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rapid uplifting
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  快速隆升
     The original summit surface or regional planation surface was mainly formed in 15~8 Ma, followed by extensional faulting and rapid uplifting of Nyainqentanghla mountains in 8~4 Ma. The Yangbajain Damxung rift belt began to form high angular normal faulting and rifted depression in 2~1.5 Ma, followed by NW trending strike slip faulting and formation of the present day river system since 1.4 Ma or so.
     原始山顶面或高原主夷平面主要形成于 15~ 8Ma ,念青唐古拉山脉开始快速隆升与两侧地块初始断陷时代为 8~ 4Ma ,羊八井 当雄 谷露盆地快速裂陷事件发生于 2~ 1.5Ma ,区域NW向走滑断裂与现今河流峡谷主要形成于 1.4Ma以来。
短句来源
     The composition and texture of the metamorphic core complex show features of symmetrical extension and asymmetric uplifting and a rapid uplifting period within 130 to 100 Ma.
     变质核杂岩的组成与结构显示了它对称伸展和不对称隆升的特征 ,130~ 10 0 Ma是其快速隆升的时期。
短句来源
     After undergoing the tectonic motions and butt jointing of south north continent in Tethys stages, the collision between continent and continent in Upper Cretaceous period and Eocene epoch, the formation of plateau rudiment in Oligocene epoch and Miocene epoch, and the intra continental deformation of rapid uplifting since Pliocene epoch, the geomorphic landscape of "high massive flattish" Qinghai Tibet Area is formed.
     并且青藏地区在经历了特提斯阶段的几次构造运动及南北大陆对接以后的白垩纪末 -始新世陆 -陆碰撞、渐新世 -中新世高原雏形的形成和上新世以来高原快速隆升的陆内变形作用以后 ,就形成了今天这种“高、大、平”的独特地貌景观。
短句来源
     Some 21 Ma ago asthenospheric upwelling resulted in partial melting of the underplated mafic rocks under the conditions of metamorphic garnet_amphibolite facies and rapid uplifting of the southern plateau.
     约21Ma前,由于软流圈物质上涌,同时造成了底侵镁铁质岩石部分熔融形成含矿岩浆和地壳快速隆升;
短句来源
     To combine zircon U-Pb SHRIMP age of Qinghe gneiss and ~(40)Ar/~(39)Ar ages of hornblende and biotite from Erqishi shearing zone,important kinetic events,including tectonics,metamorphism and fast cooling or rapid uplifting in Altai orogen during late Paleozoic were revealled. This precise and credible zircon SHRIMP age of the Qinghe gneiss possibly provides a primary evidence for study on time limit of closure of Paleo-Asia Ocean and continental thrust during the late Paleozoic.
     额尔齐斯构造剪切带中青河片麻宕的锆石U-Pb年龄,以及各种变质岩中角闪石和黑云母的~(40)Ar/~(39)Ar年龄,记录了阿尔泰造山带晚古生代时期一次重要的构造、变质作用、快速隆升的动力学过程,为研究晚古生代古亚洲洋的闭合或大陆的回返时限提供了初步的证据。
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  “rapid uplifting”译为未确定词的双语例句
     (4) similar rapid uplifting experience since 25 Ma, especially since 10 Ma;
     (4 )2 5Ma以来 ,特别是 1 0Ma以来两地都经历了快速剥露和隆升作用 ;
短句来源
     5) It has a isothermaldecompression (ITD) path and about 200 - 300Mpa decompression, which suggest continent -continent collision and a rapid uplifting.
     5)具等温降压的PT轨迹,并有200-300MPa的压力降,具有陆-陆碰撞的特征;
短句来源
     The negative correlation between the FTA and sample elevations shows there was rapid uplifting during the continent-continent collision with uplifting rate of 176m/Ma.
     磷灰石裂变径迹年龄与样品高程呈负相关关系 ,表明陆 -陆碰撞伴随有快速的抬升 ,其抬升速率为 176m/Ma。
短句来源
     These ages indicate that the mineralizing system in Xiongcun results from the intervallic relaxation (ca. 52~40 Ma) of the Himalayan-Tibetan orogen and the final telescoping from the proceeding rapid uplifting (40~38 Ma) of the orogen.
     但雄村矿床的最终套生定位,与造山带40~38Ma间的强烈挤压隆升有关。
短句来源
     The youngest single grain age is clustered at 23-26 Ma, revealing a rapid uplifting process at this time, it may correspond to the unconformity between the Paleogene and Neogene.
     最小单颗粒年龄集中在23~26Ma,反映了一次快速抬升,对应于这一地区上、下第三系之间的不整合.
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  相似匹配句对
     A rapid
     本法简便、快速,结果准确.
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     With the rapid development of the
     愿本文能为《公司法》的修改稍尽微薄之力。
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     Xo Qu River Valley has been in rapid uplifting accompanied by climate becoming worse.
     硕曲河谷在中更新世末期以来一直处于快速隆升状态,伴随快速隆升,乡城地区硕曲河谷受湿热气流影响减弱,导致气候与环境向着日趋恶化的方向演化
短句来源
     The Cretaceous Sedimentary Environments of Changtu Sag and Its Implications for the Rapid Uplifting of Yan Liao Orogen
     昌图凹陷白垩纪沉积环境对燕辽造山带隆升过程的指示
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  rapid uplifting
On one of the nights it appears that the rapid uplifting of the F-layer in the post-sunset period, in conjunction with gravity wave activity at mesospheric heights, resulted in generation of very strong plasma bubble irregularities.
      


The preliminary exploratory results about the basic-ultrabasic rocks of the Karakoram and western Kunlun Mts. are reported in this paper. The Kudi ultramafic rock bodies belong to the Alpine-type associations in general, but there are some differences between the Kudi bodies and the typical ophiolitic metamorphic peridotites in petrochemistry. At present, there is insufficient evidence to make a full interpretation of the formation of these bodies. The Middle Proterozoic metamorphic volcanics in Akazi section...

The preliminary exploratory results about the basic-ultrabasic rocks of the Karakoram and western Kunlun Mts. are reported in this paper. The Kudi ultramafic rock bodies belong to the Alpine-type associations in general, but there are some differences between the Kudi bodies and the typical ophiolitic metamorphic peridotites in petrochemistry. At present, there is insufficient evidence to make a full interpretation of the formation of these bodies. The Middle Proterozoic metamorphic volcanics in Akazi section may have originated in a strongly attenuated continental lithosphere. According to the discriminations of the rare element and REE geochemistry the Upper Proterozoic metamorphic mafic lavas in Yixikgou section probably are formed at a Mid-ocean ridge and present truce oceanic lithosphere. Late Paleozoic volcanics may have erupted in a continental margin area. Relative strong continental volcanic activity existed in Cenozoicera, in which especially the Quaternary continental floor volcanics may be related to the rapid uplifting of the Qinghai-X izang plateau. The occurrences, petrological and geochemical characteristics and erupting stages of the volcanics found in southern Kunlun Mts. have been discussed in detail in the paper.

本文报道了考察区若干基性-超基性岩体的初步考祭结果。库地岩体属于传统观念的阿尔卑斯型岩体,但与典型蛇绿岩中的变质橄榄岩有所差异;阿卡兹、一些克沟蚀变火山岩可能发育在大洋环境,而晚古生代火山岩大概是在大陆边缘喷出的。本区在新生代时期陆相火山活动相当频繁,其分布规律和岩石特征表明它们与青藏高原的隆升有密切的关系。文中还讨论了昆仑山南侧新生代火山岩喷发的期次。

The present-day physical denudation rate (PDR) and chemical denudation rate (CDR) ateach observational station located in the main river drainage areas of Hainan Island was cal-culated from extensive data (1959—1988) of suspended-particle loadings,total dissolved sclilloadings and the water-flow for the rivers.The average physical denudation rate for HainanIsland is 13.99 mg/cm~2·a and the average chemical denudation rate is 15.97 mg/cm~2·a.(?)ngeneral,the PDR and CDR for Hainan Island are much lower than those...

The present-day physical denudation rate (PDR) and chemical denudation rate (CDR) ateach observational station located in the main river drainage areas of Hainan Island was cal-culated from extensive data (1959—1988) of suspended-particle loadings,total dissolved sclilloadings and the water-flow for the rivers.The average physical denudation rate for HainanIsland is 13.99 mg/cm~2·a and the average chemical denudation rate is 15.97 mg/cm~2·a.(?)ngeneral,the PDR and CDR for Hainan Island are much lower than those for Taiwan Island(the average PDR of Central Range of Taiwan Island is at least 1365mg/cm~2·a and the CDRfor the western part of Taiwan Island is 65 mg/cm~2·a and for the eastern part of TaiwanIsland is 38mg/cm~2·a).The intensive denudation of Taiwan Island is related with the extreme-ly abundant precipitation and waterflow with the rapid uplift of the Central Range sincethe Pliocene.Li Yuanhui pointed out that the high denudation rate of the Central Rangetoday is the direct consequence of the rapid upward movement of the Taiwan Island,but therapid denudation of the Central Range,in turn,aids further uplift of the Island by an isosta-tic adjustment.The discharge rate of dissolved matter is always higher than that of the par-ticular matter in the Hawaiian rivers when the river runoff is relatively low.The CDR byriver water is almost the lowest.The CDR by groundwater is little higher.So the totaldenudation rate of the Hawaiian Islands ranges from 11 to 50mg/cm~2·a,and is similar tothose of Hainan Island.

本文根据1959—1988年水文和水质资料计算了海南岛河流多年平均物理侵蚀率(13.99mg/cm~2·a)和化学侵蚀率(15.97mg/cm~2·a)。此二值大大低于台湾岛河流侵蚀率的数值,主要原因是“台湾岛自上新世以来一直处于迅速上升运动中”。夏威夷群岛河流的物理侵蚀率和化学侵蚀率很低,但由于那里的玄武岩孔隙的渗透性强,其地下水的化学侵蚀率较高,所以地表水和地下水的总化学侵蚀率与海南岛相比不相上下。

It has been confirmed that the Quaternary dust-fall accumulation,called loess in NorthChina and Xiashu soil in the middle and lower reaches of Changjiang River,was caused mainlyby shifting and deposition of material through the force of strong north wind during ice ages ofthe Pleistocene in eastern China.One of the principal features for the Pleistocene dust-fall accumulation is its clear changein spatial distribution with the lapse of time.For example,the loess accumulation formed dur-ing the early Pleistocene...

It has been confirmed that the Quaternary dust-fall accumulation,called loess in NorthChina and Xiashu soil in the middle and lower reaches of Changjiang River,was caused mainlyby shifting and deposition of material through the force of strong north wind during ice ages ofthe Pleistocene in eastern China.One of the principal features for the Pleistocene dust-fall accumulation is its clear changein spatial distribution with the lapse of time.For example,the loess accumulation formed dur-ing the early Pleistocene migrated from the border belt of the present Loess Plateau (from about(?)°E) eastwards to the foot of the Xinganling,Yanshan,Taihang and east Qinling Mts (toabout 121°E).It was expanded to the western side of Liaodong and Shandong Peninsulas,sou-thern Jiangsu and Anhui Provinces (from about 34°N to 31°N) in the Middle Pleistocene,then to the eastern side of Liaodong Peninsula,shelf,area of Huanghai Sea which was emer-ged as land in the full-glacial stage,and the region around the Poyang Lake south of theChangjiang River (about 28°N) in the Late Pleistocene.Similarly,the grain size of the Pleistocene dust-fall accumulation increases regularly fromthe early to late Pleistocene at the same site and from the northwest to southeast for the sametime.It is shown that the intensity of winter monsoon increased continually from the glacialperiod of the earlp to late Pleistocene in eastern China.It was stated up to now that the East Asia Monsoon,called the sea-land monsoon,resultedfrom the pattern of sea-land distribution and the disparity of the thermodynamic effect betweensea and land.But,the changes of monsoon intensity during the Quaternary,especially fromthe end of early Pleistocene to the beginning of the middle Pleistocene,show that the pat-tern of monsoon circulation is under the influence of other factors.The most important factor isconsidered as the increasingly rapid uplift of the Qinghai-Xizang Plateau as a whole since thebeginning of Quaternary.The uplift of the Plateau has been strengthening the winter monsoonin East Asia in the following three aspects.1) the emerging of plateau monsoon,2) the strength-ening of the Mongolian-Siberian cold high pressure,and 3) the increased orographic di-version of westerly and even more deflection of its northern branch southward after it roundedthe Plateau.Another factor is the cooling of global climate since the middle and late Ceno-zoic,which has increased the influence of sea-land distribution and morphologic elevation onatmospheric circulation,especially in the middle latitude zone.

历史时期的雨土及近代尘暴的研究证实,风尘堆积与冬半年强冷气流活动有关。中国东部第四纪风尘堆积(黄土和下蜀土)分布的时、空变化及其粒度的不断增粗表明,第四纪以来冬季风强度是不断增加的。季风强度的变化主要与青藏高原越来越快的整体隆升有关。青藏高原上升产生了高原季风,并对西风气流和蒙古冷高压发生影响,即从三方面对季风起到增强作用。另一方面是中新生代以来地球气候变冷,使中、高纬地带的海陆分布和地形对大气环流有更大的影响。

 
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