With the guide of interaction between NS and NWW fault structure. Nianbaoyuze granite mass intruded into Triassic sand rock whose depth is over 9136m.
在南北向及北西西向断裂构造的交互作用引导下，年保玉则花岗岩侵入体侵入厚度达9136m以上的三迭系砂板岩内。
The results of this paper show:(1) The Upper Triassic Sanhedong Formation deposited in limited carbonate platform sedimentary environment of shallow marine; the temperature of paleo-sea water is mainly from 26.7℃～32.1℃, which indicates Lanping Basin located in the hot tropics during formation of the Upper Triassic Sanhedong Formation.(2) The provenance tectonic setting of sedimentary rocks from the Lanping Basin are represented by passive continental margin and continental island arc and the original source rocks were all derived from the upper continental crust, with felsic rocks dominant. So the Lanping Basin is a typical continental-type basin.(3) The evolution of Lanping Basin have undergone three different prototype basins'evolution, i. e. rift basin, depression basin and strike basin.(4) Ore-forming materials of deposits in large ore-assembly district were derived from crust (mainly from basement and stratum of basin ore-forming fluids were hot brine of basin dominant and the organic matter from source rocks of basin stratum has involved in mineralization; and mineralization epoch of deposits was about 56Ma or 30Ma, which are compatible with the times of collision of Indian plate and Eurasian plate and late strong compression stage respectively.
研究结果表明：上三叠统三合洞组的沉积环境属浅海局限台地相，沉积时古海水的温度介于26.7℃～32.1℃，反映上三叠统三合洞组沉积时兰坪盆地处于炎热的热带区；盆地沉积岩源区构造属被动大陆边缘环境和大陆岛弧环境，原始物源来自上地壳，以长英质岩石为主，兰坪中新生代盆地属典型的大陆型盆地；盆地演化经历了三个原型盆地即裂陷盆地、坳陷盆地和走滑盆地的演化过程，三个原型盆地的形成和演化明显受特提斯洋演化和印度板块与欧亚板块碰撞作用的制约；矿集区内矿床的成矿物质源自地壳、成矿流体为盆地热卤水；源自盆地生油岩地层的有机质参与了成矿作用；矿集区矿床形成时间为56Ma左右或30Ma左右，两时间分别与印度板块和欧亚板块发生碰撞和后续的强烈挤压阶段的时间相一致；中新生代兰坪盆地演化过程也是多金属大型矿集区形成的过程。
This paper analyzes the controlling factors:(1) The fault occurrence in different eras have different effects on the oil and gas accumulation; (2) Unconformity surfaces are usually major hydrocarbon migration channels and the belts of hydrocarbon accumulation; (3) The Triassic fan delta faceis and the alluvial fan facies are favorable reservoir blocks in this region; and (4) The Triassic oil reservoirs in the Wuerhe|Xiazijie area possess multiple reservoir|seal assemblages, and the Karamay Formation and the Baijiantan Formation are major regional cap rocks.
对该区控制油气成藏的各种因素进行了综合分析，指出：断裂在不同时期对油气的聚集具有不同的控制作用；地层不整合面往往成为油气运移的重要通道和油藏聚集成藏带；三叠系扇三角洲相和冲积扇相是该区有利储集体发育的主要沉积相带；乌夏地区三叠系油藏具有多套储盖组合，三叠系克拉玛依组和白碱滩组是主要的区域盖层；三叠系油藏大都为发育在鼻隆构造背景上的岩性地层油藏，这种受构造背景控制的岩性地层油气藏是该地区三叠系油气的主要成藏模式。
The underground cavities mainly include three large cavities. In the area of the left bank, rock body is mainly composed of Permian Period-Triassic Period granite and Triassic Period siltstones and mudstones (T2m). Moreover, the rock body has been more faulted, such as F1 F3 F9 and so on. In addition, there also exist a lot of joints and form complex rock mass structure.
工程区主要出露二迭纪～三迭纪花岗岩体(γ_4~3～γ_5~1)和三迭系中统忙怀组下段沉积岩T_(2m~1，发育有工程区规模最大的F_1和F_3断层，以及其它断层和大量的各类断续延伸的裂隙，岩体结构较为复杂。
The grey green illite detritus with goethite rust stain are found at the boundary clay, Permian/Triassic boundary section in Yianshi, Longyan, Fujiang and Yegang, Huangshi, Hubei.
在福建龙岩雁石和湖北黄石冶钢二叠、三叠系界线地层中发现一种灰绿色带针铁矿锈斑的伊利石碎屑。
The main natural landscape are: Songlian feng show, Ye Xia Autumn, sleeping Buddha, Stone Forest YJ, Triassic Falls, ye sea-ice maps, lin hai xue yuan, hi Stephen thomsonae, Tung tree god, five turquoise, flying stones, Kim Stone, Stone Toad, Eagle Cliff, sister-feng, Taiwan Kikunami, whiteshi xue feng, turtles drink-money, there are very rare form of wheat Danxia plot sunset, four ping-feng, Chibi valleys, monks and other odd laugh Stone wonders of up to 270 extra Department.
主要的自然景观有：莲峰耸秀、冶峡秋色，睡佛、鹰击石林、三叠瀑布、冶海冰图、林海雪原、喜泉吐珠、通天神树、五松石、飞来石、金钟石、蛤蟆石、飞鹰崖、姊妹峰、听涛台、白石雪峰、神龟清饮，还有极为罕见的丹霞地貌形成的麦积晚霞、四屏峰、赤壁幽谷、笑和尚等奇石奇景，多达270多余处。
The Triassic Period or its system of deposits.
三叠纪，三叠系地质年代中的三叠纪或沉积矿床的系
Later of Yanshan movement is main period of oil-gas migration and congregation, it is also main period of coalification in Permo-Carboniferous system ^ Triassic system and Jurassic system.
燕山晚期是盆地油气运移和聚集的主要时期，也是石炭—二叠系、三叠系及侏罗系的煤化作用的主要时期。
Application of completion tech for branch well in 9 district Triassic system of Tahe oilfield provides a new manner for development of multilayer system in different districts and meanwhile, decreases exploiting investment.
塔河油田9区三叠系分支井完井工艺技术的应用，为塔河油田不同区块多层系的高效开发，提供了新的途径和手段，同时也降低了开发投入。
The recognition of the two superimposed fold generations in South China is key to understanding the change from the Triassic continentcontinent collisionrelated tectonic system to the MiddleLate Jurassic subductionrelated tectonic system.
华南两组叠加褶皱构造的识别为进一步探讨早中生代从碰撞动力构造体系向俯冲动力构造体系转换提供了关键的构造地质学依据。
Furthermore we can set up the sequence of strata of yijianfang. Then use diagenies sequences and fluorescence analysis to seek after the mechanism of formation. At last, By researching controlled factors of reservoir and contrasting with pore-reservoir jialingjiang group Triassic System in Sichuan basin, we make evaluation to quality of reservoir.
以高频层序地层格架的建立为基础，通过成岩作用序列的建立以及地球化学手段相结合，探索了礁滩相储层的形成机制；进而，通过物性变化特征与储层控制因素研究，并结合四川盆地三叠系嘉陵江组孔隙型碳酸盐岩储层进行对比分析，进行储层质量预测评价。
There is gigantic thick land facies clastic rock layer about Jurassic system and Upper Triassic in the sunken of Chuan-xi.
钻井地质特征描述包括地层岩性、岩石力学参数、可钻性、研磨性和地应力及三地层压力体系等。
However, the Pre-Sinian system, the Cambrian system, the Ordovician system, the Triassic system, the Jurassic system and the Cretaceous system slow down the formation of high Cd value belt.
区内锌矿、煤矿和磷矿开采过程中的尾砂、废水的堆积和排放是长江宜昌段Cd高值带的重要人为污染源。
The age distribution change of detrital zircons from the sediment formed in different periods also indicates that more substances from Yangtze block entered Songpan Garze Basin from the middle period of Late Triassic, so the composition of sediment must have been altered obviously. Also the evolution of the basin sediment provenance implies that a rapid elevation of West Yangtze block occurred after the middle period of Late Triassic.
由不同时期沉积物中碎屑锆石年龄分布特征的变化表明：晚三迭世中期以后有更多扬子板块的物质进入了松潘－甘孜盆地，使盆地内沉积物的组合发生了明显的改变，这样的变化反映了晚三迭世中期以后扬子板块西缘存在一个快速抬升的过程。
Mainly occurs in the middle and lower Triassic strata, in order to sedimentary deposits.
主要赋存于中下三叠统地层中，为沉积型矿床。
The activity of Pacific Ocean tectonics range has influence on the basin more and more obviously, but Lishi fault activity and control action to Ordos basin is still not obvious in late Triassic and early-middle Jurassic, its activity should be most severe in late Jurassic from the point of view of formation and magmatite.
晚三叠世和早、中侏罗世滨太平洋构造域的活动对盆地的作用日益明显，但离石断裂带的活动和对盆地沉积的控制作用仍然不十分明显。
Indosinian movement refers to the orogenic movement during Late Triassic to Early Jurassic, it is another major epoch-making evolution in Qinghai-Tibet region.
印支运动是指发生于晚三叠世—早侏罗世阶段的造山运动，是青藏地区又一次有划时代意义的重大变革。
The first primitive dinosaurs appeared in the early Triassic period, about 230 million years ago.
最初的原始恐龙出现在三叠纪早期，大约是2亿3千万年前。
But what exactly happened towards the end of the Triassic has been much debated.
但是，在即将进入三叠纪晚期时，究竟又发生了什么令恐龙崛起，一直备受争议。
Based on the geologic background of Jia 2 Member in Jialingjiang Formation of the lower Triassic in Sichuan Basin, the li- thology, sedimentary structures, sedimentary rhyme, palaeoelimate and diagenetic evolution were analyzed.
结合四川盆地下三叠统嘉陵江组区域地质背景资料，对磨溪嘉二段的岩石类型组合、沉积构造、沉积韵律、古气候及成岩演化等沉积相标志的详细分析表明，嘉二段并非普遍发育潮坪环境，而是属于陆表海型碳酸盐岩局限—蒸发海台地相沉积，并可进一步划分为台坪、粒屑滩、滩间海、局限泻湖、蒸发泻湖5种亚相及20余种微相，类潮坪相仅出现在嘉二~2B层沉积期。