哥伦比亚和厄瓜多尔基于大地测量的地震预警系统

Lusette Karime Escobar-Rey, David Mencin, Tim Dittmann, Patricia A. Mothes, Héctor Mora-Páez
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摘要

哥伦比亚和厄瓜多尔地处世界上最多样化的构造体系之一,位于五大构造板块的交汇处(Bird,2003 年),包括许多地球物理危险体系、多个俯冲带和广泛的重大变形区域。值得注意的是,自 1900 年以来,南美洲纳斯卡板块的俯冲至少引发了七次破坏性大地震(>Mw 7),其中最大的一次是 1906 年发生的 Mw 8.8 地震。哥伦比亚和厄瓜多尔都对全球导航卫星系统(GNSS)网络进行了大量投资,以研究构造和火山变形。地震预警(EEW)系统,如美国运营的 ShakeAlert 系统(Murray 等人,2018 年,2023 年),利用实时全球导航卫星系统(RT-GNSS),在仅有地震网络饱和的情况下,迅速确定最大、破坏性最强地震的特征(Melgar 等人,2015 年,2016 年;Allen 和 Melgar,2019 年;Ruhl 等人,2019 年)。哥伦比亚和厄瓜多尔都有大量靠近海岸的脆弱人群,他们可能会在这些大型俯冲事件中遭受重大损失(Pulido 等人,2020 年),但距离足够远,RT-GNSS EEW 系统可以为这些人群和相关基础设施提供重要的预警时间。我们研究了哥伦比亚大地测量局(Servicio Geológico Colombiano Geodesia)的现状:我们研究了哥伦比亚的 Servicio Geológico Colombiano Geodesia:Red de Estudios de Deformación GNSS 网络和厄瓜多尔的 Escuela Politécnica Nacional GNSS 网络的现状、空间分布及其数据流的现状,以确定为支持哥伦比亚和厄瓜多尔境内及附近地区大型破坏性地震的实时探测和建模需要哪些增强功能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Geodetic-Based Earthquake Early Warning System for Colombia and Ecuador
Colombia and Ecuador sit at one of the most diverse tectonic regimes in the world, located at the intersection of five tectonic plates (Bird, 2003) encompassing many geophysical hazard regimes, multiple subduction zones, and broad diffuse areas of significant deformation. Notably, the subduction of the Nazca plate under South America has produced at least seven large (>Mw 7) and damaging earthquakes since 1900—the largest being the 1906 Mw 8.8 event. Both Colombia and Ecuador have made significant investments in Global Navigation Satellite System (GNSS) networks to study tectonic and volcanic deformation. Earthquake early warning (EEW) systems like the U.S.-operated ShakeAlert system (Murray et al., 2018, 2023) utilize real-time Global Navigation Satellite System (RT-GNSS) to rapidly characterize the largest, most damaging earthquakes in situations where seismic networks alone saturate (Melgar et al., 2015, 2016; Allen and Melgar, 2019; Ruhl et al., 2019). Both Colombia and Ecuador have large vulnerable populations proximal to the coast that may sustain significant damage in these large subduction events (Pulido et al., 2020) and yet farther enough away that an RT-GNSS EEW system could offer significant warning times to these populations and associated infrastructure. We examine the status of the Servicio Geológico Colombiano Geodesia: Red de Estudios de Deformación GNSS network in Colombia and the Escuela Politécnica Nacional GNSS network in Ecuador, their spatial distribution, and the current status of their data streams to determine what augmentations are required to support the real-time detection and modeling of large destructive earthquakes in and near Colombia and Ecuador.
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