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MONITORING GEODYNAMIC PROCESSES USING GEODETIC AND GRAVIMETRIC METHODS: AN EXAMPLE FROM THE WESTERN CARPATHIANS (SOUTH POLAND)

机译:用大地测量和重力法监测地球动力学过程:以西喀尔巴阡山脉为例(南波兰)

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摘要

Multidisciplinary studies conducted along two geodynamic test transects across the Polish segment of the Western Carpathians, crossing the Orava Basin in the west and the Pieniny Klippen Belt and Magura Nappe along the Dunajec River valley in the east, included gravity and geodetic surveys as well as geological investigations. Gravity and geodetic surveys were carried out annually in years 2004-2006. Their results appear to suggest recent subsidence of the Orava Basin, particularly intensive in a Quaternary graben in the northern part of the area, confirming conclusions derived from geomorphic analyses. Data obtained for the Dunajec River transect do not show any particular differentiation among individual benchmarks, what can point to either minor uplift of the entire area, minimal differences between successive slices of the Magura Nappe and the Pieniny Klippen Belt, or both. Horizontal displacements of benchmarks, different for the western and eastern transects, towards the west and SW as well east and SE, respectively, can result from general uplift of the area comprised between these transects. On the other hand, the N to NNE-oriented vectors of recent horizontal motions, observed for stations located south of the Pieniny Klippen Belt, point to the ongoing NNE-directed push of the ALCAPA block.
机译:沿着西喀尔巴阡山脉的波兰段的两个地球动力学试验断面进行多学科研究,横跨西部的奥拉瓦盆地,东部的杜纳耶茨河河谷的Pieniny Klippen带和Magura Nappe,包括重力和大地测量以及地质学调查。 2004-2006年每年进行重力和大地测量。他们的结果似乎暗示了奥拉瓦盆地最近的沉降,特别是该地区北部第四纪a陷的密集沉降,证​​实了从地貌分析得出的结论。从杜纳耶茨河断面获得的数据没有显示出各个基准之间的任何特殊区别,这可能表明整个区域出现了微小的隆升,Magura Nappe和Pieniny Klippen带的连续切片之间的差异很小,或两者兼而有之。基准线的水平位移(分别针对西部和东部样带而不同)分别朝向西部和西南以及东部和东南,这可能是由于这些样带之间的区域普遍抬升所致。另一方面,在Pieniny Klippen带以南的台站观测到的近期水平运动的N到NNE定向矢量,表明ALCAPA区块正在以NNE定向推进。

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