• Meanwhile, the fifth stage of magmatism corresponds to the post-orogenic collapse episode.

    同时,第五阶段岩浆活动对应于造山后崩塌阶段。

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  • The other intrusive bodies are post-orogenic granitoid in association with the continental uplifting and rifting.

    其余各岩体是本区造山后与大陆抬升作用以及大陆裂谷作用有关的花岗岩类。

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  • Combined with regional data, the rock formed in the collision of post-orogenic extensional tectonic setting are post-orogenic granite.

    结合区域资料分析,该期岩体形成于碰撞造山后的拉张构造环境,属于后造山花岗岩。

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  • Geochemical characteristics and regional tectonic evolution background indicate that the rocks were formed in a post-orogenic extension environment.

    地球化学特征及区域构造演化背景等表明岩石形成于挤压造山向非造山转换的后造山拉张环境。

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  • The tectonic environment of forming these units develops the epicontinental-collison orogenic environment to the late-orogenic or post-orogenic environment.

    它们的形成构造环境由陆缘碰撞造山环境向造山晚期或造山后环境演化。

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  • The evolution of the XMSZ demonstrates that the North Dabie dome is a metamorphic core complex developed in the Dabie orogenic belt during post-orogenic extension.

    晓天-磨子潭剪切带的演化指示北大别穹隆是大别造山带晚造山伸展过程中形成的变质核杂岩。

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  • The manifestations of large-scale magmatic intrusions occurring in the upper-mid crust in the cores of the orogenic belt were related to post-orogenic geological processes.

    造山带核部上中地壳存在着规模很大的岩浆岩体的显示,与造山期后的地质作用有关。

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  • Multiple oxide-diagrams for discrimination of structural environment and regional tectonic evolution background indicate that the rocks were formed in a post-orogenic extension environment.

    氧化物构造环境判别图解及区域构造演化背景反映香花岭岩体形成于后造山构造环境。

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  • Mesozoic volcanic eruption belt, which locates on Beihuaiyang area in northern part of Dabie orogenic belt, formed at post orogenic stage during Late Jurassic to Early Cretaceous.

    大别造山带北部的北淮阳中生代火山喷发岩带形成于后造山阶段的晚侏罗世—早白垩世。

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  • Mesozoic volcanic eruption belt, which locates on Beihuaiyang area in northern part of Dabie orogenic belt, formed at post orogenic stage during Late Jurassic to Early Cretaceous.

    大别造山带北部的北淮阳中生代火山喷发岩带形成于后造山阶段的晚侏罗世—早白垩世。

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