赤道西太平洋翁通爪哇海台西南部25万年以来的火山活动: 来自沉积物元素地球化学的证据

路波; 李铁刚; 于心科; 常凤鸣; 南青云; 仇晓华

doi:10.3799/dqkx.2012.S1.012

Volume 37 Issue S1

Nov. 2021

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LU Bo, LI Tie-gang, YU Xin-ke, CHANG Feng-ming, NAN Qing-yun, QIU Xiao-hua, 2012. Past 250 ka Volcanic Activities in Southwest Ontong Java Plateau, West Equatorial Pacific: Evidences from Element Geochemistry. Earth Science, 37(S1): 125-133. doi: 10.3799/dqkx.2012.S1.012

Citation:

LU Bo, LI Tie-gang, YU Xin-ke, CHANG Feng-ming, NAN Qing-yun, QIU Xiao-hua, 2012. Past 250 ka Volcanic Activities in Southwest Ontong Java Plateau, West Equatorial Pacific: Evidences from Element Geochemistry. Earth Science, 37(S1): 125-133. doi: 10.3799/dqkx.2012.S1.012

Citation:

LU Bo, LI Tie-gang, YU Xin-ke, CHANG Feng-ming, NAN Qing-yun, QIU Xiao-hua, 2012. Past 250 ka Volcanic Activities in Southwest Ontong Java Plateau, West Equatorial Pacific: Evidences from Element Geochemistry. Earth Science, 37(S1): 125-133. doi: 10.3799/dqkx.2012.S1.012

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Past 250 ka Volcanic Activities in Southwest Ontong Java Plateau, West Equatorial Pacific: Evidences from Element Geochemistry

doi: 10.3799/dqkx.2012.S1.012

LU Bo^{1, 2, 3},
LI Tie-gang^{1
,
,},
YU Xin-ke¹,
CHANG Feng-ming¹,
NAN Qing-yun¹,
QIU Xiao-hua^{1, 2}

1.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
2.
Graduate University of Chinese Academy of Sciences, Beijing 100049, China
3.
National Marine Environmental Monitoring Center, Dalian 116023, China

Received Date: 2011-08-28
Available Online: 2021-11-15
Publish Date: 2012-05-01

Abstract

Abstract

West equatorial Pacific is the key area of global change, and are important to paleo-ocean and paleo-environment reconstruction. Based on elements geochemistry of sediments of core WP7, recovered from southwest Ontong Java plateau, 4 acidic tephra inputs (2.5-6.4 ka, 57.0-61.2 ka, 79.7-88.4 ka, and 193.7-249.5 ka) and 4 mafic tephra inputs (19.8-24.4 ka, 50.0-62.6 ka, 143.2-150.5 ka, and 160.8-171.1 ka) were deciphered after normalization of Al, Na, K, Be, Ga, Rb, Zr, Nb, Cs, Ce, Hf, Ta, Th, Fe and Mg to Ti. The input of tephra changed the sediment constituents, diluted the biotic CaCO₃, darkened the sediment color, and raised the sedimentation rate.
- elements,
- geochemistry,
- tephra,
- sediments,
- west equatorial Pacific,
- Ontong Java plateau

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References(39)

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Past 250 ka Volcanic Activities in Southwest Ontong Java Plateau, West Equatorial Pacific: Evidences from Element Geochemistry

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