| Institution: | 1. https://orcid.org/0000-0003-1117-6071;2. Department of Earth and Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya, 464‐8601 Japan;3. Yusuke Shimura, Department of Earth and Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, D2‐2 (510), Furo‐cho, Chikusa‐ku, Nagoya 464‐8601, Japan.;4. Research Institute of Geology and Geoinformation, Geological Survey of Japan, AIST, Tsukuba, 305‐8567 Japan;5. Department of Geology, Faculty of Science, Shinshu University, Matsumoto, 390‐8621 Japan |
| Abstract: | Ocean plate stratigraphy (OPS) within an ancient accretionary complex provides important information for understanding the history of an oceanic plate from its origin at a mid‐ocean ridge to its subduction at a trench. Here, we report a recently discovered chert–clastic sequence (CCS) that comprises a continuous succession from pelagic sediments to terrigenous clastics and which constitutes part of the OPS in the Akataki Complex within the Cretaceous Shimanto Accretionary Complex on the central Kii Peninsula, SW Japan. As well as describing this sequence, we present U–Pb ages of detrital zircons from terrigenous clastic rocks in the CCS, results for which show that the youngest single grain and youngest cluster ages belong to the Santonian–Campanian and are younger than the radiolarian age from the underlying pelagic sedimentary rock (late Albian–Cenomanian). Thus, the CCS records the movement history of the oceanic plate from pelagic sedimentation (until the late Albian–Cenomanian) to a terrigenous sediment supply (Santonian–Campanian). |
