Art
J-GLOBAL ID：200902190613535883   Reference number：95A0351014

Synchronous variations in the content of magnetic minerals and planktonic-foraminiferal δ13C in deep-sea sediments.

深海堆積物中の磁性鉱物含量と浮遊性有孔虫炭素同位体比の同時変化
Author (4)：
SATO T

About SATO T

(Niigata Univ., Niigata, JPN)

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, 
NAKAI N

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(Geoscience Lab., Nagoya, JPN)

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, 
SHIRAI Y

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(Mie General Education Center, Mie, JPN)

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, 
KOBAYASHI K

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(Japan Marine Science and Technology Center, Yokosuka, JPN)

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Material：
Palaeogeography, Palaeoclimatology, Palaeoecology  (Palaeogeogr Palaeoclimatol Palaeoecol)

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Volume： 113  Issue： 2/4  Page： 199-215  Publication year： Feb. 1995 
JST Material Number： E0621A  ISSN： 0031-0182  CODEN： PPPYA  Document type： Article
Article type： 原著論文  Country of issue： Netherlands (NLD)  Language： ENGLISH (EN)
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Central Pacific Ocean

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,...
Semi thesaurus term：
Thesaurus term/Semi thesaurus term
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All keywords is available on JDreamIII(charged).
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飽和等温残留磁気

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,...
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JST classification (1)：
JST classification
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Geochemistry of lithosphere in general 
(DD01041C)

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Terms in the title (5)：
Terms in the title
Keywords automatically extracted from the title.
深海堆積物

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, 
磁性鉱物

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, 
含量

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, 
浮遊性有孔虫

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, 
炭素同位体比

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