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: 0746379
• 负责人: Alan Levander
• 金额: $ 13.79万
• 依托单位: William Marsh Rice University
• 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 2013-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0746379&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：在门多西诺三重连接处制造圣安德烈亚斯断层：第IIA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连接处的结构，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州-俄勒冈州海岸延伸到西经120 °，北纬37度至43度。门多西诺三联点是北美、太平洋和戈尔达板块的交汇点，相对于固定的北美参照系，它随着时间的推移向北迁移。 一组相互作用的过程与迁移的门多西诺三重结，从表面延伸到软流圈水平（100公里深），作用修改北美岩石圈从一个俯冲复合体在戈尔达俯冲带的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从软流圈到北美板块的热量和质量通量，对MTJ附近发生的过程进行了主导控制。戈尔达地壳和上覆沉积物俯冲，并成为从卡斯卡迪亚俯冲带的增生碎屑合并为一体，因为这一质量流入新兴的转换边缘，并成为结构化的圣安德烈亚斯走滑系统。与此同时，戈尔达板块南部的板块缺口导致软流圈上升和减压熔融，这使圣安德烈亚斯断层附近的北美板块发生了岩浆作用。再加工和膨胀的岩石圈变厚，形成一个小的门多西诺角造山高原，而侵蚀通量的大部分上地壳回俯冲带沿着构造控制的北向河流。在东部，Gorda-Juan de Fuca俯冲导致喀斯喀特火山，这有助于大陆地壳的增长，分离和循环。 1993- 1994年广泛的主动震源地震研究的结果提供了对MTJ区域极好的地壳控制。目前部署的宽带地震仪阵列将一直保持到2009年4月，以提供数据集，使我们能够对MTJ区域和最南端的级联的地幔和下地壳的结构、组构以及地震和地震变形进行成像。 使用各种分析技术，我们将产生一个三维的地壳和上地幔的地震速度模型，将包括在事件和强地面运动特性的北方加州和南部俄勒冈州，一个网站的潜在破坏性大地震。