- 構造地質部会

-.' .. ¸ --ῌ./ ,*** @Structural Geology, No. .., --ῌ./, ,***A
Fold structures and basal fault of the Upper Cretaceous Tochiya
Formation in the northeastern Kanto Mountains
*
Shirou Chikashige*
Abstract : Geological structures of the Upper Cretaceous Tochiya Formation, once
regarded as one of the member of the Atokura Nappe, were carefully investigated in
order to clarify the geotectonic evolution of the the Yorii-Ogawa area in the northeastern Kanto Mountains. A macroscopic overturned anticline verging northward was
recognized as well as upright folds. Their axes trend N2*ῌ2/W and plunge /ῌ+*.
A basal thrust between the allochthonous Tochiya Formation and the underlying
Mikabu greenstones cuts the fold structures and exhibits fault-rock fabrics, suggesting
a top to the north sense of shear. These evidences for the northward movement
suggest that the Tochiya Formation in the study area was a di#erent nappe from the
southward-verging Atokura Nappe of the type locality.
Key words : Tochiya Formation, Atokura Nappe, overturned fold, basal fault, paleocurrent
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Photograph of the outcrop of the southward dipping reverse beds, forming the northern limb
near the hinge of the overturned anticline in the southern area of the Tochiya Formation.
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Photographs of the outcrops of the southern limb of the overturned anticline in the
southern area of the Tochiya Formation. (a) Normal strata dipping north in the northern
part. (b) Subhorizontal normal strata in the middle part.
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Fracture zone cutting the overturned north limb at To-- in the southern area of the Tochiya Formation.
The overturned strata dipping south in the right hand of fracture zone,the normal strata dipping north in the left
hand of fracture zone are observed. Bag in front of the outcrop for scale.
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Outcrop of the basal fault of the Tochiya Formation. The hanging wall rock is conglomerate of the Tochiya Formation
and the footwall rock, Mikabu greenstone complex. ῌ Whole view of the basal fault. Black line shows the fault trace. ῍
Central part of the basal fault shown in (a). ῎ Close-up view of the fault gauge zone of about +/ cm in width. ῏ Asymmetric
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