing beyond the outcrop
title_sort seeing beyond the outcrop
publishDate 2021
url https://publishup.uni-potsdam.de/frontdoor/index/index/docId/63964
https://doi.org/10.1016/j.marpetgeo.2020.104833
long_lat ENVELOPE(16.417,16.417,78.563,78.563)
geographic Arctic
Svalbard
Billefjorden
geographic_facet Arctic
Svalbard
Billefjorden
genre Arctic Archipelago
Arctic
Billefjorden
Svalbard
genre_facet Arctic Archipelago
Arctic
Billefjorden
Svalbard
op_relation https://publishup.uni-potsdam.de/frontdoor/index/index/docId/63964
https://doi.org/10.1016/j.marpetgeo.2020.104833
op_rights https://creativecommons.org/licenses/by/4.0/
info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1016/j.marpetgeo.2020.104833
container_title Marine and Petroleum Geology
container_volume 125
container_start_page 104833
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