1) gliding structural system
滑动构造系
2) gliding tectonics
滑动构造
1.
21 coal seam and its roof,floor sandstones as focal point,have found that the whole minefield is a large sized gliding tectonics,analyzed its forming terms.
以大峪沟井田构造、二_1煤层及其顶、底板砂岩为研究重点,发现整个井田为一大型滑动构造,并分析了该滑动构造的形成条件,指出了滑动构造对煤层赋存的影响规律,为今后类似井田的勘查和开发提供了参考。
2.
The gliding tectonics is always formed in rather soft strata.
滑动构造总是在较软弱的地层中形成。
3.
The Ludian gliding tectonics is a typical model in gliding tectonics group in the Songshan-Jishan area,western Henan Province.
芦店滑动构造是河南省西部嵩(山)箕(山)地区滑动构造群中的一个典型实例。
3) gliding structure
滑动构造
1.
Tectonic control on gas geological hazard in Ludian gliding structure;
豫西芦店滑动构造区瓦斯地质灾害的构造控制作用
2.
The mechanism of gliding structure and its control on coal measures,coal seam and gas deposit are researched based on the theory of plate structure and the region tectonic evolvement,collation data systematically about coalfield geological prospecting and plenty of gas geological data that mine disclosed.
地质构造是煤与瓦斯突出的控制因素,豫西煤田中滑动构造普遍发育。
3.
The basic characteristics of gravitation gliding structure are multi layer,multi period,small scale,multi form.
肥城矿区内重力滑动构造的基本特点是具有多层次性、多期性、小规模性和形式多样性。
4) sliding structure
滑动构造
1.
Based on volcanic activities and tectonic evolution,it is suggested that the tilted fault block,sliding structures in extensional setting should be developed in Cretaceous to Cenozoic age.
结合区域火山活动和构造演化认为,该滑动构造为伸展背景下的掀斜断块型,其滑动时间为白垩纪—新生代。
2.
Basic characteristics of sliding structure of Feicheng coal field is summarized.
总结了肥城煤田滑动构造的基本特征，深入地研究了滑动构造与矿井水害之间的关系。
3.
The paper studies systematically the characteristics of Daping-Chaohua sliding structure in its boundary structure, sliding pattern, mechanical property, sliding system, underlying system and direction of movement,etc.
本文从边界构造、滑动形态特征与力学性质、滑动系统、下伏系统、运动方向等方面 ,系统地分析研究了新密大平—超化滑动构造的总体特征。
5) slip structure
滑动构造
1.
The geological structures are always highangle positive fault Xinmi coalfield always growth slip structure and between stratum slip structure,moreover resultingly between stratum slip structure have no lose of stratum,so they cannot always be found,it gravence influence coal mine building.
新密煤田是河南省的主要产煤地之一 ,其地质构造多以高角度的正断层为主 ,新密煤田还发育滑动构造和层间滑动构造 ,而层间滑动构造由于没有造成明显的地层缺失 ,在地质勘探过程中不易被发现 ,对煤矿生产建设影响较大。
6) tectonic sliding
构造滑动
补充资料：华夏系构造
简称“华夏系”。主要是由走向东北的褶皱、压性和扭压性断裂带构成。在中国东部和东南部相当发育。
形成时代比新华夏系早，约在古生代晚期。
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