作者: S. V. Shipunov , Yu. S. Bretshtein , A. V. Zhuravlev
DOI: 10.1134/S1819714008040076
关键词: Stage (stratigraphy) 、 Seismology 、 Paleomagnetism 、 Mesozoic 、 Tectonics 、 Geology 、 Deformation (mechanics)
摘要: The analysis of paleomagnetic data available for the southern Primiorye region revealed that studied objects were magnetized under regional remagnetization presumably during Late Mesozoic folding and this magnetization can be interpreted as being synfolding. interpretation is based on parameter characterizes completion degree immediately before remagnetization. It shown relaxation horizontal stresses was irregular. obtained estimates are consistent with geological Talitskii’s model tectonic deformations.