Susceptibility, hysteresis, coercivity, isothermal remanent magnetisation and thermomagnetic curve Rock Magnetic data measured at University of Liverpool (NERC Grant NE/P00170X/1)
Rock magnetic data corresponding to demagnetisation (LIV_DEMAG) and paleointensity (LIV_PI) data submitted as part of this grant. This data is divided into two subfolders, "Kappabridge" and "VFTB", corresponding to the instrument used to acquire the data. Those folders each contain one or more folders labelled with a four letter code, corresponding to a specific locality and/or experiment type, matching the letter codes in LIV_DEMAG and LIV_PI. The Kappabridge folders then contain raw data files of temperature-dependent magnetic susceptibility, and the VFTB folders contain raw data files of hysteresis, coercivity, isothermal remanent magnetisation and thermomagnetic curve measurements. CFEH corresponds to clinker samples from USA attempting to isolate an Epsilon Hematite phase. LPRM are data from Kinghorn and Wormit Bay volcanics in Scotland, ~330 Ma, specifically for samples given a lab TRM at 80uT and a PRM at 80uT. WTBY are Devonian volcanics from Wormit Bay, sampled in 2015. YDSR are data from Yandiniling Dike Swarm, Yilgarn Craton in Australia, sampled Nov 2018.
dataset
https://webapps.bgs.ac.uk/services/ngdc/accessions/index.html#item169337
name: Data
function: download
http://data.bgs.ac.uk/id/dataHolding/13607841
eng
geoscientificInformation
publication
2008-06-01
Devonian
NGDC Deposited Data
Hysteresis
Carboniferous
revision
2022
NERC_DDC
116.0000
117.5000
-31.5000
-32.5300
creation
1979
MONTANA [id=793000]
creation
1979
SCOTLAND [id=140000]
revision
2009
SCT
creation
1979
WESTERN AUSTRALIA [id=582000]
2017-06-11
2020-01-16
creation
2021-11-10
notApplicable
Temperature-dependent susceptibility - continuous heating of powdered material sample with discrete measurements of susceptibility taken whilst heating the sample to 600-700 degrees C, and then cooling back to room temperature. IRM/hysteresis/coercivity/thermoremanence - each measured in succession on the same powdered sample on the VFTB. Magnetic fields are applied to the sample to induce oscillations which are measured by the balance and this is converted into magnetisation of the sample. For the thermomagnetic curves the sample is gradually heated to 600-700 degrees C with discrete measurements taken, and then gradually cooled to room temperature.
publication
2011
false
See the referenced specification
publication
2010-12-08
false
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
.cur
The copyright of materials derived from the British Geological Survey's work is vested in the Natural Environment Research Council [NERC]. No part of this work may be reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright holder, via the BGS Intellectual Property Rights Manager. Use by customers of information provided by the BGS, is at the customer's own risk. In view of the disparate sources of information at BGS's disposal, including such material donated to BGS, that BGS accepts in good faith as being accurate, the Natural Environment Research Council (NERC) gives no warranty, expressed or implied, as to the quality or accuracy of the information supplied, or to the information's suitability for any use. NERC/BGS accepts no liability whatever in respect of loss, damage, injury or other occurence however caused.
University of Liverpool
Geomagnetism Laboratory , Oliver Lodge Building
Liverpool
L69 7ZE
originator
Professor of Palaeomagnetism
University of Liverpool
Earth, Ocean and Ecological Sciences, Geomagnetism Laboratory, Oliver Lodge Laboratories
Liverpool
L69 7ZE
principalInvestigator
British Geological Survey
distributor
British Geological Survey
pointOfContact
British Geological Survey
Environmental Science Centre,Keyworth
NOTTINGHAM
NG12 5GG
United Kingdom
+44 115 936 3100
pointOfContact
2025-03-26