Collaborative Research: Geological Constraints on ~25 Million Years of Magmatism Along an Arc-transform Junction, Wrangell Volcanic Belt, Alaska

阿拉斯加南部的兰格尔火山带位于一个复杂的构造环境中，一个大洋高原(雅库塔地块)目前正以非常低的角度碰撞并俯冲到阿拉斯加下面。在东部，一个大型的转换断层系统，德纳利断层，边界这个俯冲高原的边缘和一个主要的火山链，过去2500万年来建立的兰格尔火山带，标志着这一交叉点。这种连接在现代会聚边缘环境中很常见，由此产生的火山带记录了板块前缘相对位置的变化和上板块沿走滑断层的平移。人们对在这些复杂环境中产生熔岩的过程知之甚少。在这里，这个研究小组旨在通过对兰格尔火山带的地质、火山岩化学成分和地质年代学的综合研究来破译该带的火山岩的起源。这一结果将对火山链如何在如此复杂的构造环境中发展提供新的理解。该项目还通过以下方式造福社会或推动预期的社会成果：(1)有计划地让代表性不足的少数族裔的学生参与STEM；(2)通过在当地社区的介绍和为兰格尔-圣彼得堡大学编写解释性材料，提高公众的科学素养和公众对科学技术的参与。伊利亚斯国家公园和保护区；以及(3)通过培训研究生和本科生以及支持早期职业研究人员来发展STEM劳动力。本项目研究了采样不足的25 Ma弧形转换岩浆带-阿拉斯加州朗格尔火山带的地球化学-喷发演化。该带被一个主要的走滑断裂--德纳利断裂系统横切，位于雅库塔特平板的边缘和前缘之上。研究人员将收集兰格尔火山带的基岩、碎屑沙/鹅卵石样本，以及沉积学和构造数据。它们将确定基岩和碎屑样品的主量元素和微量元素组成，全岩的锶、钕、铅、氢和锆石的氢同位素浓度，以及40Ar/39Ar和U/Pb年代学。该项目的具体目标是：(1)确定兰格尔火山带岩浆作用的时空历史；(2)破译走滑断裂与板片熔融之间的联系，以及该板片边缘火山带的地球化学演化。这些数据将与地质填图相结合，以提供重要的新约束条件，以了解随着平板前锋向内推进，沿弧形转换结点的板片边缘岩浆活动的发展，以及走滑断层与岩浆产品地球化学之间的关系。

The Wrangell volcanic belt in southern Alaska is situated in a complex tectonic environment where an oceanic plateau (the Yakutat block) is presently colliding with and subducting beneath Alaska at a very low angle. To the east, a large transform fault system, the Denali fault, bounds the edge of this subducting plateau and a major volcanic chain, the Wrangell volcanic belt that has been built up over the last 25 million years, marks this intersection. Such junctions are common in modern convergent margin settings and the resulting volcanic belts record both variations in relative position of the leading front of the slab and translation of the upper plate along strike-slip faults. The processes that generate lavas in these complex settings are poorly understood. Here, this research team aims to decipher the origins of the volcanic rocks in the Wrangell volcanic belt through a comprehensive study of the geology, volcanic rock chemical composition, and geochronology of the belt. The results would provide a new understanding of how volcanic chains develop in such complex tectonic settings. The project also benefits society or advances desired societal outcomes through: (1) planned involvement of students from underrepresented minorities in STEM; (2) increased public scientific literacy and public engagement with science and technology through presentations in local communities and development of interpretive materials for the Wrangell-St. Elias National Park and Preserve; and (3) development of a STEM workforce through training of graduate and undergraduate students and support of early career researchers.This project examines the geochemical-eruptive evolution of an under-sampled 25 Ma arc-transform magmatic belt, the Wrangell volcanic belt in Alaska. The belt is transected by a major strike-slip fault, the Denali fault system, and located above both the edge and leading front of the Yakutat flat slab. The researchers will collect bedrock, detrital sand/cobbles samples, and sedimentological and structural data from the Wrangell volcanic belt. They will determine major and trace element composition, whole rock Sr, Nd, Pb, and Hf, and zircon Hf-isotope concentrations, and 40Ar/39Ar and U/Pb geochronology on bedrock and detrital samples. Specific objectives of the project are to: (1) determine the temporal-spatial history of magmatism of the Wrangell volcanic belt; and (2) decipher the links between strike-slip faulting, and slab melting on the geochemical evolution of this slab edge volcanic belt. These data will be integrated with geological mapping to provide important new constraints on the development of slab edge magmatism along an arc-transform junction as the leading front of the flat slab progresses inboard and the relationship between strike-slip faults and the geochemistry of magmatic products.