| 1. | Stratigraphic classification and correlation in es3 of jiuzhou - gu an tectonic belt
固安构造带沙三段地层划分与对比 |
| 2. | The central tectonic belt is complex in strata , reflected by matching up of rock blocks with different ages x lithology and scales
中间构造带地层复杂，层序混乱，表现为不同时代、不同岩性、不同规模的构造块体的相互拼贴。 |
| 3. | Jiangda tectonic belt lies in the north of the three - rivers ( nujiang , lancangjiang , and jinshajiang ) tectonic belt , sw china ; the east of changdu massif ; the west of jinshajiang faults zone
江达构造带地处西南三江构造带北段，昌都地块东缘，金沙江断裂带西侧。 |
| 4. | Tectonic - lithogenic - mineralogenetic epoch and its geologic history evolution indicate that intracontinental rifting stage ( t3 ~ e1 ) is the main metallogenic period of the jiangda tectonic belt
构造-成岩-成矿定年与地史演化研究表明，江达构造带主成矿期为陆内裂谷期。 |
| 5. | The independent jiangda tectonic belt has appeared since late carboniferous , following the jinshajiang ocean crust of subducted beneath the changdu continental crust and the continental margin arc formed in east of changdu terrane
自晚石炭世金沙江洋洋壳开始向昌都陆壳地体边缘下俯冲，形成陆缘弧以来，独立的江达构造带就得以产生。 |
| 6. | The three gorge reservoir , locating at the suture between two arc tectonic belts of daba mountain and bamianshan , has strong structural deformation and versatile structural patterns
摘要通过分析大量资料并结合野外地质工作，对三峡库区的区域构造背景及巴东组的主要构造样式进行了总结，分析了这些地质要素对三峡库区变形斜坡形成和发展的影响。 |
| 7. | They all belong to the calc - alkaline island arc series and are closely related to the evolution of the arc - basin systems of the gangdise tectonic belt . based on studies of petrology , litho - geochemistry , tectonic setting , petrogenesis and magmatic evolution , the present dissertation summarized the general evolutionary regularity of the magmatic rocks in time and space . the magmatic rock assemblages are divided into the inter - arc spreading basin t
在对研究区主要矿产分布特征、成因类型系统分析的基础上，总结了措勤地区构造岩浆演化与成矿的关系，并将研究区成矿系统划分为汇聚大陆边缘成矿巨系统、碰撞造山成矿巨系统和陆内汇聚成矿巨系统。 |
| 8. | Based on an integrated analysis of the surface geological , aeromagnetic , gravity , mt and seismic data from the area of mangnai to serteng mountains in the western qaidam basin , the authors think that the qaidam basin is sandwiched between the north kunlun block and serteng tectonic belt , including two first - order tectonic units the qaidam block and the southern margin of the qilian block and four second - order tectonic units the northern margin of the north kunlun block , qaidam basin , serteng tectonic belt and suhai lake basin in the south of the qilian block
摘要通过柴达木盆地西部茫崖赛什腾山地表地质、航磁、重力、大地电磁测深和地震资料的综合分析，认为柴达木盆地夹持在昆北地块与赛什腾构造带之间，其中包括柴达木地块与祁连地块南缘2个一级构造单元和昆北地体北缘，柴达木盆地，赛什腾构造带和祁连地块南部的苏干湖盆地等4个二级构造单元。 |
| 9. | Zijingguan fault zone is the main structure in taihang mountains that are located in the central part of 20 ~ 30 ne - striking daxing ' anling - taihan - wuling tectonic belt . it is composed of two diagonalized faults that are wulonggou - shanghuangqi fault located in the west and zijingguan - lishan fault in the east
紫荆关断裂带是大兴安岭?太行山?武陵山构造带中段太行山地区的主体构造，总体走向20 30 ，由西侧的乌龙沟?上黄旗断裂和东侧的紫荆关?灵山断裂左阶斜列组成。 |
| 10. | Through the gee stress test of finite points and finite element back - analysis , the paper concludes the geo - stress distribution pattern in different tectonic belt and various lithology strata , which will supply references to mining , design and farther decision making
摘要通过对有限个点的地应力测试，结合已知的工程地质条件，进行有限元反演计算，并对结果进行分析，得到不同构造带应力分布规律和不同岩性地层地应力的变化情况，为煤层开采设计和进一步的决策提供重要的参考依据。 |
