SCB由扬子地块(丫劝脚e Block)和华夏地块(cathaysia Block)在前寒武纪碰撞拼贴而成，江绍
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华夏古陆
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Southeast of Cathaysia block 华夏地块东南部
And cause the metamorphism in the cathaysia block during the Late Permian and Early Triassic times.
在晚二叠-早三叠期间,导致华夏地块发生印支期变质作用。
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However, these major components have no exposed counterpart rocks found in the Cathaysia block, implying that their provenance was from other continents previously linked with the Cathaysia block.
这些组分在华夏没有对应出露的岩石，说明它们主要来自另外一个曾经与华夏相邻的陆块。
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