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红色
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  “红色”译为未确定词的双语例句
    CHARACTERISTICS OF GENETIC MINERALOGY OF RED-CLAY TYPE OF GOLD DEPOSIT
    红色粘土型金矿成因矿物学特征
短句来源
    The natural ones contain water which represents absorbing apices on the area of 1500-1700 cm-1 and 3000-3700 cm-1, while dying ones and heat-treated ones are not.
    利用红外光谱可以准确地鉴别天然红色翡翠、染色红色翡翠和烧制红色翡翠,天然红色翡翠中有水的存在,在1500-1700±cm~(-1)、3000-3700±cm~(-1)有强的吸收区,而染色翡翠和烧制翡翠中不含水,在以上区域没有强吸收。
短句来源
    In hand specimens Mg-sarcopside is yallowish pink,and browish pink,in colour with glassy luster. It has Mohs’5.5-6.0.Its pecity gravity is 3.18 g/cm3.The mineral is biaxial Ng=1. 734 ,Nm=1.728,Np=1.675,R>γ.
    镁斜磷铁锰矿为肉红色块状体,玻璃光泽,摩氏硬度5.5-6.0,比重3.81,具(001)解理,在单偏光下无色或带有灰色的白色,多色性弱,突起较高,Ng=1.734,Nm=1.728,N_P=1.675,Ng-N_P=0.059,斜消光,R>Υ。
短句来源
    Pink granite was intruded in a WSW-ENE direction into the upper crust from Tianzhen to Xigeyu in 2144-2087 Ma.
    此后,在2144—2087Ma期间红色花岗岩侵位,形成花岗岩带。
短句来源
    Some researchers considered the granite to be genetically related to the gold deposit. Zircon SHRIMP dating of pink albite dyke in the mining area is 1 858±8 Ma ( 207Pb/ 206Pb) and the dating of Qingshankou granite 199±2 Ma( 206Pb/ 238U).
    应用先进的 SHRIMP测年技术 ,测得肉红色钠长岩脉的锆石 w (2 0 7Pb) / w (2 0 6Pb)年龄为 (185 8± 8) Ma,青山口花岗岩体锆石 w(2 0 6Pb) / w(2 3 8U )年龄为 (199± 2 ) Ma。
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As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments, We Know...

As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments, We Know that there a peneplanation developed on the older rocks of Nanshan till pper pliocene, and the red deposits which extended over the Nansban and its adjacent regions Were laden down in the same time. Probably laterly, a crusalt movement, which included mul iple uplifts, initiated. The present geomorphic features of Nanshan are possibly resulted from them. as the dissected summit-levels, the remnants of old peneplains Can be found on many mountain tops today. As regards quaternary glaciations of Nanshan, a more important sign ification should be ascribed to the uplifts of this mountain. Perhaps boh because of the uplifts and the Climatic changs, in Nanshan two glacio pluvial periods had occured in quaternary. When the glaciers expanded all of the mountain peaks and valleys. Later on, the glacio fluvial waters were Carrying much debris and forming sedimentary units, which have been called inland molasse formation, into piedmont plain. a distinct interval, which indicat a true interglacial stage, have been found in that formation. The following table shows the main geological changes of Cenozoic of Nanshan.

河西走廊之南延伸着雄伟的祁连山,在过去20年中一些学者曾对该山的地貌和其第四纪冰期作过一些探讨。根据本人的野外工作及最近的文献资料,我们看到,在构造运动、地貌循环和相关沉积三者之间有着紧密的联系,因而,它们可以相互解释。分析岩相和新生代沉积的分布,我们得知直到上上新世,祁连山进行着准平原化的过程,同时并沉积下红色沉积,它遍及祁连山内外。后来,地壳运动开始,它包括多次上升。现代的祁连山的面貌即是多次上升的产物。古准平原的遗跡,目前可在许多山顶发现。祁连山的第四纪冰期的发生,山地上升占有重要地位,可能正是由于上升和气候变化的同时作用,祁连山发生两次冰期——多雨时期。当时冰川遍及山峰和谷地,稍后,冰融水携带大量碎屑物质带入山足平原形成内陆磨拉石建造的沉积。在该沉积岩系中发现有一清楚的间断,这代表一次真正的间冰期。祁连山新生代的主要地质事件见84页附表。

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...

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。

Charaters of Yanan group and Zhiluo group of Jurassic system in Jiaoping, Shanxi Province are discussed in aspects of lithology, lithofacies, cycle, and evolution.

本文从岩性、岩相、旋回及演化等方面讨论陕西焦坪侏罗系延安组和直罗组的沉积特征。岩性特征表明,延安组属灰色复陆屑建造,直罗组为红色复陆屑建造。根据沉积剖面结构、成因标志划分出河床滞留、河床、天然堤、决口扇、河漫滩、洪泛平原和岸后沼泽等相,组成具二元结构的旋回。作者重点剖析J_(1-2)y_2和J_2Z_1二段的剖面结构,确定前者为高弯度河,后者为低弯度河。延安组属于气候温湿、沼泽发育的冲积平原,后期转向半干旱气候。古河流由低弯度河向高弯度河,接着又向小型高弯度河方向演化。低弯度河两侧利于成煤。直罗组属半干旱气候的冲积平原,演化特征与上述情况相似,但无沼泽沉积。总之,本区随着构造向稳定状态发展,建造由构造控制转变为古地理控制。

 
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