利用密度参数分析博尔诺瓦平原的盆地结构

Yaprak Özdağ, Oya ANKAYA PAMUKÇU
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摘要

由于受到西安纳托利亚构造体系的影响,该地区包含许多沉积盆地结构。研究区域位于伊兹密尔省内,由于其构造结构,该地区在历史上曾发生过大量地震。博尔诺瓦平原位于伊兹密尔湾内以东,由于城市化密集,极易发生地震。这一点在 2020 年 10 月 30 日的萨摩斯地震中可以清楚地观察到。在本研究中,为了更好地描述该平原的盆地效应,并获得代表广泛区域的高分辨率数据集,我们在比以往研究更大的区域内进行了微重力现场勘测。以大约 200-1000 米的可变采样间隔进行了必要的测量点分布,从而获得了 458 个点的微重力数据集。通过从为博尔诺瓦平原绘制的布格尔重力残差图中提取一个剖面图,进行了反解建模。将逆解建模获得的密度值与通过空间自相关(SPAC)方法在研究区域内获得的地震速度计算出的密度进行了比较。结果表明,两种不同方法得出的密度值高度一致。
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Analyzing Bornova Plain's Basin Structure Using Density Parameter
Due to the tectonic regime it has been subjected to under the influence of Western Anatolia, the area contains numerous sedimentary basin structures. The study area, located within the province of Izmir, is a region where a significant number of historical and instrumental earthquakes have occurred due to its tectonic structure. The Bornova Plain, located east of the inner Gulf of Izmir, is highly susceptible to earthquakes due to dense urbanization. This was clearly observed during the Samos earthquake on October 30, 2020. In this study, a microgravity field survey was conducted in a larger area than previous studies to better characterize the basin effect of the plain and obtain a high-resolution dataset representing a wide area. The necessary measurement point distribution was performed with a variable sampling interval of approximately 200-1000 meters, resulting in a microgravity dataset of 458 points. By taking 1 profile section from the residual Bouguer gravity map created for the Bornova Plain, inverse solution modeling was performed. The density values obtained from the inverse solution modeling were compared with the densities calculated from seismic velocities obtained through the spatial autocorrelation (SPAC) method conducted in the study area. A high consistency was observed between the density values obtained from the two different methods compared.
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