Magnetic fabrics of soft-sediment folded strata within a neogene accretionary complex, the Miura group, central Japan

Anisotropy of magnetic susceptibility (AMS) on the middle Miocene-Pleistoce ne sedimentary sequence in the Bose and Miura Peninsulas of central Japan w as used to study 18 sites in the northern tectonic setting and 37 sites in the southern setting. This sequence is associated with abundant synsediment ary deformation structures of folding and faulting generated in accretionar y tectonics. AMS results in different deformation settings such as the fore arc, the accretionary prism and the trench were analyzed. The shapes of the dissimilar magnetic fabrics are compared using the shape parameter (T) and the corrected anisotropy degree (P') in the so-called T-P' diagrams. Our r esults have implied that the oblate fabric of the trench sediments can be r egarded as the result of depositional and compactional processes alone. The AMS shape parameters obtained from the northern sequence (forearc) closely resemble an indication of undeformed trench sediments. In contrast, a diff erent pattern is observed in the highly prolate-shaped AMS results of the s outhern sequence. The difference apparently reflects the degree of deformat ion in the three tectonic provinces. In order to understand the deformation mechanism of the sedimentary fabric, a detailed AMS study was made on one anticline system. An AMS evolution from an oblate fabric to a prolate fabri c in the anticline system was observed. We also found that an AMS tectonic fabric occurred in the center of the anticline. Thickness correlations of t he strata under study indicate that strained sediments formed in the centra l portion of the fold. As a consequence, one can say that this mechanism ca n modify the magnetic fabric from the sedimentary form to the tectonic form in a compressional regime. (C) 2001 Elsevier Science B.V. All rights reser ved.