| 1. | Features of nappes in nanpoyang depression
南鄱阳坳陷推覆构造特征 |
| 2. | The characteristics and genesis of cleavage in daqingshan thrust
大青山逆冲推覆构造带中劈理特征及其成因 |
| 3. | Characteristic of converse nappe structure and meaning of search for coal in yima coalfield
义马煤田逆冲推覆构造特征及找煤意义 |
| 4. | The determination of cenozoic nappe structures of diancang mts and their geological significance
点苍山新生代推覆构造的确立及其地质意义 |
| 5. | Salt tectonic evolution and hydrocarbon accumulation of kuqa foreland fold belt , tarim basin , nw china
库车前陆褶皱-冲断带前缘大型盐推覆构造。 |
| 6. | Indosinian nappe structure and its hydrocarbon significance in hefei basin and north huaiyang tectonic zone
合肥盆地与北淮阳构造带印支期的推覆构造及其油气意义 |
| 7. | The formation of the nappe led to sinking of qaidam massif , nappe thrusting basin depositing persistently and the sedimentary center changed
推覆构造的形成，导致柴达木地块下沉，推覆体持续逆冲盆地持续沉积，沉积中心也变更。 |
| 8. | 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。 |
| 9. | The nappe structures made the faultage in this area developed . the faultage is along or close to meridional direction , and it offered favorable conditions for the formation of the mineralizing fluid
推覆构造使得该区断裂、断层发育，主要以南北向或近南北向断裂为主，断裂带的发育为流体的形成提供了有利的条件。 |
| 10. | The pre - jurassic basement of hefei basin was composed of thrusts . indosinian foreland thrusts in pre - jurassic bedrocks of the basin increase towards the tan - lu fault zone , indicating indosinian activity of the fault zone
合肥盆地在印支期的前侏罗纪基底主要表现为大别造山带前陆逆冲推覆构造，由一系列逆冲断层和逆冲岩片所组成。 |
