盆地

About 230 unique feature downfaulted basin in Mesozoic and kainozoc era distribute in the east continent and alongshore in China, which is the best concentric distribution area of continental facies oil-gas contain basin in the world.

陆相断陷盆地是世界上重要的含油气盆地类型之一，我国东部大陆及沿海分布着约230个各具特色的中、新生代陆相断陷盆地，是世界上最大的陆相含油气盆地集中分布区。

Great paleoenvironment change of the basins that located in northeast region of Tibet plateau is closely related to the second uplift of Tibet plateau and the formation of Asia monsoon. This conclusion was found by the analysis and correlation of magnetstratigraphy、 biostratigraphy、lithohorizon in xining basin、 lanzhou basin and linxia basin.

西宁盆地、兰州盆地、临夏盆地的磁性地层、生物地层、岩石地层的对比表明位于青藏高原东北部的周缘盆地在青藏高原的第二次隆升时被迫的进行了相应的应力调整和变形，并在刚成形的亚洲季风共同作用下，导致自身古环境发生重大变迁。

Directed under plate tectonics theories, author applied the relationship between orogenyy belt and basin, analyzation of proto-type basin restoration of Paleo-structures etc to systematically draw the Paleo-structural maps and Paleo-sedimental photographical maps on Z, O, S, D, C, P, T, J, K, E, N〓j, N1〓k, N〓k etc in Tarim basin.

以板块构造理论为指导，运用造山带与盆地、原型盆地分析、古构造分析等分析方法，系统编制了Z、O、S、D、C、P、T、J、K、E、N〓j、N〓K，N〓K等盆地及周缘古构造岩相图，全面系统地研究和恢复了塔里木大型叠合复合盆地构造演化历史，并将塔里木盆地构造演化史划分为7个构造演化阶段。

Exhibiting angle unconformities or erosion unconformities in different part of the basin, these surfaces are obvious to be recognized on seismic profiles.T1 conformity, separating Eogene from Neogene, was formed during the whole basin uplifting and erosion by the end of Eogene.T1 unconformity denuded unbearing strata differently, and the deeper and thickest erosion lies on the southern margin of the basin, which reflects the activity of southern Jiangnan paleo-terrene. In conclusion, the major erosion belts extending along NW direction reflects NE-SW compression and slipping caused the Eogene basin uplift and strengthen the earlier NW direction extending low convex, and formed the NW direction extending depress and erosion belts.

古近系和新近系之间的T1不整合面形成于古近纪末期的盆地整体抬升，对下伏地层造成不同程度的剥蚀，沿盆地南缘的剥蚀层位深，剥蚀量大，反映盆地南缘整体相对隆起，与江南古陆的隆起作用有关。T1界面剥蚀带走向以北西向为主，反映了盆地在古近纪末受到了北东－南西向的挤压或压扭作用，该作用造成盆地整体抬升，强化了北西向展布的低凸起，产生了近北西向的洼陷和剥蚀带。

Bestriding over Tianshan tectonic belt of different tectonic property and evolvement and Kuluketage causes that its structure and tectonic evolvement are clearly controlled by base tectonic and forms the deep structure character of belt form south to north with a boundary of Yanqi fracture.

4几盆地热史与古地温分析认为，焉省盆地热演化史明显不同于西部其它盆地，表现为现今地温梯度：北部凹陷平均为3.48℃/l00米，南部凹陷平均为3.06℃/100米，比相邻的塔里木盆地1.8一2.5℃/100米、吐哈盆地2.36℃/100米明显要高。

The results are shown as below.1 Tectono-thermal evolution: The history of the Songliao basin is divides into four stages, high-temperature doming and extension, high-temperature rifting, low-temperature depression, and low-temperature shrinkage. Numerical simulation of mechanical process shows that the basin appeared in the early- to late- Jurassic as a result of rapid low-angle subduction of the Pacific plate towards the northwest, of movement of the Siberian block towards the southeast, of many other influences such as internal thermal stress in the mantle, gravitational force, stress of phase transition, etc. Both the Pacific plate and the Siberian block slowed down in the early Cretaceous, and almost stopped in the middle Cretaceous with the rapid decrease of abnormal heat in the mantle below.

盆地构造热演化力源机制数值模拟研究表明：早、中侏罗世至晚侏罗世晚期，盆地演化主要是太平洋块体向北西方向以低角度快速俯冲和西伯利亚块体向东南俯冲共同作用的结果，同时也与地幔内部热力、重力、相变力以及地球自转及公转速度变化效应和上覆块体绝对运动的作用有关；早白垩世早期至早白垩世中期，来自东部太平洋块体俯冲作用的减弱，而这一时期影响盆地演化的主要力源是地幔内部热力、重力、相变力以及地球自转及公转速度变化效应和来自西伯利亚块体俯冲作用；进入早白垩世晚期至晚白垩世早期，由于双重俯冲带中西侧俯冲作用带基本停止活动，而本区地幔热能的快速衰减则控制盆地的构造热演化；晚白垩世晚期以后，太平洋块体活动加强和地幔热运动是影响盆地演化的主要动力。

Non-diapiric, the overpressured top boundaries in the south and the margin of Yinggehai basin are often deep-buried, and are distinctly controlled by the formations and their lithologies.

在裂谷或裂陷盆地中，盆地形成的构造作用主要是拉张作用，由于岩石圈的拉薄而引起盆地的形成和沉降，盆地形成后盆地内沉积物和水的充填会引起岩石圈的均衡调整下降。

Along with Tajik Basin and the Southwest Southwest Depression of Tarim Basin, Alay Basin was one of the remnant basins on the north rim of the Tethys during the Late Triassic to Paleogene, it became a peripheral foreland basin in Miocene.

阿莱依盆地是特提斯北缘盆地群中的一个，晚三叠世—古近纪与相邻的塔吉克盆地、塔里木盆地西南坳陷基本连通，中新世以后才成为分隔的周缘前陆盆地。

Whereas the seismic thermal lithosphere is about 150km thick, which means the Tarim lithosphere is not steady and became thinner. In this paper, writers analyzed the Tarim lithosphere thinning mechanism based on the tectonic thermal evolution quantitative method, and discussed three possibilities:the hotter India asthenosphere intruded under the Tarim lithosphere and made the Tarim lithosphere became unsteady;the bottom of Tarim lithosphere is heated by friction of the atheonosphere flow and washed off by the hot asthenosphere; the Xizang lithosphere delamination induced the convection, and the upflowing mentle heated the bottom of the Tarim lithosphere and make it enthinning.

本文利用构造热演化方法对塔里木岩石圈减薄的热演化过程进行了定量分析，探讨了塔里木盆地岩石圈减薄可能的三种机制：印度板块与欧亚板块碰撞后青藏高原岩石圈底部的软流圈较塔里木盆地岩石圈底部的软流圈的温度要高，青藏高原的软流圈地幔向塔里木盆地岩石圈底部侵入形成的热扰动使得塔里木盆地岩石圈底部的温度升高；塔里木岩石圈与其下流动的软流圈的摩擦剪切生热导致其岩石圈地幔底部温度升高，使得岩石圈底部发生热侵蚀，从而使得与软流圈接触的岩石圈地幔不断地加入到软流圈地幔；在塔里木盆地岩石圈的下部，青藏高原的岩石圈在该处发生了拆沉，从而诱发的软流圈地幔对流，上升的软流圈地幔流使得岩石圈地幔的温度升高而熔融，成为软流圈地幔。

In the west, there are some obvious high velocity regions, such as tectonically stabe Tarim, Junggar, Turpan, Hami basin and east of Qaidam basin, Sichuan basin and to its south, Taiwan Strait and so on. High velocities also exist in Erdos.

在中国西部，构造上相对稳定的塔里木盆地、准噶尔盆地和吐鲁番-哈密盆地，以及柴达木盆地东端、四川盆地及其南部地区，台湾海峡等是明显的高Sn速度区，鄂尔多斯地台也偏高。

He is the most remarkable man that I have ever known.

他是我知道的人中最值得注意的人。

Increased appearance of lymphocele was noticed in patients with diabetic nephropathy, congenital malformations of the urinary tract, and inflammatory diseases, including glomerulopathy and extraglomerular ones, after high-voltage radiotherapy and after removal of the renal graft.

经过高压放射疗法和切除移植肾后，在糖尿病肾病患者、泌尿系统先天性畸形患者和炎症患者身上发现淋巴囊肿有所增加，包括肾小球病和球外疾病等。