江南造山带的形成与演化
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摘要
处于扬子地块和华夏地块之间的江南造山带是理解华南地壳演化、岩浆过程和成矿效应的关键。近年来,围绕江南造山带的构造-岩浆演化产生了较大争论,因而影响到对华南显生宙岩浆-成矿事件内在联系及动力学机制的认识。本文总结了近年来对江南造山带研究大量资料,对有关江南造山带形成和演化的几个方面进行了剖析和讨论,明确了江南造山带是一个稍晚于世界典型Grenville期造山事件的新元古代的造山带,具有完整的蛇绿岩、岛弧火山岩、高压变质岩、同碰撞岩浆岩、造山磨拉石、碰撞后岩浆岩和造山后岩浆岩等与造山过程相吻合的岩石组合,经历了从洋洋俯冲、弧-陆碰撞到洋-陆俯冲、弧后盆地打开再到造山后伸展的构造过程,在华南中部形成了大量中元古代末到新元古代早期的新生地壳,很可能是显生宙成岩-成矿作用的重要物源。
The Jiangnan Orogen,which lies between the Yangtze and Cathaysia blocks,is the key to understand the crustal evolution,magmatic process and ore-forming effect of the South China. In recent years,big arguments on the tectonomagmatic evolution of the Jiangnan Orogen have strongly influenced the understanding on internal relationship between the Phanerozoic magmatism and mineralization events in South China and their dynamic machnisms. Based on the synthetic evaluation of a huge amount of geochronological and geochemical data of rocks in the Jiangnan Orogen,several important issues regarding the formation and evolution of the Jiangnan Orogen have been analyzed and discussed in this paper. It is confirmed that the Jiangnan Orogen is a Neoproterozoic orogenic belt,which was formed slightly later than the typical Grenvillian orogenic event,with complete orogeny-related rock associations,including ophiolites,arc volcanic rocks,highpressure metamorphic rocks,syn-collisional magmatic rocks,orogenic molasses,post-collisional and post-orogenic magmatic rocks. The Jiangnan Orogen subsequently experienced various tectonic processes including the ocean-ocean subduction,arc-continent collision,ocean-continent subduction,opening of back-arc basins,and post-orogenic extension. The orogeny led to the formation of extensive late Mesoproterozoic and early Neoproterozoic juvenile crust that might have contributed greatly to the Phanerozoic diagenesis and metallogesis in South China.
The Jiangnan Orogen,which lies between the Yangtze and Cathaysia blocks,is the key to understand the crustal evolution,magmatic process and ore-forming effect of the South China. In recent years,big arguments on the tectonomagmatic evolution of the Jiangnan Orogen have strongly influenced the understanding on internal relationship between the Phanerozoic magmatism and mineralization events in South China and their dynamic machnisms. Based on the synthetic evaluation of a huge amount of geochronological and geochemical data of rocks in the Jiangnan Orogen,several important issues regarding the formation and evolution of the Jiangnan Orogen have been analyzed and discussed in this paper. It is confirmed that the Jiangnan Orogen is a Neoproterozoic orogenic belt,which was formed slightly later than the typical Grenvillian orogenic event,with complete orogeny-related rock associations,including ophiolites,arc volcanic rocks,highpressure metamorphic rocks,syn-collisional magmatic rocks,orogenic molasses,post-collisional and post-orogenic magmatic rocks. The Jiangnan Orogen subsequently experienced various tectonic processes including the ocean-ocean subduction,arc-continent collision,ocean-continent subduction,opening of back-arc basins,and post-orogenic extension. The orogeny led to the formation of extensive late Mesoproterozoic and early Neoproterozoic juvenile crust that might have contributed greatly to the Phanerozoic diagenesis and metallogesis in South China.
引文
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