lithosphere

lithosphere

1. There occurred strong extension of lithosphere with NE direction in Cathaysian Block, East Sea and Japan Sea since 17 Ma, which also turned the movement direction of Indochina block from left lateral to right lateral slip.

17Ma以后,华夏、东海至日本海岩石圈均出现了强的NE向伸展,也使印支块体沿红河断裂从左旋挤出转向右旋走滑。

2. The lower degrees of mantle melting of the HT and LT2 lavas may be the result of a relatively thicker lithosphere and lower geotherm.

HT和LT2熔岩的地幔熔融程度较低，可能是与地幔柱边部的岩石圈相对较厚和地热较低有关。

3. Jiao Shuqiang and Jin Zhenming.Effective elastic thickness of continental lithosphere and its geodynamical significance.Geological Science and Technology Information, 1996. 15(2): 8-12.

[15]焦述强,金振民.大陆岩石圈有效弹性厚度研究及其动力学意义.地质科技情报,1996,15(2): 8-12.

4. FU Rong-Shan.Mantle convection and shear stress field on the base of the lithosphere in China.Journal of University of Science and Technology of China(in Chinese),1990,20:184-190.

[19]傅容珊. 地幔对流和中国岩石层底部切向应力场. 中国科学技术大学学报,1990,20:184-190.

5. Gravity Field Character and Lithosphere Tectonics in Sanjiang Region

三江地区重力场特征和岩石圈构造

6. HORIZONTAL STRESSES IN THE UPPER LITHOSPHERE

上部岩石圈的水平应力

7. These studies indicate that the continental lithosphere is characterized by heterogeneities in its thermal state, chemical composition and mechanical behavior.

不同学科的最新研究成果表明，岩石圈在热状态、化学成分和力学行为等方面具有高度非均匀性。

8. The paper constructs a correlation formula for the pressure gradient and geothermal gradient in the lithosphere with the thermocompression coefficient.

与地温梯度一样,岩石圈中的地压梯度在空间和时间上也应是复杂多变的。

9. Structure and dynamics of lithosphere and asthenosphere in the gigantic East Asian-West Pacific rift system

东亚西太平洋巨型裂谷体系岩石圈与软流圈结构及动力学

10. Keywords Northeast China epicontinental region;lithosphere;nonferrous and noble metal;metallogenic system;

东北部陆缘;有色金属;贵金属;成矿系统;

11. GEOLOGICAL BACKGROUND AND METALLOGENIC TYPES OF NONFERROUS AND NOBLE METAL RESOURCES IN THE EPICONTINENTAL LITHOSPHERE IN NORTHEAST CHINA

中国东北部陆缘成矿地质背景与有色金属贵金属成矿系统划分

12. THREE-DIMENSIONAL STRUCTURAL AND DYNAMIC TYPES OF THE CONTINENTAL MARGIN LITHOSPHERE IN SOUTHEAST CHINA

中国东南大陆边缘带岩石圈三维结构-动力学型式

13. Wu Changde Zhu Hong Deng Zongce Cui Junwen （Lithosphere Research Center; CAGS）;

中国地质科学院岩石圈研究中心;

14. Petrological structure, types and inhomogeneity of the lithosphere beneath continental China

中国大陆岩石圈岩石学结构、类型与不均一性

15. China lithosphere 3D structure database

中国岩石圈三维结构数据库

16. Three-dimensional lithosphere density distribution beneath Chinese Sea and its adjacent regions

中国海及邻域岩石圈三维密度分布

17. Highly Chemical Heterogeneity of Subcontinental Lithosphere Mantle Beneath North China and Its Major Transformation

中生代华北岩石圈地幔高度化学不均一性与大陆岩石圈转型

18. In Mesozoic, the most important interaction occurred between the crust and the mantle, whereas in the older and Cenozoic it did between the lithosphere and the asthenosphere.

中生代壳幔相互作用明显，克拉通稳定时期及新生代时期层圈之间相互作用的活跃带位于岩石圈与软流圈之间。

19. The Cenozoic basins of Linfen and Yinchuan correspond to thermal expansion sod extension of lithosphere.

临汾、银川新生代盆地对应岩石圈热胀-拉伸；

20. We intend to study the terraces further in order to ascertain what the Martian crust and lithosphere were like at the time the seismic activity led to the formation of the volcanoes.

为了探知火星地壳和岩石圈在地震活动性导致火山形成时期的样子,我们将要进一步研究梯田.

21. It is significant to know changing character of lithosphere structure in order to analyze and study regional tectonic conditions, stress field and earthquake occurrence.

了解和认识岩石圈结构及其变化特征，对于分析研究该区域构造环境、应力场和地震的发生等有重要意义。

22. PLASTIC-FLOW NETWORKS AND TECTONIC STRESS FIELD IN THE LITHOSPHERE IN CENTRAL-EASTERN ASIA

亚洲中东部岩石圈塑性流动网络与构造应力场

23. EQUILIBRIUM COMPENSATION DEPTH AND INVERSION ANALYSES FOR ELASTIC SLAB MODEL OF THE LITHOSPHERE IN THE CENTRAL ASIAN REGION

亚洲中部地区岩石圈均衡补偿深度和弹性板模型反演结果分析

24. The overall environment quality of lithosphere is good and pedosphere is not polluted.

从总体上讲,大巴山区岩石圈环境质量是较好的;

25. Ren Jishun, Chen Tingyu, Niu Baogui, Liu Zhigang and Liu Fengren.1990.Tectonic Evolution of the Continental Lithosphere and Metallogeny in Eastern China and Adjacent areas.Bijing: Science Press.

任纪舜,陈廷愚,牛宝贵,刘志刚,刘凤仁.1990.中国东部大陆岩石圈的构造演化与成矿。北京:科学出版社。

26. The altiplano which you had been to years ago was just sleeping under the lithosphere.

你在多年前登过的高原，如今沉睡在地壳的深处。

27. Electrical structures of the lithosphere along the Jiamusi massif and its eastern edge

佳木斯地块及东缘岩石圈电性结构特征

28. Keywords Kiamusze block;Nadanhada terrane;Yuejinshan rock series;MT;Collision belt;Lithosphere;

佳木斯微板块;那丹哈达地体;跃进山岩系;大地电磁;拼贴带;岩石圈;

29. Geological and Geochemical Characteristics of Anatectic Xenoliths and the Model of lithosphere in Xingyang, Henan

信阳深源包体的地质地球化学特征及其岩石圈模型

30. GEOLOGICAL INTERPRETATION OF THE LITHOSPHERE EFFECTIVE ELASTIC THICKNESS

关于岩石圈有效弹性厚度的地质理解

31. Title： Tectonic implication on the lithosphere evolution of the Tibet Plateau：Petrology and geochemistry of sodic and ultrapotassic volcanism in Northern Tibet.

关键词：青藏高原；超钾质火山岩；钠质火山岩；岩石学；地球化学；岩石圈演化

32. Casing deformation takes place in these geological environments such as plastic rock layer, fault zone, active lithosphere zone, earthquake zone and the place where sand flows.

分析了油井套管损坏的地质环境,指出在塑性岩层、断层、地壳活动、地震活动及油层出砂等地质环境中易造成油井的套管损坏。

33. The heat flow history may be recovered by using the model of pure shearing, multi-stage stretching rift basin in the lithosphere structure for the present Wanan and Zengmu basins in the western Nansha area.

分析南沙西部海区万安、曾母盆地岩石圈结构现今特徵认为，该区可应用多幕拉伸的纯剪切裂谷盆地模型恢复盆地热流历史。

34. THEORETICAL MODEL OF REFINING THERMAL STRUCTURE OF CONTINENTAL LITHOSPHERE WITH GRAVITY OBSERVATIONS

利用重力资料精化大陆岩石圈热结构的理论模型

35. The classical model considers the ASRR as a left-lateral transtension strike-slip fault which cuts through the entire lithosphere, which resulted in the spreading of South Chna Sea.

前人研究认为哀牢山红河剪切带的左移活动引发南海的张裂，因此象背山变质岩带受到横移拉张的应力所控制。

36. Lower crust processes during the lithosphere thinning in eastern China: magma underplating, replacement and delamination

华北东部岩石圈减薄中的下地壳过程:岩浆底侵、置换与拆沉作用

37. MT sounding and lithosphere thickness in North China

华北地区大地电磁测深及岩石圈厚度讨论

38. THERMAL STRUCTURE OF THE LITHOSPHERE IN NORTH CHINA

华北地区岩石圈热结构的研究

39. A GROUP VELOCITY OF SEISMIC LOVE SURFACE WAVE AND LITHOSPHERE STRUCTURE IN ANTARCTIC PENINSULA

南极半岛地区地震勒夫波群速度与岩石圈结构

40. After the collision of the Nansha block and the Kalimantan-Southwest Palawan block, the Zengmu basin and the Brunei-Sabah basin were produced as the winding of the lithosphere of the southeast margin.

南沙地块与加里曼丹-西南巴拉望地块发生碰撞后,在其东南边缘由于岩石圈弯曲而产生了曾母盆地和文莱-沙巴盆地。

41. TECTONIC EVOLUTION OF THE LITHOSPHERE PLATES AND SOME FEATURES OF THE SEDIMENTARY DISTRIBUTION IN CENOZOIC ERA IN SOUTH CHINA SEA

南海新生代岩石圈板块的演化和沉积分布的某些特征

42. It didn't calm down until the lithosphere came to cool down and high temperature lowered.

只有当地球温度逐渐降低，地壳慢慢冷却，高温退去，大地才安静下来。

43. It shows that numerical modeling is an effective means of studying lithosphere structure and evolution, and distinguished results have been achieved by using numerical modeling.

可以看出，数值模拟是岩石圈构造与演化研究的有力工具，并已经取得了卓著的成就。

44. Since the size of the Earth is essentially constant, new lithosphere can be created at the mid-ocean ridges only if an equal amount of lithospheric material is consumed elsewhere.

因为地球的大小本质上是不变的，只有同等数量的岩石圈物质在其它地方被吞没，新的岩石圈才能生成。

45. Therefore, when we use creep experimental results obtained under high temperature and pressure to directly extrapolate and explain lithosphere rheology, we can make some mistakes.

因此，用高温高压蠕变实验结果直接外推解释岩石圈流变时存在若干问题。

46. These dissolved materials thus pass from the lithosphere to the hydrosphere.

因此，这些溶解了的物质就从岩石圈转移到水圈。

47. Role of weak zone orientation in continental lithosphere extension

在大陆性岩石圈范围里弱区方位的作用

48. Discussion about the distribution of stress in lithosphere in the earth rotation

在自转条件下地壳中应力分布的探讨

49. Keywords the earth crust;lithosphere;vertical low-velocity zone;prognosis of ore resources.;

地壳;岩石圈;软流圈;垂向低速带;矿产预测;

50. Mantle ion causes normal stress and tangential stresses at the base of the lithosphere, which affect or even lead to lithospheric stress field and lithospheric deformation.

地幔物质内部的密度横向非均匀及表面板块运动引起地慢流动，并在岩石圈底部产生一个应力场。

51. a zone of the earth's mantle that lies beneath the lithosphere and consists of several hundred kilometers of deformable rock

地球中地幔的一个区域，在岩石圈之下，包括几百公里可变形的岩石

52. The rheology boundary within the mantle lithosphere,the nature of the lithosphere,the intraplate stress and thickness,the sedimentary loading are the important geodynamic factors of sedimentary ba...

地球内部流变学界限、岩石圈的性质和厚度、板内应力和沉积负荷是盆地形成的地球动力学基本机制。

53. The Deep Conformations of the Lithosphere Controlling the Swerving of the Geochemical Steep Zone

地球化学急变带急转弯变化与深部构造效应

54. a rigid layer of the lithosphere that is believed to drift slowly

地球岩石圈中非常坚硬的一层，被认为在缓慢漂移

55. a rigid layer of the lithosphere that is believed to drift slowly.

地球岩石圈中非常坚硬的一层，被认为在缓慢漂移。

56. According to geophysical data,the crust and lithosphere were obviously thickened under the belt.

地球物理资料表明，该陆内造山带下的地壳和岩石圈曾显著加厚。

57. The Earth is made up of three concentric zones: the lithosphere (solid earth), the hydrosphere(water layer), and the atmosphere.

地球由三个同心圈带组成：土壤岩石圈，水圈，大气圈。

58. The Earth's lithosphere is formed of a rather small number of major plates

地球的岩石圈是由少数大板块所组成的。

59. The garnets of M-type belong to pyrope mainly formed near the boundary between lithosphere and aesthenosphere under the megatemperature and ultrahigh pressure of Jinning or earlier orogeny.

型榴辉岩的石榴石属镁铝榴石，形成于晋宁期高温超高压条件下的岩石圈与软流圈交界附近。

60. While the Tarim block lithosphere mantle was subducting, the Kuqa rejuvenation foreland basin and rejuvenation Tianshan Mountains were formed.

塔里木岩石圈俯冲的过程中，形成库车再生前陆盆地和再生前陆冲断带以及再生天山山脉。

61. captive rocks of the lithosphere

壳源捕虏体

62. Marble is the degenerative cliff that the original rock in the lithosphere forms through action of high pressure of the high temperature inside the lithosphere.

大理石是地壳中原有的岩石经过地壳内高温高压作用形成的变质岩。

63. Continental and Oceanic Mantle Lithosphere;

大陆和海洋性覆盖物岩石圈研究介绍;

64. Contamination by continental crust or lithosphere can yield subduction-type signatures and lead to the misidentification of contaminated continental basalts as arc related ones.

大陆地壳或岩石圈的混染作用可以给出似消减带信号,并导致将受到混染的大陆玄武岩误判为岛弧玄武岩。

65. Continental lithosphere is significantly different from oceanic lithosphere in the aspect of composition, thickness and mechanical strength.

大陆岩石圈和大洋岩石圈在成分、厚度和力学强度方面有明显的差别。

66. Subcontinental lithosphere mantle

大陆岩石圈地幔

67. DUCTILE WEAKNESS-PLANE EFFECT OF PLASTIC-FLOW NETWORKS IN THE CONTINENTAL LITHOSPHERE

大陆岩石圈塑性流动网络的延性弱面效应

68. Responses of continental lithosphere to structuring, gravitation and thermodynamics largely depend on its rheological strength.

大陆岩石圈对构造作用、重力作用和热作用的响应在很大程度上取决于其流变强度。

69. METHODS TO STUDY ELECTRICAL CONDUCTIVITY OF CONTINENTAL LITHOSPHERE

大陆岩石圈导电性的研究方法

70. The Estimation of the Effective Elastic Thickness of the Continental Lithosphere and Its Geological Significance

大陆岩石圈有效弹性厚度的计算及其地质意义

71. The status of continental lithosphere rheology and experiments on creep of rocks at high temperature and high pressure

大陆岩石圈流变研究进展与高温高压流变实验现状

72. Mechanical Responses of the Continental Lithosphere to Viscous Drag and Boundary Forces

大陆岩石层对侧向推挤及底部拖曳作用的力学响应

73. The Mesozoic intraplate orogeny of the Taihang Mountains and the thinning of the continental lithosphere in North China

太行山中生代板内造山作用与华北大陆岩石圈巨大减薄

74. The Austria storehouse abundant and his research colleague saw in the American Utah's sandstone the similar break, this kind of break exposes clearly the lithosphere which is corroded by the water.

奥库博和他的研究同事在美国犹他州的砂岩看到类似的断裂，这种断裂暴露出清晰的被水腐蚀的岩石层。

75. for the continent, the crust thickness, thermal age and strain rate significantly had strong effect on the lithosphere strength.

尤其对于大陆岩石圈,地壳厚度、年龄和应变率均可显著影响岩石圈的强度。

76. The lithosphere,hydrosphere,biosphere and atmosphere are 4 interlocking pieces of the planet that together make life possible on erath.

岩圈、水圈、生物圈和大气圈一起互相作用， 才使4块形成的行星形成生命。

77. Keywords lithosphere;geologic calamity;pedosphere;environment quality of pedosphere;

岩石圈;地质灾害;土壤圈;土壤环境质量;

78. inhomogeneous characteristics of lithosphere

岩石圈不均一性

79. Below the lithosphere is the rheosphere comprising partly fused peridotite

岩石圈之下是由部分熔融的橄榄岩所组成的软流圈。

80. lithosphere mantle collision

岩石圈地幔碰撞