Late Triassic A-type granite boulders in Lower Cretaceous conglomerate of the Hida belt, Japan: Their origin and bearing on the Yamato tectonic line in Far East Asia

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Island Arc Pub Date : 2023-01-11 DOI:10.1111/iar.12475
Yukio Isozaki, Yusuke Sawaki, Hideki Iwano, Takafumi Hirata, Keitaro Kunugiza
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引用次数: 1

Abstract

To identify the origin of the Hida belt in central Japan, geochemistry and U–Pb age of zircons were analyzed for the extra-large granitoid boulders in the Lower Cretaceous fluvial conglomerate of the Jinzu Group. This study clarified that the boulders of granitoids have geochemistry of typical A-type granite, as characterized by high Nb + Y and high Ta + Yb values. U–Pb ages of igneous zircons from three individual granite boulders are concentrated at ca. 220 Ma (Late Triassic). As to Late Triassic A-type granites, there is no corresponding body previously recognized within Japan, whereas identical A-type granites occur in the eastern Songliao block on the immediate west of the Jiamusi block in NE China. The large size of boulders and the fluvial facies of the hosting conglomerate indicate their origin in the Hida belt per se, suggesting the cryptic and/or past occurrence of A-type granite, rather than in NE China. Together with the eastern Songliao block (China), Laoelin-Grodekov (LG) belt (Primorye, Russia), and Yamato Ridge (Japan Sea), the Hida belt forms a unique domain on the immediate west of GSC in Far East Asia, which is characterized commonly by the co-occurrence of Permo-Triassic and Jurassic granitoids, and probably with Late Triassic A-type granite. These confirm that Hida belt represents an allochthonous unit tectonically emplaced onto the rest of Japan, which is composed of the Phanerozoic subduction-related orogenic belt (Nipponides) developed along the Pacific side of Greater South China (GSC) since the Cambrian. For emphasizing a major geotectonic boundary of the Mesozoic granitoid provinces in Far East Asia, we propose the Yamato tectonic line between the easternmost Central Asian orogenic belt and GSC/Nipponides, which is traced for up to 3000 km from the Russia/China/North Korea border to SW Japan.

日本飞驒带下白垩统晚三叠世A型花岗岩巨砾的起源及其与远东大和构造线的关系
为确定日本中部飞驒带的成因,对金足群下白垩统河流砾岩中的超大型花岗岩类巨砾进行了锆石地球化学和U-Pb年龄分析。研究表明,花岗岩类岩石具有典型的a型花岗岩地球化学特征,具有高Nb + Y和高Ta + Yb的特征。3个花岗岩单体的火成岩锆石U-Pb年龄集中在约220 Ma(晚三叠世)。晚三叠世a型花岗岩在日本国内尚未发现对应体,而在中国东北部佳木斯地块以西的松辽地块东部也有相同的a型花岗岩。巨砾的大尺寸和承载砾岩的河流相表明,它们起源于Hida带本身,表明a型花岗岩的隐秘性和(或)过去曾出现过,而不是在中国东北。Hida带与松辽东部地块(中国)、俄罗斯滨海地区的Laoelin-Grodekov (LG)带、日本海的Yamato Ridge(日本海)一起,构成了远东GSC正西侧的一个独特的区域,其共同特征是二叠-三叠纪和侏罗纪花岗岩类共生,可能与晚三叠世a型花岗岩共生。这证实了飞驒带是由寒武纪以来沿大华南(GSC)太平洋一侧发育的显生宙俯冲相关造山带(Nipponides)组成的一个位于日本其他地区的异域构造单元。为了强调远东中生代花岗岩省的主要大地构造边界,我们提出了中亚造山带最东端与GSC/Nipponides之间的大和构造线,该构造线从俄罗斯/中国/朝鲜边境到日本西南部长达3000公里。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Island Arc
Island Arc 地学-地球科学综合
CiteScore
2.90
自引率
26.70%
发文量
32
审稿时长
>12 weeks
期刊介绍: Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.
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