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block mountain
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  断块山
     Lushan is the most typical block middle-low mountain in Shandong. The paperexpounds in detail the primary geomorphic characteristics of this block mountain ,the drainagepattern and feature of the valley,and the stepped geomorphic structure composed by three levelsof denudation surfaces within the mountain,Finally in this paper,the mountain is distinguishedinto 7 geomorphic types.
     鲁山是山东最具代表性的断块构造中一低山地.作者对该断块山地地貌的基本特征、山地中的水系及河谷发育、山地的层状地貌结构作了较详细的论述,将山地区划分了七种地貌类型.
短句来源
     Taishan Mountain is a young fault block mountain,being of an age of about 30 Ma.
     泰山作为一个年轻的断块山 ,其年龄仅 30 Ma左右。
短句来源
     Based on practical data about rock block mountain,rolling loess land(pluvial tableland),flat loess land(pluvial fan skirt)and terrace,the relation between geomorphological structure in the Weihe basin zone and active faults and neotectonic movement is studied.
     根据基岩断块山地、波状黄土塬 (洪积台地 )、平缓黄土塬 (洪积扇裙 )、阶地等较多实际资料 ,研究渭河盆地带地貌结构与活动断裂及新构造运动间的关系。
短句来源
  “block mountain”译为未确定词的双语例句
     Nitrate-ores of Tulufan-Hami basin, Xinjiang, distributes in Quaternary period deposit and saline brine in the seg of Santang lake- Naomao lake (the northern part), the seg of Tulufan-Hami (the middle part), the Kumishi seg and the depression and basin in Kuluketage-Xingxingxia block mountain(the southern part).
     新疆吐鲁番-哈密地区硝酸盐矿床分布在三塘湖-淖毛湖山间坳陷(北区),吐鲁番-哈密 山间坳陷(中区),库米什山间坳陷及库鲁克塔格-星星峡断垄内山间洼地及断陷盆地(南区)的第 四系沉积物及盐湖卤水中。
短句来源
  相似匹配句对
     Block and Z.
     B lock和Z.
短句来源
     EXPLORING BLOCK FIELD IN THE TAIBAI MOUNTAIN
     秦岭太白山地区石海探密
短句来源
     Cold Mountain
     冷山
短句来源
     Cold Mountain
     《冷山》
短句来源
     Gypsum block
     石膏砌块
短句来源
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  block mountain
In the eastern Cordillera we are not dealing with an orthogeosyncline, but with a fault-block mountain system.
      


It is suggested that North Xinjiang is not a Hercynian geosynclinal fold belt at the present stage, but a new type mobile region, diwa (geodepression) region, which has passed through geosynclinal and platform stages. The present-day mountains are not the primary mountain ranges from the Hercynian Geosyncline, but the secondary ones, block mountain ranges, created by Mesozoic-Cenozoic diwa tectonism. A triangle-shaped Precambrian basement may be present under the Junggar Basin, and the Mesozoic-Cenozoic...

It is suggested that North Xinjiang is not a Hercynian geosynclinal fold belt at the present stage, but a new type mobile region, diwa (geodepression) region, which has passed through geosynclinal and platform stages. The present-day mountains are not the primary mountain ranges from the Hercynian Geosyncline, but the secondary ones, block mountain ranges, created by Mesozoic-Cenozoic diwa tectonism. A triangle-shaped Precambrian basement may be present under the Junggar Basin, and the Mesozoic-Cenozoic tectonic movements controlled the formation of oil and gas pools.

北疆地区一般认为属海西地槽褶皱带,但据作者等研究,本区现阶段不是海西地槽褶皱带。而是经历了地槽阶段、地台阶段之后转化而成的新型活动区——地洼区。 现今所见的天山、东准噶尔、西准噶尔山系和阿尔泰山,并非海西期地槽所形成的第一代褶皱山脉,而是由于中,新生代的地洼构造活动使后海西期地台活化再升所造成的第二代山脉——地洼断褶山脉。 本区中部(准噶尔盆地)地壳较薄,约38—41公里,一般向四周逐渐加厚,显示盆地下面为幔隆,据资料分析,准噶尔盆地可能有一前寒武纪刚性基底存在,它是构成北疆地壳结构不均一性的主要成分,它对北疆构造的形成,对该盆地的演化,起着重要作用。而与地幔有紧密联系的“壳幔混熔层”的存在和北疆各壳块的相互挤压作用,无疑都是控制北疆地洼区形成演化的重要因素。 本区具有多阶段的生储盖组合。其中以地槽阶段者和地台阶段者有利。中、新生代的构造运动对油气藏的形成起着控制作用。 本区以构造为主的复式油藏最为常见。不论其形成的时代如何,都不同程度地受到地洼构造运动的影响和改造。找油的主要对象对准噶尔盆地来说是白垩系以下的隐伏构造。

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed....

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed. The Wuyi Mountain has developed into the following morphological types under the control of the geological structures and the morphological development: cuesta, block mountain, hill, gentle hill, flat-bottomed alley valley, depressed valley, terrace, etc. The Jiuqu River developed mainly along east-west and north-south strike faults, and so, it is a very meandering river.

武夷山位于福建崇安南部,面积60平方公里,山区海拔180~720米。著名的九曲溪全长9.5公里。武夷山原为剥蚀区,白垩纪初期断落下陷成为一个长条形湖盆。湖盆堆积层厚达1500米。新第三纪湖盆被挤压回升,形成单斜断块山。武夷山受构造和发育过程影响,形成以下地貌类型:单面山、块状山、丘陵、缓丘、平底巷谷、坳谷、二级阶地、一级阶地、砾石边滩和心滩、河道等。九曲溪主要是沿东西和南北向断裂发育,比较曲折。

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed....

The Wuyi Mountain is situated in the south of Chongan County, Fujian Province. It covers an area of 60 km~2, and the altitude is between 180 m and 720 m. The length of the famous Jiuqu River is 9.5 km. The Wuyi Mountain was originally a plain of denudation. It developed into a lake basin by the subsidence of the earth's crust in the early Cretaceous period. The thickness of the deposit in the lake has reached 1500m. Owing to uplifting in the late Tertiary period, a monoclinic block mountain was formed. The Wuyi Mountain has developed into the following morphological types under the control of the geological structures and the morphological development: cuesta, block mountain, hill, gentle hill, flat-bottomed alley valley, depressed valley, terrace, etc. The Jiuqu River developed mainly along east-west and north-south strike faults, and so, it is a very meandering river.

武夷山位于福建崇安南部,面积60平方公里,山区海拔180~720米。著名的九曲溪全长9.5公里。武夷山原为剥蚀区,白垩纪初期断落下陷成为一个长条形湖盆。湖盆堆积层厚达1500米。新第三纪湖盆被挤压回升,形成单斜断块山。武夷山受构造和发育过程影响,形成以下地貌类型:单面山、块状山、丘陵、缓丘、平底巷谷、坳谷、二级阶地、一级阶地、砾石边滩和心滩、河道等。九曲溪主要是沿东西和南北向断裂发育,比较曲折。

 
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