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A Model For Alternating Effusive and Explosive Rhyolite Volcanism: The -1350 A.D. Eruption of Tarawera, New Zealand

A Model For Alternating Effusive and Explosive Rhyolite Volcanism: The -1350 A.D. Eruption of Tarawera, New Zealand
交替喷发和爆炸流纹岩火山活动的模型:公元-1350 年新西兰塔拉威拉火山喷发
批准号:
9815042
负责人:
Stephen Self
金额:
$20.0万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
1999
资助国家:
美国
项目状态:
已结题
起止时间:
1999-01-01 至 2003-06-30

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中文摘要
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英文摘要
9815042SelfThe c. 1350 AD activity of Mount Tarawera was the largest (5-10 km3 magma volume) eruption in New Zealand, and one of the largest rhyolitic eruptions in the world, during the last millennium. The eruption products are locally known as the Kaharoa formation. This event featured remarkable fluctuations in eruption style from highly explosive to effusive as a major pyroclastic fall deposit and several lava domes were emplaced. This collaborative study with New Zealand volcanologists will build on earlier mapping of Tarawera volcano to produce an integrated picture of the processes of a major rhyolite eruption. Detailed field mapping of the relationships between the Kaharoa lava domes, block and ash pyroclastic flow deposits, and careful logging of the layers in the fall deposit will determine the details of the dispersal, clast characteristics, and grain size distribution. Sampling of the eruption products for granulometric, grain morphologic, and crystal and vesicle size distribution studies will help determine the physical state of the magma upon eruption and eruption mechanisms. Textural analysis of the rhyolite pyroclastics and dome lava samples, when combined with geochemical data to be obtained in the collaborative part of this study, will reveal information about the physical state (degree of undercooling, degassing, crystallization) of the magma during various phases of the eruption and the control that this exerted on the changing eruption styles. Results of the study will be a general model for this type of volcanism worldwide, further understanding of the controls on variations in eruption style in lava dome-forming volcanism by magma degassing and effusion rate, and documentation of widely dispersed plinian deposits coincident with effusive rhyolitic activity. The results will also be an integral part of a volcanic hazard assessment for future recurrences of this type of volcanism, both in New Zealand and worldwide.
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Collaborative Research: Collapse of the Valles Caldera: An Integrated Lithic and Pumice Compositional Study of the Bandelier Tuff
  • 批准号:
    9910148
  • 项目类别:
    Standard Grant
  • 资助金额:
    $10.0万
  • 财政年份:
    2000
  • 负责人:
    Stephen Self
  • 依托单位:
Quantitative Constraints on the Emplacement Style and Eruption Duration of Continental Flood Basalt Lava Flows
  • 批准号:
    9527060
  • 项目类别:
    Standard Grant
  • 资助金额:
    $22.07万
  • 财政年份:
    1996
  • 负责人:
    Stephen Self
  • 依托单位:
Emplacement of the 1991 Ignimbrite at Mount Pinatubo, Philippines: Evaluation of Present Ideas on Deposition from Pyroclastic Flows
  • 批准号:
    9419111
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $18.89万
  • 财政年份:
    1995
  • 负责人:
    Stephen Self
  • 依托单位:
Flood Basalt Eruption Mechanisms and Atmospheric Impact
  • 批准号:
    9316881
  • 项目类别:
    Standard Grant
  • 资助金额:
    $1.2万
  • 财政年份:
    1994
  • 负责人:
    Stephen Self
  • 依托单位:
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