The tectonic evolution of the east foot of the Funiushan area has gone through long-term and complicated activities from Pt1 to Mz and Cz, it forms the basic tectonics of this area.
伏牛山东麓地区经历了长期而复杂的构造演化，从新太古代到中生代、新生代不断活动，奠定了该区的基本构造格架。
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