三叠纪薄板状灰岩箱形褶皱The Box Fold of Laminated Limestone from Triassic
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箱型褶皱是官珠沟常见褶皱形态之一。箱状褶皱是强应力下形成的地层褶皱变形。主要特征是:顶部平直,两翼近于平行的箱形构造。三叠纪薄板状灰岩箱形褶皱距今约2.5亿年至2.03亿年。
Box fold is one of the common shapes in Guan E valley. Box fold is strata fold deformation formed under strong stress which is characterized by following: the top is straight; two wings are box structureclose to the line.Triassic tabular limestone box folds are about 250million to 203million years ago.