华北克拉通西部地块
参考

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图2. 华北克拉通西部陆块的简化地质图，改自王伟等，2012 & 2016。该图显示了不同时代岩石的分布。西部地块北部暴露出太古宙和古元古代岩石，其余地区则被显生宙岩石覆盖。GY-固阳花岗绿岩地体；WC-武川高级复合体。
图3a. 赵国春模型下，华北克拉通西部地块的构造划分。
图 3b. Kusky模型下，华北克拉通西部地块的构造划分。三角形表示恒山高原向北移动，向内蒙古-河北北部造山带移动。虚线表示断层。
图3c. Santosh模型下，华北克拉通西部地块的构造划分。三角形表示阴山地块向南移动。
图4. 赵国春等人提出的24.5-19.5亿年前的构造演化图。 (1) 24.5亿年前，鄂尔多斯地块的洋壳潜没到阴山地块下，形成喷出岩。 (2) 沉积岩在20-19.5亿年前沉积在鄂尔多斯地块。 (3) 两个地块在19.5亿年前相遇，之间形成孔兹岩带。
图5. Kusky等人提出的西部陆块构造演化图。 (1) 23亿年前之前，东部的五台弧和西部的外来弧潜没到年轻的西部陆块下。 (2) 外来弧与西部地块相撞，形成内蒙古-河北北部造山带。 (3) 哥伦比亚超大陆与西部地块相撞。IMNHO-内蒙古-河北北部造山带。
图6. Santosh提出的西部陆块构造演化图。阴山地块于19.2亿年前潜没到鄂尔多斯地块下，形成内蒙古缝合带，两者间有些玄武岩质洋壳。