22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1
The acid insoluble coarse fractions of the glacial-interglacial sequence of Hole 552A in the NE Atlantic are made up of varying amounts of terrigenous detritus, biogenic silica, and pyroclastic material, principally volcanic glass. Volcanic ash content varies significantly over the entire interval,...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.574.4214 2023-05-15T16:27:55+02:00 22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 Andrew C. Morton British Geological Survey Key Worth The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.4214 http://www.deepseadrilling.org/81/volume/dsdp81_22.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.4214 http://www.deepseadrilling.org/81/volume/dsdp81_22.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.deepseadrilling.org/81/volume/dsdp81_22.pdf text ftciteseerx 2016-01-08T12:41:01Z The acid insoluble coarse fractions of the glacial-interglacial sequence of Hole 552A in the NE Atlantic are made up of varying amounts of terrigenous detritus, biogenic silica, and pyroclastic material, principally volcanic glass. Volcanic ash content varies significantly over the entire interval, and the three North Atlantic ash horizons of Ruddiman and Glover (1972) can be recognized satisfactorily. The terrigenous detritus is of mixed metamorphic-basaltic type and probably originated on the Greenland landmass. Text Greenland North Atlantic Unknown Greenland |
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English |
description |
The acid insoluble coarse fractions of the glacial-interglacial sequence of Hole 552A in the NE Atlantic are made up of varying amounts of terrigenous detritus, biogenic silica, and pyroclastic material, principally volcanic glass. Volcanic ash content varies significantly over the entire interval, and the three North Atlantic ash horizons of Ruddiman and Glover (1972) can be recognized satisfactorily. The terrigenous detritus is of mixed metamorphic-basaltic type and probably originated on the Greenland landmass. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Andrew C. Morton British Geological Survey Key Worth |
spellingShingle |
Andrew C. Morton British Geological Survey Key Worth 22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 |
author_facet |
Andrew C. Morton British Geological Survey Key Worth |
author_sort |
Andrew C. Morton |
title |
22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 |
title_short |
22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 |
title_full |
22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 |
title_fullStr |
22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 |
title_full_unstemmed |
22. COARSE FRACTION OF PLIO-PLEISTOCENE SEDIMENTS FROM DEEP SEA DRILLING PROJECT HOLE 552A, NORTHEAST ATLANTIC1 |
title_sort |
22. coarse fraction of plio-pleistocene sediments from deep sea drilling project hole 552a, northeast atlantic1 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.4214 http://www.deepseadrilling.org/81/volume/dsdp81_22.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland North Atlantic |
genre_facet |
Greenland North Atlantic |
op_source |
http://www.deepseadrilling.org/81/volume/dsdp81_22.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.4214 http://www.deepseadrilling.org/81/volume/dsdp81_22.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766017505272266752 |