... fold)、倾斜褶皱(inclined fold)、倒转褶皱(overturned fold)和平卧褶皱(recumbent fold),水平褶皱(horizontal fold)和倾伏褶皱(plunging fold),线状褶皱(linear fold)和短轴褶皱(brachy fold),穹隆(dome)和盆地(basin),复式背斜(an...
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If the axial plane of a fold is essentially horizontal. Then we call it recumbent fold.
如果褶皱构造的轴面基本上是水平的,那么我们称它为平卧褶皱。
Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.
平卧褶皱若未经后来构造变动,其图面特征与水平地层区完全一样,除了褶皱转折端以外,只是一系列平行等高线的地质界线。
The trend and plunge of linear features, such as the axis of a fold, describe the azimuth of the line and its deviation from horizontal.
线性特征中的走向及倾伏(诸如褶皱的轴),描述了此线的方位角及其偏离水平面的情况。层态亦称产状。
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