Developing a comprehensive model of subduction and continental accretion at Cascadia

开发卡斯卡迪亚俯冲和大陆增生的综合模型

• 批准号: 1144771
• 负责人: Yang Shen
• 金额: $ 20.66万
• 依托单位: University of Rhode Island
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-03-15 至 2015-02-28
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1144771&HistoricalAwards=false
• 关键词: Developing; comprehensive; model; subduction; continental

Cascadia is a prime site to understand subduction dynamics and continental accretion, because it has one of the youngest subducting slabs in the world and a wide range of tectonic units. A variety of scientific questions can be addressed at Cascadia: What controls the subduction zone segmentation? What is the role of water transport in the subduction zone? Where does melting occur and how does magma migrate in the mantle and crust? And how does oceanic lithosphere accrete to the continent? Paleoseismic records show that Cascadia has a history of generating ~M9 megathrust earthquakes, so research is needed to improve the assessment of seismic and tsunami hazards from megathrust earthquakes.This project develops and implements an advanced seismological method to construct a comprehensive, high-resolution velocity model of the crust and upper mantle for the entire Cascadia subduction zone. The velocity model provides a detailed structural framework and new understanding of the subduction processes. The structural correlations of a well-resolved model help address whether serpentinization of the forearc mantle varies substantially along strike and how it is related to the subduction of sediments, pre-existing features on the slab, and melt production beneath the volcanic arc. The project tests whether the recurrence of episodic tremor and slow slip events is related to properties of the overriding plate or the subducting oceanic plate. The new crustal model helps in understanding how accretion of oceanic lithosphere contributes to continental growth and subduction evolution. Accurate and high-resolution characterization of the crust and upper mantle structure is also critical to refining seismic and tsunami hazard assessment in Cascadia.

卡斯卡迪亚是了解俯冲动力学和大陆增生的主要地点，因为它拥有世界上最年轻的俯冲板块之一和广泛的构造单元。在卡斯卡迪亚可以解决各种科学问题：是什么控制着俯冲带的分割？水在俯冲带中的作用是什么？熔融发生在哪里？岩浆如何在地幔和地壳中迁移？海洋岩石圈是如何增生到大陆上的？古地震记录表明卡斯卡迪亚有发生~M9级大逆冲断层地震的历史，因此需要开展研究，以提高对大逆冲断层地震和海啸危险性的评估。本项目开发并实施了一种先进的地震学方法，以构建整个卡斯卡迪亚俯冲带的地壳和上地幔的综合、高分辨率速度模型。速度模型提供了一个详细的结构框架和新的理解俯冲过程。结构相关性的一个很好的解决模型有助于解决是否蛇纹岩化的弧前地幔变化很大沿着走向，以及它是如何与俯冲的沉积物，预先存在的功能板，火山弧下的熔融生产。该项目测试了幕式地震和缓慢滑动事件的复发是否与上覆板块或俯冲大洋板块的性质有关。新的地壳模型有助于理解大洋岩石圈的增生作用对大陆生长和俯冲演化的影响。准确和高分辨率地描述地壳和上地幔结构对于完善卡斯卡迪亚的地震和海啸危险评估也至关重要。