The application of acceptance criteria to results of Thellier palaeointensity experiments performed on samples with pseudo-single-domain-like characteristics

被引:58
作者
Biggin, AJ [1 ]
Thomas, DN [1 ]
机构
[1] Kingston Univ, Sch Earth Sci & Geog, Geodynam & Crustal Proc Res Grp, Kingston upon Thames KT1 2EE, Surrey, England
关键词
Thellier palaeointensity; Arai plots; pTRM;
D O I
10.1016/S0031-9201(03)00127-4
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The results of a simulated Thellier palaeointensity experiment show that the low temperature portion of Arai plots produced by samples with pseudo-single-domain (PSD)-like hysteresis properties can produce significant inaccuracies despite passing conventional acceptance criteria. Furthermore, full Arai plots which fail these criteria can still produce reasonably accurate results. The evidence presented suggests that during a palaeointensity experiment: pTRM checks can fail despite no alteration occurring, pTRM tail checks are not reliable as indicators of MD-like behaviour, room temperature susceptibility monitoring is unreliable for detecting alteration, and that the minimum requirement for the f (fraction)-value should be increased from 0.15 to at least 0.5. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:279 / 287
页数:9
相关论文
共 20 条
[1]   Investigating the reasons for the failure of palaeointensity experiments:: a study on historical lava flows from Mt. Etna (Italy) [J].
Calvo, M ;
Prévot, M ;
Perrin, M ;
Riisager, J .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2002, 149 (01) :44-63
[2]   PALEO-INTENSITIES OF EARTHS MAGNETIC FIELD DETERMINED FROM TERTIARY AND QUATERNARY ROCKS [J].
COE, RS .
JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (12) :3247-+
[3]   GEOMAGNETIC PALEOINTENSITIES FROM RADIOCARBON-DATED LAVA FLOWS ON HAWAII AND QUESTION OF PACIFIC NONDIPOLE LOW [J].
COE, RS ;
GROMME, S ;
MANKINEN, EA .
JOURNAL OF GEOPHYSICAL RESEARCH, 1978, 83 (NB4) :1740-1756
[4]   Geomagnetic paleointensity derived from single plagioclase crystals [J].
Cottrell, RD ;
Tarduno, JA .
EARTH AND PLANETARY SCIENCE LETTERS, 1999, 169 (1-2) :1-5
[5]   HYSTERESIS PROPERTIES OF TITANOMAGNETITES - GRAIN-SIZE AND COMPOSITIONAL DEPENDENCE [J].
DAY, R ;
FULLER, M ;
SCHMIDT, VA .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1977, 13 (04) :260-267
[6]   A theoretical treatment of paleointensity determination experiments on rocks containing pseudo-single or multi domain magnetic particles [J].
Fabian, K .
EARTH AND PLANETARY SCIENCE LETTERS, 2001, 188 (1-2) :45-58
[7]   On the use of continuous thermomagnetic curves in paleomagnetism: a cautionary note [J].
Goguitchaichvili, A ;
Morales, J ;
Urrutia-Fucugauchi, J ;
Soler, AM .
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES, 2001, 333 (11) :699-704
[8]   Magnetic field intensity study of the 1960 Kilauea lava flow, Hawaii, using the microwave palaeointensity technique [J].
Hill, MJ ;
Shaw, J .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2000, 142 (02) :487-504
[9]   Possible mechanisms causing failure of Thellier palaeointensity experiments in some basalts [J].
Kosterov, AA ;
Prevot, M .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1998, 134 (02) :554-572
[10]   EFFECT OF MAGNETITE PARTICLE-SIZE ON PALEOINTENSITY DETERMINATIONS OF GEOMAGNETIC-FIELD [J].
LEVI, S .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1977, 13 (04) :245-259