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Fission-track age and inferred subsidence rate of the Lower to Middle Miocene Nojima Group in NW Kyushu

https://doi.org/10.5575/geosoc.111.350
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25/25 checkable references clean · checked 2026-07-22

Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a retraction, withdrawal, or removal notice.

24 without a DOI — not checked. A reference deposited without a DOI is never matched by title or guessed at; it stays outside the checked set, and this line discloses that.

The 25 checked references that resolve
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Sample assessment and interpretation of zircon ages measured by fission track method
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Fission-track age calibration using internal and external surfaces of zircon.
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Alternate senses of displacement along the Tsushima fault system during the Neogene based on fracture analyses near the western margin of the Japan Sea
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On statistical models for fission track counts
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The radial plot: Graphical assessment of spread in ages
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Fission-track dating methods: What are the real alternatives?
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MESOZOIC AND CENOZOIC CHRONOSTRATIGRAPHY AND CYCLES OF SEA-LEVEL CHANGE
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Paleomagnetism of the Early Miocene Kani Group in southwest Japan and its implication for the opening of the Japan Sea
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Standardization of fission track dating calibration: Recommendation by the Fission Track Working Group of the I.U.G.S. Subcommission on Geochronology
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International union of geological sciences subcommission on geochronology recommendation for the standardization of fission track dating calibration and data reporting
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Paleomagnetic study of the Tsushima Islands, southern margin of the Japan Sea.
resolves10.5636/jgg.43.229
Paleomagnetism and fission-track geochronology on the Goto and Tsushima Islands in the Tsushima Strait area Implications for the opening mode of the Japan Sea.
resolves10.1029/97JB01343
Differential rotations of north Kyushu Island related to middle Miocene clockwise rotation of SW Japan
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Late Cenozoic tectonics around the southern part of the Japan Sea and Kyushu.
resolves10.1016/S0040-1951(01)00068-3
A Miocene pull-apart deformation zone at the western margin of the Japan Sea back-arc basin: implications for the back-arc opening mode
resolves10.5575/geosoc.109.179
Fission-track dating of Miocene volcanic rocks from the southern margin of the Asahi Mountains, northeast Honshu arc, Japan.
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Japan Sea, opening history and mechanism: A synthesis
resolves10.5575/geosoc.109.20
Sedimentary environments of the lower Miocene Nojima Group, NW Kyushu, inferred from sedimentary facies and total organic carbon and total sulfur concentrations.
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Paleomagnetism of Tertiary rocks on the Korean Peninsula: tectonic implications for the opening of the East Sea (Sea of Japan)
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K-Ar and 40Ar/39Ar dating of the hominid-bearing Pliocene-Pleistocene sequence at Koobi Fora, Lake Turkana, northern Kenya
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Opening mode of the Japan Sea inferred from the palaeomagnetism of the Japan Arc
resolves10.5575/geosoc.96.327
Geologic age of the unconformity between the Sasebo and the Nojima groups, Northwest Kyushu and its tectonic significances.
resolves10.1029/TC009i003p00365
Rapid intra‐arc rifting in Miocene northeast Japan
resolves10.2973/odp.proc.sr.127128-1.150.1992
Miocene Pollen Stratigraphy of Leg 127 in the Japan Sea and Comparison with the Standard Neogene Pollen Floras of Northeast Japan
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no DOI — not checked岡本和夫・高橋由美子・寺地雅美, 1971, 島根県仁摩町中新世川合累層の貝化石群集. 松下久道教授記念論文集, 179-185.
no DOI — not checkedOkubo, M. and Takayasu, K., 1979, Discovery of middle Miocene molluscs at Kumi, Dogo, Oki Islands. Mem. Fac. Sci. Shimane Univ., 13, 121-130.
no DOI — not checkedTakayasu, K., 1981, Fossil molluscs from the Miocene Masuda Group at Okuda, Masuda City&minus;Molluscan fossils from various localities in Shimane Prefecture, Part 2&minus;Mem. Fac. Sci. Shimane Univ., 15, 89-108.
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no DOI — not checked棚井敏雅・尾上 亨, 1956, 佐世保炭田産の化石植物群について(予報). 地調月報, 7, 21-26.
no DOI — not checked津田禾粒, 1965, 東北浦日本の新第三紀動物群と岩相-とくに中新世中期の動物群について-. 化石, 10, 20-23.
no DOI — not checked山本博達・簑田耕造, 1973, 長崎県北西部の野島層群(中新統)中の酸性火砕流. 地球科学, 27, 213-220.
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