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author Mojtabavi, Seyedhamidreza
Wilhelms, Frank
Cook, Eliza
Davies, Siwan M
Sinnl, Giulia
Skov Jensen, Mathias
Dahl-Jensen, Dorthe
Svensson, Anders M
Vinther, Bo Møllesøe
Kipfstuhl, Sepp
Karlsson, Nanna Bjørnholt
Faria, Sergio Henrique
Gkinis, Vasileios
Kjær, Helle Astrid
Erhardt, Tobias
Berben, Sarah M P
Nisancioglu, Kerim H
Koldtoft, Iben
Rasmussen, Sune Olander
author_facet Mojtabavi, Seyedhamidreza
Wilhelms, Frank
Cook, Eliza
Davies, Siwan M
Sinnl, Giulia
Skov Jensen, Mathias
Dahl-Jensen, Dorthe
Svensson, Anders M
Vinther, Bo Møllesøe
Kipfstuhl, Sepp
Karlsson, Nanna Bjørnholt
Faria, Sergio Henrique
Gkinis, Vasileios
Kjær, Helle Astrid
Erhardt, Tobias
Berben, Sarah M P
Nisancioglu, Kerim H
Koldtoft, Iben
Rasmussen, Sune Olander
collection Datos científicos de ciencias marinas y ambientales
contents A first chronology for the East GReenland Ice core Project (EGRIP) over the Holocene and last glacial termination has been derived by transferring the annual layer counted Greenland Ice Core Chronology 2005 (GICC05) from the NGRIP core to the EGRIP core using 381 matchpoints of mainly on volcanic events and common patterns (peaks and dips) recorded by electrical conductivity measurement (ECM) and dielectrical profiling (DEP) records.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_922350
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Match points between the EGRIP core and the NGRIP2 core and corresponding GICC05 ages
Mojtabavi, Seyedhamidreza
Wilhelms, Frank
Cook, Eliza
Davies, Siwan M
Sinnl, Giulia
Skov Jensen, Mathias
Dahl-Jensen, Dorthe
Svensson, Anders M
Vinther, Bo Møllesøe
Kipfstuhl, Sepp
Karlsson, Nanna Bjørnholt
Faria, Sergio Henrique
Gkinis, Vasileios
Kjær, Helle Astrid
Erhardt, Tobias
Berben, Sarah M P
Nisancioglu, Kerim H
Koldtoft, Iben
Rasmussen, Sune Olander
Age; DEPTH, ice/snow; East Greenland Ice-core Project; EGRIP; Maximum Counting Error
A first chronology for the East GReenland Ice core Project (EGRIP) over the Holocene and last glacial termination has been derived by transferring the annual layer counted Greenland Ice Core Chronology 2005 (GICC05) from the NGRIP core to the EGRIP core using 381 matchpoints of mainly on volcanic events and common patterns (peaks and dips) recorded by electrical conductivity measurement (ECM) and dielectrical profiling (DEP) records.
title Match points between the EGRIP core and the NGRIP2 core and corresponding GICC05 ages
topic Age; DEPTH, ice/snow; East Greenland Ice-core Project; EGRIP; Maximum Counting Error
url https://doi.org/10.1594/PANGAEA.922350