2018
DOI: 10.1016/j.jseaes.2017.10.025
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Permian arc evolution associated with Panthalassa subduction along the eastern margin of the South China block, based on sandstone provenance and U–Pb detrital zircon ages of the Kurosegawa belt, Southwest Japan

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Cited by 29 publications
(18 citation statements)
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“…It is generally accepted that accretionary belts in SW Japan were accreted to the active continental margin of the South China (Cathaysia) block during subduction of the Palaeo‐Pacific Oceanic plate (Hara et al., ; Isozaki et al., ; Maruyama et al., ). However, a tectonic connection between SW Japan and the Bureya‐Jiamusi‐Khanka (BJK) massif before the opening of the Japan Sea is also supported by similarities in lithology, U–Pb ages of granitoids, faunal assemblage and the structural relationships between them (Fujii, Hayasaka, & Terada, ; Ishiwatari & Tsujimori, ; Kojima, Igor'V, Kametaka, & Ando, ; Tsutsumi, Yokoyama, Kasatkin, & Golozubov, ).…”
Section: Discussionmentioning
confidence: 99%
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“…It is generally accepted that accretionary belts in SW Japan were accreted to the active continental margin of the South China (Cathaysia) block during subduction of the Palaeo‐Pacific Oceanic plate (Hara et al., ; Isozaki et al., ; Maruyama et al., ). However, a tectonic connection between SW Japan and the Bureya‐Jiamusi‐Khanka (BJK) massif before the opening of the Japan Sea is also supported by similarities in lithology, U–Pb ages of granitoids, faunal assemblage and the structural relationships between them (Fujii, Hayasaka, & Terada, ; Ishiwatari & Tsujimori, ; Kojima, Igor'V, Kametaka, & Ando, ; Tsutsumi, Yokoyama, Kasatkin, & Golozubov, ).…”
Section: Discussionmentioning
confidence: 99%
“…Numerous studies have used detrital zircon U–Pb dating to discuss the provenance and tectonic evolution of various accretionary belts in Japan (e.g. Aoki et al., ; Hara, Hirano, Kurihara, Takahashi, & Ueda, ; Isozaki et al., ; Tsutsumi, Yokoyama, Terada, & Sano, ; Zhang, Takeuchi, Ohkawa, & Matsuzawa, ); however, Hf isotopic studies are still rare. New Hf data from accretionary belts in Japan could be compared with the existing Hf data of late Palaeozoic rocks in the eastern margin of the Asian continent to offer new insight into the tectonic evolution of the Japanese Islands.…”
Section: Introductionmentioning
confidence: 99%
“…Recently, an oceanic island arc (proto-Japan arc) outboard of eastern south China has been delineated by some geologists to interpret the geological history of SW Japan in the Paleozoic (Figure 11a; e.g., Cocks & Torsvik, 2013;Domeier & Torsvik, 2014;Isozaki et al, 2010). The subduction of the Paleo-Pacific plate beneath the proto-Japan arc may have started in the Early Paleozoic (Aoki et al, 2015;Hara et al, 2018;Zhang et al, 2018), consistent with its counterpart along the Paleo-Pacific east Gondwana margin (Cawood & Buchan, 2007). According to this model, eastern south China was in a distal continental back-arc setting related to the subduction of the Paleo-Pacific Ocean plate beneath the proto-Japan arc (Figure 11a).…”
Section: 1029/2018jb015520mentioning
confidence: 99%
“…However, Permian arc magmatism has not been discovered along the coastal provinces of southeast China so far. Instead, it occurs in SW Japan (Hara et al, 2018;Zhang et al, 2018, and references therein). Thus, Japan could have acted as a source for these Permian-Jurassic sedimentary rocks (L. Hu et al, 2015), which was once a part of the southeast China margin until Middle Jurassic time (Figure 11b; e.g., Hara et al, 2018;Jahn, 2010;Zhang et al, 2018).…”
Section: 1029/2018jb015520mentioning
confidence: 99%
“…They are U-Pb age data of detrital zircon from sandstones or psammitic schist of the Akiyoshi, Suo, Maizuru and Ultra-Tamba belts, as well as Triassic non-marine to shallow marine formations of the Nariwa, Asa and Mine groups. Additionally, we have compiled U-Pb detrital zircon age data from various other sources, such as Tsutsumi et al (2000Tsutsumi et al ( , 2009 Hara et al (2017Hara et al ( , 2018, Uchino (2017), Zhang et al (2018) and the supplementary file of this paper (available online at https://doi.org/10.1017/S0016756818000742). Figure 6 shows that there are three major peaks in detrital zircon distribution, marked by the Early Permian to Early Triassic, Early to Late Jurassic, and middle to Late Cretaceous age clusters.…”
Section: Accretionary History and Detrital Zircon Datamentioning
confidence: 99%