Stratigraphy and Sedimentology of the Tombigbee Sand Member, Eutaw Formation (Cretaceous-campanian stage), of Northeastern Mississippi
dc.contributor.author | Soens, David Dale | |
dc.date.accessioned | 2025-06-26T16:11:27Z | |
dc.date.available | 2025-06-26T16:11:27Z | |
dc.date.issued | 1984 | |
dc.description | Electronic Thesis or Dissertation | |
dc.description.abstract | The Tombigbee Sand Member of the Eutaw Formation in northeastern Mississippi, can be divided into four lithofacies and six biofacies that define an inner nerit:k to middle neritic marine transgressive sequence. The lithofacies range from medium~~ to fine-grained sands deposited above wave base, to silts and clays deposited in lower energy environments. The biofacies a.re defined by assemblages of benthic micro-faunal morphotypes,, The morphotypes exhibit a substrate preference and are associated with certain lithofacies. The lithofacies and biofacies are locally correlatable~ However, the updip variability of the :i.nner neritic environment prohibits regional correlative use of the lithofacies and biofacies. The potential use of the lithofacies and biofacies as a correlative tool for the Tombigbee increases downdip as the more stable middle neritic marine environments are encountered. | |
dc.format.extent | 184 p. | |
dc.format.medium | electronic | |
dc.format.mimetype | application/pdf | |
dc.identifier.uri | https://ir.ua.edu/handle/123456789/16728 | |
dc.language.iso | en_US | |
dc.publisher | University of Alabama Libraries | |
dc.rights | All rights reserved by the author unless otherwise indicated. | |
dc.subject | Geology, Stratigraphic--Cretaceous | |
dc.title | Stratigraphy and Sedimentology of the Tombigbee Sand Member, Eutaw Formation (Cretaceous-campanian stage), of Northeastern Mississippi | |
dc.type | Thesis | |
etdms.degree.department | University of Alabama. Department of Geology. | |
etdms.degree.discipline | Geology | |
etdms.degree.grantor | The University of Alabama | |
etdms.degree.level | master's | |
etdms.degree.name | M.S. |