The reasons for seismic activity in this region can be related to neotectonic movements
(including glacio-isostatic rebound) as recorded in the southeastern Baltic Sea area of the Fennoscandian ice sheet margin zone.
The problem of determining neotectonic movements
in the Bochnia salt mine lies in separating tectonic from human-induced movements.
Further implementation of OSL dating, and particularly the introduction of cosmogenic radionuclide dating (CRN), is essential to surpass that limitation and to better characterize the timing of the neotectonic movements
(uplift/subsidence and fault slip) and to estimate strain rates.
Rahni explained the genesis of eskers with direct influence of Late-Glacial tectonic movements on the bedrock-glacier association and suggested block-wise neotectonic movements
with their amplitudes reaching tens of metres.
associated with the Sudetic Marginal Fault were superimposed on this older tectonic structure.
It documents significant role of neotectonic movements
during their genesis, despite they are flown through with greater streams, and create together with adjacent slope surfaces within the study area a very various spectrum of landforms.
Geological data on neotectonic movements
of the Earth's crust in the Estonian S.
Previous interpretations of neotectonic movements
occurring in the Fore-Sudetic Block assumed reactivation of main faults that were already formed in the Variscan orogeny, an in the Opole Depression also during the Late Cretaceous--Early Palaeogene orogeny.
Differential neotectonic movements
on either side of this thrust (uplift in the south and subsidence in the north) made their appearance also in the last glacial and Holocene times.
This type of alternation of morphostructures, which shows varying rates of neotectonic movements
, may reflect either concurrent isostatic adjustment or Quaternary remnant folding (Zuchiewicz, 1991).
1983, The age problem of lower limit of neotectonic movements
and their phases in SW Poland (in Polish, with English summ.
1993, An attempt at application of selected morphometric methods to estimation of neotectonic movements
in the Sudety Mountains, SW Poland, and their foreland.