助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   tectonic sedimentary 的翻译结果: 查询用时:0.008秒
图标索引 在分类学科中查询
所有学科
地质学
石油天然气工业
更多类别查询

图标索引 历史查询
 

tectonic sedimentary
相关语句
  构造沉积
     Zhifang region of East Junggar oregenic belt can be divided into five tectonic sedimentary provinces,which are:Ertai,Kaokesaiergai,Beitashan,Kelamaili and Bogoda.
     东准噶尔造山带纸房地区自晚志留世—泥盆纪可划分为哈甫提克山、绵脊梁、色克森巴依、塔克札勒、博格达五个构造沉积区。
短句来源
     On the map,divides the QTP and its adjacent regions into 2 tectonic domains (the special grade units),5 acient plates(the first units),4 suture zones and 9 sheets(the second grade units),and 9 deep &big shell or curtain thrusts(include suture zone)and 45 tectonic sedimentary settings with clear plate tectonic characters and close contributing factors(the third grade units). It provides a new model of studying the regional plate tectonics.
     该图将青藏高原及邻区划分为 2个构造域 (特级单元 )、5个古板块 (一级单元 )和 4条缝合带、9个板段 (二级单元 )及 9条深大壳幔断裂 (含缝合带 ) ,45个板块构造特征明显、成因联系密切的构造沉积环境 (三级单元 ) ,为区域板块构造研究提供了一个新范型。
短句来源
     The authors studied structure and deposition setting which formed reservoir forming dynamic system in Dongpu Depression, and classified the depression into two large tectonic sedimentary cycles and five evolutional periods.
     分析了形成东濮凹陷成藏动力学系统的构造沉积背景 ,将东濮凹陷划分为 2个大的构造沉积旋回和 5个演化阶段。
短句来源
     By the continental dispersion, the spreading of ocean, the drift and the collision of the continental plates, the oceanic subduction and destruction, crustal uplift, orogenesis, the continental-continent collision and the depession in continent, the complited tectonic sedimentary environment and the plate tectonic units were formed in the processing of long geological historic evolution.
     在漫长的地史演化过程中,大陆裂解和大洋扩张,大陆板块的飘移与碰撞,洋壳俯冲与大洋消亡,地壳隆升与造山,陆陆碰撞及陆内裂陷等活动频频发生,形成了极其复杂的构造沉积环境及板块构造体系。
短句来源
  构造-沉积
     From the geologic point of view, land desertification in Northern China is mainly controlled by geologic backgrounds such as tectonic sedimentary characteristics, hydro geologic conditions, global climatic changes, especially the monsoon current in East Asia,which were formed since the ascent of the Qinghai Tibet plateau.
     中国北方土地荒漠化主要受青藏高原隆升以来形成的构造 -沉积特征、水文地质条件、全球气候变化、尤其是亚洲季风等地质背景控制。
短句来源
  “tectonic sedimentary”译为未确定词的双语例句
     Especially Yanshan movement curtain Ⅱ and Ⅲ, and Himalayan movement affected the tectonicevolution in the basin. Furthermore these two movements controlled holistic tectonic sedimentary pattern of the basin.
     认为盆地中、新生代以来发生了二次大规模的构造运动,即印支运动、燕山运动和喜马拉雅运动,尤其是燕山运动晚期和喜马拉雅运动对盆地的构造演化起着深远的影响,这两次运动控制着盆地的总体构造、沉积格局。
短句来源
     In order to summarize the rules of hydrocarbon accumulation and distribution in Ordos Basin objectively, it is necessary to research the tectonic sedimentary evolution and the accumulation of natural gas.
     以含油气盆地整体、动态、综合分析研究为原则; 以古亚洲、特提斯、滨太平洋三大构造域交切、叠合和复合,控制和影响着鄂尔多斯盆地在不同构造演化阶段的形成和发育为指导思想。
短句来源
     In this thesis,writer take the north steep slope zone of Dongying Dpression as target area and take Sha III- and Sha IV Member as purpose stratum, study on tectonic,deposition and reservoir,emphasesing on analying of forming of dynamic background of tectonic,sedimentary sequence and pool-forming.
     本文以东营凹陷北部陡坡带为研究区以沙三-沙四段为主要目的层位,通过开展东营凹陷北部陡坡带构造、沉积、储层等为基本内容的基本地质特征研究,重点对东营凹陷北部陡坡带构造、沉积层序以及成藏动力学背景进行了深层次探讨。
短句来源
     The principal strata exposed in the central sector of the Da Hinggan Mountains are the Permian marine volcanic sedimentary series,which constitutes the main host rocks of copper polymetallic deposits. It has higher abundances of the ore forming elements Cu,Pb,Zn,Ag and Sn and thus is the important source of major ore forming substances. The spatial temporal distribution of different deposit types is closely related to the Early Permian tectonic sedimentary environment.
     二叠纪海相火山沉积岩系是大兴安岭中段出露的主要基底地层,是铜多金属矿床的主要赋矿围岩,其中成矿元素Cu、Pb、Zn、Ag、Sn均具有较高的丰度值,是形成矿床的重要物质来源,而不同矿床类型的时、空分布与早二叠世古构造沉积环境密切相关
短句来源
     The high frequency T-R cyclical sequences superimposing on the tectonic sedimentary cycle lacked the Type I sequence boundary because of the steep margin of the fault basin and the little change of lake level Main factors controlling the development of the T-R cycle are the episodic movement of structure(fault)and the higher frequence T-R cycle is related to Milankovitch climate cycle.
     由于断陷湖盆的边缘坡度陡峭,以及湖平面升降幅度有限,因此,叠加于构造-沉积族目之上的更高频T-R旋回层序缺乏I型层序边界,控制T-R旋回发育的主要因素是区内构造(断层)的幕式活动,而更高频的T-R旋回的形成则与米兰柯维奇气候旋回相关联。
短句来源
  相似匹配句对
     ON THE TECTONIC EVOLUTION OF SEDIMENTARY BASINS IN SOUTHEASTERN CHINA
     中国东南地区沉积盆地的构造演化
短句来源
     THE TRIASSIC SEDIMENTARY-TECTONIC EVOLUTION IN SOUTHERN XIZANG
     西藏南部三叠纪沉积-构造演化
短句来源
     and tectonic movement.
     (3)与深部地质作用有关;
短句来源
     Criticize and Tectonic
     批判与建构
短句来源
     sedimentary conditions.
     在沉积上、构造上有独特之处。
短句来源
查询“tectonic sedimentary”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  tectonic sedimentary
The largest deposits are hosted by breccias of tectonic sedimentary, volcanic or phreatomagmatic origin.
      


Deposition is usually controlled by tectonic movements. The so-called tec-tonic-sedimentary facies is the sedimental facies that are controlled by varioustectonic factors in different tectanic units and evolution stages. In the JizhongDepression, the factors controlling the deposition include followings: 1. differen-tial vertical movements and their strengths; 2. paleotopography is controlledby synsedimentary structures; 3. paleotopography is controlled by gravitationaltectonic, and 4. lake level...

Deposition is usually controlled by tectonic movements. The so-called tec-tonic-sedimentary facies is the sedimental facies that are controlled by varioustectonic factors in different tectanic units and evolution stages. In the JizhongDepression, the factors controlling the deposition include followings: 1. differen-tial vertical movements and their strengths; 2. paleotopography is controlledby synsedimentary structures; 3. paleotopography is controlled by gravitationaltectonic, and 4. lake level undulation resulted from the tectonic events. The tectonic unites of the Jizhong Depression are very clear in stripped dis-tribution. As the basement uplifted gradually from west to east, the depo-centermoved correspondingly. Accorrding to its characteristics, the depression mightbe divided into three tectonic belts, i.e. a stable subsident belt; an alter-nated belt of elevation and subsidence and the last one that subsided first andthen uplifted. Correspondingly, there are three tectonic-sedimentary facies, i.e.,1. stable subsidence lake facies; 2. alternating fluvial-lake facies: and 3. flu-vial facies with first subsiding, soon elevating. On the tectonic unit of depression, there are six types of the tectonic-sedimentary facies: 1.shore-shallow lake facies of lake-depression; 2. deep-hemideeplake facies of lake-depression; 3. submarine fan of steep slopes or/and faultedscarps; 4. gravitative slumping along the steep faults; 5. subequeous fan ongentle slope; 6. delta facies on gentle slope. According to the structure of paleo-1ake basin, the depression might be di-vided into enclosed fault depression: semi-enclosed fault depression and non-enclosed fault depression. They correspond to three tectonic-sedimentary facies inthe Jizhong Depression as stated above. The first two are favourable for hydro-carbon accumulation, but the last one is not.

本文以构造-沉积相的概念,划分了冀中坳陷下第三系构造-沉积相的类型,论述了在次级构造因素控制下沉积相带在时间、空间上的分布规律。 冀中坳陷由东向西划分为三个构造-沉积相带。冀中坳陷的14个小凹陷,分属上述三带。由于次级构造因素的控制,文中提出8种不同类型的、各具特色的构造-沉积相。 根据凹陷的结构特征将其分为封闭式、半封闭式和非封闭式三种盆地结构类型。

In this paper, based on the field work in 1988, the authors suggested some ideas about late Jurassic to Cretaceous sedimentary-tectonic development of the southern Xizang as follows.The Upper Jurassic and Lower Cretaceous in southern Xizang could be divided into five tectonic-sedimentary area, they are: 1. north Himalaya area, which was the north continental margin of the Gandwanalandj 2. Larguigan-gri area, corresponding to the continental slope; 3. Yarlung Zangbo area, representing...

In this paper, based on the field work in 1988, the authors suggested some ideas about late Jurassic to Cretaceous sedimentary-tectonic development of the southern Xizang as follows.The Upper Jurassic and Lower Cretaceous in southern Xizang could be divided into five tectonic-sedimentary area, they are: 1. north Himalaya area, which was the north continental margin of the Gandwanalandj 2. Larguigan-gri area, corresponding to the continental slope; 3. Yarlung Zangbo area, representing the oceanic basin of the 'Himalaya-Tethys'; 4. Xigaze area, which was the forearc basin in front of the Gangdesi magmatic arc; 5. Lhasa area, dominated by the late Jurassic to Cretaceous intraarc basin.During late Jurassic, with the spreading of 'Himalaya-Tethys and the thinning of the crust in this area, a deep-water oceanic basin was formed. In the both side of the oceanic basin, the different continental margins occurred. In Himalaya area of the south side, a series of stable-type clastic and carbonate sediments accumulated on the continental shelf, in which the carbon-ate-plateform facies and tidal-flat facies were dominant. Northward, in the Larguigangri area there were some deeper water sediments, represented by siliceous rocks, deep-water red mudstone and carbonate rocks, which implied the incompensated sedimentation on the continental slope. Meanwhile, some deep-water deposits, such as radiolaria- bearing abyssal mudstone and siliceous rocks accumulated in Yarlung Zangbo area, associated with a large number of ophiolites and olistostromes, marked the position of a oceanic basin. Above mentioned showed that the sea-water gradually deepened from south to north, and the tectonic-paleogeographical framework was of a transition from the shallow sea of continental shelf through deeper sea of continental slope to the abyssal oceanic basin, all of which indicated the future of a passive continental margin on the south side of 'Himalaya-Tethys' ocean. On the north side, across the Gangdise magmatic arc, some carbonate-plate-form type limestone of Duodigou Formation accumulated in the Lhasa intraarc basin.In early Cretaceous, the extension of 'Himalaya-Tethys' reached the maximum, which led to widespread deepen of sea water. In Himalaya area, for example at the Gucuo section, we could find the early Cretaceous thick black shale with a lot of large ferriconcretions, reminicent of the Oceanic Anoxic Event in Mid-Cretaceous of the world. At the same time, we might see some thick black shale, siliceous shale with large number of pyrite, yielding belemnite and ammonoides in Larguigangri area, in which there were many deepwater sedimentary structures,such as submarine slides and olistostromes, representing the deep-water deposition on the continental slope. To the north, lower Cretaceous was characterized by deep-water sediments of oceanic basin as upper Jurassic. But there were a series of onshore -nearshore ocal-bearing clastic and shallow sea shelf carbonate-clastic rocks of early Cretaceous in Lhasa intraarc basin, in which included also some delta and tidal-flat deposits.By late Cretaceous, while the'Himalaya-Tethys'ocean subducted northward, the southern Xizang remained the tectonic-sedimentary framework as previous, but the sea-water began to shallow, particularly in Himalaya area, that the deep-water black shale was replaced by the shallow sea shelf-facies carbonate-terristrial clastic rocks. In the same time, some flysch deposits, represented by the Ngamring Formation, accumulated in Xigaze forearc batin. It is worthy to point out that there were some distinctive sedimentary structures such as groove marks, load casts and graded sequenced in lower part of Ngamring Formation, indicating the deep-water turbidite flysch deposits. But in its upper part, the ripple marks, storm graded bedding and shallow water trace fossils were discovered, showing that sedimentary environment of upper part had been rather shallow sea than deep-water, and the basin had begun to uplift in middle late Cretaceous. It may be suggested that the collision of the Himal

根据岩石组合特征、沉积构造和沉积相序的分析,结合岩石化学测试数据和粒度分析结果,将西藏南部的晚侏罗世一白垩纪地层划分为5个沉积区,从南往北依次为:喜马拉雅陆棚-外陆棚沉积区;拉轨岗日斜坡沉积区;雅鲁藏布深海盆地沉积区;日喀则弧前盆地沉积区;拉萨弧间盆地沉积区。进一步确定了西藏南部沉积与构造演化的时空关系。

1. Lakes in Yunnan and Tibet plateaus, which developed along with regional deep-great belts during Pliocene and Early Pleistocene are of unity and synchronism in spacial and temporal distribution. These lakes were formed by tensional faults with regional upheaval and dissociation of Yunnan Plateau, as a result of collision of Indian Plate with Tibet Plate.2. According to the comprehensive analysis of spore-pollen, molluska, ostracoda, age dating of paleomagnetic, 14C and uranium series, and sedimentary...

1. Lakes in Yunnan and Tibet plateaus, which developed along with regional deep-great belts during Pliocene and Early Pleistocene are of unity and synchronism in spacial and temporal distribution. These lakes were formed by tensional faults with regional upheaval and dissociation of Yunnan Plateau, as a result of collision of Indian Plate with Tibet Plate.2. According to the comprehensive analysis of spore-pollen, molluska, ostracoda, age dating of paleomagnetic, 14C and uranium series, and sedimentary sequence obtained from deep cores, it can be found that the strata may be regarded as a continue accumutation in 3.4Ma including the periods of upper Pliocene, Pleistocene and Holocene. The evolution process of lake basin shows a shallow-deep-shallow environmental change.3. The largest thickness and rate of sedimnt in fault basin are not located in their geometrical center, but in one side near the main fault. For the sedimentation pattern of the fault basin, there exist two transport systems, longitudinal and lateral, the latter can be divided into steep slope and gentle slope. All these features show that the sedimentary process was controlled by fault action in the lake basin.4. Tectonic-sedimentary evolution in fault basin has experienced the following general trend: limnology stage of preliminary tension, deep water stage of strongly sagging period and shallow water stage of late filling period, lithologically experienced: coarse-fine-coarse. Different models of sediment can be formed in each stages.

对取自1980—1986年的样品分析表明:云南断陷湖泊自上新世随着区域性隆起断裂拉张形成以来,经历了裂陷早期沼泽、深陷期深水、充填后期浅水的构造-沉积演化阶段,揭示了深水湖泊以重力流为特色;中等水深湖泊横向搬运以重力流、纵向搬运以三角洲为特色;浅水湖泊以河流三角洲为特色的沉积模式。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关tectonic sedimentary的内容
在知识搜索中查有关tectonic sedimentary的内容
在数字搜索中查有关tectonic sedimentary的内容
在概念知识元中查有关tectonic sedimentary的内容
在学术趋势中查有关tectonic sedimentary的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社