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Gravimetric gradient, Sicily and southern Calabria, Italy (Central Mediterranean)

机译:重力梯度,意大利西西里岛和卡拉布里亚南部(地中海中部)

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A powerful cartographic tool in identifying major tectonic lineaments and/or ancient margins along the Sicilian and southern Calabria Orogenic system (southern Italy) has been obtained by producing the 1:250,000 scale digital contour map of gravity anomalies available for the Italian region. By processing contour maps, an ‘elevation model’ of the gravity anomalies for Sicily and southern Calabria was produced. The ‘elevation model’ was used to generate a slope representation of the gravity trend that is presented in this paper at 1:500,000. The map covers an area of about 95,000?km~(2) and includes both the inland areas of Sicily and southern Calabria and the adjacent seas. The color of the pixels varies from blue, where no significant variation of the gradient occurs, to red with the steepest gradients. Taking into account (i) the nature of rocks which are involved in the analyzed orogenic system and (ii) the juxtaposition of rocks with different densities is usually controlled by faults, the thematic map here presented can provide an additional tool for a regional scale tectonic interpretation of this sector of the Central Mediterranean.
机译:通过制作意大利地区可用的1:25万比例尺的重力异常数字等高线图,已获得了一种强大的制图工具,可用于识别西西里和南部卡拉布里亚造山带系统(意大利南部)的主要构造界线和/或古边缘。通过处理等高线图,生成了西西里岛和卡拉布里亚南部重力异常的“高程模型”。 “海拔模型”用于生成重力趋势的斜率表示,本文以1:500,000表示。该地图占地面积约95,000?km〜(2),包括西西里岛和卡拉布里亚南部的内陆地区以及邻近的海域。像素的颜色从蓝色(渐变没有明显变化)到红色(渐变最陡)不等。考虑到(i)所分析的造山系统所涉及的岩石的性质以及(ii)不同密度的岩石的并置通常受断层控制,因此,此处介绍的专题图可为区域尺度构造提供额外的工具解释中地中海地区。

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