Collaborative Research: Investigating Initiation and History of the Aleutian Arc and Composition and Significance of North Pacific Seafloor via Dredge Samples from the R/V Sonne

俯冲是一个基本的构造过程，影响地球的物理和化学演变，并对人类产生许多重要的潜在影响，包括地震和火山灾害，以及作为俯冲岩浆作用的常见产物的矿产资源。 因此，与俯冲有关的过程是公众广泛关注的主题，也是地球科学领域广泛调查的主题。尽管对阿拉斯加-阿留申俯冲系统进行了近世纪的研究，但仍有几个关键问题没有得到解答，包括俯冲带是如何以及何时形成的，以及俯冲的太平洋板块在多大程度上有助于阿拉斯加-阿留申火山下产生的岩浆的形成。该项目将使来自南卡罗来纳州大学和威斯康星大学麦迪逊分校的一组美国科学家能够精确确定阿留申弧形成的时间，并描述正在进入和从这个活跃的火山弧喷发的产物。这是一项合作努力，涉及研究生和本科生，博士后，以及来自德国，俄罗斯和美国的研究人员。该项目的所有数据将向公众开放。该项目有两个广泛相关的主题：1）限制阿留申岛弧的俯冲开始和早期演化的时间，2）描述阿留申岛弧和堪察加岛弧的俯冲输入，并将其与控制岛弧岩浆形成的过程联系起来。作为德国-俄罗斯BERING项目的一部分，对德国R/V索内号SO 249考察队的样品进行分析，将对阿留申弧形成的时间和早期弧产物的地球化学提供限制。该项目还将获得阿留申弧西部邻近北太平洋海底样本的地球化学数据，包括皇帝北方海山东部和西部的地点。这项研究将有助于更好地了解俯冲输入和火山输出之间的地球化学联系，并将提供新的限制和显着改善阿留申群岛和堪察加半岛的弧岩浆成因模型。该奖项反映了NSF的法定使命，并已被认为是值得通过使用基金会的智力价值和更广泛的影响审查标准进行评估的支持。

Subduction is a fundamental tectonic process that shapes the Earth's physical and chemical evolution and has many important potential human impacts, including seismic and volcanic hazards, as well as mineral resources, which are common products of subduction magmatism. As a result, subduction-related processes are the subject of broad public interest and widespread investigation in the geosciences. Despite almost a century of research on the Alaska-Aleutian subduction system, several key questions remain unanswered including how and when the subduction zone was formed and to what extent the subducting Pacific plate contributes to the creation of magma generated beneath Alaska-Aleutian volcanoes. This project will allow a group of U.S. scientists from the University of South Carolina and the University of Wisconsin-Madison to precisely determine the timing of Aleutian arc formation and to characterize the products that are entering and have erupted from this active volcanic arc. This is a collaborative effort involving graduate and undergraduate students, post-docs, and researchers from Germany, Russia and the United States. All data from this project will be made available to the public. The project has two broadly related themes: 1) Constraining the timing of subduction initiation and early evolution of the Aleutian arc, and 2) Characterizing subduction inputs to both the Aleutian and Kamchatka arcs and relating them to the processes controlling arc magma formation. Analyses of samples from Expedition SO249 of the German R/V Sonne as part of the German-Russian BERING project will provide constraints on the timing of Aleutian arc formation and the geochemistry of the early arc products. The project will also obtain geochemical data for north Pacific seafloor samples adjacent to the western Aleutian arc, including sites both east and west of the northern Emperor seamounts. This study will help better understand geochemical linkages between subduction input and volcanic output, and will provide new constraints and significantly improve models of arc magma genesis for the Aleutians and Kamchatka.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.