华北克拉通东部地块
参考

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东部地块中出露的太古宙基岩分布图和胶辽吉带的位置。
地幔柱模型显示了超基性和玄武岩大火成岩省的形成。地球深处的物质上升，侵入岩石圈，拉伸了地壳。大量岩浆在地表喷发，成为大火成岩省。
岩浆弧系统中，显示出具有镁铁质和长英质物质的岩浆的双模火山活动。俯冲打样板块和下层大陆地壳的部分熔化导致了片麻岩成分的不同。
形成胶辽吉带的弧-陆碰撞横截面。
一系列演化图显示了东西地块的俯冲和陆陆碰撞。形成了跨华北造山带。