[S-IT19] East Asia geodynamics: New perspectives, top to bottom

[SIT19-P01] Strain localization and development of deformation bands in a forearc coal-bearing Paleogene fold and thrust belt, Hokkaido, northern Japan

Hiromi Kaji^1,2, *Toru Takeshita¹ (1.Department of Natural History Sciences, Graduate School of Science, Hokkaido University, 2.Oyo Co. Ltd.)

Keywords:Forearc basin deposits, Fold and thrust belts, Flexure, Deformation bands, Coal layers, Image analysis

Many studies have recently shown that deformation bands develop in porous sandstones constituting fold and thrust belts. We have analyzed microstructures of deformation bands in one such fold and thrust belt consisting of the Upper Eocence Urahoro Group, Hokkaido, northern Japan, which is typical forearc basin deposits. In the study area, the folds have a wavelength of c. 1-2 km, the axis of which trends NNE-SSW and plunges nearly horizontally, where the strata generally dip either east or west at moderate angles. However, there is one flexure in the eastern part of the study area, where deformation bands are pervasively developed only in the Shakubetsu Formation, which contains mudstones and coal layers other than sandstones. In the other parts of the Urahoro Group in the study area, only sandstones occur without the development of deformation bands. Deformation bands could have formed at the maximum burial depth around 1.5 km inferred from the thickness of overlying strata, which conforms to the one (1.5-2.5 km) inferred from the vitrinite reflectance values (%Ro) of the coal layers (c. 0.5) from the Shakubetsu Formation. The deformation bands are inferred to have originated as phyllosilicate bands, which developed into cataclastic bands with increasing strain in sandstones of the Shakubetsu Formation with up to c. 10 volume % of phyllosilicate. Coal seams, which flow into some deformation bands and smear them, also played a similar role to phyllosilicate in their development. In the cataclastic bands, the detrital grains in host sandstones are crushed into the sizes less than a half to one third of the original one, and also abrased during the formation of deformation bands. The latter fact can be revealed by a higher circularity of grains as well as its higher dependence on grain size in the deformation bands than in the host parts.