Collaborative Research: How have orogenies, rifting, and recent mantle dynamics shaped the lithosphere beneath the New England Appalachians?

合作研究：造山运动、裂谷和最近的地幔动力学如何塑造新英格兰阿巴拉契亚山脉下方的岩石圈？

• 批准号: 2146804
• 负责人: Paul Karabinos
• 金额: $ 11.78万
• 依托单位: Williams College
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-07-01 至 2025-06-30
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2146804&HistoricalAwards=false
• 关键词: Collaborative; Research; How; orogenies; rifting

Continents represent a key component of the Earth’s plate tectonic system. Plate tectonics appears to be unique among all planetary bodies in our solar system and plays a crucial role in making our planet hospitable to life. Continents are formed and modified by fundamental plate tectonic processes, including volcanism, mountain-building, collisions with other continental masses, and rifting or breakup of supercontinents. Understanding the evolution of continental lithosphere (that is, the crust and uppermost mantle beneath continents) through time remains one of the most important challenges in Earth science. This project will study the processes that have shaped the continental lithosphere beneath the New England Appalachians through geologic time using a multi-disciplinary approach that includes seismic imaging of the crust and upper mantle, the analysis of geological structures, and dating the motion on ancient faults. The investigators will carry out detailed imaging using seismic waves from distant earthquakes measured at seismometers deployed in two linear arrays (one across New York and Massachusetts, the other across Vermont, New Hampshire, and Maine). They will pair their seismic imaging work with studies of geologic structures exposed at the surface that will provide essential context on its plate tectonic history. The integration of information obtained from both approaches will illuminate the processes that have shaped the lithosphere beneath New England through the geologic past, opening a window into how continental lithosphere evolves as a part of the Earth’s plate tectonic system.This project aims to understand how rifting, subduction, and terrane accretion have shaped lithospheric structure beneath New England: Does the lithosphere preserve a record of subduction and accretion or does lithospheric structure heal over time? How do subsequent accretion events overprint the structure of earlier collisions? How did Mesozoic rifting affect the structure of Paleozoic accretions? Are recent to ongoing mantle processes modifying the lithospheric structure? The investigators will analyze data from the NEST (New England Seismic Transects) experiment, a deployment of ~25 broadband seismometers that is configured to resolve crustal targets on length scales that are appropriate for direct linkage with geological structures. They will apply a suite of imaging techniques (receiver function analysis, body wave travel time analysis, wavefield migration imaging, and SKS splitting measurements) that will provide a comprehensive view of both the isotropic and anisotropic structure of the New England crust and upper mantle, including the region underlain by the so-called Northern Appalachian Anomaly (NAA). The U-Pb geochronology work will focus on the identification and analysis of xenocrystic (inherited) cores in zircon grains from arc plutonic and volcanic rocks from the Shelburne Falls and Bronson Hill arcs, in order to understand the history and timing of Taconic (and later) orogenic processes. The investigators will also conduct field work and structural analyses to investigate the extent and relative timing on frontal thrusts of basement massifs and the Taconic Mountains in western New England and New York, and the Connecticut Valley border fault system in central New England. They will constrain the timing of deformation by collecting and dating samples via 40Ar/39Ar geochronology from these regions, in order to determine how widespread reactivation of old faults (and displacement on new faults) has been throughout the region. The project emphasizes undergraduate involvement in cross-disciplinary research and field work, particularly by participants from groups that have been historically underrepresented in Earth science, enabled by collaboration among faculty at a liberal arts college and research institutions.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

大陆是地球板块构造系统的重要组成部分。板块构造在我们太阳系的所有行星体中似乎是独一无二的，在使我们的星球适合生命方面发挥着至关重要的作用。大陆的形成和修改基本板块构造过程，包括火山活动，造山运动，与其他大陆块碰撞，和裂谷或分裂的超级大陆。了解大陆岩石圈（即大陆之下的地壳和上地幔）随时间的演化仍然是地球科学最重要的挑战之一。该项目将采用多学科方法，包括地壳和上地幔的地震成像、地质结构分析和确定古代断层运动的年代，研究地质时期形成新英格兰阿巴拉契亚山脉下大陆岩石圈的过程。调查人员将利用部署在两个线性阵列（一个横跨纽约和马萨诸塞州，另一个横跨佛蒙特州、新罕布什尔州和缅因州）的地震仪测量的来自遥远地震的地震波进行详细成像。他们将把他们的地震成像工作与暴露在地表的地质结构研究结合起来，这将为板块构造历史提供必要的背景。综合这两种方法获得的信息将阐明地质历史中形成新英格兰岩石圈的过程，为大陆岩石圈作为地球板块构造系统的一部分如何演化打开一扇窗户。本项目旨在了解裂谷、俯冲和俯冲吸积如何形成新英格兰岩石圈结构：岩石圈是否保存了俯冲和增生的记录，或者岩石圈结构是否随时间愈合？随后的吸积事件如何覆盖早期碰撞的结构？中生代裂谷作用如何影响古生代增生的结构？最近到正在进行的地幔作用是否正在改变岩石圈结构？研究人员将分析来自NEST（新英格兰地震断面）实验的数据，该实验部署了约25个宽带地震仪，其配置用于在适合与地质结构直接联系的长度尺度上解析地壳目标。他们将应用一套成像技术（接收器功能分析，体波走时分析，波场迁移成像和SKS分裂测量），这将提供一个全面的看法都各向同性和各向异性结构的新英格兰地壳和上地幔，包括该地区的所谓的北方阿巴拉契亚异常（NAA）。U-Pb地质年代学工作的重点是鉴定和分析谢尔本福尔斯和布朗森山弧的弧深成岩和火山岩中锆石颗粒中的捕虏晶（继承）核，以了解塔康尼克（及以后）造山过程的历史和时间。调查人员还将进行实地工作和结构分析，以调查新英格兰西部和纽约的基底断层和塔科尼克山脉以及新英格兰中部的康涅狄格谷边界断层系统的前缘逆冲断层的范围和相对时间。他们将通过40 Ar/39 Ar地质年代学从这些地区收集和测定样品来限制变形的时间，以确定整个地区旧断层（和新断层上的位移）的广泛复活。该项目强调本科生参与跨学科研究和实地工作，特别是来自地球科学领域历史上代表性不足的群体的参与者，通过文科学院和研究机构的教师之间的合作实现。该奖项反映了NSF的法定使命，并通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。