Kinematic models of recent motion of the Earth's crust on the territory of Croatia, Slovenia and Bosnia and Herzegovina

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geofizika Pub Date : 2015-12-31 DOI:10.15233/GFZ.2015.32.10
N. Rožić
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引用次数: 4

Abstract

Based on relative height displacement grid models of the Earth’s crust, related to the territory of the Croatia, Slovenia and Bosnia and Herzegovina, which were created by modelling of the benchmark height data contained in levelling networks of the Austrian precise levelling (APN), and First (INVT) and Second (IINVT) levelling of high accuracy, possibility of creation of uniformly accelerated or decelerated motion model and uniform motion model of Earth’s crust is analyzed. Kinematic laws of straight-line benchmark height motion has been applied to the values of Earth’s crust height displacements that are associated with the nodes in the grid models of relative height displacements created between explicit epochs APN and INVT, and APN and IINVT. This application enabled determination of motion kinematic parameters associated with the grid nodes. Kinematic parameter’s determination, structuring and including in a separate grid models, in analogy to the relative height displacement grid models, along with definition of basic kinematic equations of uniformly accelerated or decelerated motion and uniform motion of Earth’s crust, allowed for the territory of the Croatia, Slovenia and Bosnia and Herzegovina kinematic models creation.
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克罗地亚、斯洛文尼亚和波斯尼亚-黑塞哥维那境内最近地壳运动的运动学模型
基于奥地利精确水准网(APN)和高精度第一次(INVT)和第二次(IINVT)水准网中包含的基准高度数据建模建立的克罗地亚、斯洛文尼亚和波斯尼亚和黑塞哥维那领土相关的地壳相对高度位移网格模型,分析了建立地壳均匀加速或减速运动模型和地壳均匀运动模型的可能性。将直线基准高度运动的运动学规律应用于地壳高度位移的值,这些高度位移与APN和INVT之间以及APN和IINVT之间创建的显式时代相对高度位移网格模型中的节点相关联。该应用程序可以确定与网格节点相关的运动运动学参数。运动学参数的确定、构造和包括在一个单独的网格模型中,类似于相对高度位移网格模型,以及地壳均匀加速或减速运动和均匀运动的基本运动学方程的定义,允许克罗地亚、斯洛文尼亚和波斯尼亚和黑塞哥维那领土的运动学模型的创建。
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来源期刊
Geofizika
Geofizika 地学-地球化学与地球物理
CiteScore
1.60
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: The Geofizika journal succeeds the Papers series (Radovi), which has been published since 1923 at the Geophysical Institute in Zagreb (current the Department of Geophysics, Faculty of Science, University of Zagreb). Geofizika publishes contributions dealing with physics of the atmosphere, the sea and the Earth''s interior.
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