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New evidence from the southeastern U.S. for eustatic components in the late Holocene Sea levels

Datos Bibliográficos

ID12134202
AutoresDonald J Colquhoun (University of South Carolina, autor de correspondencia), Mark J Brooks (University of South Carolina)
Año1986
Volumen1
Número3
Páginas275-291
Fecha de publicación1986-04-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaGeoarchaeology (JOURNAL)
Identificadores de la revistaISSN: 0883-6353 • E-ISSN: 1520-6548
EditorialWiley (PUBLISHER • GB)
DOI10.1002/gea.3340010304
OpenAlexW2013801691
IdiomaEN
Citas recibidas26
Referencias citadas9

Changes in Holocene sea level through time have been attributed to eustatic, isostatic, and neotectonic processes. Eustatic changes imply global expression through linkage in world climate, or changes in ocean water or basin volume, while isostatic adjustment and neotectonic distortion involve regional or local geophysical parameters which must be ascertained. A Holocene sea level curve is being developed for the southeastern United States through a study of marsh stratigraphy and archaeologic sites located in marsh and interriverine areas. The curve is evaluated in light of intensive investigations of regional and local tectonic elements. Both major and some minor trends in sea level change are shown to include significant eustatic components

Geography · Geomorphology · Holocene · Physical geography · Post-glacial rebound · Sea level · Structural basin · Tectonic uplift · Tectonics · Geology and Paleoclimatology Research · Geophysics and Gravity Measurements · Oceanographic and Atmospheric Processes · Geology · Oceanography · Paleontology · Stratigraphy

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Obras citantes distintas26
Citas por año0,65
Intervalo de citas1986 - 2025 (40)
Velocidad de citaciónrecent
Altamente citadoNo
Tipos de citaNeutras: 25
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