碎屑变形;
From Paleoproterozoic Era to late Archeozoic Erathem, it was formed metamorphic complex after deformation and metamorphism from solid liquid facies to soft liquid facies, and it was formed epimetamorphic clastic rock and carbonate rock at Mesoproterozoic-Neoproterozoic Erathem.
古元古晚太古界经历了固流相柔流相变形变质作用后形成变质杂岩(包括表壳岩和变质侵入岩),中新元古界为浅变质碎屑岩和碳酸盐岩。
The early extensional fault controlled the structure systems, forming a series of compound structures of horst and graben and sedimentary facies in which many early sedimentary characters on slope, such as glide deformation and clastic flow can be seen.
早期伸展断层控制了同期的构造和沉积特征,形成一系列复式地垒和地堑的结构,在斜坡带见滑动变形、碎屑流等构造现象。
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