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Paleomagnetic investigations of the basal Borove Formation in the Liptov Depression (Central-Carpathian Paleogene basin)

机译:利普托夫(陷(中喀尔巴阡古近纪盆地)基底波罗夫组的古磁研究

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摘要

The results of the paleomagnetic investigation from 9 localities of the Central-Carpathian Paleogene basalBorove Formation in the Liptov Depression (Central Slovakia) demonstrate complicated tectonic evolution in the cen-tral area of the Western Carpathians. The eastern rotations are predominant in the southern and western rotations in thenorthern margins of the Liptov Depression. Paleodeclinations vary from 92° to 269° and paleoinclinations from 7° to59°. The dextral and sinistral fault systems explain different values of paleorotations in relatively closely situatedlocalities. The obtained results generally support the model of tectonic escape from the south-west to north-east direc-tion. Low inclination in some localities offers various explanations.
机译:利普托夫(陷(斯洛伐克中部)中喀尔巴阡山脉古近纪基底波罗夫组9个地区的古磁研究结果表明,西喀尔巴阡山脉中央地区构造演化复杂。利普托夫凹陷北部边缘的东部和南部旋转主要发生在东部。古倾斜度从92°到269°不等,古倾斜度从7°到59°不等。右旋和窦性断层系统在相对较近的位置解释了古隆起的不同值。所获得的结果通常支持从西南向东北方向的构造逃逸模型。在某些地区倾斜度较低,可以提供各种解释。

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