Evaluating the Processes and Timescales of Rhyolitic Differentiation

评估流纹岩分化的过程和时间尺度

• 批准号: 0538214
• 负责人: Frank Ramos
• 金额: $ 15.37万
• 依托单位: Central Washington University
• 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
• 起止时间: 2006-08-01 至 2008-10-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0538214&HistoricalAwards=false
• 关键词: Evaluating; Processes; Timescales; Rhyolitic; Differentiation

Intellectual merit: U-series isotopes have revolutionized our ability to evaluate magmatic timescales and will be used in conjunction with Rb/Sr systematics to constrain the time in which large volumes of intraplate rhyolite are generated. The timing and processes involved in the generation of silicic magmas are relevant to modeling activity at potentially explosive volcanoes, with significant climate and volcanic hazard implications. Baitoushan volcano (NE China/North Korea) is ideally suited for such studies because it has produced multiple young high silica rhyolites including a large volume (~100 km3) pyroclastic eruption as recently as ~1000 AD. All eruptive units are sufficiently young that both short-lived 238U-230Th-226Ra and 235U-231Pa isotopic systems as well as long-lived radiogenic isotopes can be used in combination to assess magmatic timescales. Moreover, sampling is sufficient to carry out the proposed work, thus saving on the time and cost of the proposed research. Timing of magmatic fractionation events involved in the generation of associated mafic and silicic magmas in this volcano will be evaluated through analysis of accessory phenocryst minerals. Single crystal Pb and Sr isotope analyses will also be used as tracers to quantify the effects of open-system processes such as crustal contamination, magma recharge, and post-eruption alteration. In combination these data will allow detailed assessment of such processes on the overall evolution of the volcano as well as their effects on the fidelity of the various isotopic dating methods.Broader Impacts include (1) involvement of an undergraduate into cutting-edge research in the geological sciences, (2) international collaborations, and (3) relevance to volcanic risk assessment. Regarding the latter point, a "seismic crisis" at Baitoushan within the last decade raised concerns that the volcano could erupt again in the near future. Better understaning of the timescale of magma evolution could be useful in predicting future activity. Finally, Baitoushan's location on the border between China and North Korea (DPRK) has potential political significance, and contributions to understanding volcanic behavior could promote international 'good will'.

智力价值：U系列同位素彻底改变了我们评估岩浆时间尺度的能力，并将与Rb/Sr系统学结合使用，以限制大量板内流纹岩生成的时间。 硅岩浆生成的时间和过程与潜在爆发性火山的模拟活动相关，对气候和火山灾害具有重大影响。白头山火山（中国东北部/朝鲜）非常适合此类研究，因为它产生了多个年轻的高硅流纹岩，其中包括最近约公元 1000 年的大体积（约 100 平方公里）火山碎屑喷发。 所有喷发单元都足够年轻，因此可以组合使用短寿命 238U-230Th-226Ra 和 235U-231Pa 同位素系统以及长寿命放射性同位素来评估岩浆时间尺度。 此外，抽样足以开展拟议的工作，从而节省了拟议研究的时间和成本。将通过对副斑晶矿物的分析来评估与该火山中相关镁铁质和硅质岩浆生成相关的岩浆分馏事件的时间。单晶铅和锶同位素分析也将用作示踪剂，以量化开放系统过程的影响，例如地壳污染、岩浆补给和喷发后蚀变。结合这些数据，可以详细评估此类过程对火山整体演化的影响，以及它们对各种同位素测年方法保真度的影响。更广泛的影响包括 (1) 本科生参与该领域的前沿研究地质科学，(2) 国际合作，以及 (3) 与火山风险评估的相关性。对于后一点，白头山近十年来的“地震危机”引发了人们对火山在不久的将来可能再次喷发的担忧。更好地了解岩浆演化的时间尺度可能有助于预测未来的活动。 最后，白头山位于中国和朝鲜边境，具有潜在的政治意义，对了解火山行为的贡献可以促进国际“善意”。