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Table 1 Brief information on the sampled sites and associated age constraints of the Northeast (NE) China volcanic field analyzed in this study

From: New absolute paleomagnetic intensity data from Cenozoic basalts of Northeast China and exploring rock-magnetic parameters for efficient sample preselection on the Tsunakawa–Shaw paleointensity method

Site name

Name of basalt/volcanic field

Sampling locality

Age info

Area name

Lat. (° N)

Lon. (° E)

14175

Naitoushan Basalt/CVF

Naitoushan

42.33219

128.14203

Miocene (Liu 1983, 1987, 1988; Chun and Cheong 2020)

14192

Toudao Basalt/CVF

Yaoshui

42.52450

128.05640

 ~ 2.8 ~ 1.9 Ma (Wei et al. 2007),

 ~ 2.5 Ma (sample B5102 of the same outcrop in Lee et al. 2021)

14181

Toudao Basalt/CVF

Baomacun

42.41610

128.04347

same as those of site 14192

14182

Toudao Basalt/CVF

Jinjiangcun

41.97798

127.55910

same as those of site 14192 (the same site as where the sample B4182 was collected in Lee et al. 2021)

14183

Baishan Basalt/CVF

Jinjiangcun

41.98098

127.56295

 ~ 1.4 ~ 0.9 Ma (Wei et al. 2007),

 ~ 1.1 Ma (the Baishan Basalt sample B5104 in Lee et al. 2021)

14201

Longgang Basalt/LVF

Longgang

42.49373

126.47533

 ~ 1.2 Ma (basanite at Dalongwan area in Liu 1987),

 ~ 0.9 Ma (unpublished direct K–Ar data, credit by Dr. Y. S. Lee)

14222

Jingpohu Basalt/JVF

Jingpohu

44.07695

128.99215

Late Pleistocene to Holocene around Xingshan area (Liu et al. 1989; Yan and Zhao 2008),

 ~ 0.12 Ma (unpublished direct K–Ar data, credit by Dr. Y. S. Lee)

14226

Jingpohu Basalt/JVF

Jingpohu

44.06550

128.94912

Late Pleistocene to Holocene (Liu et al. 1989; Yan and Zhao 2008),

 ~ 0.08 Ma (unpublished direct K–Ar data, credit by Dr. Y. S. Lee)

  1. CVF, LVF, and JVF represent the Changbaishan (Baekdusan), Longgang, and Jingpohu volcanic fields, respectively