T183 Fluvio-Deltaic Processes and Their Stratigraphic Record (Posters)
Monday, 23 October 2017
9:00 AM - 6:30 PM
Halls 4EF
LOWER MISSISSIPPI RIVER DELTA DEEP-SEATED SUBSIDENCE RATE DYNAMICS, BIAS, AND SPATIAL-TEMPORAL DEPOCENTER COMPLEXITIES THROUGH THE NEOGENE
Paper number: T183-8
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
-
Mike D. BlumUniversity of Kansas, Lawrence, KS
-
Harry H. RobertsDepartment of Oceanography and Coastal Sciences, Baton Rouge, LA
-
Richard H. FillonEarth Studies Group, Punta Gorda, FL
Abstract
New chronostratigraphic data compiled from over 225,000 wells across the Gulf of Mexico (GOM) reveal a remarkable, negative log-log ‘Sadler’ relationship between shallow and deep-seated subsidence processes. Additionally, substantial northern GOM fluvial depocenter shifts and sediment supply signatures may be discerned through the Neogene coincident with sequence boundaries. This improved understanding of Lower Mississippi River Delta deep-seated subsidence rate variability, dynamics, and measurement bias begins to unravel the spatial-temporal complexity inherent in fluvio-deltaic systems and related clastic basin-fill successions providing critical baseline model constraints for more accurate coastal wetland loss estimates, regional Holocene sea level curves, and future engineered flood control solutions.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-296570
© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.