| 1. | Kuqa basin ; north thrust belt ; gas source ; baicheng sag
库车盆地北部冲断带气源拜城凹陷 |
| 2. | Deformation characteristics and time of cenozoic thrust belt in southern margin of jiuquan basin
酒泉盆地南缘新生代冲断带的变形特征和变形时间 |
| 3. | Structure geological evidences on natural gas origin in the north thrust belt of kuqa basin , northwestern china
库车盆地北部冲断带气源的构造地质学证据 |
| 4. | Structure geological evidences on natural gas origin in the north thrust belt of kuqa basin , northwestern china
库车盆地北部冲断带气源的构造地质学证据 |
| 5. | Fans sedimentation and exploration direction of fan hydrocarbon reservoirs in foreland thrust belt of the northwestern junggar basin
准噶尔盆地西北缘扇体形成演化与扇体油气藏勘探 |
| 6. | Buried rift basins under the thin - skinned fold - thrust belts in the south segment of the western sichuan foreland basin and their geological significance
川西前陆盆地南段薄皮冲断构造之下隐伏裂谷盆地及其油气地质意义 |
| 7. | Wuxia fault belt in the eastern part of northwestern margin of junggar basin is an important part in the thrust belt of the northwestern margin
摘要乌夏断裂带位于准噶尔盆地西北缘的东部，是西北缘冲断带的一个重要组成部分。 |
| 8. | The present longmenshan foreland basin lies between the longmenshan thrust belt and the longquanshan fault . the dayi conglomerate at the bottom of the chengdu basin , although people of the past having studied a certain degree , hasn " t same sugest
大邑砾岩的地质时限为上新世-早更新世，时代界定在4 . 6ma - 0 . 82ma之间，显示该区第三纪与第四纪之间是连续沉积的，其间不存在构造事件。 |
| 9. | Firstly , based on the basin prototype , the triassic and jurassic mudstone and coal , the main source rocks of the basin , did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly , because of the thrusting happened in late cenozoic , the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly . thirdly , the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow . as a result , the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas , but also developed simultaneously when the gas migration happened
从盆地构造史研究的角度认为库车盆地的天然气主要来源于北部山前冲断带： 1受原型盆地构造格局的制约，三叠系侏罗系烃源岩发育的最有利位置不是在拜城凹陷，而是在克依构造带及其以北的北部山前冲断带2晚第三纪以来的逆冲推覆作用使得烃源岩提早进入高过成熟阶段，并以产气和凝析油为主3逆冲推覆作用所产生的北倾逆断层控制天然气自下而上自北而南运移，位于运移路线上的克依构造带和秋里塔格构造带的东段与烃源岩的排气期匹配较好，从而使这些地区最富集天然气。 |
| 10. | In the process of same one regional stress field , the tectonic evolution and oil and gas geologic condition of kuqa foreland thrusting belt and the southern margin of junggar basin all show much similar characteristics , both of them developed multi - set mature source rocks , and formed multi - set high - quality reservoir - cover combinations , and developed various traps
天山造山带的形成与演化对于其两侧盆地的展布、基底性质、沉积盖层的规模、盆地整体结构特征、后期破坏等具有重要的影响和控制作用。 |
