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china movement
相关语句
  中国运动
     Sun Zhong-shan and New China Movement
     孙中山与新中国运动
短句来源
     New China Movement set up by Sun Zhong shan had deep significance at present.
     孙中山所开创的新中国运动具有深刻的现时代意义。
短句来源
  “china movement”译为未确定词的双语例句
     faulted anticline faulted nose structure formed in Karamay movement of the end of Late Triassic, was reformed and developed by Indo China movement and early middle Yanshan movement;
     圈闭构造为形成于晚三叠世末期的克拉玛依运动,经中-早期燕山运动的继承和发展起来的断背斜-断鼻构造;
短句来源
     Characteristics of structural evolution and coalbed methane controlling were researched. The results indicate that since the Indo China Movement, the physical characteristics of coal reservoir has been controlled by structural evolution obviously. Bordered by the northern Suxian fault trended EW, the exploration prospect of coalbed methane in the north area is not good.
     研究了淮北地区地质构造演化及控气特征 ,结果认为 :淮北地区印支期以来的构造演化对煤储层物性控制作用十分显著 ,以 EW向的宿北断裂为界 ,北部地区煤层气勘探前景不佳 ,南部地区的东部 ,煤层的展布受褶皱形态的控制 .
短句来源
     Sichuan Bureau of Surveying and Mapping is compiling the new edition of Atlas of Sichuan Province in order to provide surveying and mapping service for the Development of the West China Movement.
     为了在西部大开发中更好地为四川的经济发展提供测绘保障服务 ,四川省测绘局决定重新编制《四川省地图集》。
短句来源
  相似匹配句对
     The Classfication Movement in China
     分类法运动在中国
短句来源
     China In Olympic Movement
     中国奥运大事记
短句来源
     China.
     第一部分:建国初期的严重灾情。
短句来源
     Movement
     虚实修身运动
短句来源
     CHINA
     中国
短句来源
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  china movement
Thus a new understanding about the Indo-China movement has arisen.
      
Indo-China movement in the Middle and Late Triassic periods and at the end of Triassic period gave the region an important transformation.
      


The Datong coal field evolved into a diwa stage as a result of Indo——China movement. The Yungang diwa (geodepression) occurs as a short belt in the northern part of the Luliang anteclise in the Yishan platform.The diwa began to take shape at the end of the Triassic. It has received thick-bedded formations of polymineralic sandstone of continental facies (coal-bearing and red-rock formations) and contains 7 layered groups and 14 coal seams. The formations cover the under lying strata with unconformity....

The Datong coal field evolved into a diwa stage as a result of Indo——China movement. The Yungang diwa (geodepression) occurs as a short belt in the northern part of the Luliang anteclise in the Yishan platform.The diwa began to take shape at the end of the Triassic. It has received thick-bedded formations of polymineralic sandstone of continental facies (coal-bearing and red-rock formations) and contains 7 layered groups and 14 coal seams. The formations cover the under lying strata with unconformity. A large number of short axial folds with faults, NE—and NW—trending, are well-developed in the region. Three episodes of magmatic activity, beginning with intrusion of acid to intermediate rocks and ending with widespread extrusion of basalt, have been recognized along fractures. Paleobotanic fossils in the lower formation are composed of early and late assemblages of coniopteris-phoeniopsis. The diwa migrated northwestwards. The formation and development of the diwa controlled the distribution and metamorphism of coal.The study of diwa-type coal-bearing formation in the region has clarified the age of P_1~2, P_1~2 and J_1, and distinguished between Meso zoic and Paleozoic structural layers. Some geological problems have been correspondingly solved.

大同煤田由印支运动进入地洼阶段。地洼呈短带状分布在伊陕地台区吕梁台隆的北部。 云岗地洼始于三叠纪末,形成巨厚的陆相复矿砂岩建造(含煤建造及红色建造等),含煤7组14层。与下伏地层不整合接触。短线褶曲发育,分北东和北西两组,伴有断裂。沿断裂从中酸性岩侵入到玄武岩大面积喷发有三次岩浆活动。下部建造中古植物为coniopteris—pboeniopsis早晚两个组合。地洼的活动中心向西北侧向迁移。地洼的形成与发展对中,古生代煤层赋存、煤变质关系密切。 该煤田地洼型含煤建造的研究,进一步澄清(J_1与P_1~2、P_2~1)地层时代。区分出中、古生代构造层。一些地质问题相应地解决。

The investigation of Huaiyang epsilom type ( E type ) has been attracting the interest of many geologists since the E-type structural systems were Founded by Professor Li Si-Guang, but so far, the frocess of forming the frontal arc has been rarely explained. The grontal arc in the regiong ranging from Huo county to Lu-jian County, Anhui Province, belongs to the northeast part of the far east limb of the E-type. According to the data gathered in the region when the author joined in the surface geological investigation...

The investigation of Huaiyang epsilom type ( E type ) has been attracting the interest of many geologists since the E-type structural systems were Founded by Professor Li Si-Guang, but so far, the frocess of forming the frontal arc has been rarely explained. The grontal arc in the regiong ranging from Huo county to Lu-jian County, Anhui Province, belongs to the northeast part of the far east limb of the E-type. According to the data gathered in the region when the author joined in the surface geological investigation in the past two or three years in order to to study the geo-structural control over the formation and distribution of coal-kields, the fiontal arc has developed for a long time and run through some complerx processes, which may be divided by the stage of formation into three phases, the pre-phase; the erogenic phase and the post-phase. The deve-lopments of Cathgsian tectonic system which occurs in the south of china generally have governed the researched regions until the end of lndo-China movement. At the early yenshan movement the frontal arc had been formed by the compounding of new tectonism, and in the late orogenic period the shape of the arc had encountered some distortion as welt as strong increment. However, the arcuates hape of the arc is still visible.

自李四光教授创立山字型构造以来,淮阳山字型构造的研究受到人们的重视,但涉及淮阳山字型形成过程方面的论述尚少。安徽省和县至庐江一带是该山字型前弧东冀的东北邯分,笔者近二、三年中为研究该地区构造对煤田形成及分布的控制作用,曾参加过地面地质调查工作,从获得的地质资料分析,淮阳山字型前弧东冀有长期的、复杂的形成过程并可以分出成型前期、成型期及改造期。印支旋回及其以前的时期乃是区域上华夏系构造发育时期,燕山早期重接复合为山字型前弧东冀,燕山中晚期及其后它受到进一步的加强与改造,但前孤东冀构造仍然醒目。

After the Indo-China movement, the crustal development of south China evolved from the platform stage into the diwa stage. According to the plate tectonics theory, the continental crust of the eact margin of south China at that time was just converted from the cont- inental margin of island arc type into that ot Andes type. Thus the "ancient Pacient plate" subducted directly under the "ancient Eurasia plate" so that the consolidated continental crust fo south of Chia underwent buckling and...

After the Indo-China movement, the crustal development of south China evolved from the platform stage into the diwa stage. According to the plate tectonics theory, the continental crust of the eact margin of south China at that time was just converted from the cont- inental margin of island arc type into that ot Andes type. Thus the "ancient Pacient plate" subducted directly under the "ancient Eurasia plate" so that the consolidated continental crust fo south of Chia underwent buckling and blockfaulting movement with extensive magmatic intrusion and extrusion. The charateristics of diwa tectonics agree with plate movement in time, space and causes, indicating that the two theories are very similar.

印支运动后,中国东南部地壳演化由地台阶段转入地洼阶段。按板块构造观点应属由岛弧型陆缘转化为安底斯陆缘,古太平洋板块直接俯冲于古欧亚板块之下,致使已固结刚化的东南陆壳,发生强烈的拱曲、断拗和空前发育的岩浆火山活动。地洼造构造特征与板块运动在时间上、空间上和基因上的一致,显示了两者之间是十分相近的。

 
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