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• W814682870 abstract "A study of anisotropy of magnetic susceptibility(AMS) was conducted on the Cambrian-Triassic strata in the northeastern part of the Okchon belt. A total of 951 independently oriented core samples were collected from 103 sites throughout the area. The study results show that 13 sites are characterized by magnetic lineation, 28 sites by load foliation, and 23 sites by tectonic foliation. Magnetic lineations created by paleocurrent are predominant in the Cambro-Ordovician sedimentary rocks (mostly limestones). Load foliations caused by the weight of the overlying strata occur throughout the area regardless of the geologic age of the strata. Tectonic foliations created by compressional tectonic force show a gradual regional variation in direction: Direction of compression axes derived from tectonic foliation in the southwestern part of the study area (Yongwol area) is approximately E-W, while it changes gradually into WNW-ESE and NW-SE in the central part of the study area (Pyongchang, Yemi and Chongson area). It becomes finally N-S in the northeastern part of the study area (Kangneung area). Such compressional directions are compatible with the thrust directions in each area. It is therefore concluded that the major thrusts in the study area have been formed during this compressive deformational phase, such as the Kagdong thrust, the Pyongchang shear zone and the Paegunsan syncline. The compression directions of Cambrian-Permian strata achieve better clustering without the bedding-tilt correction, whereas those of early Triassic strata become better clustered after the bedding-tilt correction. This fact indicates that the time of tectonic compression was between late Permian to early Triassic time. The direction of compression was NW-SE. In view of the fact that the compression and thrust directions coincide with each other, the compressive stress was associated with the Songnim Disturbance, a major orogenic event in the Korean peninsula. The Songnim Disturbance must have been in turn an expression of the South/North China Blocks collision, a late Permian to the early Triassic event suggested by palaeomagnetic data. The collisional force was transferred to the surrounding area, forming the fanning trajectory from a promontory with a variation of stress direction from area to area as described above." @default.
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• W814682870 date "1998-01-01" @default.
• W814682870 modified "2023-09-23" @default.
• W814682870 title "Palaeomagnetic Results from the Okchon Belt: Anisotropy of Magnetic Susceptibility(AMS) and Tectonic Stress Field in the Northeastern Okchon Belt" @default.
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