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Interactions Between Deformation And Fluids In The Frontal Thrust Region Of The Nantroseize Transect Offshore The Kii Peninsula, Japan: Results From Iodp Expedition 316 Sites C0006 And C0007, E Screaton, G Kimura, D Curewitz, G Moore, F Chester, O Fabbri, Christopher L. Fergusson, F Girault, D Goldsby, R Harris, F Inagaki, T Jiang, Y Kitamura, M Knuth, C-F Li, L Claesson Liljedahl, L Louis, K Milliken, U Nicholson, N Riedinger, A Sakaguchi, E Solomon, M Strasser, X Su, A Tsutsumi, A Yamaguchi, K Ujiee, X. Zhao
Interactions Between Deformation And Fluids In The Frontal Thrust Region Of The Nantroseize Transect Offshore The Kii Peninsula, Japan: Results From Iodp Expedition 316 Sites C0006 And C0007, E Screaton, G Kimura, D Curewitz, G Moore, F Chester, O Fabbri, Christopher L. Fergusson, F Girault, D Goldsby, R Harris, F Inagaki, T Jiang, Y Kitamura, M Knuth, C-F Li, L Claesson Liljedahl, L Louis, K Milliken, U Nicholson, N Riedinger, A Sakaguchi, E Solomon, M Strasser, X Su, A Tsutsumi, A Yamaguchi, K Ujiee, X. Zhao
Faculty of Science - Papers (Archive)
Integrated Ocean Drilling Program (IODP) Expedition 316 Sites C0006 and C0007 examined the deformation front of the Nankai accretionary prism offshore the Kii Peninsula, Japan. In the drilling area, the frontal thrust shows unusual behavior as compared to other regions of the Nankai Trough. Drilling results, integrated with observations from seismic reflection profiles, suggest that the frontal thrust has been active since similar to 0.78-0.436 Ma and accommodated similar to 13 to 34% of the estimated plate convergence during that time. The remainder has likely been distributed among out-of-sequence thrusts further landward and/or accommodated through diffuse shortening. Unlike results of …
743 ± 17 Ma Granite Clast From Jurassic Conglomerate, Kamiaso, Mino Terrane, Japan: The Case For South China Craton Provenance (Korean Gyeonggi Block?), Allen Phillip Nutman, Y Sano, K Terada, H Hidaka
743 ± 17 Ma Granite Clast From Jurassic Conglomerate, Kamiaso, Mino Terrane, Japan: The Case For South China Craton Provenance (Korean Gyeonggi Block?), Allen Phillip Nutman, Y Sano, K Terada, H Hidaka
Faculty of Science - Papers (Archive)
The polymict Kamiaso Conglomerate (Mino Terrane, Japan) contains Jurassic to Palaeoproterozoic clasts—probably derived from Korean basement that lay nearby to the northwest at time of deposition. Clast K2 broke cleanly into two halves during sampling (but the halves were recombined for zircon separation). A third of the K2 zircons are colourless euhedral prisms with oscillatory zoning, with no inheritance and yielded a SHRIMP U/Pb date of 743±17 Ma. Two thirds of K2 zircons are brown oscillatory-zoned corroded prisms with a date of 1860±8 Ma, with inherited cores up to ∼2460 Ma. A likely explanation for this could be that clast …