Visualizing Paleocurrents in a Web Application using GPlates

Paleocurrents are flow directions derived from features of sedimentary rocks that reveal the sense of the current of wind or water that deposited the sediment. In 2015, Brand, L. et al (doi:10.1038/sdata.2015.25) created a global database of paleaocurrents, which contains over 1,000,000 measurements...

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Main Authors: Sapkota, Anjan, Alférez, Germán Harvey, Chadwick, Arthur V
Format: Text
Language:unknown
Published: Knowledge Exchange 2023
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Online Access:https://knowledge.e.southern.edu/facworks_comp/16
https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1344812
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spelling ftsouthadventuni:oai:knowledge.e.southern.edu:facworks_comp-1015 2024-02-11T09:58:46+01:00 Visualizing Paleocurrents in a Web Application using GPlates Sapkota, Anjan Alférez, Germán Harvey Chadwick, Arthur V 2023-12-14T08:00:00Z https://knowledge.e.southern.edu/facworks_comp/16 https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1344812 unknown Knowledge Exchange https://knowledge.e.southern.edu/facworks_comp/16 https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1344812 Faculty Works Paleocurrents GPlates Data Visualization Computer Sciences Earth Sciences text 2023 ftsouthadventuni 2024-01-20T23:36:52Z Paleocurrents are flow directions derived from features of sedimentary rocks that reveal the sense of the current of wind or water that deposited the sediment. In 2015, Brand, L. et al (doi:10.1038/sdata.2015.25) created a global database of paleaocurrents, which contains over 1,000,000 measurements worldwide: North America, South America, Australia, Great Britain, parts of Western Europe, China, Africa fairly well represented. Antarctica, Eastern Europe, Asia modestly represented. Russia poorly represented. The contribution of this research project is a web application that uses the GPlates’ Application Programming Interface (API) to visualize global paleocurrents through time in an interactive way based on the data collected by Brand et al. This visualization shows the following: Precambrian: North American paleocurrents are variable and show no distinctive continent-wide patterns. Paleozoic: Paleocurrents show patterns that are continent-wide and typically flow towards the southwest across the continent. Mesozoic: Patterns are continent-wide and typically flow toward the east across the continent. North American paleocurrents are again variable and do not show continent-wide patterns. These trends are not expected in the model of conventional basinal geology. These trends show sedimentation on a scale larger than that predicted by conventional geologic models, suggesting such models may be inadequate. Continent-wide paleocurrents are unexpected (anomalous) but recognized and probably could be accommodated in conventional models. Supracontinental (megatrends) are unexpected and unrecognized and probably cannot be accommodated in conventional models. Text Antarc* Antarctica Southern Adventist University: KnowledgeExchange@Southern
institution Open Polar
collection Southern Adventist University: KnowledgeExchange@Southern
op_collection_id ftsouthadventuni
language unknown
topic Paleocurrents
GPlates
Data Visualization
Computer Sciences
Earth Sciences
spellingShingle Paleocurrents
GPlates
Data Visualization
Computer Sciences
Earth Sciences
Sapkota, Anjan
Alférez, Germán Harvey
Chadwick, Arthur V
Visualizing Paleocurrents in a Web Application using GPlates
topic_facet Paleocurrents
GPlates
Data Visualization
Computer Sciences
Earth Sciences
description Paleocurrents are flow directions derived from features of sedimentary rocks that reveal the sense of the current of wind or water that deposited the sediment. In 2015, Brand, L. et al (doi:10.1038/sdata.2015.25) created a global database of paleaocurrents, which contains over 1,000,000 measurements worldwide: North America, South America, Australia, Great Britain, parts of Western Europe, China, Africa fairly well represented. Antarctica, Eastern Europe, Asia modestly represented. Russia poorly represented. The contribution of this research project is a web application that uses the GPlates’ Application Programming Interface (API) to visualize global paleocurrents through time in an interactive way based on the data collected by Brand et al. This visualization shows the following: Precambrian: North American paleocurrents are variable and show no distinctive continent-wide patterns. Paleozoic: Paleocurrents show patterns that are continent-wide and typically flow towards the southwest across the continent. Mesozoic: Patterns are continent-wide and typically flow toward the east across the continent. North American paleocurrents are again variable and do not show continent-wide patterns. These trends are not expected in the model of conventional basinal geology. These trends show sedimentation on a scale larger than that predicted by conventional geologic models, suggesting such models may be inadequate. Continent-wide paleocurrents are unexpected (anomalous) but recognized and probably could be accommodated in conventional models. Supracontinental (megatrends) are unexpected and unrecognized and probably cannot be accommodated in conventional models.
format Text
author Sapkota, Anjan
Alférez, Germán Harvey
Chadwick, Arthur V
author_facet Sapkota, Anjan
Alférez, Germán Harvey
Chadwick, Arthur V
author_sort Sapkota, Anjan
title Visualizing Paleocurrents in a Web Application using GPlates
title_short Visualizing Paleocurrents in a Web Application using GPlates
title_full Visualizing Paleocurrents in a Web Application using GPlates
title_fullStr Visualizing Paleocurrents in a Web Application using GPlates
title_full_unstemmed Visualizing Paleocurrents in a Web Application using GPlates
title_sort visualizing paleocurrents in a web application using gplates
publisher Knowledge Exchange
publishDate 2023
url https://knowledge.e.southern.edu/facworks_comp/16
https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1344812
genre Antarc*
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genre_facet Antarc*
Antarctica
op_source Faculty Works
op_relation https://knowledge.e.southern.edu/facworks_comp/16
https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1344812
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