日本西南部古近系弧前构造碎屑岩分布格局的新制约因素——四国西部岛满带多梅基组碎屑锆石U-Pb年龄

IF 0.2 Q4 GEOGRAPHY, PHYSICAL Journal of Geography-Chigaku Zasshi Pub Date : 2021-10-25 DOI:10.5026/jgeography.130.707
Tomohito Nakano, Y. Isozaki, Y. Tsutsumi
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引用次数: 2

摘要

摘要对代表日本西南部古近系弧前斜坡台地沉积的高知县西部Shimanto带Domeki组(Fm) 2个砂岩进行了碎屑锆石U - Pb年龄测定。结果表明,两个样品均含有丰富的古新世和晚白垩世锆石,前白垩世颗粒含量极低。说明多木组的物源主要为日本西南部三仁带的长英质火成岩,即同古火山弧。Domeki组锆石年龄谱与弧前主盆地(Kii半岛上部的Izumi群和关东的Kanohara砾岩/Yorii组)的同期砂岩年龄谱基本一致。这表明古新世弧前域普遍存在单一组成的陆源碎屑,包括大陆一侧的主弧前盆地和海沟一侧的小台地盆地,从里奥克带南缘到石曼托带中部,横跨弧前域80多公里。同时也证实了晚白垩世至古新世在日本西南部弧前稳定连续沉积了大量弧源碎屑,沿弧长超过1000公里。目前的资料限制了日本西南部古近纪两次大规模构造事件的时间,即良奥和三巴川带之间的中构造线的起始和高p /T三巴川片岩的首次地表暴露,不早于古新世/始新世边界(约10 ~ 10年)。56
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New Constraints on the Distributary Pattern of Clastics in Fore-arc and Tectonics in Paleogene SW Japan: U–Pb Ages of Detrital Zircons of the Domeki Formation in the Shimanto Belt, Western Shikoku
― 707 ― Abstract U ­ Pb ages of detrital zircons are measured for two sandstones of the Domeki Formation ( Fm ) in the Shimanto belt, western Kochi, which represent bench deposits on the Paleogene fore-arc slope in SW Japan. The results show that both samples are replete with Paleocene and Late Cretaceous zircons, and they have extremely small quantities of pre-Cretaceous grains. This indicates that the provenance of the Domeki Fm was occupied mainly by felsic igneous rocks of the San-in belt in SW Japan, i.e., coeval volcanic arc. The age spectrum of zircons in the Domeki Fm is almost identical to those of coeval sandstones deposited in the main fore-arc basin ( uppermost Izumi Group in the Kii peninsula, and Kanohara Conglomerate/Yorii Fm in Kanto ) . This suggests the ubiquitous supply of terrigenous clastics of the monotonous composition into the Paleocene fore-arc domain, including both the main fore-arc basin at the continent side and minor bench basins at the trench side, for more than 80 km across the arc from the southern margin of the Ryoke belt to the central Shimanto belt. Also confirmed is the stable and continuous deposi-tion of voluminous arc-derived clastics on the fore-arc of SW Japan from the Late Cretaceous to Paleocene for more than 1000 km along the arc. The present data constrain the timings of two large-scale tectonic episodes in Paleogene SW Japan, i.e., the initiation of the Median Tectonic Line between the Ryoke and Sanbagawa belts and the first surface exposure of high-P/T Sanbagawa schists, to have been no earlier than Paleocene/Eocene boundary ( ca . 56
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