triassic

triassic

1. The BS basin is a Tertiary sedimentrary basin occurred on Ordovician,Silurian Carboniferous and Triassic basement strata.

BS盆地是发育在奥陶纪、志留纪、石炭纪及三叠纪基底地层之上的第三纪沉积盆地。

2. YANG Xiao-ping,QIU Yi-nan.Formation process and distribution of laumontite in Yanchang Formation (Upper Triassic)of Ordos Basin[J].Acta Sedimentologica Sinica,2002,20(4):628-632.

[2]杨晓萍,裘怿楠.鄂尔多斯盆地上三叠统延长组浊沸石的形成机理、分布规律与油气关系[J].沉积学报,2002,20(4):628-632.

3. Chen Liezu.Early Triassic Ichthyosauria fossils from Chaoxian county, Anhui.Regional Geology of China, 1985, (15): 139-146.

[6]陈烈祖. 安徽巢县早三叠世鱼龙化石. 中国区域地质,第15辑, 1985, 139-146.

4. Triassic is the principal reservoir and production horizon in Akekulei region of NortheasternTarim Basin.

三叠系是塔东北阿克库勒地区的主要储产层系，砂体发育，分布广泛。

5. The Triassic coelurosaur dinosaurs were small, nimble and built to survive in the harsh Triassic landscape.

三叠纪时期的恐龙体型都比较小，动作敏捷，能够在荒芜的三叠纪中生存。

6. At the end of Triassic period, the marine sedimentation on Qaidam Massif (including its surroundings) has ended, and interior basin started to develop in Qaidam area.

三叠纪末的印支运动结束了柴达木地块及其周缘地区的海相沉积史，使柴达木地区进入陆内盆地发育新时期。

7. Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental-island arc collusion stage after the close of Paleo-Tethys ocean.

三叠纪沉积盆地建立在晚古生代褶皱基底之上,形成于古特提斯洋闭合后,造山早期的弧陆碰撞阶段。

8. Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental island arc colliusion stage after the close of Paleo Tethys ocean.

三叠纪沉积盆地建立在晚古生代褶皱基底之上，形成了古特提斯洋闭合后，造山早期的弧陆碰撞阶段。

9. 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

10. In Triassic and Lower-Middle Jurassic, there is the acid diagenetic ambient, where inter-pore fluid is from the organic acid released from the coal measures during diagenesis.

三迭系至中下侏罗纪煤系为酸性成岩环境，它们在成岩过程中释放的有机酸使隙间流体呈酸性。

11. Donglan gold ore deposit has been found in interstratified fractured silicic alteration belt within flych sedimentary formation of lower Banna formation of midle Triassic.

东兰金矿产于中三叠世早期板纳组复理石沉积建造层间破碎硅化蚀变带中。

12. As a Mesozoic and Cenozoic superposed basin on a cratonic basement,East China Sea shelf basin has three periods of tectonic evolution:Late Triassic(?

东海陆架盆地为发育于克拉通基底之上的中、新生代叠合盆地,该盆地经历了晚三叠世(?

13. The Triassic of the Central European basin represents a typical marine influenced terrigenous sequence.

中欧盆地三叠系是典型的海陆过渡相沉积,松辽盆地白垩系是含有海侵事件记录的陆相河湖盆地。

14. And the main reservoirs include Cambrian sandstones, Ordovician sandstones and Triassic sandstones.Thick marls, dolomite, anhydrite and rock salt are excellent regional seals.

主要储层包括寒武系、奥陶系和三叠系砂岩，区域良好盖层是巨厚的泥灰岩、白云岩、硬石膏和岩盐。

15. As for the main reservoir-caprock assemblage , the Carboniferous volcanic rock is the reservoir while the Permian and Triassic mudstone is the cap rock.

主要的储盖组合是以石炭系火山岩为储层,二叠系和三叠系泥岩为盖层。

16. It is mainly distributed in the fourth part of the Beisi Formation of the lower Triassic, exhibiting tidal flat characteristics and located between the underlying HST and the upper TST.

主要见于下三叠统北泗组第四段，具潮坪特点，层序上处于下伏的HST和上覆的TST之间。

17. Wu-Xia fault belt is a large-scale overthrust belt developed from Late Carboniferous to Triassic and faults mostly develop below the Triassic.

乌尔禾-夏子街断裂带是一个晚石炭世至三叠纪发育起来的大型逆掩断裂带,断层主要发育在三叠系以下层位,侏罗系以上近于单斜形态。

18. The supercontinent of Pangea, mostly assembled by the Triassic, allowed land animals to migrate from the South Pole to the North Pole.

二亿三千七百万年前：三叠纪末，泛大陆开始裂解、分离大部分在三叠纪拼合而成的泛大陆，使得陆地动物可以从南极到北极迁徙。

19. From Permian to Triassic, the development of the contemporaneous thrust faults is piggyback propagation, and it is overstep propagation from Triassic to Jurassic.

二叠纪到三叠纪断裂发育为前展式，三叠纪到侏罗纪断裂发育为后展式。

20. The West Tianhan Orogen may undergo a post-collisional collapse since Permian.And the magmatic activities may continu to early Triassic.

二叠纪开始西天山地区处于后碰撞造山阶段，该阶段的岩浆活动可能一直持续到早三叠纪。

21. Late Permian to Triassic rifting and subsidence resulted in the deposition of as much as 9 kilometers of Triassic strata, locally injected with sills.

二叠纪晚期到三叠纪断裂和下沉作用形成了大约9千米厚的第三纪沉积地层，在其中有岩床的切入。

22. From the Early Triassic to Late Tiassic,the depocenter and subsidence center moved southward progressively,while the frontal uplift retreated toward the foreland continually.

从早三叠世到晚三叠世， 盆地的沉积和沉降中心持续南迁，前缘隆起则持续向前陆方向后退。

23. Era A unit of the geological time scale that is made up of several periods, e.g. the Mesozoic Era comprises the Triassic, Jurassic, and Cretaceous periods.

代：量度地质时期的分类单位，代由若干时期组成，如中生代包括三叠纪、侏罗纪和白垩纪。

24. A terrestrial Triassic chronostratigraphical system based upon tetrapods has been suggested and to be improved in application.

以脊椎动物为基础的陆相三叠纪年代地层划分方案有待在推广应用中得以完善。

25. Based on the sandstone compositions analysis of the Upper Triassic Xujiahe Formation in Western Sichuan Basin,the authors tried to discuss the paleogeographic evolution of the study area.

作者单位：成都理工大学“油气藏地质与开发工程”国家重点实验室沉积地质研究院;

26. Early Triassic Daye Group and Middle-late Triassic Puqi Group are host rocks of Fe-Cu deposits in the eastern Hubai.

侵入接触带构造,捕虏体接触带构造,断裂叠加接触带构造,断裂构造是矿床的容矿构造。

27. Six geological formations in the parks contain fossils of a wide range of ancestors of mammals, dinosaurs and plants revealing the evolution of vertebrates and the nature of palaeo-environments in the Triassic Period.

公园含有六个不同的地质层，化石囊括了哺乳动物祖先、恐龙、到植物等广阔物种，反映了脊椎动物的进化过程以及三叠纪时期的地球古环境。

28. Triassic ammonites,fossil plants and radiolaria occurred in normal sedimentary micritic limestone,detrital rock and silica rock and represented the sediment age of the Bayankelashan Group.

其中三叠纪的菊石、古植物、放射虫等标准化石分子产于正常沉积的泥晶灰岩、碎屑岩、硅质岩等岩层中,代表巴颜喀拉山群的沉积时代,且在纵向与横向上控制程度高。

29. Their formation time was not later than Early Carboniferous (C 1), and the emplacement took place before the formation of Late Triassic Yiwanshui Formation (T 3 y ).

其形成时代不晚于早石炭世（C1），侵位在晚三叠世一碗水组（T3y）之前。

30. Life in the late theropod Triassic cretaceous.

兽脚类生活在晚三叠纪至白垩纪。

31. There are large areal clastic reservoirs in the Permian,Triassic and Jurassic in eastern part of southern margin of Junggar basin.

准噶尔盆地南缘东段二叠系、三叠系以及侏罗系大面积分布碎屑岩储集层,其沉积环境多变,非均质性明显。

32. Formation factors and mechanism of the laumontite in upper Triassic Yanchang group of Jingan oilfield are analyzed.

分析了靖安油田上三叠系延长统浊沸石的形成条件及形成机理。

33. Lichuan synclinorium from Silurian System to Triassic System has 7 combinations of oil source rock, reservoir and cap rock .

利川复向斜从志留系-三叠系具有7个生储盖组合。

34. The synthetic sloughing mechanism of coal beds in Jurassic and Triassic systems of Tarim Basin was studied by using chemical analysis and mechanical methods.

利用化学分析和力学研究,探讨了塔里木盆地依奇克里克区块侏罗系和三叠系煤层的坍塌机理。

35. The synthetic sloughing mechanism of coalbed in the Jurassic and Triassic systems was studied by chemical analysis and mechanical methods.

利用化学分析和力学研究方法,探讨了侏罗系和三叠系煤层的坍塌机理和防塌钻井技术对策。

36. The hydro-geological parameters of Triassic age coal bed 3 of Dongtan Coal Mine be calculated with it.

利用相关方程求出了全东滩矿3煤砂岩顶板含水层的水文地质参数。

37. Rare earth elements(REE) and trace elements were used to analyse source rock and source direction of Yanchang Formation of the Upper Triassic in Ordos Basin.

利用稀土元素和微量元素,分析鄂尔多斯盆地中部上三叠统延长组母岩类型和物源方向。

38. The Kuangshanliang and Tianjingshan present a duplex which comprises of a shallow fault-bend fold of late Triassic and a deep blind stacking anticline imbricated by several thrust sheets of Cenozoic.

北部的矿山梁和天井山构造几何学上表现为一个双重构造，浅层是一个晚三叠世形成的断层转折褶皱；

39. The paleozoic source rock in North China went into the main oil generating period at the end of Triassic.

华北地区古生界生油岩在三叠纪末已进入主要生油期。

40. South Tianshan: a Late Paleozoic or a Triassic orogen?

南天山:晚古生代还是三叠纪碰撞造山带?

41. County formation hypoplasia, missing the entire Paleozoic sector in the health sector and the Triassic.

县内地层发育不全，缺失整个古生界和中生界的三叠系。

42. Besides, there are large scale of tight sandstone gas-reservoirs occurred in sandstone formations which are interbedded or nearly the hydrocarbon source rock of deep buried Triassic and Jurassic.

另外,埋深较大的侏罗系及三叠系中与烃源岩互层或很近的砂岩中存在规模很大的致密砂岩气藏;

43. Both source rocks in Permian Lucaogou Formation in Tainan depression and Middle-Upper Triassic Xiaoquangou Formation in Tuokexun depression have experienced two hydrocarbon-generating processes.

台南凹陷二叠系芦草沟组烃源岩和托克逊凹陷中上三叠统小泉沟组烃源岩均具有两次油气生成过程。

44. Tuba basin is a composite petroliferous basin evolved in multistage tectonic movement and developed multiplex hydrocarbon source rock of Permian, Triassic and Jurassic.

吐哈盆地是在多期构造运动背景下发展起来的一个复合性含油气盆地。

45. Sequence stratigraphy and tectonic evolution of the Triassic strata in the Tanggula Mountain area, Xizang （ZHOU Jia-yun, WEN Hua-guo, LI Yong，et al.

唐古拉山地区三叠纪层序地层分析及构造演化（周家云，文华国，李勇，等）

46. The shallow polyhalite potash deposit in Sichuan are distributed in the north plunge top of Huayingshan anticline where is anhydrock of earlier Mesozoic Triassic period.

四川浅层杂卤石钾矿分布于华蓥山背斜北倾没端下中三叠统之硬石膏岩层中。

47. Sichuan basin is known for Triassic brine to have be widely spread with rich resources, excellent quality, higher industrial value and a long tapping history.

四川盆地三叠纪卤水分布广泛,资源丰富,品质优异,是我国开发利用时间最早,工业价值最高的卤水资源。

48. Triassic evaporite series in Sichuan basin contains high amounts of carbonate components made up of calcite, dolomite as well as of rich magnesite.

四川盆地三叠纪蒸发岩系普遍含碳酸盐组分,除方解石、白云石外,常出现大量菱镁矿。

49. The oolite beach of the lower Triassic Feixianguan Formation in eastern Sichuan basin developed in themargin of carbonate platform, and platform margins are always related to ocean trough.

四川盆地东部下三叠统飞仙关组鲕滩主要发育在碳酸盐岩台缘带上,而台缘带与海槽密切相关,找到了海槽就意味着找到了鲕滩。

50. It has been found Proterozoic Mayuan group, metamorphic rock and Triassic Changlin formation, Nanyuan formation in the area.Ductile shear zone and hydrothermal deposits occur in the volcanic rocks.

在“尤德地体”中,目前已发现元古界麻源群变质岩和侏罗系长林组、南园组,火山岩中均存在韧性剪切带型矿床和热液交代充填矿床。

51. In the middle Triassic residuum in mid Sichuan basin, there exist not only hydrocarbon traps such as old grottoes and buried hills but also many minor faults.

在川中地区中三叠统风化壳中,不仅分布着古岩溶、古潜丘等类型的油气圈闭,而且还有一定数量的小断层。

52. During our first three expeditions, we never gave a second thought to the gravels that overlay the Triassic rock outcrops in the southwestern part of the island.

在我们头三个田野季节里，岛上西南部三叠纪岩层露头处上面覆盖的碎石，我们从不留意。

53. In different phases of the entire Triassic evolution,thrust compressional stresses increased gradually and weakened gradually.The paleogeographic features in various phases were different.

在整个三叠纪演 化的不同时期，逆冲挤压应力逐渐增强又逐渐减弱，各时期盆地的古地理特征不同。

54. At the same time, This paper discusses the distribution of the different sand bodies combination in the Triassic Chang 8 oil formation in chrono-stratigraphic frameworke.

在此基础上探讨了不同砂体组合在长8层序地层格架中的展布规律。

55. In the tight Upper Triassic sandstone with low porosity and permeability, the distributary channel sand body would be the beneficial target.

在致密低孔低渗的上三叠统厚层砂岩中，分流河道砂体储集性能最好，是勘探的有利目标层。

56. This paper divides4 plus successions of early triassic epoch Feijian tan group in Pingle sag west section.

在萍乐坳陷西段早三叠世飞剑潭组划分出4个正层序。

57. Based on facies, paleontology, magnetism stratigraphy and geological events from outcrop sections, this paper has dealt with models and mechanisms of sequences from Triassic to Cretaceous.

基于露头剖面的沉积相、古生物、磁性地层以及地质事件的综合研究 ,探讨了三叠纪、侏罗纪和白垩纪的层序地层模式及其形成机制。

58. Triassic black mudstones are extensively distributed in Tarim basin with great thickness and higher content of total organic matter (TOC) and extractable organic matter (EOM).

塔里木盆地三叠系暗色泥岩分布广、厚度大、有机碳和可溶有机质含量高。

59. The fluctuant form of top Ordovician in Benxi, early and middle Triassic determined the later reformation of reservoir.Its structure presented a pattern of "high in the middle, low in east-west".

奥陶系顶面在本溪期-早中三叠世的起伏形态决定了岩溶储层的后期改造，其在沉积演化过程中，始终处于中部高、东西低的构造格局。

60. Like the Palaeozoic Era, the Mesozoic Era has been divided into smaller units of geological time called period. Triassic is the oldest period of Mesozoic followed successively by Jurassic and Cretaceous Periods.

如同古生代一样，中生代也可划分成一些叫纪的较小的时间单位。三叠纪是中生代中最老的一一个纪，然后依次为侏罗纪和白垩纪。

61. The tectonic evolution history of Tianshan is an example.In the Triassic, it was once uplifted to form the mountains with thick molasse accumulation on both its sides, Junggar and Tarim Basins.

如天山山脉的构造演化，三叠纪天山曾经一度隆起成山，两侧的准噶尔和塔里木盆地中堆积了巨厚的磨拉石；

62. Analysis of the fossil associations of dasycladalean algae in the Middle and Upper Triassic of Croatia is given with the emphasis on the stratigraphical ranges of particular species and associations.

对克罗地亚中三叠统和上三叠统的粗枝藻属化石组合的分析 ,侧重于特定的种和相关化石的地层分布方面。

63. Petrologically, new discovery includes a suite of the Late Permian-Early Triassic ophiolites in the southern part of the surveyed area and ophiolites in Duolie, Dagring Village.

岩石方面，在测区南部新发现了一套晚二叠世一早三叠世蛇绿岩。

64. Petrologically, the ultramafic-mafic rocks within the Lhari fault are redefined as the ophiolites dated back to the Late Triassic in age.

岩石方面，确定了发育于嘉黎断裂带中的超镁铁质-镁铁质岩为嘉黎缝合带内的蛇绿岩，形成于晚三叠世；

65. Northeast Sichuan Basin is a Mesozoic-Cenozoic basin with complex tectonics, Triassic formation based on marine deposits was an important potential resource and reservoir.

川东北地区是一个具有复杂构造的中新生代盆地,以海相沉积为主的三叠系是重要的储层。

66. Permo - Triassic in east Sichuan gas field has many features, such as good condition on hydrocarbon generation and oil &gas reserves, developed feature and many payzone.

川东气田二、三迭系具有良好的油气生、储条件,裂缝发育,产层多。

67. The Upper Triassic classic reservoir of west Sichuan is a kind of sandstone with low porosity and permeability , intercalated by mudstone layers with abnormally high pressure.

川西上三叠统碎屑岩储层是一套低孔、低渗，具高异常地层压力的致密砂泥岩层。

68. Upper Triassic clasolite reservoirs in West Sichuan are a set of tight sand-mud rocks with low porosity-low permeability, high aqueous saturation and abnormal high pressure.

川西上三叠统碎屑岩储层是一套低孔渗，高含水饱和度，具高异常地层压力的致密砂泥岩层。

69. In the central part of west Sichuan, the upper Triassic tight clastic strata is not only developed with many original pools, but also associated with secondary pools.

川西中部地区上三叠统碎屑岩中既发育有原生气藏也伴生有丰富的“次生气藏”,并以“次生气藏”埋深浅、气质好、经济效益高而引起人们的广泛重视。

70. Manaoke gold deposit situated in Northwestern Sichuan is hosted in mid Triassic detrital and carbonate rocks.

川西北的马脑壳金矿床为一赋存于三叠系碎屑岩、碳酸盐岩系的大型微细浸染型金矿床。

71. The widely developed Upper Triassic coalmeasure source rocks have provided sufficient gases for the pool formed in the Western Sichuan Depression.

川西坳陷广泛发育上三叠统煤系烃源岩,为煤成气成藏提供了充足的气源。

72. Gas-bearing carbonatite of marine facies is the main pay reservoirs of Feixianguan Formation of Triassic, Changxing Formation of Permian and Huanglong Formation of Carboniferous.

建南气田的主要产气层是三叠系飞仙关组、二叠系长兴组和石炭系黄龙组海相碳酸盐岩储集层。

73. The Jurassic and Triassic reservoirs in Zhidan area have low porosity and permeability,and are highly compacted.

志丹地区侏罗系、三叠系储层是低孔、低渗储层,压实程度高,地质解释模型与测井解释模型拟合复杂。

74. The Upper Triassic ,Lower and Middle Jurassic loos...

找矿目的层是上三叠统和下、中侏罗统的疏松砂岩层。

75. By means of the distributions of relatively low oil potential area on the top of Ordovician,Carbonferous and Triassic System during several geologic periods,i...

据此，结合油源、储层分布等特点，分析了油气运移和聚集条件，并指出了有利聚集区。

76. Nappes are products formed in the compressional State by Indo-China movement in late Triassic Period.

推覆体是挤压环境下的产物，它形成于晚三叠世末期的印支运动。

77. Abstract :The Yangtze paraplatform is a large craton characterized by development of carbonate formations.Typical Sinian to Middle Triassic cover sediments contain many carbonate formations.

提要： 扬子准地台为大型克拉通碳酸盐发育的地区，从震旦系到中三叠统为典型盖层沉积，其中许多地层中不乏碳酸盐沉积。

78. Abstract： The Gacun deposit is a typical massive sulfide deposit associated with Late Triassic seafloor calc-alkaline felsic volcanics (VHMS).

摘 要： 呷村矿床是一个与晚三叠世海相钙碱性酸性火山岩系有关的典型块状硫化物(VHMS)矿床。

79. Abstract: The strata overlying the Triassic in the Mosuowan on the whole occur as a monocline and the traps are mostly related to faults, which may fall into the deep and shallow fault systems.

摘 要： 莫索湾地区三叠系以上地层整体近单斜形态，圈闭大都与断层相关，并且断层在纵向上可划分为深、浅2套断层系统。

80. Triassic basin is the main oil and gas bearing basin in Algeria, with excellent geologic conditions for hydrocarbon accumulation.The main source rock is Lower Silurian shale.

摘要三叠盆地是阿尔及利亚的主要含油气盆地，油气成藏地质条件优越，主要烃源岩为下志留统页岩。