Paleomagnetic evidence for the Gothenburg geomagnetic excursion during the Pleistocene–Holocene transition recorded in the Paleo-Danyang Lake, eastern China

Chen, Zhongliang; Yuan, Feng; Zhang, Jinzhe; Shen, Shihao; Li, Xiaohui; Meng, Hua; Jowitt, Simon M.

doi:10.1016/j.jseaes.2019.104140

Journal of Asian Earth Sciences

2020

DOI: 10.1016/j.jseaes.2019.104140

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Paleomagnetic evidence for the Gothenburg geomagnetic excursion during the Pleistocene–Holocene transition recorded in the Paleo-Danyang Lake, eastern China

Zhongliang Chen

Feng Yuan

Jinzhe Zhang

et al.

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Geomagnetic Field Excursions of the Brunhes Chron. P.1: A Historical Overview and Current State of Research

BAKHMUTOV,

MELNYK,

HLAVATSKYI

et al. 2023

VKNUGEOL

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The use of the palaeomagnetic method in stratigraphy is based on the evidence of geomagnetic field polarity changes (inversions) as well as the existence of excursions, short-term (up to 10 ka) deviations of the virtual geomagnetic pole from its usual position, which occurred sometimes only on a regional scale. The excursions as magnetostratigraphic benchmarks are a powerful tool in the correlation of the Quaternary deposits. In 19601990 particular attention was paid to them as important correlation markers across the regional chronostratigraphic scales of the Quaternary. However, the quantity of the Brunhes chron excursions, their stratigraphic position and ages have been debatable. In recent years, many papers have been published clarifying the nature, age, and duration of excursions in various deposits. In the first part of the article a detailed overview of the Brunhes chron excursions is provided, considering the current state of the issue of determining their suitability.

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Geomagnetic Field Excursions of the Brunhes Chron. P.1: A Historical Overview and Current State of Research

BAKHMUTOV,

MELNYK,

HLAVATSKYI

et al. 2023

VKNUGEOL

View full text Add to dashboard Cite

show abstract

First Results of the Comprehensive Analysis, Including the Paleomagnetic Studies, of Sediment Cores from the East Siberian Sea

Elkina,

Gusev,

Ryabchuk

et al. 2024

jour

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The bottom sediments of the Russian Arctic seas have been studied to varying degrees. The least attention has been paid to the East Siberian Sea, the Quaternary geology of which remains largely overlooked. This article summarizes the results of a comprehensive research on the East Siberian Sea, including the first paleomagnetic analysis of nine sediment cores collected during three cruise expeditions as part of the program “State Geological Mapping of the Territory and Continental Shelf of the Russian Federation at the Scale of 1:1 000 000”. The results obtained show that the processes and conditions of sedimentation vary in different parts of the East Siberian Sea.

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Paleomagnetic evidence for the Gothenburg geomagnetic excursion during the Pleistocene–Holocene transition recorded in the Paleo-Danyang Lake, eastern China

Cited by 2 publications

References 55 publications

Geomagnetic Field Excursions of the Brunhes Chron. P.1: A Historical Overview and Current State of Research

Geomagnetic Field Excursions of the Brunhes Chron. P.1: A Historical Overview and Current State of Research

First Results of the Comprehensive Analysis, Including the Paleomagnetic Studies, of Sediment Cores from the East Siberian Sea

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