thrust nappe meaning in Chinese
冲断推覆体
逆冲推覆体
Examples
- Features and genetic mechanism of thrust nappe and sliding nappe structures in the xiajiang area , central jiangxi
赣中峡江地区推滑覆构造特征及成因机制 - The present thrust nappe structure formed in late jurassic according to comprehensive analysis of sedimentary , structure and fission track tesing result
据沉积、构造和裂变径迹测试结果综合分析认为，现今所见的贺兰山逆冲推覆构造形成于晚侏罗世。 - Hengshanbu part have three secondary parts which are tiekesumiao , eastern taole and south of selunkademiao . the zhouzishan part of is charactered by thrust nappe which is composed by faults thrust from west to east , anticlines and synclines , involving much of proterzoic , palozoic and very limited mesozoic in which a suite of conglomerate is found in the front of thrust fractures in late - jurassic
桌子山段以发育一系列由西向东逆冲的断裂和背向斜组成的推覆体系为特点，卷入地层多为元古界-古生界，中生界分布有限，其中晚侏罗世地层在逆冲断裂前缘普遍见一套砾岩，故推测该段逆冲构造形成于晚侏罗世。 - It is concluded that non - structural reservoirs will be major types of prospecting ; the slope belts with high swells are of conditions for forming large - scale stratigraphic reservoirs ; in complex piedmont thrust nappe there are many targets and high potentials for exploration ; jundong ( eastern junggar ) area and around wulungu depression are not " dead areas of hydrocarbon generation " , they should be regarded as favorable backup positions of prospecting
非构造油气藏将是下步主要的油藏勘探类型，高凸起的斜坡带具备形成大型地层油气藏的有利条件，复杂山前逆冲推覆构造带勘探目标多、潜力大，环乌伦古坳陷及?东地区并非“生烃死亡区” ，也是有利的后备勘探阵地。 - The gangue minerals are mostly carbonating minerals , fluorite , barite , celestite and so on ; the rock alteration is slightly silicified , carbonated , baritizated , celestited , which is low - temperature alteration . because of continual downgoing extrusion from india plate to euro - asian plate , there are some thrusting nappe structures in lanping basin related to the orogens on the two sides
矿床中矿石矿物发育典型的中低温热液成因的矿物组合，如黝铜矿系列、方铅矿、黄铜矿等，脉石矿物主要为碳酸盐类矿物、萤石、重晶石、天青石等；围岩蚀变主要发育弱硅化、碳酸盐化、重晶石化、天青石化等低温蚀变组合。