20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1

ABSTRACT A paleomagnetic investigation of the Late Cretaceous sediments of the Maud Rise, Antarctica, recovered in Holes 689B and 690C provides a fairly complete magnetostratigraphic record ranging from Chron C33N through Chron C29R. The Cretaceous/Tertiary boundary is shown to occur in Chron C29R a...

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Main Authors: Kennett P F Barker, J P, Al, N Hamilton
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1061.5445
http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1061.5445 2023-05-15T14:04:40+02:00 20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1 Kennett P F Barker J P Al N Hamilton The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1061.5445 http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1061.5445 http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf text ftciteseerx 2020-04-19T00:20:20Z ABSTRACT A paleomagnetic investigation of the Late Cretaceous sediments of the Maud Rise, Antarctica, recovered in Holes 689B and 690C provides a fairly complete magnetostratigraphic record ranging from Chron C33N through Chron C29R. The Cretaceous/Tertiary boundary is shown to occur in Chron C29R at Site 690. Text Antarc* Antarctica Unknown Maud Rise ENVELOPE(3.000,3.000,-66.000,-66.000)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ABSTRACT A paleomagnetic investigation of the Late Cretaceous sediments of the Maud Rise, Antarctica, recovered in Holes 689B and 690C provides a fairly complete magnetostratigraphic record ranging from Chron C33N through Chron C29R. The Cretaceous/Tertiary boundary is shown to occur in Chron C29R at Site 690.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Kennett P F Barker
J P
Al
N Hamilton
spellingShingle Kennett P F Barker
J P
Al
N Hamilton
20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1
author_facet Kennett P F Barker
J P
Al
N Hamilton
author_sort Kennett P F Barker
title 20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1
title_short 20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1
title_full 20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1
title_fullStr 20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1
title_full_unstemmed 20. MESOZOIC MAGNETOSTRATIGRAPHY OF MAUD RISE, ANTARCTICA 1
title_sort 20. mesozoic magnetostratigraphy of maud rise, antarctica 1
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1061.5445
http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf
long_lat ENVELOPE(3.000,3.000,-66.000,-66.000)
geographic Maud Rise
geographic_facet Maud Rise
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1061.5445
http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_20.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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