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- Longmen Shan structure zone 龙门山构造带
- Millimetre by millimetre, the Longmen Shan are being sliced and displaced much like salami. 不同于喜马拉雅山脉，西藏与其断层的震颤，伴随持续不断的小规模地震，形成了其南部的边界。
- The recent earthquake in Sichuan occurred under some of the steepest and most rugged mountains in the world, the Longmen Shan: the Dragon's Gate Mountains. 最近在四川发生的地震就发生在在世界上一些最险峻陡峭、最崎岖蜿蜒的山脉，龙门山即龙之门山。
- The shear zone is a secondary structure zone of the syn-collision stage of Southern Tarim block with Ili-Isaik block. 该剪切带属南侧塔里木与伊犁－伊塞克两陆块碰撞缝合构造同碰撞期的次级构造带。
- GEOMORPHIC AND SEDIMENTARY EVIDENCE FOR REVERSION OF STRIKE-SLIP DIRECTION IN LONGMEN SHAN FAULT ZONE 龙门山断裂带走滑方向的反转及其沉积与地貌标志
- The Yinggehai basin is characterized by high thermal gradients and overpressure.The diapir structure zone contains rich resources of oil and gas. 莺歌海盆地是中国近海最重要的天然气探区之一,具有超高温及异常高压的独特地质条件,中央坳陷形成了众多巨型泥底辟构造。
- The deposit is located at Qimantage back-arc rift structure zone, and hosted within Tieshidasi group volcanic rocks of upper Ordovician. 肯德可克钴铋金矿床是近几年来在东昆仑地区发现的重要钴多金属矿床类型。
- Several sections of Longtan Formation within Baishi Goujia klippe in the middle south section of Longmenshan structure zone are described. 详细描述了龙门山构造带中南段白石-苟家大型飞来峰多条龙潭组地层剖面,讨论了龙潭组的岩石组合特征及其横向变化规律。
- Duhuangling gold deposits occurred in the quartz diorite(porphyry)of Late Yanshan Epoch,the deposits are directiy controlled by EW trending fault structure zone. 杜荒岭金矿赋存于燕山晚期的石英闪长(斑)岩中,严格受近EW向断裂构造带控制。
- Lianmuqin Formation of Cretaceous,Shengbei structure zone of Shengbei Sag,Turban-Harmy basin,belongs to typical fan-deltaic front sedimentary system of north sediment source. 吐哈盆地胜北洼陷胜北构造带白垩系连木沁组属于典型的北物源扇三角洲前缘沉积体系,其砂体埋藏深度较浅,储层物性较好,向北上倾尖灭型岩性圈闭发育。
- The shear zone extends eastward to Irenharbirga and is cut by "Tianshan Main Structure zone", and goes westward via Adengbulake gorge of northern Muzart river valley to Ala-Aiger pass, then connects with "Nigulaev line". 剪切带向东至伊连哈比尔孕山被“天山主干断裂”截断，向西经北木札尔特河谷的阿登布拉克沟在国境附近的阿拉爱格尔山口附近与邻国“尼古拉耶夫线”相接。
- Sedimentary Responses to Late Cenozoic Thrusting and Strike-slipping of Longmen Shan along Eastern Margin of Tibetan Plateau 青藏高原东缘龙门山晚新生代走滑挤压作用的沉积响应
- The Wulashan gold-bearing ore veins are located in late Archean Wulashan group high grade metamorphic area (mainly at amphibolite facies, even to granulite facies),and controled by Wulashan fault structure zone. 乌拉山含金矿脉赋存于晚太古界乌拉山群高级变质岩区（变质程度以角闪岩相为主，可达麻粒岩相），受控于乌拉山断裂构造带。
- From inside out-wards the arcuate structure can be divided intofour nappe structure zones and each zone con-trols coalfield prediction area. 弧形构造由内向外可划分为4个推覆构造带,每个带都是一个煤田预测区,它有益于在该区寻找新的煤田。
- Li Tianbin.The feature and formation mechanism of arciform thrust-nappe structure zone of the southern Ningxia[J].Journal of Geomechanics,1999,5(3):22-27(in Chinese with English abstract). [19]李天斌.;宁夏南部弧形推覆构造带特征及演化[J]
- U nderground water consists of Quaternary pore water, bedrock fissure water and ve in fissure water in structure zones. 矿区地下水类型有第四系孔隙水、基岩裂隙水和构造带脉状裂隙水等三类。
- The Qinjiatun reverse structural zone is a tine ridge anticline developed above the e... 这些反转构造发育在深层生烃凹陷附近,生、运、聚、储的配置关系极佳,是重要的油气圈闭。
- Longmen Shan Faults 龙门山断裂
- The Kuco-Gamba Basin in the southern Tibet is located in the northern Himalayas structural zone, and is distributed in an east-west direction. 摘要西藏古错-岗巴盆地呈东西向展布，位于北喜马拉雅构造分区。
- Longmen Shan fault belt 龙门山断裂带
