首页> 外文会议>12th World Conference on Earthquake Engineering >SOME PRELIMINARY RESULTS AND ANALYSIS OF DIFFERENT GEODYNAMIC TECHNIQUES WITH SPECIAL REMARK ON GPS AND TILTMETER MEASUREMENTS IN CROATIA
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SOME PRELIMINARY RESULTS AND ANALYSIS OF DIFFERENT GEODYNAMIC TECHNIQUES WITH SPECIAL REMARK ON GPS AND TILTMETER MEASUREMENTS IN CROATIA

机译:克罗地亚GPS和倾斜仪测量的特殊意义的不同地动力技术的某些初步结果和分析。

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Croatia lies in a region, which is seismotectonically very active. The main reasons for this are the Adriatic microplate movements towards the Dinarides, with its different specific densities of rock masses in the crust. There are several zones in the Adriatic Sea but also along the Adriatic Coast experiencing in the past heavy earthquakes with damages in cities (Dubrovnik, Makarska, Rijeka, Ston, and Zadar). Also, there are some local zones in the inland regions (Gospic, Knin, Zagreb and others) which are not directly coupled with the above mentioned dynamics. Therefore, several different measuring methods and techniques applied in different zones are used (and others are planned) to determine the changes in position, height, tilting, and gravity, which will enable the creation of better earthquake prevention models. Two main projects for deformation monitoring are still running. The first project is: a) The monitoring of the Adriatic Sea area deformations with a part of the inner land, and the other is b) the local deformation net of the broader area of Zagreb. The monitoring is based on GPS measurements. For the investigation of the present tectonic activities in the Adriatic Sea area, a wider GPS network was established. The network consists of 22 stations that are distributed over Croatia (17), Slovenia (3) and Italy (2). In 1996, the network was extended towards the south and west with 7 stations in Albania (4) and Italy (3). The GPS network has to be remeasured several times and from the repeated data, velocity vectors will be calculated. The results of the deformation analysis, based on the analytical surface deformation theory, indicates three different deformation zones in the investigated area. Tilt measurements in combination with gravity measurements in the future along the coast will have to prove the theory of three separate microplates in the Adriatic basin. To observe earthquake precursors (if they occur), continuously on-line tiltmeter measurements are planned. Since the Geophysical Institute in Zagreb has been recording earthquakes for more than hundred years till now, these data are to be included as well. Also an absolute gravity network with selected measuring points which will cover the main part of Croatia as well as a GPS permanent network is planned in the future. The combination of data from different origin will enable the usage of crust behaviour models in future. Based on such models a better understanding of earthquake origins and prevention, especially around cities could be obtained.
机译:克罗地亚位于一个地震活动非常活跃的地区。造成这种现象的主要原因是亚得里亚海的微板块向Dinarides方向移动,地壳中岩石质量的比重不同。亚得里亚海以及亚得里亚海沿岸都有数个区域,在过去的大地震中,城市遭受了破坏(杜布罗夫尼克,马卡尔斯卡,里耶卡,斯托和扎达尔)。另外,内陆地区有一些地方区域(戈斯皮克,克宁,萨格勒布等)与上述动态没有直接联系。因此,在不同区域使用了几种不同的测量方法和技术(并计划了其他方法)来确定位置,高度,倾斜度和重力的变化,这将有助于创建更好的防震模型。变形监测的两个主要项目仍在运行中。第一个项目是:a)用一部分内陆监测亚得里亚海区域的变形,另一个是b)萨格勒布较广区域的局部变形网。监视基于GPS测量。为了调查亚得里亚海地区目前的构造活动,建立了更广泛的GPS网络。该网络由分布在克罗地亚(17),斯洛文尼亚(3)和意大利(2)的22个电台组成。 1996年,该网络向南和西扩展,在阿尔巴尼亚(4)和意大利(3)设有7个站点。 GPS网络必须重新测量几次,然后从重复的数据中计算出速度矢量。基于分析表面变形理论的变形分析结果表明了研究区域中的三个不同变形区域。未来沿海岸的倾斜测量与重力测量的结合将必须证明亚得里亚海盆地中三个独立的微板的理论。为了观察地震前兆(如果发生),计划进行连续在线倾斜仪测量。由于萨格勒布的地球物理研究所迄今已记录了一百多年的地震,因此这些数据也要包括在内。此外,未来还将规划一个具有选定测量点的绝对重力网络,该测量点将覆盖克罗地亚的大部分地区,以及一个GPS永久网络。来自不同来源的数据的组合将使将来能够使用地壳行为模型。基于这样的模型,可以更好地了解地震的起源和预防,特别是在城市周围。

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