Understanding the deformation and processes that link ductile flow in the deep continental crust with frictional processes in the upper crustal seismogenic zone

了解将深部大陆地壳中的延性流与上地壳地震带中的摩擦过程联系起来的变形和过程

• 批准号: RGPIN-2020-05658
• 负责人: Grujic, Djordje
• 金额: $ 2.19万
• 依托单位: Dalhousie University
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2020
• 资助国家: 加拿大
• 起止时间: 2020-01-01 至 2021-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=717791
• 关键词: Understanding; deformation; processes; link; ductile

Subduction zonesregions of Earth's crust where one tectonic plate dives beneath anotherare usually but not always associated with frequent, violent earthquakes. Occasionally, the downgoing plate slides slowly, smoothly and almost silently under the overriding plate. Canadian scientists have contributed to the research of seismic slow signals with geophysical observations of the Cascadia subduction zone. However, field observations, rock experiments and theoretical developments are also needed to advance our understanding of these newly identified fault slip phenomena. The proposed research program, with implications for future earthquakes offshore western Canada, aims to (a) expand our knowledge of mechanical processes that link mega earthquakes in the upper crust to steady and continuous slip in the lower crust via the brittle-ductile transition zone, which hosts the seismic slow signals, and (b) test a set of innovative methods to determine the ages of pre-instrumental earthquakes. (a) The importance of this research lies in the potential relationship between the fault transition zone and the parts of faults that generate destructive earthquakes. Some calculations find that the probability of a large earthquake occurring during a slow-slip event is 30100 times greater than background probabilities. My research program involves interdisciplinary studies of exemplary exposed megathrust systems that record different stages of their development. Continental megathrust systems will be investigated via integration of observations across a range of scales and approaches, including field studies, microanalyses, thermochronology, geochronology, and numerical modelling. (b) Deformation data obtained from faulted rocks should be interpreted in the context of temporal or spatial variations in seismic processes. Thus, precise and accurate dating is crucial and entails developing innovative techniques that directly link age data to evidence of seismic slip in the rock record. This goal is achievable because of recent developments in our understanding of the physics of signals from minerals released via exposure to heat produced by seismic slip, and improvements in related analytical methods. To test the new techniques, we selected several locations where a surface earthquake rupture of known age provides access to samples suitable for attaining this goal. In addition to taking a leadership role in the discipline, Canada will benefit from this research by further understanding the processes responsible for Earth's major evolutionary steps, which can then feed into policy development for geohazard and environmental protection. Program goals will involve Canadian and international collaborators and train 2 PhD and 2 MSc graduate students, 1 PDF and undergraduates who will become knowledgeable in science communication and international and earthquake research, collaborate with world-leading research groups and gain access to world-class infrastructure.

俯冲带是地壳的一个板块俯冲到另一个板块之下的区域，通常但并不总是与频繁的强烈地震有关。偶尔，下行板块会缓慢、平稳、几乎无声地滑到上覆板块之下。加拿大科学家通过对卡斯卡迪亚俯冲带的地球物理观测，对地震慢信号的研究作出了贡献。然而，现场观测，岩石实验和理论的发展，也需要推进我们对这些新发现的断层滑动现象的理解。拟议的研究计划，与未来的地震加拿大西部近海，目的是（a）扩大我们的知识的机械过程，连接在上地壳的大地震，在下地壳稳定和连续滑动通过脆-韧性过渡带，其中主机的地震慢信号，和（B）测试一套创新的方法来确定的年龄前仪器地震。 (a)这项研究的重要性在于断层过渡带与产生破坏性地震的断层部分之间的潜在关系。一些计算发现，在慢滑事件期间发生大地震的概率是背景概率的30100倍。我的研究计划涉及典型的暴露的巨型逆冲断层系统，记录其发展的不同阶段的跨学科研究。将通过一系列尺度和方法的综合观测，包括实地研究、微观分析、热年代学、地质年代学和数值建模，对大陆巨型逆冲断层系统进行研究。 (b)从断层岩石获得的变形数据应在地震过程的时间或空间变化的背景下进行解释。因此，精确和准确的年代测定是至关重要的，需要开发创新技术，直接将年龄数据与岩石记录中地震滑动的证据联系起来。这一目标是可以实现的，因为我们对矿物通过暴露于地震滑动产生的热量而释放的信号的物理学的理解最近有所发展，并且相关分析方法有所改进。为了测试新技术，我们选择了几个地点，在那里已知年龄的地表地震破裂提供了适合实现这一目标的样本。 除了在这一学科中发挥领导作用外，加拿大还将从这项研究中受益，进一步了解地球主要演变步骤的过程，然后将其纳入地质灾害和环境保护政策的制定。计划目标将涉及加拿大和国际合作者，并培养2名博士和2名硕士研究生，1名PDF和本科生，他们将成为科学传播和国际地震研究方面的知识，与世界领先的研究小组合作，并获得世界一流的基础设施。