1) reclined fold
斜卧褶皱
1.
Detailed field observation and structural mapping show that reclined folds were well developed on various scales in some districts with exposed UHP metamorphic rocks in the Donghai area, northern Jiangsu, China.
详细的野外观察和制图证实 ,在苏北东海地区的驼峰、房山及虎山等超高压 (UHP)变质带岩石出露地段 ,都有不同尺度的斜卧褶皱发育。
2) reclining isocline
斜卧等斜褶皱
3) recumbent isocline
伏卧等斜褶皱
4) recumbent fold
平卧褶皱
1.
The pattern of paleofold in Xuefeng thrust nappe was near recumbent fold thrusting toward northwest during Caledonian.
加里东期,雪峰推覆体古褶皱样式为向西北推覆的近平卧褶皱构造。
2.
Shape of the orebodies is controlled by large recumbent folds which are developed along foliation S2 in the period S3.
江浪穹隆体的变形变质对早期的矿源层具改造、矿液初步富集作用；构造岩性层控制了李伍铜矿床的产出与分布，Ｓ３期沿Ｓ２面理发育起来的大型平卧褶皱控制了矿体的空间形态，成穹阶段形成的滑脱剪切带是矿液运移的通道，也是找矿的有利场所，该带中次级逆冲断面及ＥＷ向挤压时期形成的Ｓ３面理挠曲是容矿空间，变形与成穹作用双重机制对该矿床构造的形成至关重要。
5) recumbent fold
伏卧褶皱
6) Recumbent fold
卧褶皱
补充资料：叠加褶皱
| 叠加褶皱 superimposed folds 已经褶皱的岩层再次弯曲变形而形成的褶皱。叠加褶皱在造山带十分发育，在变质岩中亦常见。就其形成时间而言，叠加褶皱可以是两个或两个以上构造旋回中的褶皱变形的叠加，也可以是同一构造旋回不同构造幕的褶皱变形的叠加 ，甚至可是同一期递进变形过程中晚期增量应变对早期褶皱的叠加。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条