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1)  brink sag
边缘凹陷
1.
In the process of rift-subsidence evolvement,some fault-blocks succession rift and subside for a long period,becoming the host sags of the primary oil source center,and the others show the less range of subsidence or strong denudation,becoming the brink sags,all these just because of the difference in structu.
根据成因和所起的构造作用,可以将边缘凹陷分为4种类型,即废弃型、调节型、过渡型和改造型。
2)  hollow of infraorbital margin
眶下缘凹陷
1.
Methods To release fat in orbital septum with lower pouches taxis operation through skin and lower pouches taxis operation through conjunctiva, and to sew up and fix and fill the hollow of infraorbital margin.
方法:经皮肤入路下睑袋整复术与经结膜入路下睑袋整复术中释放眶隔内脂肪,缝合固定填充眶下缘凹陷区。
2.
Objective To discusses the influence with the lower pouches taxis operation to the entire shape of lower eyelid,by moving ocular orbicularis under lower eyelid downwards to rehabilitate the hollow of infraorbital margin.
方法经皮肤入路下睑袋整复术中在去除眶内多余脂肪同时,在眶下缘处剪开并分离眼轮匝肌形成扇形肌瓣,缝合固定填充眶下缘凹陷区。
3)  well base rim
凹陷式轮缘
4)  collapsing of the edges
边缘塌陷
5)  marginal depression
边缘坳陷
1.
According to the viewpoint,suggestions are made that C-subduction belt is between old folded mountains and inland basin marginal depressions in geotectonic location;in the early stage,it belongs to normal faults followed by.
这一观点认为,C-俯冲带在大地构造位置上处于古老褶皱山系与内陆盆地边缘坳陷之间;C-俯冲带早期为正断层,后期转化为逆断层,成为盆地坳陷边缘主动向山系潜滑的俯冲断层;C-俯冲带有着良好的成油条件,在逆冲带形成早期往往发育着较厚海相和海陆过渡相沉积,后期形成前渊盆地,在中、新生代可形成良好的湖相成油环境;青藏高原的崛起除了与新生代印度板块与欧亚板块发生碰撞有关外,还与龙门山C-俯冲活动有关;C-俯冲不仅在中国中西部存在,也存在于中国的东部地区,C-俯冲观点的提出,丰富、完善了板块学说关于中、新生代造山带形成的模式,是中国地学工作者在大陆构造理论上的创新。
6)  marginal subsidence
边缘沉陷
补充资料:凹陷骨折


凹陷骨折
depressed fracture

为致伤物直接冲击颅盖骨所致,由间接暴力沿脊柱上传造成枕骨大孔区环形凹陷骨折少见。它占颅盖骨折的1/3,多发于颞部,其次为额部和顶部。骨折的尖端常刺破硬膜和损伤脑实质,造成局限性脑挫裂伤和各种颅内血肿及外伤性癫痫。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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