| 1. | The chezhen depression as a fault basin is located in the northeastern part of the bohaiwan basin in shandong
摘要车镇凹陷古近系沙河街组三段上亚段二段下亚段是较为典型的深断陷型三级层序。 |
| 2. | Santanghu basin is a congruent & reconstruct innertief , which developed on the basis of rift - fault basin of permian
三塘湖盆地是一个在二叠纪裂谷-断陷盆地基础上发展起来的叠合、改造型山间盆地。 |
| 3. | Hegang coal field , of the type of a ( inland ) faulted basin far from the sea , was formed in the early neo - jurassic age about 140 million years ago
鹤岗煤田约形成于一亿四千多万年前的晚侏罗世初期，是远海内陆断陷盆地型煤田。 |
| 4. | Lying in the east of heilongjiang province , yishu graben is a cenozoic fault basin comprising two large second - class structural units , i . e . , tangyuan and fangzheng fault basins
摘要依舒地堑位于黑龙江省东部，为新生代断陷盆地，汤原断陷和方正断陷为其两个面积较大的二级构造单元。 |
| 5. | The sedimentary geochemistry analysis indicates that the middle and lower yangtze basin is the craton basin , and shangrao and mingxi basins are the continental margin fault basins in the early triassic
早三叠世的中下扬子混积盆地属克拉通边缘盆地，而上饶和明溪碎屑岩盆地则为大陆边缘断陷盆地。 |
| 6. | Niuxintuo area in liaohe depression is a fault basin , tectonic movement is complex and fault is developed at the basement and at the late stage , where the conditions for creating various hydrocarbon reservoirs are provided
摘要辽河坳陷牛心坨地区为断陷湖盆，基底及后期的构造活动复杂，断层发育，具有形成各类隐蔽油气藏的地质条件。 |
| 7. | In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric , karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
目前开展的可有效利用的地下水资源调查评价将该区划分为隆起带裸露岩溶分布区、沉降带边缘褶皱构造控制岩溶分布区和断陷盆地隐伏岩溶分布区。 |
| 8. | The fault at the east boundary of tangyuan fault basin is a basin - controlling fault , and the faults at both the east and the west boundaries of fangzheng fault basin are also a basin - controlling fault , with the west boundary fault at fangzheng being the major one
断层的生长指数分析表明，依舒地堑内部的北西向断裂与边界断裂的活动具有一致的规律性，都起到协调边界断裂演化发展的作用。 |
| 9. | According to granite ages cutting ruptures , mineralized quartz veins ages corresponding to fold deformation and formation ages of bilateral faulted basin , deformation age are limited , that are 100 ~ 65ma for one and form 65ma to the present for two and three
根据断裂截切的花岗岩体年龄、同期褶皱变形的含矿石英脉年龄以及断裂两侧断陷盆地的形成时代，大致限定第1期变形时代为100 65ma ，第2 、 3期变形时代为65ma现今。 |
| 10. | Compared with lehua manganese deposit in pingxiang - leping faulted basin , which is a sedimentary hydrothermal superimposed type , both orebodies are different obviously in orebody scale , ore type and tenor of manganese etc . , it should be a deposit with different genetic type
并与萍一乐断陷盆地内的沉积加热液叠改型乐华锰矿床进行了对比分析，二者在矿体规模、矿石类型、锰品位等方面存在显著差别，应属不同成因类型的矿床。 |
