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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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North Atlantic
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Great Bahama Bank (1)
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Indian Ocean
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West Indian Ocean (1)
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Indian Ocean Islands
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Maldive Islands (1)
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United States
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South Carolina
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Horry County South Carolina (1)
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geologic age
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Cenozoic
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Quaternary (1)
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Tertiary
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Neogene
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Miocene
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upper Miocene (1)
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Pliocene
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lower Pliocene (1)
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Primary terms
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Atlantic Ocean
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North Atlantic
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Great Bahama Bank (1)
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Cenozoic
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Quaternary (1)
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Tertiary
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Neogene
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Miocene
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upper Miocene (1)
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Pliocene
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lower Pliocene (1)
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continental shelf (1)
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geophysical methods (3)
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Indian Ocean
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West Indian Ocean (1)
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Indian Ocean Islands
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Maldive Islands (1)
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paleoclimatology (1)
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plate tectonics (1)
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sea-level changes (2)
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sedimentary structures
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biogenic structures
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carbonate banks (1)
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sedimentation (1)
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sediments
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carbonate sediments (1)
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clastic sediments
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sand (1)
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marine sediments (2)
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United States
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South Carolina
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Horry County South Carolina (1)
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sedimentary structures
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sedimentary structures
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biogenic structures
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carbonate banks (1)
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sediments
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sediments
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carbonate sediments (1)
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clastic sediments
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sand (1)
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marine sediments (2)
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Fragmentation, rafting, and drowning of a carbonate platform margin in a rift-basin setting
Current and sea level control the demise of shallow carbonate production on a tropical bank (Saya de Malha Bank, Indian Ocean)
The Quaternary stratigraphic architecture of a low-accommodation, passive-margin continental shelf (Santee Delta region, South Carolina, U.S.A.)
Periplatform drift: The combined result of contour current and off-bank transport along carbonate platforms
Monsoon-induced partial carbonate platform drowning (Maldives, Indian Ocean)
Quaternary Sedimentation in the Molengraaff Paleo-Delta, Northern Sunda Shelf (Southern South China Sea)
Abstract The seven seismic units recognized in the Molengraaff paleo-delta on the Sunda Shelf underlying the postglacial unit can be interpreted as prograding shelf-margin lowstand wedges deposited during forced regressions. Speculative age estimates of these units were made by correlating the interpreted lowstand wedges with the SPECMAP δ 18 Ocurve. This correlation suggests that the oldest unit reaches back to 570 ka, that the mean sedimentation rates during glacial times are comparable to modern prodelta rates, and that the tectonic subsidence rate of the outermost shelf depressions during the latest Pleistocene was of the order of 27 cm/kyr. Subsidence (which was differential) also occurred in postglacial times. The rate at the shelf edge is of the order of 2.5 m/kyr, and the differential displacements are taken up by growth-fault activity. The outer Sunda Shelf was the delta plain of the Molengraaff River system during the last glacial, during which major fluvial entrenchment did not take place because of the low gradient. Sand ridges formed by transgressive reworking of Late Pleistocene material mark the modern water-depth range of 135–145 m. Mass wasting and fan deposition are important processes on the continental slope during regressions and lowstands.