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RUI: Paleomagnetic Study of Transitional Fields Recorded Throughout the Cenozoic by Australasian Lavas

RUI: Paleomagnetic Study of Transitional Fields Recorded Throughout the Cenozoic by Australasian Lavas
RUI:澳大利亚熔岩在整个新生代记录的过渡场的古地磁研究
批准号:
0715181
负责人:
Kenneth Hoffman
金额:
$11.29万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2006
资助国家:
美国
项目状态:
已结题
起止时间:
2006-12-01 至 2009-08-31

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中文摘要
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Hoffman0230347The most remarkable feature of Earth's magnetic field is its ability to reverse polarity, and much of our knowledge of this phenomenon has come from the paleomagnetic record found in rocks. The goal of this project is to locate, sample and analyze transitional field behavior recorded in Australasia by hotspot-erupted lavas that comprise the Great Dividing Range of Eastern Australia and New Zealand's South Island volcanoes. These volcanics are known to span the past 70 Ma, that is, the entire Cenozoic period, and thus offer an unprecedented opportunity to investigate aspects of Earth's reversing geodynamo from a single regional site over considerable geologic time. In particular, the investigators plan to test the claim that an inordinate number of transitional virtual geomagnetic poles (VGPs) associated with several available paleomagnetic reversal records are found near Australia. This observation has prompted an intriguing possibility, namely, that a concentration of magnetic flux emanating from Earth's fluid outer core below Australasia has largely dominated the field structure during many past reversals, and further, that this flux feature is a consequence of long-standing physical conditions of the lowermost mantle. Because the volcanics of Australia and New Zealand are almost directly above the claimed flux concentration, the project is designed to test this hypothesis. It is anticipated that results from this project will shed light on whether the lower mantle has had such a pronounced effect on the transitioning field over much, or all, of the Cenozoic period, and if so, whether any observable variation, or drift, of the flux feature has occurred since the end of the Mesozoic. In addition, an attempt will be made to determine both paleointensity over this span of time as well as precise radiometric ages of the lava sections. The project will be assisted by undergraduate physics majors working on their senior projects (a mandatory requirement for graduation at Cal Poly State University), exposing them to many aspects of original basic research. Dr Gary Acton of Texas A& M University and Professor Brad Singer of the University of Wisconsin will collaborate on this research.--
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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
RUI: Paleomagnetic Phase of a Collaborative Study to Spatially and Temporally Delineate the Matuyama-Brunhes Polarity Reversal as Recorded in Tahitian Lava Flows
RUI: Paleomagnetic Study of the Matuyama-Brunhes Reversal from Dated Lava Sequences on Tahiti, French Polynesia
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