加里东期(寒武纪—志留纪)加里东期是中国较强烈的岩浆活动期。
adj. Caledonian
...加里东期;;中华力西—印支期;;兴蒙造山带;;古亚洲洋 [gap=1003]Keywords: tectonic assemblage of igneous rocks;tectonomagmatic stage;Caledonian stage;Middle Variscan-Indosinian stage;Xing'an-Mongolian orogenic belt;Paleoasian Oce..
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山体岩石为加里东期花岗岩和大理石，距今4——6亿年。
Rock Hill Caledonian granite and marble ago 4-6 billion years.
该类型构造形成于加里东期末，是该区加里东造山期后隆升背景的产物。
This kind of structure is the product under background of the uplift in Caledonian postorogenic phase formed at the end of the Caledonian Stage.
加里东期断裂控制了加里东岩溶储层的发育，由此预测了加里东期岩溶储层的发育区带。
Based on the domination of Caledonian faults on the development of Caledonian karst reservoirs, this paper predicts the development area of Caledonian karst reservoirs.
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