Collaborative Research: Taking the Pulse of the Northwest Hawaiian Ridge: Implications for Flux Variations and Mid-Cenozoic Pacific Plate Motions

合作研究：把握西北夏威夷海脊的脉搏：对通量变化和中新生代太平洋板块运动的影响

基本信息

批准号：
1834758
负责人：
Michael Garcia
金额：
$ 27.14万
依托单位：
University of Hawaii
依托单位国家：
美国
项目类别：
Standard Grant
财政年份：
2018
资助国家：
美国
起止时间：
2018-09-01 至 2024-08-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1834758&HistoricalAwards=false
关键词：
Collaborative Research Taking Pulse Northwest

项目摘要

The evolution of the Hawaiian Islands and how and why magmatism on the Big Island changes over time is important to understand both from a scientific and practical point of view. The island of Hawaii is the most recent expression of a chain of islands (the Hawaiian-Emperor Chain) related to a single upwelling in the mantle (i.e. a mantle plume) that periodically punches up through the ocean crust and erupts massive amounts of lava onto the seafloor and builds islands. The Hawaiian-Emperor Chain is not only the classic example of a mantle plume, it is also the hottest known. This plume has been active for 80 million years and has formed a trail of volcanoes extending ~6000 km in length from Hawaii to the northwestern reaches of the Pacific Ocean. Despite the importance of this chain, not only to our understanding of the origin and evolution of mantle plumes but also to how tectonic plates move across the face of the Earth over time, there are still major gaps in our knowledge of the age progression of the eruptions and chemical variations of the erupted lavas along the chain. This research analyzes twenty newly-collected rock samples from eleven volcanoes along the northwestern part of the Hawaiian-Emperor Chain. This work provides new age dates using state-of-the-art argon-argon dating techniques and collects whole-rock geochemistry on the lavas, as well as data on a suite of radiogenic isotopes to determine mantle temperatures associated with the eruptions. These data will be used to better understand the magmatic evolution of the Hawaiian mantle plume and how its age progression better constrains Pacific Ocean basin plate tectonics. Broader impacts of the work include student training and providing biologists with better information about the biogeography and radiation of native Hawaiian species across the ocean. Results of the research work will be used to create a new interactive exhibit on the Hawaiian Islands and the Hawaiian-Emperor Chain for the Bishop Museum in Honoloulu, in collaboration with museum staff. This provides a major public outreach vehicle for science as the Bishop Museum attracts hundreds of thousands of visitors a year from the US and abroad. The Hawaiian-Emperor Chain is the most well-defined mantle plume on the planet and is optimal for evaluating mantle plume related processes and assessing their relationship to plate tectonics and tectonic plate motion. This research uses 20 newly collected samples from eleven volcanoes that were collected on an oceanographic expedition characterizing the northwest region of the Hawaiian-Emperor Chain using remotely operated vehicles in the new US Hawaiian Marine Monument. Information on the geochemistry and mineralogical relationships of these samples will be generated using a wide variety of observational and analytical techniques. In addition to petrographic and mineralogical examination of the samples, whole rock geochemical data will be collected, as will mass spectrometric data on the composition and ratios of the radiogenic isotopes: lead, strontium, neodymium, and hafnium. Olivine compositions will also be determined. The research will compile and correct, to common standards, all published data from the northwest part of this island chain and combine it with the new data to create a comprehensive geochemical and age date database that can be used to test models for this part of the chain's formation and evolution during the Cenozoic. Results will be modeled using geochemical and geophysical approaches to provide fundamental new insights into mantle plumes and plate kinematics. New geochemical data will be used to determine the long-term evolution of the Hawaiian mantle plume source components and to evaluate whether there have been systematic variations in mantle temperature, melting pressure, and/or source lithology over time. The new ages will be utilized to revise Cenozoic Pacific plate motions and to compute differential motions as proxies for stress changes along the island chain with time to evaluate the effects of plate motion on magma flux rate.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

从科学和实践的角度理解夏威夷群岛的演化以及大岛上的岩浆作用如何以及为何随时间变化非常重要。夏威夷岛是一系列岛屿（夏威夷-皇帝链）的最新表现形式，与地幔中的单一上升流（即地幔柱）有关，该上升流周期性地冲破洋壳并向海洋上喷发大量熔岩。海底并建造岛屿。夏威夷皇帝链不仅是地幔柱的经典例子，也是已知最热门的例子。这个羽流已经活跃了 8000 万年，形成了一条从夏威夷到太平洋西北地区绵延约 6000 公里的火山尾迹。尽管这条链很重要，不仅对我们理解地幔柱的起源和演化，而且对构造板块如何随着时间的推移在地球表面移动，我们对地幔柱的年龄进展的了解仍然存在重大差距。沿链喷发的熔岩的喷发和化学变化。这项研究分析了夏威夷-皇帝链西北部 11 座火山中新采集的 20 个岩石样本。这项工作利用最先进的氩-氩测年技术提供了新的年龄日期，并收集了熔岩的全岩地球化学数据，以及一套放射性同位素的数据，以确定与喷发相关的地幔温度。这些数据将用于更好地了解夏威夷地幔柱的岩浆演化以及其年龄进展如何更好地限制太平洋盆地板块构造。这项工作的更广泛影响包括学生培训以及为生物学家提供有关夏威夷本土物种跨洋生物地理学和辐射的更好信息。研究工作的结果将用于与博物馆工作人员合作，为檀香山主教博物馆创建一个关于夏威夷群岛和夏威夷皇帝链的新互动展览。这为科学提供了一个主要的公共宣传工具，因为毕夏普博物馆每年吸引数十万来自美国和国外的游客。夏威夷-皇帝链是地球上最清晰的地幔柱，最适合评估地幔柱相关过程并评估它们与板块构造和构造板块运动的关系。这项研究使用了从 11 座火山中新采集的 20 个样本，这些样本是在一次海洋学考察中使用遥控车辆在新的美国夏威夷海洋纪念碑中收集的，该海洋学考察描绘了夏威夷-皇帝链的西北地区。有关这些样本的地球化学和矿物学关系的信息将通过各种观测和分析技术生成。除了样品的岩相学和矿物学检查外，还将收集全岩石地球化学数据，以及有关放射性同位素（铅、锶、钕和铪）的成分和比率的质谱数据。橄榄石的成分也将被测定。该研究将按照通用标准编译和修正该岛链西北部的所有已发布数据，并将其与新数据相结合，创建一个综合的地球化学和年龄日期数据库，可用于测试该岛链这一部分的模型。新生代链的形成和演化。将使用地球化学和地球物理方法对结果进行建模，以提供对地幔柱和板块运动学的基本新见解。新的地球化学数据将用于确定夏威夷地幔柱源成分的长期演化，并评估地幔温度、熔化压力和/或源岩性是否随时间发生系统变化。新年龄将用于修正新生代太平洋板块运动并计算微分运动作为沿岛链随时间变化的应力变化的代理，以评估板块运动对岩浆通量率的影响。该奖项反映了 NSF 的法定使命，并被视为值得通过使用基金会的智力优点和更广泛的影响审查标准进行评估来支持。