[1ch301-08] R12[レギュラー］岩石・鉱物の変形と反応

[R12-O-2] 北海道東部の前弧含石炭古第三系褶曲帯中の変形バンドの発達と歪集中

加地 広美^1,2、*竹下 徹¹ (1. 北海道大学理学部地球惑星科学科、2. 応用地質株式会社)

キーワード：前弧海盆堆積物、古第三系、褶曲帯、変形バンド、歪集中

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 Middle Eocence Urahoro Group, eastern 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. 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.