U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province

YU Fu-Sheng; YUAN Wan-Ming; HAN Song; MA Zhi-Bang; JIN Ke

Chinese Physics C> 2003, Vol. 27> Issue(11) : 1039-1043

U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province

Institute of High Energy Physics, CAS, Beijing 100039, China2 Institute of Geology and Geophysics, CAS, Beijing 100029, China3 Information of Geological and Mineral Resource Bureau of Jilin, Changchun 130022, China

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Abstract：
Longgang volcanic swarm belongs to one of volcanic areas which have been active since modern times. In view of multiple eruptions during histories, it is very important to determine age of every eruption for evaluating volcanic hazards. The alkaline basalt samples taken from Dayizishan and Diaoshuihu are analyzed by U-series component method, after magnetic separation. The ages of the two samples are (71±9)ka, (106±13)ka before presence, respectively. These data indicate that there exist intensively eruptive activities during late Pleistocene.

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YU Fu-Sheng, YUAN Wan-Ming, HAN Song, MA Zhi-Bang and JIN Ke. U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province[J]. Chinese Physics C, 2003, 27(11): 1039-1043.

YU Fu-Sheng, YUAN Wan-Ming, HAN Song, MA Zhi-Bang and JIN Ke. U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province[J]. Chinese Physics C, 2003, 27(11): 1039-1043. shu

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Received: 2003-03-30
Revised: 1900-01-01

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province

Corresponding author: YU Fu-Sheng,

Institute of High Energy Physics, CAS, Beijing 100039, China2 Institute of Geology and Geophysics, CAS, Beijing 100029, China3 Information of Geological and Mineral Resource Bureau of Jilin, Changchun 130022, China

Received Date: 2003-03-30

Accepted Date: 1900-01-01

Available Online: 2003-11-05

Abstract: Longgang volcanic swarm belongs to one of volcanic areas which have been active since modern times. In view of multiple eruptions during histories, it is very important to determine age of every eruption for evaluating volcanic hazards. The alkaline basalt samples taken from Dayizishan and Diaoshuihu are analyzed by U-series component method, after magnetic separation. The ages of the two samples are (71±9)ka, (106±13)ka before presence, respectively. These data indicate that there exist intensively eruptive activities during late Pleistocene.

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U-Series Component Dating for Late Pleistocene Basalt of Longgang, Jilin Province

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