Is the North-Eastern Japan a part of the North-American Plate?

Kinugasa, Yoshihiro

doi:10.5026/jgeography.99.13

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“…The southwest extension of the Kita‐Touzaki anticline of sheet II probably extends to near the northern end of the ISTL (Figs 2,7). The northernmost segment of the ISTL has been inactive recently (Kinugasa 1990) but there is a possibility that thrust sheet II was continuous with the northernmost ISTL in the early Pleistocene.…”

Section: Discussionmentioning

confidence: 99%

Fault‐related folds and an imbricate thrust system on the northwestern margin of the northern Fossa Magna region, central Japan

Okamura

2003

Island Arc

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The Nishikubiki Mountains, which are located on the northwestern margin of the northern Fossa Magna region, central Japan, and the area offshore to the north of the mountains are underlain by folded and faulted Neogene and Quaternary sequences. The folds are composed of open, symmetric anticlines or tight, asymmetric anticlines trending north 20–70° east. On the basis of the geometry of the anticlines and growth strata, the symmetric and asymmetric anticlines are interpreted as fault‐bend folds and fault‐propagation folds, respectively. The formation of the anticlines is attributed to the growth of an imbricate thrust system composed of three thrust sheets that developed, from southeast to northwest, mainly in the late Pliocene, early Pleistocene, and middle Pleistocene–Holocene. The horizontal component of the northwestern‐most sheet was estimated to be approximately 1.2 km on the basis of the width of the growth triangle, and the thickness of the sheet at its southeast margin was estimated to be 8.5 km on the basis of area balancing along one of the seismic profiles. The thrust is inferred to extend to a depth of more than 10 km toward the southwest. The three thrust sheets are probably connected by a detachment zone along the boundary between the upper and lower crusts. The anticlines are bounded by the Itoigawa–Shizuoka Tectonic Line (ISTL) to the west and by lateral ramps or tip lines to the northeast. The ISTL possibly continues northward offshore into the Toyama Trough. The structural model proposed in this paper suggests that similar thrust systems are wide spread in the northern Fossa Magna region and that active deformation zones have migrated and switched during the past 2–3 million years along the fold belt.

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Section: Discussionmentioning

confidence: 99%