_version_ 1867171020276760576
author Avery, Rachael S
Xuan, Chuang
Kemp, Alan E S
Bull, Jonathan M
Cotterill, Carol
Fielding, J James
Pearce, Richard B
Croudace, Ian W
author_facet Avery, Rachael S
Xuan, Chuang
Kemp, Alan E S
Bull, Jonathan M
Cotterill, Carol
Fielding, J James
Pearce, Richard B
Croudace, Ian W
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_917458
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle Paleosecular geomagnetic variation for the Holocene measured from U-channels 2014-2016
Avery, Rachael S
Xuan, Chuang
Kemp, Alan E S
Bull, Jonathan M
Cotterill, Carol
Fielding, J James
Pearce, Richard B
Croudace, Ian W
+54-03/57PC; +54-03/64PC; +54-03/67PC; +54-03/68PC; AGE; British Geological Survey; Calculated; COMPCORE; Composite Core; Confidence interval lower limit; Confidence interval upper limit; Declination; Holocene; Inclination; lake sediments; Lake Windermere, United Kingdom; Magnetic; Palaeomagnetic; Paleomagnetic; Paleosecular variation; PC; Piston corer; Principal component analyses (PCA); Relative paleointensity proxy; U-channel; Windermere; WINPSV-12K
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.
title Paleosecular geomagnetic variation for the Holocene measured from U-channels 2014-2016
topic +54-03/57PC; +54-03/64PC; +54-03/67PC; +54-03/68PC; AGE; British Geological Survey; Calculated; COMPCORE; Composite Core; Confidence interval lower limit; Confidence interval upper limit; Declination; Holocene; Inclination; lake sediments; Lake Windermere, United Kingdom; Magnetic; Palaeomagnetic; Paleomagnetic; Paleosecular variation; PC; Piston corer; Principal component analyses (PCA); Relative paleointensity proxy; U-channel; Windermere; WINPSV-12K
url https://doi.org/10.1594/PANGAEA.917458