Decadal‐Scale In Situ Scanning of a Stalagmite From Southwest China Reveals Blake Geomagnetic Excursion Structure

Abstract We present a decadal‐scale paleomagnetic analysis of a stalagmite collected from Shuixi Cave, southwest China, spanning 89−123 ka. Our findings include: (a) Magnetite is the dominant magnetic mineral, and paleomagnetic directions can be obtained via demagnetization; (b) Magnetic scanning at...

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Detalhes bibliográficos

Principais autores:	Zhongshan Shen, Youwei Li, Liang Yi, Huafeng Qin, Jian Wang, Yibing Li, Hai Cheng
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2026-01-01
coleção:	Geophysical Research Letters
Assuntos:	the Blake excursion the post‐Blake excursion the skalamaelifell excursion in situ magnetic scanning speleothem paleomagnetism last interglacial
Acesso em linha:	https://doi.org/10.1029/2025GL117878
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