Triggered slip events following the 2010 and 2021 Haiti earthquakes and their implications to seismic hazard in Hispaniola

伊斯帕尼奥拉岛是加勒比海人口最多的岛屿，分为海地和多米尼加共和国两个国家。它也是北美和加勒比海板块相互挤压和滑动的地方，利用了两个主要的断层系统：岛南部的恩里基洛芭蕉园断层(EPGF)和北部的北半球断层(SF)。这两条断层都是活跃和危险的；EPGF在2010年和2021年海地毁灭性地震中破裂，总共造成超过25万人死亡和90亿美元的损失。2010年地震后，预计下一次破裂的EPGF部分没有发生；2021年的地震发生在断层的其他地方。每次地震后，基于卫星的雷达数据显示，EPGF的部分区域继续滑动，根本没有产生任何小地震，这暗示这些部分可能不会产生大地震。通过调查所有SF和EPGF区段来跟进这一发现，对于评估整个伊斯帕尼奥拉的地震风险和了解2021年地震发生的原因至关重要。该项目将主要使用基于卫星的雷达和GPS数据，以及来自当地机构的地震仪数据，以确定EPGF和SF的运动和地震潜力。该项目将促进佛罗里达国际大学(FIU)与海地和多米尼加共和国的利益攸关方以及法国和韩国科学家之间的合作。伊斯帕尼奥拉岛拥有Enriquillo车前花园断裂带(EPGFZ)和北太平洋断裂带(SFZ)断层系统，这些断层系统容纳了北美-加勒比(NA-CA)转换板块边界这一部分的大部分应变。NA-CA走滑速率在EPFGZ和SFZ上被分割为~17 mm/yr，而相对运动的缩短分量(~5 mm/yr)通过逆冲断层被调节。对破坏EPGFZ的2010年和2021年MW7.0型海地地震的研究表明，大部分地震矩发生在能够进行扭压运动的逆冲断层上。此外，在两次大地震之后，卫星雷达显示EPGFZ上发生了诱发的触发滑动，这表明EPGFZ的部分可能会蠕动。此外，2010年地震后具有最大库仑破裂应力的断层段在2021年地震期间没有破裂。两次地震的动力学表明，EPGFZ具有发震分段性。SFZ曾发生历史上的大地震，并能够在7.6兆瓦的地震中破裂。该研究项目将综合C波段哨兵-1和L波段ALOS-2飞行任务的卫星雷达数据、全球导航卫星系统(GNSS)观测数据以及海地和多米尼加共和国相关地方机构的地震数据，来表征EPGFZ和SFZ沿线的应变分配和累积。主要研究工作包括：(1)探测瞬时无震滑移事件，(2)计算EPGFZ和SFZ的地震间表面速度场，(3)约束将表征船闸断层段深度、蠕变或从船闸向蠕变过渡的力学模型。研究项目产品将极大地帮助岛屿的地震危险性评估。这一奖项反映了NSF的法定使命，并通过使用基金会的智力优势和更广泛的影响审查标准进行评估，被认为值得支持。

Hispaniola is the most populous island in the Caribbean and is split into two countries, Haiti and the Dominican Republic. It is also where the North American and Caribbean plates push toward and slide past past each other, making use of two major fault systems: the Enriquillo Plantain Garden Fault (EPGF) in the south part of the island and the Septentrional Fault (SF) in the north. Both faults are active and hazardous; the EPGF ruptured in the devasting 2010 and 2021 Haiti earthquakes, together causing over 250,000 deaths and US$ 9 billion in damage. After the 2010 earthquake, sections of the EPGF that were expected to rupture next did not; the 2021 earthquake occurred elsewhere on the fault. After each earthquake, satellite-based radar data showed that parts of the EPGF were continuing to slip without producing any small earthquakes at all, hinting that these segments might not generate large earthquakes. Following up on this finding by investigating all SF and EPGF segments is crucial for assessing seismic risks throughout Hispaniola and for understanding why the 2021 earthquake happened where it did. This project will primarily use satellite-based radar and GPS data, along with seismometer data from local agencies, to determine the motion and earthquake potential of the EPGF and the SF. The project will foster collaboration between the Florida International University (FIU) and stakeholders in Haiti and the Dominican Republic, as well as scientists in France and South Korea.The island of Hispaniola hosts the Enriquillo Plantain Garden Fault Zone (EPGFZ) and Septentrional Fault Zone (SFZ) fault systems that accommodate most of the strain at this part of the North America-Caribbean (NA-CA) transform plate boundary. NA-CA strike-slip rate of ~17 mm/yr is partitioned on the EPFGZ and SFZ while a shortening component of the relative motion (~5 mm/yr) is accommodated via thrust faulting. Studies of the Mw 7.0 2010 and Mw 7.2 2021 Haiti earthquakes that ruptured the EPGFZ suggested that most of the seismic moment occurred on thrust faults that take up transpressional motion. Also, following both large earthquakes, satellite-based radar revealed an induced triggered slip on the EPGFZ, suggesting that segments of the EPGFZ may creep. Furthermore, the segments of the fault with the maximum Coulomb Failure Stress following the 2010 earthquake did not rupture during the 2021 earthquake. The dynamics of two earthquakes indicate that the EPGFZ is seismogenically segmented. The SFZ hosted historical large earthquakes and is capable of rupturing in a Mw ~7.6 earthquake. This research project will characterize strain partitioning and accumulation along the EPGFZ and SFZ by synthesizing satellite-based radar data from the c-band Sentinel-1 and L-band ALOS-2 missions, Global Navigation Satellite Systems (GNSS) observations, and earthquake data from the relevant local agencies in Haiti and the Dominican Republic. The main research activities include (1) detecting transient aseismic slip events, (2) calculating interseismic surface velocity fields of the EPGFZ and SFZ, and (3) constraining mechanical models that will characterize fault segment depth of lock, creeping, or transition from lock to creeping. The research project products will greatly aid in the seismic hazard assessment of the island.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.