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Active tectonics in the eastern margin of the bohemian massif - based on the geophysical, geomorphological and GPS data

机译:波希米亚地块东缘的活跃构造-基于地球物理,地貌学和GPS数据

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摘要

One of the leaved out fault active systems at Southern Moravian can be considered the so called Diendorf - ?ebín tectonic zone (DCTZ), that is seismically active in its southern segment (in Austrian). The Waitzendorf fault is a part of the DCTZ, with intensive morphological signs. The terrain recognizance along the eastern margin of the Dyje Dome confirmed many indications showing evidence of geodynamic activity. The facets, old land slides and rock falls indicate recent activity in the environs of Znojmo area. The paper offers interpretation of the geodetic results (GPS) using morphological and geophysical data from all area of the DCTZ.
机译:摩拉维亚南部被遗忘的断层活动系统之一可以被称为所谓的Diendorf-?ebín构造带(DCTZ),在其南部部分(奥地利)具有地震活动性。 Waitzendorf断层是DCTZ的一部分,具有强烈的形态标志。 Dyje Dome东边缘的地形识别结果证实了许多迹象,显示出地球动力学活动的迹象。刻面,旧的滑坡和岩石崩塌表明Znojmo地区周围地区最近的活动。本文使用DCTZ所有区域的形态学和地球物理数据对大地测量结果(GPS)进行了解释。

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