Geomagnetic paleointensity variations in the northern South China Sea since the Late Pleistocene-Reference-Cited by-同舟云学术

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Geomagnetic paleointensity variations in the northern South China Sea since the Late Pleistocene

Published:2024-01 Issue: Volume:324 Page:108452
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Yang Xiaoqiang,Su Zhihua,Wei Gangjian,Zhang Tingwei,Chen Qiong,Ye Yulan

Funder

National Natural Science Foundation of China

Government of Guangdong Province

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference59 articles.

1. Dipole and nondipole evolution of the historical geomagnetic field from instrumental, archeomagnetic, and volcanic data;Arneitz;J. Geophys. Res. Solid Earth,2021

2. Comparing remanence anisotropy and susceptibility anisotropy as predictors of paleomagnetic inclination shallowing in turbidites from the Scotian rise;Bijaksana;Phys. Chem. Earth,1997

3. Role of spherical particles on magnetic field recording in sediments: experimental and numerical results;Bilardello;Phys. Earth Planet. In.,2013

4. Evidence for multiple paleomagnetic intensity lows between 30-50 ka BP from a western Equatorial Pacific sedimentary sequence;Blanchet;Quat. Sci. Rev.,2006

5. A new high-resolution geomagnetic paleointensity record for the North American Holocene: a comparison of sedimentary and absolute intensity data;Brachfeld;J. Geophys. Res.,2000

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