1857年沿Caggiano断层系统(意大利南部亚平宁山脉)Mw ~ 7级地震的古地震证据

IF 3.3 1区 地球科学 Q1 GEOGRAPHY, PHYSICAL
Paolo Galli , Simone Bello , Francesco Brozzetti , Antonio Galderisi , Giuseppe Naso , Antonio Pignalosa , Gianluca Benedetti , Massimo Comedini , Edoardo Peronace
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引用次数: 0

摘要

1857年发生在意大利亚平宁山脉南部的坎帕尼亚-巴西利卡塔地震是地中海历史上最具灾难性的地震之一(里氏7.1级),估计死亡人数在1.1万至1.9万人之间。它由一对主震组成,在几分钟内相互发生,影响了北部瓦洛迪迪亚诺和北部阿格里山谷之间的大片地区,这两个第四纪山间盆地被马达莱纳山脉隔开。地震很可能是由两个相邻的正断层的级联破裂引发的,它们的确切长度和位置是不确定的,并且存在争议,特别是关于南部的断层。本次研究的重点是北部正断层,这里称为Caggiano断层系统,该断层横跨马达莱纳山脉中-新生代碳酸盐岩,向北西-东南方向延伸约32公里。在利用20世纪50年代的航空照片和激光雷达衍生的DTM绘制断层崖后,我们对整个断层迹线进行了地质实地调查,并进行了古地震挖沟的电阻率层析成像准备。随后,我们挖掘了沟渠和坑,收集了大量样本进行放射性碳测年。结果为末次冰期后的极大期-全新世提供了确凿的地表断裂证据,表明卡吉亚诺断层系统是1857年地震的可靠候选,以及更早的事件,如1561年的地震和之前没有记录的中世纪和罗马时代的地震。这些发现为未来的地震危险性评估做出了强有力的贡献,这需要可靠的识别和活动断层系统的发震特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Paleoseismic evidence for the Mw∼7 1857 earthquake along the Caggiano fault system (southern Italian Apennines)
The 1857 Campania-Basilicata earthquake in the southern Italian Apennines ranks among the most catastrophic events in Mediterranean history (Mw 7.1), with an estimated death toll ranging between 11,000 and 19,000. It consisted of a pair of mainshocks occurring within minutes of each other, affecting a vast region between the northern Vallo di Diano and the northern Agri Valley, two Quaternary intramontane basins separated by the Maddalena Range. The earthquakes were likely triggered by the cascading rupture of two adjacent, aligned normal faults, whose exact length and location are uncertain and debated, especially concerning the southern one. This study focuses on the northern normal fault, here named Caggiano fault system, which extends NW-SE for approximately 32 km across the Meso-Cenozoic carbonate of the Maddalena Range. After mapping the fault scarp using 1950s aerial photos and LiDAR-derived DTM, we conducted geological field survey of the entire fault traces, performing electrical resistivity tomography preparatory to paleoseismic trenching. Subsequently, we excavated trenches and pits, collecting numerous samples for radiocarbon dating. Results provide conclusive evidence of surface faulting to the post-Last Glacial Maximum-Holocene, indicating the Caggiano fault system as a reliable candidate for the 1857 earthquake, as well as earlier events, such as the one in 1561 and previously undocumented earthquakes in the Middle Age and Roman times. These findings represent a robust contribution to future seismic hazard assessments, which require reliable identification and seismogenic characterization of active fault systems.
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来源期刊
Quaternary Science Reviews
Quaternary Science Reviews 地学-地球科学综合
CiteScore
7.50
自引率
15.00%
发文量
388
审稿时长
3 months
期刊介绍: Quaternary Science Reviews caters for all aspects of Quaternary science, and includes, for example, geology, geomorphology, geography, archaeology, soil science, palaeobotany, palaeontology, palaeoclimatology and the full range of applicable dating methods. The dividing line between what constitutes the review paper and one which contains new original data is not easy to establish, so QSR also publishes papers with new data especially if these perform a review function. All the Quaternary sciences are changing rapidly and subject to re-evaluation as the pace of discovery quickens; thus the diverse but comprehensive role of Quaternary Science Reviews keeps readers abreast of the wider issues relating to new developments in the field.
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