2019 CSDMS meeting-052: Difference between revisions
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|CSDMS meeting abstract=Sequence is a modular 2D (i.e., profile) sequence stratigraphic model that is written in Python and implemented within the Landlab framework. Sequence represents time-averaged fluvial and marine sediment transport via differential equations. The modular code includes components to deal with sea level changes, sediment compaction, local or flexural isostasy, and tectonic subsidence and uplift. Development of the code was spurred by observations of repetitive stratigraphic sequences in western Turkey that are distorted by tectonics. | |CSDMS meeting abstract=Sequence is a modular 2D (i.e., profile) sequence stratigraphic model that is written in Python and implemented within the Landlab framework. Sequence represents time-averaged fluvial and marine sediment transport via differential equations. The modular code includes components to deal with sea level changes, sediment compaction, local or flexural isostasy, and tectonic subsidence and uplift. Development of the code was spurred by observations of repetitive stratigraphic sequences in western Turkey that are distorted by tectonics. | ||
|CSDMS meeting posterPDF=Michael_Steckler_CSDMS_Conference_Poster_final.pdf | |||
|CSDMS meeting posterPNG=Michael_Steckler_CSDMS_Conference_Poster_final.png | |||
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Latest revision as of 17:32, 27 May 2019
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Sequence Stratigraphic Modeling in Landlab
Michael Steckler, Lamont-Doherty Earth Observatory Palisades New York, United States. steckler@ldeo.columbia.edu
Eric Hutton, University of Colorado - Boulder Boulder Colorado, United States. hutton.eric@gmail.com
David Ologan, M.I.T. Cambridge Massachusetts, United States. ologand@bxscience.edu
Gregory Tucker, University of Colorado - Boulder Boulder Colorado, United States. gtucker@colorado.edu
Sequence is a modular 2D (i.e., profile) sequence stratigraphic model that is written in Python and implemented within the Landlab framework. Sequence represents time-averaged fluvial and marine sediment transport via differential equations. The modular code includes components to deal with sea level changes, sediment compaction, local or flexural isostasy, and tectonic subsidence and uplift. Development of the code was spurred by observations of repetitive stratigraphic sequences in western Turkey that are distorted by tectonics.
