Paleomagnetic field variation with strong negative inclination during the Brunhes chron at the Banda Sea, equatorial southwestern Pacific

NCUIR > College of Earth Sciences > Graduate Institute of Geophysics > journal & Dissertation > Item 987654321/27542

Please use this identifier to cite or link to this item: http://ir.lib.ncu.edu.tw/handle/987654321/27542

Title:	Paleomagnetic field variation with strong negative inclination during the Brunhes chron at the Banda Sea, equatorial southwestern Pacific
Authors:	Huang,YS;Lee,TQ;Hsu,SK;Yang,TN
Contributors:	地球物理研究所
Keywords:	GEOMAGNETIC-FIELD;SECULAR VARIATION;SEDIMENTARY RECORDS;MAGNETIC-FIELD;EAST INDONESIA;0-5 MA;INTENSITY;REVERSAL;PALEOINTENSITY;CONSTRAINTS
Date:	2009
Issue Date:	2010-06-29 18:40:36 (UTC+8)
Publisher:	中央大學
Abstract:	We reconstruct the earth magnetic field in the Brunhes epoch at the Banda Sea by studying the paleomagnetic data from core MD012380, collected during the International Marine Global Change Study (IMAGES) VII Cruise in 2001. Magnetic analysis is carried out for whole core with a sampling spacing of 1 cm by using u-channel. Magnetic susceptibility (chi), nature remanent magnetization (NRM), anhysteretic remanent magnetization (ARM), and isothermal remanent magnetization (IRM) are measured in our paleomagnetic experiment. Results show the low latitude geomagnetic field variation at the Banda Sea during the last similar to 820 kyr. Except for the Brunhes/Matuyama boundary (BMB), there is no clear signal of reverse events in paleo- inclination and paleo-declination patterns. However, the synthetic paleointensity curve displays the asymmetrical saw-tooth pattern that can be used for determining reverse events, and shows a maximum intensity drop at the BMB. The characteristics of paleointensity provide a useful tool to identify reverse signals and improve the difficulties from only using inclination and declination patterns, especially at low latitude. With the help of paleointensity, inclination and declination, we have identified five reverse events. Furthermore if we consider the secular variation effect, we think that the strong negative inclination observed in our study may be the zonal time-averaged field with paleo secular variation, rather than non-dipole effect within the Brunhes epoch. (c) 2008 Elsevier B.V. All rights reserved.
Relation:	PHYSICS OF THE EARTH AND PLANETARY INTERIORS
Appears in Collections:	[Graduate Institute of Geophysics] journal & Dissertation

Files in This Item:

File	Description	Size	Format
index.html		0Kb	HTML	495	View/Open

社群 sharing

Loading...