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红色建造
相关语句
  red formation
     They intrude into the red formation K_1n and river-lake facies Em, which are more basic than the Triassic granite and show characteristics of syncollision and volcanic arc granite.
     侵入于红色建造K1n及河湖相Em中,比三叠纪花岗岩更偏基性,地球化学特征显示同时具同碰撞及火山弧花岗岩性质。
短句来源
  “红色建造”译为未确定词的双语例句
     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.
     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。
短句来源
     In southwestern Henan,a series of Me sozoic-Cenozoic supracrustal faul t and basins are filled with red molasses-like formation in whic h contain aboundant oolithias of din osaurs,formed in the postorogenic s t age of the east Qinling orogenic belt,and controlled by the great and active NW-SE-trending strike-slip or thrust faults along one or two sides o f the basins.
     位于河南西南部的东秦岭造山带,在后造山阶段形成了一系列NW—SE向的中、新生代地壳表层断陷盆地,堆积了一套类磨拉石红色建造,含有丰富的恐龙蛋化石。 盆地两侧或一侧都有长期活动的大断裂控制,具有走滑、逆冲性质。
短句来源
  相似匹配句对
     Red
     红色(英文)
短句来源
     Fashionable Red
     红色当道
短句来源
     Regional Construction
     地区建造
短句来源
     Poetic Construction
     诗意的建造
短句来源
     Among which,there are the developed oil gas bearing formation,coal bearing formation and red continental clastic rock formation.
     其中发育有含油气建造、含煤建造红色陆相碎屑岩建造
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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。

In southwestern Henan,a series of Me sozoic-Cenozoic supracrustal faul t and basins are filled with red molasses-like formation in whic h contain aboundant oolithias of din osaurs,formed in the postorogenic s t age of the east Qinling orogenic belt,and controlled by the great and active NW-SE-trending strike-slip or thrust faults along one or two sides o f the basins.In these basins,there a re wide-opened folds,flexures and normal faults developed under the te ctonic stress fields of compression with local extension...

In southwestern Henan,a series of Me sozoic-Cenozoic supracrustal faul t and basins are filled with red molasses-like formation in whic h contain aboundant oolithias of din osaurs,formed in the postorogenic s t age of the east Qinling orogenic belt,and controlled by the great and active NW-SE-trending strike-slip or thrust faults along one or two sides o f the basins.In these basins,there a re wide-opened folds,flexures and normal faults developed under the te ctonic stress fields of compression with local extension or the alternating of transition during the late Yanshan(fromⅢ-V phases)and early Himalayan cycles.

位于河南西南部的东秦岭造山带,在后造山阶段形成了一系列NW—SE向的中、新生代地壳表层断陷盆地,堆积了一套类磨拉石红色建造,含有丰富的恐龙蛋化石。盆地两侧或一侧都有长期活动的大断裂控制,具有走滑、逆冲性质。盆内发育不同规模的舒展褶皱或突起,断层以正断层为主,规模较小,方向分散。盆地发展经历了燕山(Ⅲ-V幕)和喜山旋回两个阶段,构造应力场以总体挤压、局部拉伸为特征,且经历了多次挤压、拉张交替转化。

In Mesozoic-Cenozoic era, many medium-small-sized sedimentary basins had been formed in Yanbian draped-faulted region of Jilin Province. The basement of these basins is constituted of U-riched granite body produced during late Hercynian- early Yanshan period. Uranium-mineralization has been found in coal-bearing formation, oil-bearing formation and in tint layer of red formation. On the bases of analyzing of uranium source, geologic tectonic, palaeoclimatology, paleogeography, hydrogeology and reconstruction,...

In Mesozoic-Cenozoic era, many medium-small-sized sedimentary basins had been formed in Yanbian draped-faulted region of Jilin Province. The basement of these basins is constituted of U-riched granite body produced during late Hercynian- early Yanshan period. Uranium-mineralization has been found in coal-bearing formation, oil-bearing formation and in tint layer of red formation. On the bases of analyzing of uranium source, geologic tectonic, palaeoclimatology, paleogeography, hydrogeology and reconstruction, it is concluded that there is a prominent prospect to discover large in-situ sandstone-type uranium deposits in Yanji basins.

吉林省延边褶断区在中新生代时期形成了许多中、小型沉积盆地。盆地的基底主要为华力西晚期和燕山早期的富铀花岗岩体,盆地群中已发现含煤沉积建造中的铀矿化、含油建造中的铀矿化和红色建造浅色层中铀矿化。从铀源、地质构造、古气候条件、岩相古地理环境、水文地质、后生改造作用等方面分析,延吉盆地具有寻找大型地浸砂岩型铀矿的良好前景。

 
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