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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Southern Africa
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South Africa
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Eastern Cape Province South Africa (1)
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KwaZulu-Natal South Africa (1)
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West Africa
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Mesozoic
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Primary terms
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Africa
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West Africa
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Far East
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Middle East
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carbon
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Cenozoic
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Quaternary
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middle Holocene (2)
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upper Holocene (6)
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Pleistocene
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upper Pleistocene
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Weichselian
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Younger Dryas (2)
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upper Quaternary (5)
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Siwalik System (1)
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Tertiary
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Neogene
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Miocene
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lower Miocene
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Burdigalian (1)
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middle Miocene (1)
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Pliocene
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lower Pliocene (1)
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-
-
Paleogene
-
Eocene
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Green River Formation (1)
-
-
Oligocene
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Frio Formation (1)
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-
Paleocene
-
lower Paleocene
-
Danian (1)
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-
-
-
-
-
Central America
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Chordata
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Vertebrata
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Southern Europe
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pyroclastics
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Indian Ocean (1)
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Invertebrata
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Mollusca (1)
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Protista
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Foraminifera
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Rotaliina
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Orbitoidacea
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Ammonia
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Ammonia beccarii (1)
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Elphidium (1)
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isotopes
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stable isotopes
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land use (4)
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Mesozoic
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Lower Cretaceous
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Albian
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upper Albian (1)
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Kiowa Formation (1)
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Spirit River Formation (1)
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Swale Estuary
Revisiting the stratigraphic development of the postglacial, transgressive paleo-Changjiang (Yangtze River) mouth: A journey from tide-dominated estuary to delta
Delaware Shelf Valley: Estuary Retreat Path, Not Drowned River Valley
Abstract Major components and terminology of systems a) Marine sand bodies attached to shoreline and associated with barrier island, deltas, capes or tidal-inlets: shore face, delta fringe (delta front), transgressive marine sand (LeBlanc, 1972, Fig. 14.1); cape-associated shoal with transverse ridges and swales (Fig. 14.3); tidal inlet or estuary shoals (tidal deltas?) (Fig. 14.21, 14.22). b) Offshore bars (may have any orientation relative to shoreline trend); sand ridges and swales of Swift, et al. (Fig. 14.2); sand bank of Nelson and Bray (Fig. 14.7); tidal current ridges of Off (Fig. 14.8); linear sand bank of Caston (Fig. 14.9). Terminology: central bar, bar margin, interbar (Exum and Harms, 1968); similarity of facies to foreshore, short face and shelf (Fig. 14.51). Bars may have either fining upward or coarsening upward grain sizes. c) Palimpsest sand on shelf floor (transgressive sheet sand) d) Bar sands overlying submarine scour surfaces. Processes and genetic units (facies — lithologic associations) a) Complicated and diverse: normal and storm-generated wave and tidal currents, superimposed on stable, submerging (deepening) or shoaling conditions on shelf, with variation in sediment input. Modern shelves: relict sand blanket; sand shoals; ridge and swale sands; mud blanket. b) Inferred storm hydraulic regime associated with cape-associated shoal and shoal retreat massif (Figs. 14.3, 14.4). c) Sand bank (shoal) on mud-dominated shelf (Figs. 14.5–14.7). d) Tidal current dominated sand movement forming linear sand banks after Caston (Figs. 14.9–14.13). e) Sediment movement and sand distribution tidal inlet shoals, Sapelo Island area, Georgia; (Figs. 14.20–14.22; 12.6–12.8) f) Shallow wave activity
Selecting the location, and the initial investigation of the SERC soft clay test bed site
Abstract Components and terminology of barrier island systems (Figs. 12.1–12.4) a) Beach (back shore, fore shore), shore face, dunes, beach ridge, swale, barrier flat (wash-overs), tidal inlet (or estuary). b) Terminology problems offshore bar versus barrier bar shoreline for reference ocean versus lagoon c) Shorelines of emergence and submergence Processes controlling development, modification and lateral changes of shoreline sands (includes shore face). a) Wave-generated currents in shore face zone (effective wave base). b) Tide-and wave-generated currents — beach, inlets, tidal channels. c) Storm effects superimposed on normal processes. d) Longshore drift — movement of sand along littoral zone from source areas which may be: a) rivers, b) cannibalizing along shoreline, c) reworking of ancient deposit on sea floor during submergence. e) Eolian — coastal dunes (processes described in Lecture 10) f) Ground water table fluctuations in ridge and swale topography; oxidation processes; root systems. g) Biogenic: response of organisms making biogenic structures to energy, rates of sedimentation and food supply. h) Highest rates of sedimentation in general shoreline zone; slower rates landward and seaward; rates of lateral accretion high compared to vertical accumulation; high energy deposits prograde over those of lower energy, therefore coarsening upward sequence (Fig. 12.5) (except in tidal channel area where reverse is found). i) Barrier island (shoreline) accretes seaward by addition of sand in beach zone (forming beach ridge or chenier) and also in direction of long shore drift. Genetic Units (facies-lithologic associations) a) Barrier island — lagoon sequence — (Fig. 12.5, 12.30–12.32). Example
Origin and Development of Texas Shoreline: ABSTRACT
The qualitative and quantitative classification of modern clastic marginal-marine depositional systems, Trinidad
Rapid wetland expansion during European settlement and its implication for marsh survival under modern sediment delivery rates
Residual Sediment Transport Paths on a Tidal Sand Bank: A Comparison Between the Modified McLaren Model and Bedform Analysis
Late Quaternary Sequence Stratigraphy of a Slowly Subsiding Passive Margin, New Jersey Continental Shelf
SEDIMENTARY FACIES AND DEPOSITIONAL ENVIRONMENTS OF DIVERSE EARLY PALEOCENE FLORAS, NORTH-CENTRAL SAN JORGE BASIN, PATAGONIA, ARGENTINA
Residual Transport Model in Correlation with Sedimentary Dynamics over an Elongate Tidal Sandbar in the Gironde Estuary (Southwestern France)
Tidal Flat Sedimentation in Bairenkonda Formation of the Tirumala Hills, Southwestern Part of the Cuddapah Basin, Andhra Pradesh
Holocene Evolution of the East Texas Coast and Inner Continental Shelf: Along-Strike Variability in Coastal Retreat Rates
Abstract Geomorphological, geochemical and geochronological investigations of Holocene fluvial sedimentary sequences have been undertaken within a range of upland, piedmont and lowland valley floor reaches in the Yorkshire Ouse catchment, northern England. The aims of these studies have been to: (a) evaluate the effects of prehistoric and historic land-use change on catchment erosion and sediment delivery to river channels and floodplains; (b) establish the degree to which episodes of river erosion and sedimentation are controlled by climate-related variations in flood regime; and (c) assess the spatial heterogeneity of river response to environmental change and how this is likely to influence short- and long-term sediment storage, as well as sediment transfer to the Humber Estuary. Similar discontinuities in the Holocene alluvial record are evident at many sites in the Yorkshire Ouse catchment, though local differences in river sensitivity to externally imposed change have resulted in a complicated and often unique relationship between river behaviour and environmental change. The large proportion of particulate-borne contaminant metals (resulting predominantly from historical mining) stored in the Vale of York strongly indicates that sediment delivery from the Ouse catchment to the Humber Estuary during the Holocene may have been relatively low. This suggests that the degree of connectivity between river, estuarine and coastal transport systems, as well as spatial and temporal variations in fluvial sediment storage, are the key controls of long-term land-ocean sediment fluxes.