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east guangdong area
相关语句
  粤东地区
     Waterproofing Technique of Highway Tunnel in East Guangdong Area
     粤东地区公路隧道的防水技术
短句来源
     According to the geological and climatic condition of East Guangdong area, and combining the waterproofing principle of highway tunnels, this paper probes into the mode of waterproofing of highway tunnels, construction measures ensuring waterproofing quality.
     针对粤东地区地质、气候条件情况,结合公路隧道的防水原则,探讨该地区公路隧道的防水形式以及保证防水质量的施工措施。
短句来源
  相似匹配句对
     b and Guangdong N.
     b ,以及广东株N .
短句来源
     BEACHSOLL AND ITS UTILIZATION IN EAST GUANGDONG
     粤东海涂土壤及其利用
短句来源
     b, Guangdong N.
     b和日本株N .
短句来源
     THE MANGROVE IN COAST OF EAST GUANGDONG PROVINCE
     粤东的红树林
短句来源
     Discussion on the Development of the Coastal Area in the East Guangdong
     粤东沿海地区的区域发展
短句来源
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Among villages in East Guangdong area,clan power has been influential and is now under reconstruction.Clan organizations are expanding its power into admistration at local levels and worse still,a few of them are developing towards vicious power,which has brought about mass events in some places and hidden trouble to social security.Thus,only by solving these problems and enhancing the administrative ability at villages and towns,can the development tendency of clan power be fundamentally restrained.

粤东农村是一个宗族势力活跃的社区, 宗族势力现今还在不断重建, 宗族组织不断渗透地方基层组织, 个别地方宗族势力还向黑恶势力发展, 引发了个别地方的群体事件, 给社会治安带来隐患。只有加快改革, 切实解决“三农”问题, 提高农村基层的执政能力, 才能从根本上抑制宗族势力的抬头。

According to the geological and climatic condition of East Guangdong area, and combining the waterproofing principle of highway tunnels, this paper probes into the mode of waterproofing of highway tunnels, construction measures ensuring waterproofing quality.

针对粤东地区地质、气候条件情况,结合公路隧道的防水原则,探讨该地区公路隧道的防水形式以及保证防水质量的施工措施。

The Nanling belt is distributed on the strong folded-deformed basement and developed the largest scale Early Mesozoic granitoids and rifting basins in South China. The basement is composed of the metamorphosed Neoproterozoic—Ordovician flysch-volcanic series and the non-metamorphosed Late Devonian—Early Triassic sedimentary rocks. Five regional fault zones were recognized, which are closely related to tectonic evolution of the Nanling belt, including the Pingxiang—Guilin, the Longyan—Haifeng, the Ganjiang River,...

The Nanling belt is distributed on the strong folded-deformed basement and developed the largest scale Early Mesozoic granitoids and rifting basins in South China. The basement is composed of the metamorphosed Neoproterozoic—Ordovician flysch-volcanic series and the non-metamorphosed Late Devonian—Early Triassic sedimentary rocks. Five regional fault zones were recognized, which are closely related to tectonic evolution of the Nanling belt, including the Pingxiang—Guilin, the Longyan—Haifeng, the Ganjiang River, the Chaling—Guangchang and the Wuzhou—Sihui that affected the size, distribution and attitude of Meso-Cenozoic basins. Both material source and geodynamical setting forming the Nanling belt were constrained by the Dabie orogenic belt to the north and the Indosinian orogenic belt to the southwest. Three sub-EW trending granitic zones occupied this belt and were controlled by deep-seated structure and shallow-seated folding-faulting. The ages of bodies in the three granitic zones show a migrate trend from west to east and become younger toward Pacific direction. The sub-EW trending Mesozoic granitoid zones were developed along the fault zones of paleo-Tethys tectonic regime, magmatic doming extensional tectonics and metamorphic core complex occurred in the intersection of two group faults. Mesozoic—Cenozoic basins were divided into three types, namely the T_3—J_1 para-foreland basin, the J_2 rifting basin and the K_1—Paleogene fault-depression basin including the K_1 volcanic accumulation basin and the K_2—Paleogene fault depression basin. The pre-Mesozoic basins were mainly affected by Tethys regime and Indosinian tectonic event, the basins since Cretaceous were co-constrained by both Pacific regime and intral-continental deep-seated tectonic-magmatism. Studied results suggest that the Wuyishan belt is a Late Mesozoic geographic and paleo-climate boundary, the Ganjiang River fault is a western boundary of the Late Mesozoic volcanic zone and the Western Fujian—Southern Jiangxi—East Guangdong area was a sub-EW trending Middle Jurassic intra-continent rifting zone. The Mesozoic—Cenozoic basins and granitic ranges have an evident connection of space-time and origin, they co-built the South China basin and range tectonic system. Four coupling types of basin and range were recognized, namely thrusting type, strike-slip type, extensional faulted depression type and unconformity type. Finally, pre-Mesozoic tectonism, Indosinian tectonic event and transposition of two tectonic regimes were discussed. Geological facts and studied data don't support the viewpoint that a Late Pasleozoic ocean existed in the eastern South China. The basins that were formed between J_2 and J_3 display distinctly differences on the mechanical nature, rock assemblages and stress field, which is an important mark of tectonic transposition from the Paleo-Asian-Tethys regime to the Pacoific regime. The eastern Nanling belt is one of the best candidates of tectonic transposition position.

南岭构造带发育在强烈褶皱变形的基底之上,发育了华南地区最大规模的早中生代花岗岩和裂谷盆地。基底由变质的新元古代—奥陶纪复理石-火山岩系和未变质的晚泥盆世—早三叠世沉积岩系所组成。与南岭带构造演化关系最为密切的区域断裂带有萍乡—桂林、龙岩—海丰、赣江等5条,制约着中、新生代岩体和盆地的分布、规模和产状。无论是物质来源还是形成与演化的动力学背景,南岭构造带均离不开其北面的大别造山带和南西面的印度支那造山带。南岭地区存在3条近东西方向的花岗质岩带,严格受深部构造制约,岩体常受褶皱和断裂构造控制。3个花岗岩带中的岩体时代,具有横向上北老南新、走向上西老东新、朝大洋方向年轻化的迁移演化规律,中生代东西向的花岗岩带是在古特提斯构造域近东西向的断裂带基础上发育的,岩浆热隆伸展构造和变质核杂岩多数发育在两组大断裂的交汇处。在研究区厘定出3种基本盆地类型,晚三叠世—早侏罗世发育类前陆盆地,中侏罗世发育裂谷盆地,早白垩世属火山-沉积断陷盆地,晚白垩世以来则几乎全是箕状断陷盆地。前中侏罗世盆地构造主要受特提斯构造域和印支期碰撞的影响,晚侏罗世以来盆地构造则主要受太平洋构造作用和陆内深部构造的联合制约。武夷山是晚中生代的古地理与气候...

南岭构造带发育在强烈褶皱变形的基底之上,发育了华南地区最大规模的早中生代花岗岩和裂谷盆地。基底由变质的新元古代—奥陶纪复理石-火山岩系和未变质的晚泥盆世—早三叠世沉积岩系所组成。与南岭带构造演化关系最为密切的区域断裂带有萍乡—桂林、龙岩—海丰、赣江等5条,制约着中、新生代岩体和盆地的分布、规模和产状。无论是物质来源还是形成与演化的动力学背景,南岭构造带均离不开其北面的大别造山带和南西面的印度支那造山带。南岭地区存在3条近东西方向的花岗质岩带,严格受深部构造制约,岩体常受褶皱和断裂构造控制。3个花岗岩带中的岩体时代,具有横向上北老南新、走向上西老东新、朝大洋方向年轻化的迁移演化规律,中生代东西向的花岗岩带是在古特提斯构造域近东西向的断裂带基础上发育的,岩浆热隆伸展构造和变质核杂岩多数发育在两组大断裂的交汇处。在研究区厘定出3种基本盆地类型,晚三叠世—早侏罗世发育类前陆盆地,中侏罗世发育裂谷盆地,早白垩世属火山-沉积断陷盆地,晚白垩世以来则几乎全是箕状断陷盆地。前中侏罗世盆地构造主要受特提斯构造域和印支期碰撞的影响,晚侏罗世以来盆地构造则主要受太平洋构造作用和陆内深部构造的联合制约。武夷山是晚中生代的古地理与气候分隔带;赣江带是晚中生代的火山岩界线;闽西—赣南—粤东地区存在一个近东西向的中侏罗世陆内裂谷带。区内存在3种盆-岭耦合类型:挤压逆冲型(少量)、走滑剪切型(少量)和伸展拆离型(大量)。中、新生代盆地构造和花岗岩山岭有着密切的时空与成因联系,共同构成了华南盆岭构造体系。最后对前中生代构造作用、印支期构造事件、两种构造体制的转换等问题进行了探讨。晚泥盆世—中三叠世研究区为浅海—滨海环境,几乎没有岩浆活动,龙潭期曾区域抬升为陆,地质事实不支持华南东部存在晚古生代深海洋盆的观点;南岭地区J2和J3之交形成的两类不同力学性质、岩石组合、应力场特征的盆地构造,是特提斯向太平洋构造域转变的宏观标志;南岭东段是这两种构造体制叠置和转换的重要位置之一。

 
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