Collaborative Research: The Burma Arc from Collision Kinematics to Subduction Tectonics as Observed from a Passive seismic experiment (BACKSTOP)

合作研究：被动地震实验观察到的从碰撞运动学到俯冲构造的缅甸弧（BACKSTOP）

• 批准号: 1928786
• 负责人: James Ni
• 金额: $ 20.71万
• 依托单位: New Mexico State University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-08-01 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1928786&HistoricalAwards=false
• 关键词: Collaborative; Research; Burma; Arc; Collision

When two tectonic plates collide, one may slide underneath the other. This process, called subduction, often occurs when an oceanic plate meets a continental plate. The subducting oceanic plate, or subducting slab, sinks into the Earth's mantle affecting the regional mantle flow. This often generates mountain building and volcanic activity on land, like in Cascadia and Andean mountains. The volcanos may form along a curved chain called an arc. Colliding continental plates also build mountain ranges, like the Alps and the Himalayas. These processes are responsible for large earthquakes and volcanic eruptions threatening human lives and activity. Here, the researchers study a plate boundary coupling subduction with continental collision. Subduction of the Indian oceanic plate occurs along the Indo-Burma arc. It transitions to collision along the Himalayan Mountains. The scientists leverage on an international collaboration between five countries and the U.S. They use seismology, the study of seismic waves propagating through the Earth, to image in 3D mantle and crustal structures. Deploying 24 seismic stations in key locations in Myanmar, they analyze data from these instruments and ~900 other stations in surrounding India, Bangladesh and China. A primary objective is to unveil the processes responsible for the growth of the southeastern Tibetan Plateau. Another one is to quantify the effect of the Indian slab geometry on the mantle flow. The project improves the understanding of the regional tectonics. Its outcomes have strong implications for seismic and volcanic hazard assessment in Myanmar; a region which faces large dramatic events. The project provides support for two graduate students in Missouri and New Mexico, as well as the development of scientific collaborations in Myanmar. The three-year award was co-funded by NSF Prediction of and Resilience against Extreme Events (PREEVENTS) program. Here, the team investigates the role of the Indian slab beneath Burma as a "backstop" to the mantle flow around the eastern Himalayas. They also study how this impacts the growth of the southeastern Tibetan Plateau. The project consists of two components: (1) data collection from a temporary seismic array that links large arrays in India/Bangladesh and China; (2) the synthesis of data from a large number of existing stations across the region. The data acquisition component consists of 24 temporary broad-band stations deployed in key regions lacking any seismic instruments. The second component is a collaborative effort with scientists from Myanmar, India, Singapore, China, and Germany. The combined seismic network of over 900 stations spans an area of 1800 km by 2000 km. It completely covers the entire Indo-Burma Arc. The scientists use 3-D seismic tomography and anisotropic surface wave tomography to image the Indian slab beneath the Indo-Burma subduction zone. This enables them to compare flow and lithospheric deformation around eastern Himalayas and in the Indo-Burma back-arc. The project outcomes constrain the dynamics of the deformation associated with the Indian collision and subduction, and how the transition from subduction to continental collision occurs. The gained insight into the regional tectonics, as well as crustal attenuation, is key to improve seismic and volcanic hazard forecasting in Myanmar and surrounding regions.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.

当两个构造板块碰撞时，一个板块可能会滑到另一个板块下面。这个过程称为俯冲，通常发生在海洋板块与大陆板块相遇时。俯冲海洋板块或俯冲板片下沉到地幔中，影响区域地幔流。这通常会在陆地上产生造山和火山活动，例如卡斯卡迪亚山脉和安第斯山脉。火山可能沿着一条称为弧线的弯曲链形成。碰撞的大陆板块也会形成山脉，如阿尔卑斯山和喜马拉雅山。这些过程导致了威胁人类生命和活动的大地震和火山爆发。在这里，研究人员研究了板块边界俯冲与大陆碰撞的耦合。印度洋板块的俯冲沿着印度-缅甸弧发生。它过渡到喜马拉雅山脉沿线的碰撞。科学家们利用五个国家和美国之间的国际合作，利用地震学（研究地震波在地球上传播的学科）来拍摄 3D 地幔和地壳结构图像。他们在缅甸的关键地点部署了 24 个地震台，分析来自这些仪器以及印度、孟加拉国和中国周边约 900 个其他台站的数据。主要目标是揭示青藏高原东南部增长的过程。另一项任务是量化印度板块几何形状对地幔流的影响。该项目增进了对区域构造的了解。其结果对缅甸的地震和火山灾害评估具有重大影响；一个面临重大戏剧性事件的地区。该项目为密苏里州和新墨西哥州的两名研究生提供支持，并为缅甸的科学合作发展提供支持。该奖项为期三年，由 NSF 极端事件预测和恢复力 (PREEVENTS) 项目共同资助。 在这里，研究小组调查了缅甸下方的印度板片作为喜马拉雅山脉东部地幔流的“后盾”的作用。他们还研究了这如何影响青藏高原东南部的增长。该项目由两个部分组成：（1）从连接印度/孟加拉国和中国大型阵列的临时地震阵列收集数据； (2)综合全地区大量现有站点的数据。数据采集​​部分由部署在缺乏任何地震仪器的关键地区的 24 个临时宽带站组成。第二部分是与缅甸、印度、新加坡、中国和德国科学家的合作努力。由 900 多个台站组成的联合地震台网覆盖面积 1800 平方公里 x 2000 平方公里。它完全覆盖了整个印缅弧。科学家们使用 3D 地震层析成像和各向异性表面波层析成像对印缅俯冲带下方的印度板块进行成像。这使他们能够比较喜马拉雅山脉东部和印缅弧后的流动和岩石圈变形。该项目的成果限制了与印度碰撞和俯冲相关的变形动力学，以及从俯冲到大陆碰撞的过渡如何发生。对区域构造和地壳衰减的深入了解对于改善缅甸及周边地区的地震和火山灾害预报至关重要。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力优势和评估进行评估，被认为值得支持。更广泛的影响审查标准。