塔里木盆地
- 与 塔里木盆地 相关的网络例句 [注:此内容来源于网络,仅供参考]
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The Kuche Basin, located between the Tianshan intracontinental orogenic belt and the Tarim plate, Xinjiang Uygur Autonomous Region, northwest China, is the tectonic element in the Mesozoic-Cenozoic time, and belongs to a new type of intracontinental flexural basin in the classification of the basin.
库车盆地位于天山陆内造山带与塔里木板块之间,是中新生代发育的构造单元,在盆地分类上属于一种新的陆内挠曲盆地。
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Tarim developed into a backarc basin of Laurasia in the splitting of Pangia.
泛大陆的裂解过程中,塔里木地块成为北方劳亚古陆的边缘弧后盆地。
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1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.
1:25万地质填图进一步揭开了青藏高原地区大地构造的奥秘:阿尔金山是昆仑,祁连-秦岭造山系的一部分;阿尔金断裂确是一条大型转换断层;木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带;松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地;冈底斯带曾经历了重要的印支造山运动;不存在从古生代延续到三叠纪的大洋盆地,即不存在所谓古特提斯或永久特提斯;古生代时期,在青藏高原地区亦不存在具古生物,古地理分隔意义的大洋盆地,当时,包括中朝,扬子,塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南,属冈瓦纳大陆结构复杂的北部边缘;雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹,它们均是从三叠纪起就发展成大洋裂谷带的;以雅鲁藏布江带为主洋盆带的特提斯洋,从三叠纪晚期开始消减,经历了印支,燕山,喜马拉雅3个阶段脉动式板块汇聚造山过程。
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In Jurassic-Paleogene, the West Kunlun, West Tianshan, Tarim and the Central Asia exhibited a relatively quiet period after the orogenic movement. Due to extension, these area displayed peneplain tectonic geomorphologic landscape.
侏罗纪,西昆仑、西天山、塔里木大陆及中亚—带都处于造山期后的相对宁静期,以仲展构造作用为主,主要表现为准平原化的构造地貌景观,沉积有高成熟度的侏罗纪含煤岩系,塔西南表现为陆内伸展盆地,这一时期可持续到早第三纪。
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These results have yielded new intraplate evidence for con-straining the relation between the Tarim plate and the supercontinent.
碎屑锆石测年资料为研究塔里木板块与超大陆的关系提供了来自盆地内部的证据。
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Chagan sag is a secondary tectonic unit in Chagandelesu Depression, northeastern Yingen-Ejinaqi basin, and the basement of the basin is a Paleozoic fold belt of continental margin or island arc at the connection region of North China plate* Tarim plate and Kazakstan plate, with the character of erogenic belt.
查干凹陷属于银根—额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元,其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带,具有古生代造山带的性质。
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The multicycle tectonic evolution of Tarim craton controls the formation of superimposed the Tarim Basin,petroleum-geology conditions as well as the features of composite petroleum system ,thus determines hydrocarbon distribution and resources potential in the basin.
塔里木克拉通多旋回构造演化控制了塔里木叠合盆地的形成及石油地质条件和复合含油气系统特征,进而决定了油气的分布和资源潜力。
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In the Middle and Late Cambrian, similar to the lithofacies palaeogeographic pattern of the Early Cambrian, the land area was gradually reduced, the basin area was enlarged, while the Tarim carbonate platform changed little.
中寒武世和晚寒武世的岩相古地理格局与早寒武世相似,但陆地面积逐渐缩小,盆地面积逐渐扩大,塔里木碳酸盐岩台地变化不大。
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The Tarim block and the Junggar block subducted in the opposite direction beneath the Tianshan Mountains.
塔里木地块和准噶尔地块相向俯冲于天山之下,造成了山系的急剧隆升和冲断推覆,在构造重荷作用下,沿着天山南、北山前发育了陆内俯冲型前陆盆地,这一特点已为大多数学者所共识。
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The results of the study indicate:(1) the stress, strain and velocity fields as well as the uplift rates of the model are consistent essentially with those of the prototype in nature;(2) the major driving force for intraplate tectonic deformation in central-eastern Asia results mainly from the compression of the Indian plate;(3) the existence of the RSBs, such as those of Tarim, Alxa, Ordos and Sichuan basin, is one of the basic origins for the development of large-scale compressional basins and the table-like uplift of the Qinghai-Tibet plateau;(4) The netlike plastic-flow in the lower lithosphere is faster than the displacement in the upper layer, controlling the tectonic stress and deformation fields in the upper crust;(5) the weakness layer distributed discontinuously in the middle crust influences the level of difference between the stress directions in the lower lithosphere and those in the seismogenic layer.
研究结果表明:(1)模型中的应力场、应变场、位移速度场和地表隆升速率,与自然条件下的实际状况基本相符;(2)中东亚板内构造变形的驱动力源主要来自印度板块的推挤作用;(3)塔里木、阿拉善、鄂尔多斯、四川盆地等相对稳定块体的存在是促成大型压性盆地形成和青藏高原平台式隆升的基本原因之一;(4)岩石圈下层的网状塑性流动超前于上层,控制上层的构造应力场和变形场;(5)中部地壳的非连续分布软弱层影响上、下层之间应力方向的差异程度。
- 推荐网络例句
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The split between the two groups can hardly be papered over.
这两个团体间的分歧难以掩饰。
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This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.
这种做法不仅鼓励了更多的反应,而且减少跟风的可能性。
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The new PS20 solar power tower collected sunlight through mirrors known as "heliostats" to produce steam that is converted into electricity by a turbine in Sanlucar la Mayor, Spain, Wednesday.
聚光:照片上是建在西班牙桑路卡拉马尤城的一座新型PS20塔式太阳能电站。被称为&日光反射装置&的镜子将太阳光反射到主塔,然后用聚集的热量产生蒸汽进而通过涡轮机转化为电力