Dispersion and deposition of terrigenous sediment on continental terraces

J. J. Veevers

Research output: Contribution to journalArticleResearchpeer-review

Abstract

Each continent is flanked by a continental terrace, divisible into a continental shelf, a continental slope and, in many areas, a coastal plain. Terrigenous sediments entering the ocean are fractionated into two major components: sand is shaped by longshore currents into linear bodies within a few kilometres of the shore; mud is deposited as blankets down‐current outside the sand. Continental terraces and their sediments result from the interplay of various factors, namely, rate of sediment supply, intensity of oceanographical processes, rate of subsidence or uplift, influence of tectonics, and the effect of Quaternary sea‐level changes. In the northwestern Gulf of Mexico, deposition is dominated by supply near the shore, and by the effect of sea‐level changes elsewhere. On the Orinoco‐Trinidad Shelf, sediment is deposited only where protection is provided against the swell and currents. The Sahul Shelf has a very low supply of terrigenous sediment, and relict sediments of the Holocene transgression (mainly carbonates) are widespread.The internal structure of many continental terraces, revealed by continuous acoustic reflection profiling, shows that the continental terraces existed in the past and are not merely the results of the special conditions that prevailed during the Quaternary.

LanguageEnglish
Pages1-4
Number of pages4
JournalJournal of the Geological Society of Australia
Volume14
Issue number1
DOIs
Publication statusPublished - 1 Jan 1967
Externally publishedYes

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terrace
sediment
sea level change
longshore current
sand
shelf sediment
swell
continental slope
coastal plain
transgression
continental shelf
mud
subsidence
acoustics
uplift
Holocene
carbonate
tectonics
ocean
effect

Cite this

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abstract = "Each continent is flanked by a continental terrace, divisible into a continental shelf, a continental slope and, in many areas, a coastal plain. Terrigenous sediments entering the ocean are fractionated into two major components: sand is shaped by longshore currents into linear bodies within a few kilometres of the shore; mud is deposited as blankets down‐current outside the sand. Continental terraces and their sediments result from the interplay of various factors, namely, rate of sediment supply, intensity of oceanographical processes, rate of subsidence or uplift, influence of tectonics, and the effect of Quaternary sea‐level changes. In the northwestern Gulf of Mexico, deposition is dominated by supply near the shore, and by the effect of sea‐level changes elsewhere. On the Orinoco‐Trinidad Shelf, sediment is deposited only where protection is provided against the swell and currents. The Sahul Shelf has a very low supply of terrigenous sediment, and relict sediments of the Holocene transgression (mainly carbonates) are widespread.The internal structure of many continental terraces, revealed by continuous acoustic reflection profiling, shows that the continental terraces existed in the past and are not merely the results of the special conditions that prevailed during the Quaternary.",
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Dispersion and deposition of terrigenous sediment on continental terraces. / Veevers, J. J.

In: Journal of the Geological Society of Australia, Vol. 14, No. 1, 01.01.1967, p. 1-4.

Research output: Contribution to journalArticleResearchpeer-review

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