• 研究区的褶皱平行褶皱组成隔档褶皱

    The folds in the investigated area belong to ejective fold type, which is composed of parallel folds;

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  • 背斜隔挡式平行褶皱纵向变异很大形成多种圈闭类型,具有不同、水分布规律

    The high-steep anticline belt belonged to barrier parallel fold is greatly variant in vertical, forming many types of traps and being of various gas-water distribution laws.

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  • 角度整合褶皱变形平行不整合是板内造变形重要记录

    Angular unconformity belongs to an intraplate folded - orogenic deformation. Parallel unconformity is the record of intraplate epeirogenic deformation.

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  • 推覆体发育了与边界断层平行的侧断坡次级断层相关褶皱背斜;

    On the lateral border of the nappe, lateral and oblique fault-slope secondary fault-related folded anticlines parallel to boundary faults were developed.

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  • 平卧褶皱未经后来构造变动图面特征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。

    Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.

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  • 平卧褶皱未经后来构造变动图面特征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。

    Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.

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