Dispersal of glacially derived sediment over part of the continental shelf of south Iceland and the geometry of the resultant sediment bodies-Reference-Cited by-同舟云学术

Dispersal of glacially derived sediment over part of the continental shelf of south Iceland and the geometry of the resultant sediment bodies

Published:1988-09 Issue:1-4 Volume:83 Page:193-223
ISSN:0025-3227
Container-title:Marine Geology
language:en
Short-container-title:Marine Geology

Author:

Boulton G.S.,Thors K.,Jarvis J.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference20 articles.

1. Proximality trends in modern storm sands from the Helgoland Bight (North Sea) and the implications for basin analysis;Aigner;Senckenbergiana Marit.,1982

2. Circulation on the New England continental shelf: response to strong winter storms;Beardsley;Geol. Res. Lett.,1974

3. Sonographs of the Sea Floor;Belderson,1972

4. The structure of the sediments beneath Breidamer-kursandur and the form of underlying bed rock;Bogadóttir,1986

5. Stratigraphy and structure of a coastal sediment wedge of glacial origin inferred from sparker measurements in glacial lake Jökulsarlon in southeastern Iceland;Boulton;Jökull,1983

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