Stratigraphic reconstruction of the lower–middle Miocene Goto Group, Nagasaki Prefecture, Japan

نویسندگان

چکیده

The Goto Islands are located at the westernmost tip of Japan archipelago, and preserve a lower–middle Miocene sedimentary sequence deposited during rifting continental margin opening Sea Japan. stratigraphy Group new K–Ar, fission-track, U–Pb age data were used to determine initial conditions in southwest thickness is 2000–3000 m. lower unit (ca. 22–17.6 Ma) consists thick, greenish, volcaniclastic rocks with basaltic volcanic material, representing stages rifting. middle ?17.6 alternating sandstones shales lacustrine meandering fluvial environments syn-rift basin period activity. upper 17.6–16.8 thick fluvial–deltaic facies that rapid subsidence margin. This was by large system flowed into These sequences contain relatively cooler warmer flora (Daijima-type) record warm Climatic Optimum. felsic (16.8 ~ 15.4 unconformably overlie Group, granitic magmatism 16–14.5 occurred after sedimentation Group. widespread lacustrine, meandering–braided fluvial, vast deltaic systems volcanism, formed due produced horst-and-graben early arc along eastern Eurasia. events from 22.0 16.8 Ma before formation

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ژورنال

عنوان ژورنال: Island Arc

سال: 2022

ISSN: ['1038-4871', '1440-1738']

DOI: https://doi.org/10.1111/iar.12456