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Vrancea (Romania) Subcrustal Earthquakes: Historical Sources and Macroseismic Intensity Assessment

机译:弗朗塞(罗马尼亚)亚地壳地震:历史资料和宏观地震烈度评估

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The aim of the present paper is that of bringing in additional information regarding the macroseismic effects of the historical earthquakes that occurred on the Romanian territory with the purpose of improving the macroseismic maps. It is known the fact that in time, the Romanian territory has been shaken by strong earthquakes, most of them being centered within Vrancea Zone, which is situated at the bending zone of the South-Eastern Carpathians. As results from the contemporaries' notes, such major earthquakes occurred also during the 19 th century, on the 26 th of October 1802 and the 23 rd of January 1838, causing numerous victims and major material damages. Additional information that refer to the macroseismic effects produced by the above mentioned earthquakes, have been recently discovered due to the investigation of old books fund which exists in some monasteries and museums. The results of the investigation were concretized in discovering 37 historical records that allowed us to make a correct interpretation of the destroying impact of these earthquakes over the society and the environment. New elements regarding the research of these earthquakes were obtained after reevaluating the information from certain areas (especially from the epicentral zone), concerning the environmental effects. In this paper, the information referring to these earthquakes, identified as a result of investigating historical sources, are interpreted and evaluated with the purpose of assigning some seismic intensities for elaborating the macroseismic maps.
机译:本文的目的是提供有关罗马尼亚领土上发生的历史地震的宏观地震影响的更多信息,以期改善宏观地震图。众所周知,罗马尼亚领土一度被强烈地震震撼了,大部分地震集中在位于东南喀尔巴阡山脉弯曲带的弗朗塞区(Vrancea Zone)内。从同时代人的笔记中得出的结果,这样的大地震也发生在19世纪,即1802年10月26日和1838年1月23日,造成了无数的受害者和重大的财产损失。由于对一些修道院和博物馆中存在的旧书资金的调查,最近发现了有关上述地震产生的宏观地震影响的其他信息。调查的结果具体化了,发现了37个历史记录,使我们能够正确解释这些地震对社会和环境的破坏性影响。在重新评估了某些地区(尤其是震中地区)有关环境影响的信息后,获得了有关这些地震研究的新要素。在本文中,解释和评估了与这些地震有关的信息,这些信息是通过调查历史震源而确定的,目的是分配一些地震烈度来绘制宏观地震图。

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