Collaborative Research: Elucidating the Geologic Record of Late Paleozoic Subduction Initiation Along the Southwestern Margin of Laurentia, Southern California and Sonora, Mexico

合作研究：阐明南加州劳伦西亚和墨西哥索诺拉西南缘晚古生代俯冲起始的地质记录

• 批准号: 1322043
• 负责人: Robinson Cecil
• 金额: $ 18.5万
• 依托单位: The University Corporation, Northridge
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2013
• 资助国家: 美国
• 起止时间: 2013-08-01 至 2018-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1322043&HistoricalAwards=false
• 关键词: Collaborative; Research; Elucidating; Geologic; Record

The principle aim of this project is to document the timing and response of the southwestern Laurentian margin to the initiation of subduction during late Paleozoic time. Although the recycling of lithosphere at subduction zones is a fundamental part of plate tectonic theory, the manner by which subduction zones initiate is a poorly constrained process, largely because there are few modern examples and ancient examples are largely not recognized or well preserved. Unique sequences of sedimentary and volcanic rocks exposed in southern California (El Paso Mountains region) and northern Mexico (Carborca Block) will be investigated in order to better understand how subduction inception is recorded in stratigraphic successions and how the paleogeography of continental margins evolves in response to the onset of plate convergence. We propose that continental margin successions recording subduction initiation will have predictable deepening and shallowing trends and distinct changes in sand composition and detrital zircon provenance through time reflecting the changing paleogeography of source regions. An additional geochemical and geochronologic investigation of volcanic sequences and coeval intrusions will be used to constrain the timing and petrogenesis of magmatic products, which we suggest will record conditions unique to cold, nascent continental arc settings. Results of this project may contribute significantly to global models of the birth and development of subduction zones. This project is a multi-disciplinary and collaborative effort between researchers at California State University - Northridge and Northern Arizona University, which are both minority-serving institutions. In addition to the science goals of the project, this research will provide training and mentorship for masters level and undergraduate students and promote the involvement of underrepresented groups in STEM research. Sample collections and study results will be used for the development of resources for teaching, community outreach, and further research.

该项目的主要目的是记录晚古生代期间西南劳伦森边缘俯冲开始的时间和响应。虽然俯冲带岩石圈的再循环是板块构造理论的基本组成部分，但俯冲带的形成方式是一个不受约束的过程，主要是因为现代的例子很少，而古代的例子基本上没有被认识或保存完好。将对加州南部（埃尔帕索山脉地区）和北方墨西哥（Carborca地块）出露的独特沉积岩和火山岩序列进行调查，以便更好地了解俯冲开始如何记录在地层序列中，以及大陆边缘的古地理如何响应板块会聚的开始而演变。我们建议，大陆边缘继承记录俯冲开始将有可预测的加深和变浅的趋势和砂的组成和碎屑锆石的来源，通过时间的变化，反映了不断变化的古地理源区的明显变化。火山序列和同时代侵入体的额外的地球化学和地质年代学调查将用于限制岩浆产物的时间和岩石成因，我们建议将记录独特的条件，冷，新生大陆弧设置。该项目的成果可能对俯冲带的诞生和发展的全球模型做出重大贡献。该项目是加州州立大学-北岭分校和北方亚利桑那大学的研究人员之间的多学科协作努力，这两所大学都是为少数群体服务的机构。除了该项目的科学目标外，这项研究还将为硕士和本科生提供培训和指导，并促进代表性不足的群体参与STEM研究。样本收集和研究结果将用于教学资源的开发，社区推广和进一步的研究。