SITE 398, LEG 47B, EASTERN NORTH ATLANTIC

Cretaceous, organic-rich, dark-colored shales and mudstones were drilled in the Vigo Seamount area on DSDP Leg 47B. Despite their relative richness, their organic matter is predominantly de-rived from detrital material of continental origin. Some contribution of marine organic matter is apparent in...

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Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
North Atlantic
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.514.598
http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf
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record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.514.598 2023-05-15T17:29:40+02:00 SITE 398, LEG 47B, EASTERN NORTH ATLANTIC The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.514.598 http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.514.598 http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf text ftciteseerx 2016-01-08T09:48:43Z Cretaceous, organic-rich, dark-colored shales and mudstones were drilled in the Vigo Seamount area on DSDP Leg 47B. Despite their relative richness, their organic matter is predominantly de-rived from detrital material of continental origin. Some contribution of marine organic matter is apparent in the middle to upper Albian and Cenomanian sediments. An immature stage of evolution can be assigned to all the samples. Text North Atlantic Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Cretaceous, organic-rich, dark-colored shales and mudstones were drilled in the Vigo Seamount area on DSDP Leg 47B. Despite their relative richness, their organic matter is predominantly de-rived from detrital material of continental origin. Some contribution of marine organic matter is apparent in the middle to upper Albian and Cenomanian sediments. An immature stage of evolution can be assigned to all the samples.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title SITE 398, LEG 47B, EASTERN NORTH ATLANTIC
spellingShingle SITE 398, LEG 47B, EASTERN NORTH ATLANTIC
title_short SITE 398, LEG 47B, EASTERN NORTH ATLANTIC
title_full SITE 398, LEG 47B, EASTERN NORTH ATLANTIC
title_fullStr SITE 398, LEG 47B, EASTERN NORTH ATLANTIC
title_full_unstemmed SITE 398, LEG 47B, EASTERN NORTH ATLANTIC
title_sort site 398, leg 47b, eastern north atlantic
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.514.598
http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf
genre North Atlantic
genre_facet North Atlantic
op_source http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.514.598
http://www.deepseadrilling.org/47_2/volume/dsdp47pt2_18.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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