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A scattering region near the core–mantle boundary under the North Atlantic

✍ Scribed by Luisa Braña; George Helffrich


Book ID
108745562
Publisher
John Wiley and Sons
Year
2004
Tongue
English
Weight
743 KB
Volume
158
Category
Article
ISSN
0956-540X

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It is suggested that the GRIP Greenland ice-core should constitute the stratotype for the Last Termination. Based on the oxygen isotope signal in that core, a new event stratigraphy spanning the time interval from ca. 22.0 to 11.5 k GRIP yr BP (ca. 19.0-10.0 k 14 C yr BP) is proposed for the North A