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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

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中文摘要
翻译
PI将继续探索夏威夷、社会岛和留尼汪岛等热点地区以及其他目前正在调查的松山时代火山中记录的野外行为。在不同的完成阶段,对与莫洛凯岛、莫雷亚岛和留尼汪岛上记录的奥杜瓦伊和留尼汪岛上的事件相对应的六个过渡区进行了研究。对于每一次调查,他将进行完整的矢量研究,特别是利用新改进的多样本方法来确定绝对古强度。为了确定所涉及的实际反转,他还将获得每个迄今未标明日期的截面的辐射年龄。
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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