大天使加布里埃尔和迈克尔教堂墙壁的地震变形(克里米亚费奥多西亚)

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS Seismic Instruments Pub Date : 2022-04-21 DOI:10.3103/S0747923922020074
D. A. Moisieiev, A. M. Korzhenkov, A. N. Ovsyuchenko, A. S. Larkov
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引用次数: 0

摘要

对Kaffa-Feodosia(克里米亚东南部)的亚美尼亚大天使加布里埃尔教堂和迈克尔教堂建筑结构的系统性破坏进行了调查。变形包括建筑构件的倾斜、旋转和拖动位移,窗户和入口上方拱形结构的铰链部分下垂,以及大范围的裂缝,包括“花”结构形式的连续接缝和接缝组合。四次地震形成了一系列的系统性破坏。最早的地震(事件A),局部烈度为IL = VIII-IX (MSK-64),震中位于克里米亚南发震区的下沉轴上。这件事之后,教堂得到了修复:建造了一个具有反作用力功能的小教堂,许多窗户都用石头填满以保持稳定。地震很有可能发生在1423年。这一年代测定得到了1423年富纳要塞城墙地震发震变形数据的支持。下一次地震(事件B)很有可能发生在17 - 18世纪之交,沿南亚速地震发震带的一段发生。局部地震振动烈度为IL = VII-VIII (MSK-64)。18世纪下半叶,在进行了大规模的修复工程后,发生了地震C。地震b造成的破坏在教堂西立面的拱门和平台上保存得特别完好。导致这些破坏的最大地震振荡发生在≈130°-160°轴上。局地地震烈度为IL = 7 ~ 8 (MSK-64)。上一次地震(事件D)发生在1875年。我们的数据大体上与这一事件的可用参数化一致。其震中位于克里米亚南部发震区;强度为IL = 7 ~ 8 (MSK-64)。
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Seismic Deformations in the Walls of the Church of the Archangels Gabriel and Michael (Feodosia, Crimea)

Systematic damage to building structures of the Armenian Church of the Archangels Gabriel and Michael Church in Kaffa–Feodosia (southeast Crimea) are investigated. The deformations include tilts, rotations, and drag displacements of building elements, sagging of the hinge parts of arched structures above windows and entrances, and a wide range of fissures, including continuous joints and joint assemblies in the form of “flower” structures. Sets of systematic damage were formed by four earthquakes. The epicentral area of the earliest earthquake (event A) with a local intensity IL = VIII–IX (MSK-64) was located along the submeridional axis in the South Crimean seismogenic zone. After this event, the church was repaired: a chapel with counterforce function was built, and many windows were filled with stones for stability. The earthquake occurred in 1423 with a high probability. This dating is supported by seismogenic deformation data on 1423 earthquake in the walls of the Funa fortress. The next earthquake (event B) occurred with a high probability at the turn of the 17th–18th centuries along one of the segments of the South Azov seismogenic zone. The local seismic vibration intensity was IL = VII–VIII (MSK-64). Earthquake C occurred in the second half of the 18th century after large restoration works, which repaired the damage of event B. Its consequences have been especially well preserved in the arches and platbands of the western facade of the church. Maximum seismic oscillations that led to these damages acted along the ≈130°–160° axis. The local seismic intensity was IL = VII–VIII (MSK-64). The last earthquake (event D) occurred in 1875. Our data generally coincide with the available parameterization of this event. Its epicentral area was in the South Crimean seismogenic zone; intensity was IL = VII–VIII (MSK-64).

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来源期刊
Seismic Instruments
Seismic Instruments GEOCHEMISTRY & GEOPHYSICS-
自引率
44.40%
发文量
45
期刊介绍: Seismic Instruments is a journal devoted to the description of geophysical instruments used in seismic research. In addition to covering the actual instruments for registering seismic waves, substantial room is devoted to solving instrumental-methodological problems of geophysical monitoring, applying various methods that are used to search for earthquake precursors, to studying earthquake nucleation processes and to monitoring natural and technogenous processes. The description of the construction, working elements, and technical characteristics of the instruments, as well as some results of implementation of the instruments and interpretation of the results are given. Attention is paid to seismic monitoring data and earthquake catalog quality Analysis.
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