| 1. | Beijing aotaihua refrigeration and air conditioning equipment company is a domestic leading supplier of professional air conditioning and heat exchange equipment
北京奥太华制冷空调设备有限责任公司是制冷空调换热设备的专业制造企业。 |
| 2. | There are n ' t late paleozoic - mesozoic structural layer in xiaoqinling , so taihua group upheaval area and its bilateral ruptures are critical sectors of investigation
因此，本文研究的重点区段为小秦岭太华群隆升带及其南北两侧断裂带。 |
| 3. | Beijing aotaihua refrigeration and air conditioning equipment company is a domestic leading supplier of professional air conditioning and heat exchange equipment
公司介绍：北京奥太华制冷空调设备有限责任公司是制冷空调换热设备的专业制造企业。 |
| 4. | Beijing aotaihua refrigeration and air conditioning equipment company is a domestic leading supplier of professional air conditioning and heat exchange equipment
公司说明：北京奥太华制冷空调设备有限责任公司是制冷空调换热设备的专业制造企业。 |
| 5. | Conclusion the taihua complex in the area is a metamorphic complex undergone low - angle overthrust from the south to the north and uplifting lately by fault blocking , rather than a mcc
结论小秦岭地区的太华杂岩解释为经历了从南向北的铲状逆冲推覆和后期抬升块断剥露的变质杂岩更为合理。 |
| 6. | From rocks and sediments , we know the region of xiaoqingling is provided with typical two laies model of the earth " s crust , it " s basement is taihua group of primeval , it " s cover rocks is sediment and lava
从地层和岩石上看，小秦岭地区具有典型的地壳双层模式，其基底是太古代太华群，盖层为沉积岩类和火山岩类。 |
| 7. | Methods a contrast is made between the characteristics of typical mcc and the taihua complex in the xiaoqinling based on investigation and analysis of structural evolution of the xiaoqinling
方法总结前人归纳的变质核杂岩特征，与小秦岭地区发育的太华杂岩特征进行对比，再通过对小秦岭地区燕山期后褶皱、南北两侧发育的断裂进行分析和构造演化史研究。 |
| 8. | Completed in 1690 in the qing dynasty , the mansion comprises hills , ponds and pavilions , etc . the antithetical couplets of 180 words written by sun ran , a poet of the qing dynasty are the longest of the kind in china
太华寺始建于元代，由天王殿大雄宝殿缥缈楼一碧万顷阁水树长廊及南北厢房组成。大华寺素以花木繁茂著称，寺内名花荟萃，争奇斗艳，尤以山茶玉兰最有名。 |
| 9. | The first phase involves the formation of thrusting and napping towards nww accompanied by extensive igneous activity and mineralization . the second phase corresponds to the development of asymmetrical small fold downwards north and south . the final phase the cenozoic is marked by strong brittle fractures activity resulting in the sharp heave of the landform of xiaoqinling aera
太华群内的褶皱及南北两侧断裂分析表明，小秦岭燕山期至少经历3期变形，第一期为sse nww向的褶皱变形作用；第2期为南北向正断下滑剪切作用；第3期为脆性正断作用。 |
| 10. | Tectonic analysis controlling gold mine mineralization in taihua group suggest that ductile fractures chang into brittle - ductile ones going with upliftling of xiaoqinling area after in - china orogeny . brittle fractures form on the basis of brittle - ductile ones that develop and inherit the characteristic of the latter stress field . folds and faults analysis in taihua group and its bilateral reveal that yanshanian tectonic evolution of xiaoqinling area undergo at least three phases of deformation
太华群内金矿成矿构造分析表明，印支期碰撞造山后小秦岭挤压抬升，控矿韧性剪切带向脆韧性转化( 207 148ma ) ，在脆韧性剪切带基础上叠加改造形成容矿断裂，脆性断裂的发育继承了韧脆性剪切带发育时的应力场特征。 |
