The volcanic rocks formed in a tectonic environment of deep thermal collapse eruption in the Early-Mid Permian late-orogenic phase.
构造环境为早中二叠世造山后期深部热力塌陷火山喷发环境。
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。
The rocks coexist closely, distributing in a narrow and long belt in the Late Precambrian orogenic belt in northern Liaoning.
它们紧密共生，呈狭长的带状分布于辽宁北部晚前寒武纪造山带内。
应用推荐