Paleosecular geomagnetic variation for the Holocene measured from U-channels 2014-2016

Dataset

DOI

Inclination, declination, and relative palaeointensity calculated as a composite (WINPSV-12K) of four sediment cores (+54-03/57PC, +54-03/64PC, +54-03/67PC, +54-03/68PC) from Windermere, UK, spanning the Holocene. The inclination and declination are reliable, but the RPI is not reliable and should not be used in publications. It is made available for those who wish to plot it anyway.For each variable we have included the calculated values and the 5% and 95% confidence envelope limits. Values are calaculated for every 50 year timestep.

Identifier
DOI	https://doi.org/10.1594/PANGAEA.917458
Related Identifier	https://doi.org/10.1016/j.epsl.2017.08.025
Metadata Access	https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.917458

Provenance
Creator	Avery, Rachael S ; Xuan, Chuang ; Kemp, Alan E S; Bull, Jonathan M ; Cotterill, Carol ; Fielding, J James ; Pearce, Richard B; Croudace, Ian W
Publisher	PANGAEA
Contributor	University of Southampton
Publication Year	2020
Rights	Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess	true

Representation
Resource Type	Dataset
Format	text/tab-separated-values
Size	2106 data points
Discipline	Earth System Research
Spatial Coverage	(-2.955W, 54.316S, -2.936E, 54.410N); Lake Windermere, United Kingdom