Collaborative Research: Subduction Dynamics, Mantle Structure, and Cenozoic Tectonic Evolution of South America

合作研究：南美洲俯冲动力学、地幔结构和新生代构造演化

• 批准号: 1565475
• 负责人: Susan Beck
• 金额: $ 28.99万
• 依托单位: University of Arizona
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2016
• 资助国家: 美国
• 起止时间: 2016-06-01 至 2021-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1565475&HistoricalAwards=false
• 关键词: Collaborative; Research; Subduction; Dynamics; Mantle

The physics behind several fundamental aspects of the South American tectonics remains elusive. For example, various geological records suggest that the Andes Mountains started to shorten significantly since at least 40 million years ago. However, paleo-altimetry proxy data reveal that most of the surface elevation of the Andes remained relatively low until as late as 20 or 15 million years ago, a time frame that is inconsistent with the shortening history. Furthermore, the early Cenozoic arc volcanism along the central Andes suddenly shifted more than 500 km inland around 30 million years ago and formed widespread silicic volcanic activity that continues to the present. Consequently, a clear relationship among these tectonic events is lacking. An important reason is that both the mantle structures beneath South America and their dynamic evolution remain poorly understood. In this proposal, the team plans to carry out a multidisciplinary research project to attempt to improve our knowledge about the observational records of surface tectonics, deep mantle seismic properties, and their geodynamic relationship with the temporal evolution of subduction beneath the continent. By collecting more data related to the tectonic history of South America and to the present-day mantle interior, they will build a sophisticated 4-dimentional geodynamic model using data assimilation, in order to quantitatively reproduce the past subduction history. Ultimately, the team hopes to better understand the Cenozoic evolution of the South American continent. The team plans to achieve this goal through a collaborative research effort that involves seismology (led by PI Beck), geology (led by PI DeCelles), and geodynamics (led by PI Liu). They propose to reproduce the Cenozoic subduction history beneath South America and associated continental deformation using geodynamic models constrained by geophysical and geological observations. This project includes interdisciplinary training of several graduate students at two institutions, and also involves undergraduates at both institutions who will be involved in the research and will all students will participate in a summer field trip to western U.S. Cordillera as an analog for the South American Cordillera. This multi-disciplinary combination will provide a unique opportunity for the students to understand orogenic systems at plate scale.Multiple fundamental questions exist about the Cenozoic tectonic history of South America, including the asynchronous crustal shortening and surface uplift/subsidence history of the Andes, and the enigmatic Central Andean flare-up magmatism occurring during the late Cenozoic. None of the earlier proposed geodynamic models for the Cenozoic evolution of South America could simultaneously explain all these tectonic records and it is unclear whether these different physical processes could co-exist and interact in reality. An important reason for the existence of these alternative models is the uncertain subduction and mantle dynamics due to our imperfect knowledge of deep mantle structures beneath South America. Key observational constraints on the geodynamic and tectonic evolution include an improved present-day mantle seismic structure, especially in the lower mantle, a better identified relationship among structural deformation, surface uplift and magmatic history within western South America, and time-dependent geodynamic models that are consistent with these observational records.

南美洲构造的几个基本方面背后的物理学仍然难以捉摸。例如，各种地质记录表明，安第斯山脉至少从4000万年前开始显著缩短。然而，古测高代用数据显示，安第斯山脉的大部分表面海拔一直相对较低，直到2000万或1500万年前，这一时间框架与缩短的历史不一致。此外，新生代早期沿安第斯山脉中部沿着的弧火山活动在大约3000万年前突然向内陆移动了500多公里，形成了广泛的弧火山活动，并一直持续到现在。因此，这些构造事件之间缺乏明确的关系。一个重要的原因是，南美洲的地幔结构及其动态演化仍然知之甚少。在这项提案中，该团队计划开展一个多学科研究项目，试图提高我们对地表构造观测记录，深部地幔地震特性及其与大陆俯冲时间演变的地球动力学关系的认识。通过收集更多与南美洲构造历史和现今地幔内部相关的数据，他们将利用数据同化建立一个复杂的四维地球动力学模型，以定量再现过去的俯冲历史。最终，该团队希望更好地了解南美洲大陆的新生代演化。 该团队计划通过涉及地震学（由PI Beck领导），地质学（由PI DeCelles领导）和地球动力学（由PI Liu领导）的合作研究来实现这一目标。他们建议使用地球动力学模型，通过地球物理和地质观测的约束，再现南美洲下方的新生代俯冲历史和相关的大陆变形。该项目包括两个机构的几个研究生的跨学科培训，也涉及两个机构的本科生谁将参与研究，并将所有学生将参加夏季实地考察美国西部科迪勒拉作为南美科迪勒拉的模拟。 这种多学科的结合将为学生提供一个独特的机会，了解造山系统在板块尺度上。多个基本问题存在的新生代构造历史，包括异步地壳缩短和表面隆起/沉降的历史，安第斯山脉，和神秘的中安第斯耀斑岩浆活动发生在晚新生代。早期提出的南美洲新生代演化的地球动力学模型都不能同时解释所有这些构造记录，目前还不清楚这些不同的物理过程是否可以共存，并在现实中相互作用。这些替代模型存在的一个重要原因是不确定的俯冲和地幔动力学，由于我们不完善的知识，在南美洲的深部地幔结构。地球动力学和构造演化的关键观测约束包括改进的现今地幔地震结构，特别是在下地幔，更好地确定南美洲西部的构造变形，地表隆起和岩浆历史之间的关系，以及与这些观测记录一致的时间相关的地球动力学模型。