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Neotectonics of Southeast Jamaica Derived From Marine Seismic Surveys and Gravity Cores

机译:牙买加东南部的新分子学源自海洋地震调查和重力核心

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Tectonics in Southeast Jamaica is poorly understood, but the region may contain currently unknown faults that could generate large-magnitude earthquakes. This study constrains tectonics in Southeast Jamaica by collecting and analyzing seismic and shallow sediment core data in and around Kingston Harbor. Seismic results reveal a previously unrecognized strike-slip fault system that accommodates strain via a complex mix of compression and extension. The faults appear to be a blind extension of one major fault (i.e., The Bull Bay Strike-Slip Fault) within the Enriquillo-Plantain Garden Fault Zone. This fault system may represent significant hazards to Kingston Jamaica because the fault is active, located less than 5 km from the city, and a complete rupture of the fault could generate a M-w 5.8-6.9 earthquake. Our analyses highlight the need for continued paleoseismic studies, both onshore and offshore Jamaica.
机译:牙买加东南部的构造知之甚少,但该地区可能含有目前可能产生大幅度地震的未知故障。本研究通过收集和分析金斯敦港及其周围地区及其附近的地震和浅沉积物核心数据来限制东南部牙买加的构造。地震结果揭示了先前未识别的防滑故障系统,其通过复杂的压缩和延伸组合容纳应变。该故障似乎是Reasizillo-Plantain园林故障区内的一个主要故障(即,公牛湾滑动故障)的盲目延伸。这种故障系统可能代表牙买加危险,因为故障活动,距离城市不到5公里,故障完全破裂可能会产生M-W 5.8-6.9地震。我们的分析突出了在陆上和海上牙买加持续古姿性研究的需要。

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