Collaborative Research: Element Recycling from UHP Metasediments: Evidence and Consequences

这是一项研究的超高压（UHP）变质沉积物，已被俯冲到75公里，量化元素循环过程中脱水和/或熔融提取在火山弧。研究的目的是了解物质进出俯冲带和火山弧的通量。反过来，这是理解全球地球化学的基础，也是MARGINS倡议的中心目标。这项对超高压变质沉积岩样品的研究将为主要元素和微量元素以及同位素交换温度计收集新的数据。将选定的变质沉积物中的微量元素与正常细粒沉积岩中的微量元素进行比较，以确定与熔体提取或脱水有关的系统变化。结果应提供的预算的关键元素在俯冲变质沉积物，并提取这些元素通过流体和熔体运输到弧下的岩浆成因区。更广泛的影响包括培训两名研究生，在论文和谈话中介绍结果，在SedDB全球沉积岩数据库中存档数据，以及通过网络和PI的非正式讲座进行广泛的持续外展工作。

This is a study of ultrahigh-pressure (UHP) metasediments that have been subducted to 75 km, to quantify element recycling processes during dehydration and/or melt extraction at volcanic arcs. The aim of the research is to understand the fluxes of material into and out of subduction zones and volcanic arcs. In turn, this is fundamental to understanding global geochemistry, and is a central goal of the MARGINS Initiative. This research on UHP metasedimentary samples will collect new data for major- and trace-element and isotope exchange thermometers. Trace elements in selected metasediments will be compared to those in normal fine-grained sedimentary rocks to identify systematic changes associated with melt extraction or dehydration. The results should provide constraints on the budget of key elements in subducting metasediments, and the extraction of these elements via fluid and melt transport into the zone of magma genesis beneath arcs. Broader impacts include training of two graduate students, presentation of results in papers and talks, archiving of data in the SedDB global sedimentary rock data base, and extensive, ongoing outreach efforts via web and informal lectures by the PI's.