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in mesozoic     
相关语句
  地区中生代
     STRESS FIELD EVOLUTION IN MESOZOICERA IN ERGUN REGION AND ITS RELATIONSHIP TO GOLDLEADZINC ORE DEPOSITS
     额尔古纳地区中生代应力场演化及其与金铅锌矿的关系
短句来源
     In Ergun region the volcanic activities are very violent in Mesozoic era ,the volcanic rocks are mainly formed in late Jurassic to early Cretaceous (150-100Ma).
     额尔古纳地区中生代火山活动强烈,其主要的活动期间为晚侏罗世至早白垩世(150~100Ma)。
短句来源
     Study on Geo thermal History in Mesozoic Era of ZQ Depression in Zhangwu Area
     彰武地区中生代张强凹陷地热史研究
短句来源
     In Mesozoic,the activity of Chengbei fault,Chengbei 20 fault,Chengbei 30 north fault and their sub-faults developed in Chengdao area take the dominant position,and the main faults generally experience a negative reversion process.
     结果表明,埕岛地区中生代以埕北断层、埕北20断层、埕北30北断层及其派生断层活动为主,主断层的发育演化普遍经历了由逆到正的构造负反转过程;
短句来源
     Geochemical Characteristics of Eclogite Xenoliths in Mesozoic Intrusive Complex from Xu-Huai Area and Its Tectonic Significance
     榴辉岩类捕虏体的地球化学特征及其构造意义——来自徐淮地区中生代侵入杂岩中的信息
短句来源
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  在中生代
     On this premise, the uplifting ratio of the Taihang tectonomagmatic belt in Mesozoic era is 0 421 ̄0 253mm/a,and the uplifting height is 8799 ̄5288m.
     在这个前提下,太行山构造岩浆带在中生代时期的抬升速率为0.421~0.253mm/a,隆升高度为8799~5288m。
短句来源
     ④fracture tectonic of Era Paleozoic continuedto grow in Mesozoic era and fold formation in EW direction.
     ④古生代断裂构造在中生代继续生长以及东西向褶皱的形成。
短句来源
     This superimposed fold interface image of discordant axial trace (E-W and NE) developed in the Cretaceous continental basin suggests that the basin could have been the result of tectonic inversion and progressive deformation in Mesozoic under special boundary conditions when the area was controlled by the active continental margin of East China. 
     这种发育在田坂陆相红盆中的以E—W向和NE向两组不同轴迹方向相复合的褶皱叠加干扰图像的成因可能是在盆地所处的特殊边界条件下,受中国东部大陆边缘活动带的控制,导致田坂盆地在中生代末发生构造反转及递进构造变形作用的结果。
短句来源
     In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
     在中生代,该盆地的形成与演化受特提斯构造带的控制。
短句来源
     In Mesozoic, due to oblique subduction of Pacific plate toward Asian continent plate at a low angle, the tectonic patterns of Eastern China changed from E-W direction to NE and NNE.
     在中生代时期,太平洋板块向亚洲大陆板块东缘低角度斜向俯冲,导致中国东部由EW向构造体制转变为NE、NNE向构造体制。
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  西藏中生代
     Sedimentary Evolution of the Coqen Basin in Mesozoic
     西藏中生代措勤盆地的沉积演化
短句来源
  中生代
     Based on simulation of EASY % Ro,paleogeothermal gradient was 4. 29℃/100m in Mesozoic and 3. 3℃/100m in Paleogene in Jiyuan Depression.
     通过EASY%Ro模拟计算,济源凹陷中生代地温梯度为4.29℃/100m,新生代古近纪地温梯度约为3.3℃/100m;
短句来源
     The eclogite gravels,which are found in Mesozoic Fenghuangtai and Maota nchang Formations in the north margin of the Dabie Orogenic Be lt,are rich in K 2 O(1.21%),∑REE(278μg /g),LILE(such as Rb,Ba,K and Th),and(La /Yb ) N ratio(14.4),on the basis of the analysis of major elements,rare earth elements(REE)and trace elements.
     大别造山带北缘中生代地层凤凰台组和毛坦厂组中榴辉岩砾石的主元素、稀土元素以及微量元素具有如下特征,主元素中K2O富集(1.21%),高∑REE(278μg/g),高(La/Yb)N(14.4)和大离子亲石元素(LILE,如Rb、Ba、K和Th等)富集。
短句来源
     In Mesozoic era,the basin had different developing stages of primary rifting(T 3-J 1),peripheral foreland basin(J 2-J 3)and retroarc foreland basin(K 1-K 2) Thousands meters Mesozoic strata was developed in the northern downwarped zone.
     中生代盆地演化上经历了初始裂谷 (T3— J1 )、周缘前陆盆地 (J2 — J3)、孤后前陆盆地 (K1 — K2 )等阶段。
短句来源
     On this premise, the uplifting ratio of the Taihang tectonomagmatic belt in Mesozoic era is 0 421 ̄0 253mm/a,and the uplifting height is 8799 ̄5288m.
     在这个前提下,太行山构造岩浆带在中生代时期的抬升速率为0.421~0.253mm/a,隆升高度为8799~5288m。
短句来源
     Sedimentary Characteristics of the Yanqi Prototype Basin in Mesozoic Era and the Determination of the Basin Boundaries
     焉耆中生代原型盆地沉积特征与盆地边界的确定
短句来源
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      in mesozoic
    Updating and Recoding Enamel Microstructure in Mesozoic Mammals: In Search of Discrete Characters for Phylogenetic Reconstructio
          
    New Studies of Enamel Microstructure in Mesozoic Mammals: A Review of Enamel Prisms as a Mammalian Synapomorphy
          
    Changes in Mesozoic paleogeography also appear to clarify several other puzzling aspects of early angiosperm history and distribution, including their early appearance at middle latitudes.
          
    Dasycladaceae are important indexfossils in Mesozoic shallow-water limestones of Romania.
          
    Gravitational deformations in mesozoic rocks of the carpathian mountain ranges
          
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    Based on the data collected in the recent years by the scientific expedition in the Qinghai-Xizang region, the principal structural features of Himalayas and Qinghai-Xizang Plateau are discussed from viewpoint of plate tectonic theory.In the light of a lot of data, such as on the geological history, the sedimentary characteristics, the distribution of Gondwana sedimentary facies, ophiolite suite, melange and exotic blocks, the crustal deformation nature, the regularity of magmatic activity and paired metamorphic...

    Based on the data collected in the recent years by the scientific expedition in the Qinghai-Xizang region, the principal structural features of Himalayas and Qinghai-Xizang Plateau are discussed from viewpoint of plate tectonic theory.In the light of a lot of data, such as on the geological history, the sedimentary characteristics, the distribution of Gondwana sedimentary facies, ophiolite suite, melange and exotic blocks, the crustal deformation nature, the regularity of magmatic activity and paired metamorphic belt on both sides of Yarlung Zangbo River, this work deals with the pattern and nature of plate motion, makes a subdivision of Himalayan orogeny and gives a preliminary analysis of its character as well.A possible model on formation of Qinghai-Xizang Plateau by multi-underthrusting and multi-matching is presented and it is suggested that the Bangong Co-Dongqiao tectonic belt can probably serve as the northern boundary of Gondwana land. And we propose a new mechanism that the Yarlung Zangbo Jinag tectonic belt was opened in Mesozoic and closed in Early Tertiary.

    本文根据近年来对青藏高原广泛开展的考察所积累起来的实际材料,以板块构造观点,简要讨论了青藏高原主要构造特征。文章以地质历史、沉积特征、冈瓦纳相沉积、蛇绿岩套、混杂岩和外来岩块的分布、变形特征、岩浆活动的规律以及雅鲁藏布江两侧变质带的特点,论证了喜马拉雅地区板块活动的方式和特征,对喜马拉雅运动进行了分期并对各期运动的性质作了分析。文章提出了冈瓦纳大陆的北界可能是班公湖—东巧构造带以及雅鲁藏布江构造带在中生代拉开、早第三纪闭合机制的新设想。

    The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system. In general,...

    The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system. In general, this paper deals with only the Shenyan-Qingyuan section.

    浑河断裂带在前震旦纪就开始活动,中生代时期活动剧烈,至第三纪和第四纪初、浑河断裂带的构造活动更为频繁强烈。本文主要讨论浑河断裂带自沈阳至清原县草市地段从第三纪以来的新构造活动的一些形迹。

    Based on the vicwpoint of "Comparative historical Geology" , it is pointed out in this paper that the developing history of the crust in the north of Jiangxi Province can be divided into threestages. In chronological order they are the stage of geosyncline, the stage of platform and the stage of mobilization of structural magma i.e.Diwa. Seven source-beds, which possessed differential formational types, were formed during the differential periods of the first and second stage. The source-beds provided material...

    Based on the vicwpoint of "Comparative historical Geology" , it is pointed out in this paper that the developing history of the crust in the north of Jiangxi Province can be divided into threestages. In chronological order they are the stage of geosyncline, the stage of platform and the stage of mobilization of structural magma i.e.Diwa. Seven source-beds, which possessed differential formational types, were formed during the differential periods of the first and second stage. The source-beds provided material base for the ore magma of the third stage. When the ore magma intruded into those source-beds once again, it often produced industrial complex deposits with composite geneses.The mobilization of structural magma within the third stage was connected closely with "active epicontinental" of the western pacific in Mesozoic Era. The NW trending large basal fault belts with tension shearing, which crossed the strike of "active epicontinental", are usually the important matallographic provinces in that time

    本文用“地质历史分析”的方法,指出江西省北部地壳先后经历过:地槽、地台、地洼三个发展阶段。前两个阶段的不同时期,形成了七个建造类型不同的“矿源层”,为第三阶段的含矿岩浆提供了物质基础,当这种岩浆侵入到矿源层中时,常能形成多因复成矿床。 第三发展阶段与中生代西太平洋的“活动陆缘”密切相关,与活动陆缘走向横切的北西向张剪性基底大断裂带,常是重要的成矿带。

     
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