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Geological Features and Physical and Mechanical Properties of the Gorgoglione Building Stone of Basilicata (Southern Italy)

机译:巴斯利卡塔(南部意大利)Gorgoglione建筑石的地质特征和身体和力学性能

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Since prehistoric times stones have been widely employed in the construction of historic buildings, floors, and claddings in rural and urban areas. Among the Italian natural stones, the sandstone belonging to the Gorgoglione Formation, known as the Gorgoglione Stone, quarried and worked near the homonymous village in Basilicata (Southern Italy), is usually used as a building material. The Gorgoglione Stone consists of well-cemented turbidite sandstones deposited in a Middle-Upper Miocene thrust-top basin unconformably resting on the external nappes of the Southern Apennine thrust belt. In the Gorgoglione area, it can be observed in either numerous natural outcrops or quarries. This study aims to highlight the geological peculiarities of the Gorgoglione Stone and, in particular, it is focused on its mechanical characterization for assessing the most effective use when employed in construction, such as public and civil buildings, road construction, paving, and small works of art. Based on the experimental results, obtained by samples collected from different quarries, axial stress-strain curves have been plotted, whose analysis has delivered the deformation behavior and the strength characteristics of the stone. The elastic modulus, uniaxial compressive strength, and axial strain at stress peak have been estimated for several specimens. The measured values are typically of a medium-high-strength sandstone. The tested specimens of sandstone exhibit a typical behavior of an elastic-brittle rock, characterized by a linear path and a failure typically of axial splitting. With regard to the results of the physical tests, they showed that the analyzed sandstone is characterized by quite low density and by medium-high porosity and water absorption.
机译:由于史前时代石头已被广泛用于农村和城市地区的历史建筑,地板和覆盖物的建设中。在意大利天然石头中,属于Gorgoglione的砂岩,被称为Gorgoglione Stone,在巴西利卡塔(意大利南部)的同名村附近的争吵和工作,通常用作建筑材料。 Gorgoglione石块由沉积在南部亚平线推力皮带的外部Nappes上的中上部内肾上腺推力顶部盆地中沉积在中上部内肾上腺推力顶部盆中的井塌砂岩。在Gorgoglione地区,它可以在许多天然露头或采石场中观察到。本研究旨在突出Gorgoglione石头的地质特性,特别是它专注于在建筑中使用时评估最有效的使用的机械表征,例如公共和民用建筑,道路建设,铺路和小型作品艺术的。基于从不同争吵收集的样品获得的实验结果,已经绘制了轴向应力 - 应变曲线,其分析提供了石材的变形行为和强度特性。据估计了几种样品的弹性模量,单轴抗压强度和应力峰处的轴向应变。测量值通常是中高强度砂岩。砂岩的测试标本表现出弹性脆性岩石的典型行为,其特征在于线性路径和通常轴向分裂的故障。关于物理测试的结果,他们表明分析的砂岩的特征在于密度相当低,中高孔隙率和吸水性。

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