Collaborative Research: MARGINS--The Relationship Between Water, Trace Elements and Slab Dehydration Across the Mariana and Izu-Bonin Arcs

知识价值。水在俯冲带中的作用在很大程度上是基于B、Ba、K、Rb和U等流体流动元素的行为，而不是直接通过水的测量来理解的。这是因为大多数弧的研究依赖于地面熔岩的数据，这些熔岩在脱气过程中遭受了挥发性损失。已发表的实验研究和跨中美洲弧的熔体包裹体研究表明，水不断地从横跨弧的厚板中释放出来。这与流体可动元素的行为相反，流体可动元素从板上逐渐剥离，并表现出系统的交叉弧变化。本研究的一个基本目的是评估IBM系统的两个不同部分——马里亚纳和伊豆-波宁弧——的水、微量元素和氢和硼的稳定同位素的释放情况。这些位置具有不同的倾角和俯冲速率，因此我们将确定这些物理参数是否对渐进脱水过程中的流体行为有任何影响。本研究的第二个目标是测试板状流体的微量元素和B同位素代表如何很好地跟踪流体向IBM地幔源的输送，以及D/H和B同位素是否追踪类似的流体释放过程，或者每个系统是否独特地追踪不同的脱水阶段。我们提出了一个系统的研究挥发物（CO2, H2O， S， Cl和F），流体可溶性元素（B, Cl, Ba， K， Rb等）和稳定同位素（H， B）在玻璃和橄榄石熔融包裹体（MIs）海底熔岩使用离子探针技术。这项工作将由B同位素的多收集器ICPMS分析以及主要元素的电子探针测量来补充。这些样本包括来自马里亚纳群岛的一套新的交叉链火山，来自马里亚纳海槽的弧后熔岩和玻璃，以及来自伊豆-波宁弧和弧后的熔岩。弧岩浆含水量与流体流动微量元素之间的相关性（或缺乏相关性）将对利用现有微量元素和同位素数据但尚未测量含水量的其他俯冲带地球化学特征的解释产生重要影响。更广泛的影响。该项目将补充正在进行的MI研究，调查劳盆地的融化过程，以及边缘俯冲工厂倡议的科学目标，并将促进美国和日本五个机构科学家之间的合作。该项目将支持伍兹霍尔海洋研究所（WHOI）的一位早期职业女性科学家。作为WHOI和NSF-REU暑期实习项目的一部分，PI将在项目的第二年指导一名本科生，向他们介绍离子微探针技术。这项工作还将引入新的分析方案，以帮助恢复在2002年10月的一场火灾中严重受损的nsf支持的WHOI离子探测设施。

Intellectual Merit. The role of water in subduction zones is largely understood based on behavior of fluid-mobile elements such as B, Ba, K, Rb and U, rather than on measurements of water directly. This is because most studies of arcs rely on data from subaerial lavas which have suffered volatile loss through degassing. Published experimental studies and melt inclusion studies across the Central American arc suggest that water is released continuously from the slab across the arc. This is contrary to the behavior of fluid mobile elements, which are progressively stripped from the slab and show systematic cross-arc changes. A fundamental aim of this study is to evaluate the release of water, trace elements, and stable isotopes of hydrogen and boron across two contrasting segments of the IBM system - the Marianas and the Izu-Bonin arcs. These sites have different dip angles and subduction rates, thus we will determine whether these physical parameters have any impact on fluid behavior during progressive dehydration. The second objective of this study is to test how well trace element and B-isotopic proxies for slab fluids track fluid delivery to IBM mantle sources, and whether D/H and B isotopes trace similar fluid release processes or whether each system uniquely traces different stages of dehydration. We propose a systematic study of volatiles (CO2, H2O, S, Cl, and F), fluid soluble elements (B, Cl, Ba, K, Rb and others) and stable isotopes (H, B) in glasses and olivine hosted melt inclusions (MIs) from submarine lavas using ion microprobe techniques. This work will be complemented by multicollector ICPMS analyses of B isotopes, as well as electron microprobe measurements of major elements. The samples include a new suite of cross-chain volcanoes from the Marianas, back-arc lavas and glasses from the Mariana Trough, and lavas from the Izu-Bonin arc and back-arc. The correlation (or lack thereof) between arc magma water contents and fluid-mobile trace elements will have an important impact on the interpretation of geochemical signatures at other subduction zones with existing trace element and isotopic data but where water contents have not yet been measured.Broader Impacts. This project will complement ongoing MI studies investigating the melting process in the Lau Basin, as well as the scientific objectives of the MARGINS Subduction Factory initiative, and will foster collaboration between scientists at five institutions in the US and Japan. The project will support a female early career scientist at Woods Hole Oceanographic Institution (WHOI). As part of a WHOI and NSF-REU summer intern programs, the PI will mentor an undergraduate student during the 2nd year of the project, introducing them to ion microprobe techniques. This work will also result introduce new analytical protocols to help revitalize the NSF-supported WHOI ion probe facility which was seriously damaged in a fire in October of 2002.