Burdur Fault (BF) is located in Fethiye Burdur Fault Zone and it has formed in three main sections as Gölbaşı–Gökçebağ, Burdur and Yassıgüme–Çendik. The Neogene Basin is a NE–SW oriented depression basin which forms Plio-Quaternary aged lacustrine and alluvial deposits. Paleo-seismic structures on lacustrine sediments were studied with three excavation surfaces at the BF segments in Burdur settlement area. The relationships between different paleo-seismic structures were explained in detail. Although we have obtained new data for the timing of past earthquakes, it is to determine the shear rate of BF segments. Lacustrine sediments and alluvium sequences showing clear evidence of the shearing movement effects were observed. Studies on slopes of foundation excavations on BF segments and near the segment were investigated. Stratified lacustrine sediments observed, each of consisting thin clay layers which is weakly developed in the marl unit excavation surfaces near the Gökçebağ segment. Thin layered lacustrine sediments developed that intersect with a parallel–parallel fractures that filled with collapsed sediments expose near the Burdur segment. In both excavation surfaces, the lower sedimentary unit is covered with a fine sand. The claystone and marl intercalations are discontinuous in the lateral direction and consist of alluvial and lacustrine deposits observed in excavation surfaces near the Yassıgüme–Çendik segment. This study emphasizes that the importance of geological structure has a significant impact on the formation of fault segments.

中文翻译：

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从基础开挖中评估古构造数据：案例研究Burdur断层段（土耳其）

Burdur断层（BF）位于费特希耶Burdur断层带，它由三个主要部分组成，分别是Gölbaşı–Gökçebağ，Burdur和Yassıgüme–Çendik。新近纪盆地是NE-SW导向的depression陷盆地，形成了上新世第四纪的湖相和冲积沉积物。在Burdur居民区的高炉段上，利用三个开挖面研究了湖相沉积物的古地震结构。详细解释了不同古地震结构之间的关系。尽管我们获得了过去地震发生时间的新数据，但它是确定高炉区段的剪切速率的方法。观察到湖草碱沉积物和冲积层序列显示出明显的剪切运动效应证据。研究了高炉段及其附近段基坑开挖的边坡。观察到分层的湖相沉积物，每个由薄薄的粘土层组成，这些粘土层在Gökçebağ段附近的泥灰单元开挖面中发育较弱。形成了薄层湖泊沉积物，该沉积物与平行-平行裂缝相交，裂缝中充满了塌陷的沉积物，并在Burdur段附近暴露出来。在两个挖掘面中，下部的沉积单元都被细砂覆盖。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。每个由薄薄的粘土层组成的层，在Gökçebağ段附近的泥灰单元开挖面中发育较弱。薄层湖相沉积物与平行-平行裂缝相交，裂缝中充满了塌陷的沉积物，在Burdur段附近暴露出来。在两个挖掘面中，下部的沉积单元都被细砂覆盖。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。每个由薄薄的粘土层组成的层，在Gökçebağ段附近的泥灰单元开挖面中发育较弱。形成了薄层湖泊沉积物，该沉积物与平行-平行裂缝相交，裂缝中充满了塌陷的沉积物，并在Burdur段附近暴露出来。在两个挖掘面中，下部的沉积单元都被细砂覆盖。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。形成了薄层湖泊沉积物，该沉积物与平行-平行裂缝相交，裂缝中充满了塌陷的沉积物，并在Burdur段附近暴露出来。在两个挖掘面中，下部的沉积单元都被细砂覆盖。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。形成了薄层湖泊沉积物，该沉积物与平行-平行裂缝相交，裂缝中充满了塌陷的沉积物，并在Burdur段附近暴露出来。在两个挖掘面中，下部的沉积单元都被细砂覆盖。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。粘土岩和泥灰岩层合物在横向上是不连续的，由在Yassıgüme–Çendik段附近的挖掘面中观察到的冲积物和湖相沉积物组成。这项研究强调，地质构造的重要性对断层段的形成具有重大影响。