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Application of amino acid geochronology to stratigraphy of late Cenozoic marine units of Atlantic Coastal Plain
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Department of Geology, University of Delaware, Newark, Del
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(1979)
Ph.D. Diss.
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Belknap1
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3
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84918405144
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Surfacial morphology and subsurface stratigraphy of the flood tidal deltas on the Atlantic Coast of Delaware
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College of Marine Studies, University of Delaware, Newark, Del
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(1981)
M.S. Thesis
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Carey1
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4
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Genesis and preservation of Quaternary paralic deposits on Delmarva Peninsula
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Department of Geology, University of Delaware, Newark, Del
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(1981)
Ph.D. Diss.
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Demarest1
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7
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0010681257
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Time-stratigraphic aspects of a formation interpretation of surficial Pleistocene deposits by anology with Holocene paralic deposits southeastern Delaware
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(1981)
Geology
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Demarest1
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8
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Post-Pleistocene history of the United States inner continental shelf: significance to origin of barrier islands
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(1976)
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Field1
Duane2
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10
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84918405143
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Geological development of the southern portion of Assateague Island, Virginia
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Department of Geology, University of Delaware, Newark, Del
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(1978)
M.S. Thesis
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Goettle1
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11
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0018723559
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Nexus: New model of barrier island development
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S.P. Leatherman, Academic Press, New York, N.Y
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(1979)
Barrier Islands
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Halsey1
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12
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0018668010
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Barrier island morphology as a function of tidal and wave regime
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S.P. Leatherman, Academic Press, New York, N.Y
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(1979)
Barrier Islands
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Hayes1
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15
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Composition and origin of the inorganic fraction of southern New Jersey coastal mud deposits
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(1983)
Geol. Soc. Am. Bull.
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Sedimentary facies patterns and geologic history of a Holocene transgression
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(1971)
Geol. Soc. Am. Bull.
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Kraft1
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20
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Three-dimensional analysis of Pleistocene and Holocene coastal sedimentary units at Bethany Beach, Delaware
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University of Delaware, Newark, Del
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(1981)
M.S. Thesis
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McDonald1
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21
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Landward transport of bottom sediments in estuaries of the Atlantic Coastal Plain
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Meade1
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Sediment distribution and evolution of tidal deltas along a tide-dominated shoreline, Wachapreague, Virginia
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Sediment. Geol.
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Morton1
Donaldson2
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Geomorphic cycles in ebb deltas and related patterns of shore erosion and accretion
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Oertel1
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