Collaborative Research: Making the San Andreas Fault at the Mendocino Triple Junction: Part II

合作研究：在门多西诺三重交界处制造圣安德烈亚斯断层：第二部分

• 批准号: 0745899
• 负责人: Eugene Humphreys
• 金额: --
• 依托单位: University of Oregon Eugene
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-02-15 至 2011-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0745899&HistoricalAwards=false
• 关键词: Collaborative; Research; Making; San; Andreas

Collaborative Research: Making the San Andreas Fault at the Mendocino Triple Junction: Part IIA dense array of broadband seismographs have been deployed to investigate the structure of the Mendocino Triple Junction, the northernmost terminus of California's famed San Andreas fault system. The study area extends from the California-Oregon coast to 120o W longitude, and from 37 degrees to 43 degrees North latitude. The Mendocino Triple Junction, the site where the North America, Pacific and Gorda plates meet, migrates northward with time relative to a fixed North American reference frame. A set of interacting processes associated with the migrating Mendocino Triple Junction, extending from the surface to asthenospheric levels ( 100 km depth), act to modify North America lithosphere from a subduction complex at the Gorda subduction zone to the San Andreas transform plate boundary. The mantle imparts a dominant control on the processes occurring near the MTJ through its control on plate strength and kinematics and the flux of heat and mass from the asthenosphere to the North American plate. Gorda crust and overlying sediment subduct and become incorporated with accretionary terranes from the Cascadia subduction zone as this mass flows into the emerging transform margin and becomes structured into the San Andreas strike-slip system. Simultaneously, slab gap opening south of the Gorda slab causes asthenospheric ascent and decompression melting, which magmatically underplates North America near the San Andreas fault. The reprocessed and inflated lithosphere thickens to create a small Cape Mendocino orogenic plateau, while erosion fluxes large fractions of the upper crust back to the subduction zone along tectonically controlled north-trending rivers. To the east, Gorda-Juan de Fuca subduction results in the Cascade volcanoes, which contribute to continental crust growth, segregation and recycling. Results of an extensive active source seismic study in 1993-94 provide excellent crustal control in the MTJ region. The broadband seismograph array now deployed will remain in place through April 2009, to provide a dataset that will enable us to image the structure, fabric, and seismic and aseismic deformation of the mantle and lower crust in the MTJ region and the southernmost Cascades. Using a variety of analysis techniques we will produce a 3-D seismic velocity model of the crust and upper mantle that will be included in event and strong ground motion characterization for northern California and southern Oregon, a site of potentially devastating great earthquakes.

合作研究：在门多西诺三重交界处制造圣安德烈亚斯断层：第二部分：密集的宽带地震仪阵列已被部署来调查门多西诺三重交界处的结构，这是加州著名的圣安德烈亚斯断层系统的最北端。研究区域从加利福尼亚-俄勒冈海岸延伸到西经1200度，从北纬37度延伸到43度。门多西诺三重交汇处是北美、太平洋和戈尔达板块交汇的地方，相对于一个固定的北美参照系，它随着时间向北移动。与门多西诺三结迁移相关的一系列相互作用过程，从地表延伸到软流层（100公里深），将北美岩石圈从戈达俯冲带的俯冲复合体改造为圣安德烈亚斯转换板块边界。地幔通过控制板块强度和运动学以及软流层向北美板块的热量和质量通量，对发生在MTJ附近的过程起着主要的控制作用。戈达地壳和上覆沉积物俯冲，并与卡斯卡迪亚俯冲带的增生地体合并，这些物质流入新兴的转换边缘，并构造成圣安德烈亚斯走滑体系。同时，戈尔达板块以南的板块裂口打开，引起软流圈上升和减压融化，使北美洲在圣安德烈亚斯断层附近的岩浆板块底部。经过再加工和膨胀的岩石圈增厚，形成了一个小的门多西诺角造山带，而侵蚀作用将大部分上地壳沿着构造控制的北向河流流回俯冲带。在东部，戈达-胡安-德富卡俯冲形成喀斯喀特火山，这促进了大陆地壳的生长、分离和再循环。1993- 1994年广泛的活源地震研究结果为MTJ地区提供了良好的地壳控制作用。现在部署的宽带地震仪阵列将一直保留到2009年4月，以提供一个数据集，使我们能够对MTJ地区和最南端的喀斯喀特地区的地幔和下地壳的结构、结构、地震和地震变形进行成像。使用多种分析技术，我们将生成地壳和上地幔的三维地震速度模型，该模型将包括在北加州和俄勒冈州南部的事件和强地面运动特征中，这是一个潜在的破坏性大地震地点。