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Paleomagnetic Studies of Transitional Behavior Recorded in Pleistocene Lavas with Emphasis on Long-Lived Field States

Paleomagnetic Studies of Transitional Behavior Recorded in Pleistocene Lavas with Emphasis on Long-Lived Field States
更新世熔岩记录的过渡行为的古地磁研究,重点是长寿的磁场状态
批准号:
9205603
负责人:
Kenneth Hoffman
金额:
$20.0万
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
1992
资助国家:
美国
项目状态:
已结题
起止时间:
1992-08-01 至 1996-07-31

项目摘要

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中文摘要
翻译
PI将继续探索在夏威夷、社会岛和留尼汪热点以及其他目前正在调查的地区记录的松山时代火山的现场行为。在不同的完成阶段,对六个过渡带的研究对应于在莫洛凯岛、莫雷阿岛和留尼汪岛记录的奥杜瓦伊和留尼汪亚年代之间的事件。对于每次调查,他将进行完整的矢量研究,特别是利用新改进的多标本方法来研究绝对古强度。为了确切地确定所涉及的实际反转,他还将获得迄今为止尚未确定日期的每个剖面的辐射年龄。
英文摘要
The PI will continue exploration of field behavior as recorded in Matuyama-aged volcanics from the Hawaii, Society Island and Reunion hotspots and others currently under investigation. In various stages of completion are studies of six transition zones corresponding to events which bound the Olduvai and Reunion subchrons recorded on the islands of Molokai, Moorea and Reunion. For each investigation, he will conduct complete-vector studies utilizing, in particular new-refined multi-specimen approach to absolute paleointensity. In order to ascertain with certainty the actual reversals involved,m he will also obtain radiometric ages for each thus far undated section.
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会议论文
Comprehensive Study of the Mid-Cenozoic Liverpool, Australia, Reversal: Construction of a Highly Detailed, Full-Vector Paleomagnetic Record From Southern Hemisphere Lavas
  • 批准号:
    1015360
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $26.94万
  • 财政年份:
    2010
  • 负责人:
    Kenneth Hoffman
  • 依托单位:
RUI: Paleomagnetic Study of Transitional Fields Recorded Throughout the Cenozoic by Australasian Lavas
  • 批准号:
    0715181
  • 项目类别:
    Standard Grant
  • 资助金额:
    $11.29万
  • 财政年份:
    2006
  • 负责人:
    Kenneth Hoffman
  • 依托单位:
RUI: Paleomagnetic Study of Transitional Fields Recorded Throughout the Cenozoic by Australasian Lavas
RUI: Paleomagnetic Phase of a Collaborative Study to Spatially and Temporally Delineate the Matuyama-Brunhes Polarity Reversal as Recorded in Tahitian Lava Flows
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