助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   扬子准地台 的翻译结果: 查询用时:0.201秒
图标索引 在分类学科中查询
所有学科
地质学
更多类别查询

图标索引 历史查询
 

扬子准地台
相关语句
  yangtze para-platform
     The diagenesis on the sandstones bitumen bearing in certain regions and sections of the southern margin,Yangtze Para-platform is discussed in this paper.
     本文对扬子准地台南缘一些地区和层段的含沥青砂岩的成岩作用进行了论述。
短句来源
  “扬子准地台”译为未确定词的双语例句
     12±2 Ma is the youngest age for granitoids in the Panxi rift zone and even in the whole Yangtze Paraplatform.
     (12±2)×10~6a的年龄值是攀西裂谷带内,甚至整个扬子准地台内最年轻的花岗岩年龄值。
短句来源
     Shanghai is at Abstract the northeastern end of the Yangtze paraplatform.
     上海地处扬子准地台的东北端。
短句来源
     -Distribution of "3Ni +Cr + V" in wide-spaced samples can distinctly reveal the boundary between the Yangtze paraplatform and the Caledonian fold symbol in Jiangxi.
     4.超低密来样品中“3Ni+Cr+V”的分布能较好地反映扬子准地台与华南加里东精皱系在省内的分界线。
短句来源
     The lower crust forms the fourth layer(about 36 km-Moho),which is thick in the west and thin in the east. The thickness of this layer gradually reduces from the Qinghai-Tibetan plateau to the Erdos platform and the Yangtze paraplatform with different velocity gradient at different location.
     第4层(埋深约在36 km—Moho)为下地壳,是一个契形层,总的趋势是西厚东薄,青藏高原较厚逐渐向鄂尔多斯地块和扬子准地台方向变薄,各处的地震波速度梯度不尽相同.
短句来源
     Northwest Yunnan is a situated in the zone of three geological tectonic unitsbounded by Yangtze Platfonn on-east, Garze fold system, and Shangjiang foldsystem on-west and southwest.
     滇西北地区地处三大地质构造单元交汇区,东部为扬子准地台,北部是甘孜褶皱系,西和西南是三江褶皱系。
短句来源
更多       
  相似匹配句对
     The author considers that there arethree subspecies of Neophocaena phocaenoides existing in the Chinese waters, thatis, N.
     亚种N.
短句来源
     Shanghai is at Abstract the northeastern end of the Yangtze paraplatform.
     上海地处准地台的东北端。
短句来源
     The Superimposed Fold Features of Yangtze Paraplatform of Yanshan Period in Guizhou
     贵州境内准地台燕山期叠加褶皱特征
短句来源
     Yangtze paraplatform is a major distribution region for geothermal anomaly.
     准地台区是本省地热异常的主要分布区。
短句来源
     The Activation of the Southwestern bordering of Yangtze Paraplatform and the forming of Youjiang Geosyncline
     准地台西南陆缘的活化与右江地槽的形成
短句来源
查询“扬子准地台”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
没有找到相关例句


The north part separated by Tanlu fault zone in Anhui province belongs to the North China Platform but the south part to the Lower Yangzi Quasi-platform They consist of thicker Meso-Paleozoic marine sediments. A series of Meso-Cenozoic continental deposit basins are developed on the different basement. Most of these marine and continental strata are rich in organic material, belong to a stable reducing environment and possess favourable conditions for oil-gas generation. The organic- material has highly been...

The north part separated by Tanlu fault zone in Anhui province belongs to the North China Platform but the south part to the Lower Yangzi Quasi-platform They consist of thicker Meso-Paleozoic marine sediments. A series of Meso-Cenozoic continental deposit basins are developed on the different basement. Most of these marine and continental strata are rich in organic material, belong to a stable reducing environment and possess favourable conditions for oil-gas generation. The organic- material has highly been matured. There have been found many kinds of oil-gas showings in Anhui province. which shows a better prospect for gas exploration.

安徽境内郯庐断裂带以北属华北地台,以南属下扬子准地台,它们是由巨厚的中、古生代海相沉积组成,其上发育了一系列中新生代陆相沉积盆地。这些海、陆相沉积的多数层位,有机质丰富,为稳定的还原环境,具良好的生油气条件,有机质成熟度高,省内已见多种类型的油气显示,展示了很好的天然气勘探前景。

Hunan is rich in fluorite mineral resources. According to the industrial type of mineral deposit, it can be classified into four classes: the veintype deposits found in the contact zone between magmatite and noncarbonate rock, the strata bound deposits of fluorite and fluorite-Pb-Zn ores found in carbonate rock, and the deposits formed by the epigene action of weathering. Each type of the above mentioned deposits, according to its pecularities, can be subdivided into a number of types. Hunan province is situated...

Hunan is rich in fluorite mineral resources. According to the industrial type of mineral deposit, it can be classified into four classes: the veintype deposits found in the contact zone between magmatite and noncarbonate rock, the strata bound deposits of fluorite and fluorite-Pb-Zn ores found in carbonate rock, and the deposits formed by the epigene action of weathering. Each type of the above mentioned deposits, according to its pecularities, can be subdivided into a number of types. Hunan province is situated between two first order structure units. The strata-bound fluorite mineral deposits are formed in the area of the Yangtze meta-platform, west of Tongdao-Xupu major fracture. Fluorite mineral deposits, the formation of which are controlled by the lithology, are formed in south China Caledonian-Indosinian Fold Belt, east of the major fault. The geological struc-ture, magma activity and stratigraphy plays an important role in controlling the formation of the deposits mentioned above. Fluorite is the most important fluorine-bearing mineral. Fluorine is abundant in the crust and universally participates in the pneumatolytic and hydrothermal processes of the formation of ore deposits during the granite magmatism and the later stage of evolution of the magma. It can form not only monofluorite mineral de-posit but also fluorite-polymetallic deposit. It is of significance to use fluorine as the direct or indirect basis to look for fluorite mineral deposits.

湖南省萤石矿产资源丰富,按矿床类型分四类:Ⅰ类产于岩浆岩和碎屑岩中的脉状充填萤石矿床;Ⅱ类产于酸性岩桨岩与碳酸盐岩接触带中萤石矿床;Ⅲ类产于碳酸盐岩中层控萤石矿床;Ⅳ类外生风化矿床。每类又按其矿床特征分若干亚类。矿石类型有单一萤石和伴生萤石两种。湖南省处于两个一级构造单元之间,以通道一溆浦大断裂为界,以西为扬子准地台区,形成层控萤石矿床,受构造—地层—碳酸盐岩联合控制;大断裂以东为华南加里东—印支褶皱带,形成岩控萤石矿床,受构造—岩浆岩—地层联合控制。

The diagenesis on the sandstones bitumen bearing in certain regions and sections of the southern margin,Yangtze Para-platform is discussed in this paper. It is suggested that the diagenesis in Majiang Anticline Belt is dominated dy early stage dolomite cementation and by the corrosion and replacement of dolomite in clasts. The late Guangxi movement caused the formation and then the successively upliftings of the anticline in the area. The axis of the anticline was eroded and eluviated by atmosphere fresh water,...

The diagenesis on the sandstones bitumen bearing in certain regions and sections of the southern margin,Yangtze Para-platform is discussed in this paper. It is suggested that the diagenesis in Majiang Anticline Belt is dominated dy early stage dolomite cementation and by the corrosion and replacement of dolomite in clasts. The late Guangxi movement caused the formation and then the successively upliftings of the anticline in the area. The axis of the anticline was eroded and eluviated by atmosphere fresh water, resulted the development of secondary pores in dolomites, which would be favourable for oil/gas accumulations. The maturities of sandstone minerals in the eastern flank of Majiang Anticline, Wuxi, Changshu and Huangqiao areas are rather high and the diagenesis are mainly quartz overgrowth and kaolinites filling the primary pores. The bitumen was filled into the residual primary pores of quartz overgrowth,so that the accumula-tion of oil/gas is unfavourable and poor.

本文对扬子准地台南缘一些地区和层段的含沥青砂岩的成岩作用进行了论述。指出麻江背斜中带的成岩作用以早期白云石胶结作用和白云石溶蚀交代石英碎屑为主,晚期广西运动使该区形成背斜并继续抬升,背斜轴部遭到剥蚀和大气淡水淋溶,致使白云石被溶蚀形成大量次生孔隙,利于石油储集;麻江背斜东翼和无锡、常熟、黄桥地区的砂岩矿物成熟度高,成岩作用以石英次生加大和高岭石充填原生孔隙为主,沥青充填在石英次生加大残留的原生孔隙中,储集条件略差;安吉康山及下扬子广大地区中上志留统的砂岩,由于浅变质泥岩屑含量高,它们在上覆巨厚地层压力下,表现为强烈的机械压实作用所引起的碎屑彼此镶嵌以及粘土杂基的充填,致使砂岩储集性能最差,仅能形成以构造断裂为主的脉状沥青。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关扬子准地台的内容
在知识搜索中查有关扬子准地台的内容
在数字搜索中查有关扬子准地台的内容
在概念知识元中查有关扬子准地台的内容
在学术趋势中查有关扬子准地台的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社