Collaborative Proposal: Developing argon techniques to elucidate earthquake chronologies (DATEEQ)

合作提案：开发氩气技术来阐明地震年表 (DATEEQ)

• 批准号: 2126105
• 负责人: Heather Savage
• 金额: $ 30.09万
• 依托单位: University of California-Santa Cruz
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-09-01 至 2024-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2126105&HistoricalAwards=false
• 关键词: Collaborative; Proposal; Developing; argon; techniques

Our understanding of how earthquakes start, propagate, and stop is hindered by the fact that they occur deep underground where we cannot directly observe faults before, during, and after the quake. To better study what faults do at depth, one can drill through them or look at faults that used to be buried deep in the Earth but have been exposed at the surface. In this study, the researchers look at rock samples from drill cores through faults to identify areas of the fault that have experienced earthquake slip. Because individual earthquakes can slip along zones with small thicknesses - just millimeters compared to the total fault thickness of 10s-100s of meters) - it is unlikely that the whole fault will have experienced earthquakes. The goal of this study is to develop a new technique to determine not only where earthquakes have occurred in a fault, but when. This is important because longer earthquake records (on the million-year timescale) allow to better understand earthquake cycles and develop better earthquake forecasts. Here, by measuring the ratio of radioactive potassium to its decay product argon in the fault rocks, the team determine how long it has been since the rock was heated by earthquakes. This is a novel application of one of the best-established geological dating techniques. The study takes advantage of the fact that earthquakes generate a lot of heat from friction; the generated heat can reset the potassium-argon clock, thereby recording the time of the earthquake in the rock record. The project supports graduate and undergraduate students at University of California – Santa Cruz (UCSC, a Hispanic serving Institution) and Columbia University. It broadens participation in Earth Sciences by involving students from underrepresented group at UCSC and from the City University of New York. It also fosters outreach to local schools and the public.To characterize past earthquake occurrences, the researchers first run a series of experiments to determine how fast the argon is liberated from its host mineral when heated by an earthquake. They run these experiments on several different rocks at different times and temperatures (up to several hundred degrees in just a few seconds). The experiments allow quantifying how fast argon diffusion occurs. Next, the team measure potassium and argon in drill core rocks from major faults including the subduction zone off of northern Japan (which hosted the 2011 Mw 9.1 earthquake) and the Hikurangi subduction zone off of the North Island of New Zealand. Previous work on these cores using a geochemical method for measuring rock temperature has demonstrated that hot earthquakes have occurred on these faults. However, this previous method, using the change in molecular structure of organic matter when heated, only provides a temperature estimate with no indication of when the earthquake occurred. By combining dating and geochemical methods, the researchers create dated records of earthquake slip over millions of years.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.

我们对地震如何开始、传播和停止的理解受到阻碍，因为地震发生在地下深处，我们无法直接观察地震前、中、后的断层。为了更好地研究断层在深处的作用，人们可以钻穿它们，或者观察过去深埋在地球深处但已暴露在地表的断层。在这项研究中，研究人员通过断层查看岩心中的岩石样本，以确定经历过地震滑动的断层区域。由于单个地震可以沿着厚度很小的区域沿着--与10 - 100米的总断层厚度相比，只有几毫米）--整个断层不太可能经历过地震。这项研究的目的是开发一种新的技术，不仅可以确定地震发生在断层的哪里，而且可以确定地震发生的时间。这一点很重要，因为更长的地震记录（在百万年的时间尺度上）可以更好地了解地震周期，并制定更好的地震预报。在这里，通过测量断层岩石中放射性钾与其衰变产物氩的比例，研究小组确定了岩石被地震加热的时间。这是一种最成熟的地质测年技术的新应用。这项研究利用了地震会从摩擦中产生大量热量的事实;产生的热量可以重置钾氩钟，从而在岩石记录中记录地震的时间。该项目支持加州-圣克鲁斯大学（UCSC，一个西班牙裔服务机构）和哥伦比亚大学的研究生和本科生。 它扩大了对地球科学的参与，让来自UCSC和纽约城市大学的代表性不足的学生参与进来。为了描述过去发生的地震，研究人员首先进行了一系列实验，以确定当地震加热时，氩从其宿主矿物中释放出来的速度。他们在不同的时间和温度下在几种不同的岩石上进行这些实验（在几秒钟内达到几百度）。实验允许量化氩气扩散发生的速度。接下来，研究小组测量了来自主要断层的岩心岩石中的钾和氩，这些断层包括日本北方的俯冲带（2011年发生了9.1级地震）和新西兰北岛的Hikurangi俯冲带。以前的工作，这些核心使用地球化学方法测量岩石温度已经证明，热地震发生在这些断层。然而，这种以前的方法，利用有机物加热时分子结构的变化，只提供了一个温度估计，没有指示地震发生的时间。通过结合测年和地球化学方法，研究人员创建了数百万年来地震滑动的日期记录。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。