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
   生物礁型 的翻译结果: 查询用时:0.14秒
图标索引 在分类学科中查询
所有学科
更多类别查询

图标索引 历史查询
 

生物礁型
相关语句
  reef type
     The old dolomitic type oil pool developed in the intraplatform limestone strata of the Permian Maokou Formation is formed in the interior part of the attached platform, and is marked by oil indication and is obviously different to those old oil pools of sponge reef type.
     这些古油藏大多以沥青显示为主,特别是发育在连陆台地边缘以及孤立台地上的二叠系海绵生物礁型古油藏。
短句来源
     The founding of giant oil-gas fields in the craton basin of West China shows that the Ordovician of Tazhong area in Tarim Basin is the major exploration target for reef type of oilfields,the Cambrian oils beneath the salt-rocks and in the good dolomite reservoirs are also expected to be found.
     中国西部克拉通盆地寻找大油田的情况表明,塔里木盆地塔中地区奥陶系是生物礁型油田的主要勘探方向,寒武系的盐下及白云岩储层中的油气值得关注;
短句来源
  “生物礁型”译为未确定词的双语例句
     So we should pay more attention to the domination of the global regularity of organic evolution on the development of reefs besides that of regional tectonic evolution as we look for reef-type oil and gas reserviors in southern China.
     因此在南方寻找生物礁型油气藏时,除了应当重视本区构造演化的控制作用外,还应极大地注意全球性生物演化规律的控制作用。
短句来源
     The exploration of Ordovician carbonate rocks in Tazhong area began in 1989, but the large Ordovician Condensate Gas Field was discovered in TZ-ⅠBreak Slope until 2005, in which there are more than 150 million tons of proved and controlled reserves in-place. The field is also the first Ordovician carbonate reef field in China.
     塔中奥陶系碳酸盐岩的勘探始于1989年,直至2005年发现塔中Ⅰ号坡折带奥陶系碳酸盐岩凝析气田,探明加控制石油地质储量1.5×108t(油当量),是我国目前发现的第一个奥陶系生物礁型大油气田。
短句来源
  相似匹配句对
     (3)D shape.
     D
短句来源
     (2)C shape;
     C ;
短句来源
     THE REERS OF CHANGXING PERIOD AND THE REEF GAS ACCUMULATION IN SICHUAN BASIN
     四川盆地长兴期生物礁及礁气藏
短句来源
查询“生物礁型”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
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  reef type
The distribution of all gases, especially methane and hydrogen, show peak concentrations coincident with the PGE and gold reef type horizons.
      
The currents also appear to be responsible, in part, for marked orientation and elongation of patch reefs in a north-west/ south-east direction and for a gradation of patch-reef type across the study area.
      
Two basic types of reef can be discerned, one dominated by Porites lutea and faviid species and the other by Montipora ramosa and Acropora aspera, reef type apparently being governed by the degree of exposure to water movement.
      
"Serpulid/algal/cement reefs", developed in the upper part of the section, represent a new subtype of "algal/cement reefs", a special reef type restricted to the Artinskian to Carnian time interval.
      
TheTubiphytes boundstones represent a particular reef type not yet described in detail from the Upper Jurassic.
      
更多          


The evolution underwent six main stages, possessing the characteristics of golbal organic evolution regularity. The reflection of its prosperity and decline is striking on the age distribution characters of the reefs. The first period of great prosperity in southern China was in the Early Devonian to the early phase of Late Devonian, 97 reefs in the peeriod have been found, and no one in the later Phase of Late Devonian (Famennian Stage)found up to now. The second period of that was the Permina , 148 reefs...

The evolution underwent six main stages, possessing the characteristics of golbal organic evolution regularity. The reflection of its prosperity and decline is striking on the age distribution characters of the reefs. The first period of great prosperity in southern China was in the Early Devonian to the early phase of Late Devonian, 97 reefs in the peeriod have been found, and no one in the later Phase of Late Devonian (Famennian Stage)found up to now. The second period of that was the Permina , 148 reefs in the Permian have been found. They are distinct in organic charac- ters. But no reef has been found in Early Trissic so far. Both of the times of no reef found coincide exactly with two great events of global organic extincition of F/F and T/P. So we should pay more attention to the domination of the global regularity of organic evolution on the development of reefs besides that of regional tectonic evolution as we look for reef-type oil and gas reserviors in southern China.

造礁生物演化经历了六个主要发展阶段,具有全球性演化规律特征,其盛衰变化在中国南方礁丘的时代分布上反映较为醒目。早泥盆世至晚泥盆世早期,为生物礁发育的首次鼎盛期,已发现的礁体达97个,而至今尚未发现晚泥盆世晚期(法门期)的生物礁;二叠纪是第二次鼎盛期,已发现该时期的礁丘达148个之多,生物特征明显,而至今也尚未发现早三叠世时期的礁体。中国南方这一礁丘时代分布特征恰好与 F/F和T/P两次全球性巨大生物绝灭事件相吻合。因此在南方寻找生物礁型油气藏时,除了应当重视本区构造演化的控制作用外,还应极大地注意全球性生物演化规律的控制作用。

Various types of the old oil pools are developed in the Late Paleozoic strata of the Dianqiangui area, those developed in reef rocks of Devonian and Permian are especially widespread. These old oil pools, especially for those belonging to sponge reef types that are developed in the margin of attached carbonate platform and on the isolated platforms, are almost characteristic of asphalt indications. The old dolomitic type oil pool developed in the intraplatform limestone strata of the Permian Maokou Formation...

Various types of the old oil pools are developed in the Late Paleozoic strata of the Dianqiangui area, those developed in reef rocks of Devonian and Permian are especially widespread. These old oil pools, especially for those belonging to sponge reef types that are developed in the margin of attached carbonate platform and on the isolated platforms, are almost characteristic of asphalt indications. The old dolomitic type oil pool developed in the intraplatform limestone strata of the Permian Maokou Formation is formed in the interior part of the attached platform, and is marked by oil indication and is obviously different to those old oil pools of sponge reef type. Apart from the potential source rocks that are constituted by deep water argilutites of interplatform basin, the hydrocarbon source for the old dolomitic type oil pool in Wudang of Guyang maybe come from the potential source rocks that are composed of the shallow platform dark limestone of the Permian Qixia Formation underlying the Maokou Formation.The stratigraphic position and the outputting features for this old dolomitic type oil pool indicate several regularities as follow: Firstly, two third-order sequences can be divided in the limestone strata of the Maokou Formation ; Secondly, the dolomitic type reservoir is frequently formed in the top part of the third-order sequence, which is genetically related to the shoaling process of sedimentary environment caused by the forced regression; Thirdly, in the process of both accumulation and migration of oil and gas the special oil pool of the stratigraphic-lithologic type could be formed in the top part of the carbonate third-order sequence. All of these features show that the finding of this old dolomitic type oil pool could provide an important clue for the future exploration of oil and natural gas.

在滇黔桂地区的晚古生界中发育各种类型的古油藏,尤其以泥盆系和二叠系的生物礁型古油藏最为引人注目。这些古油藏大多以沥青显示为主,特别是发育在连陆台地边缘以及孤立台地上的二叠系海绵生物礁型古油藏。发育在连陆台地内部的贵阳乌当二叠系茅口组白云岩型古油藏以油显示为特征,而与二叠系海绵生物礁型古油藏存在明显的区别。由于远离二叠系深水台盆相泥页岩系构成了潜在性烃源岩系,该古油藏的主要烃源可能来自浅水台地相的栖霞组暗色灰岩。该古油藏的产出特征和地层位置表明:在由大套灰岩组成的二叠系茅口组所构成的两个三级层序之中,与强迫型海退过程相关的环境变浅过程中常常有利于白云石化而形成白云岩型储集层,在相关的油气聚集与运移过程中形成较为特殊的地层和岩性油气藏,这为今后的油气勘探提供了具有一定价值的线索,因而具有较为重要的油气勘探意义。 

The exploration of Ordovician carbonate rocks in Tazhong area began in 1989, but the large Ordovician Condensate Gas Field was discovered in TZ-ⅠBreak Slope until 2005, in which there are more than 150 million tons of proved and controlled reserves in-place. The field is also the first Ordovician carbonate reef field in China. The main hydrocarbon pays are in the upper section of Lianglitage Formation (O2). The reservoir is composed of limestone of shelf-edged carbonate reef bank which is controlled by the break...

The exploration of Ordovician carbonate rocks in Tazhong area began in 1989, but the large Ordovician Condensate Gas Field was discovered in TZ-ⅠBreak Slope until 2005, in which there are more than 150 million tons of proved and controlled reserves in-place. The field is also the first Ordovician carbonate reef field in China. The main hydrocarbon pays are in the upper section of Lianglitage Formation (O2). The reservoir is composed of limestone of shelf-edged carbonate reef bank which is controlled by the break slope. The oil reservoir is a large stratified lithologic trap in which hydrocarbon is distributed along the long and narrow TZ-Ⅰ Break Slope. The exploration history of the field, the geological characteristics of the reservoir and the revelation to exploration are revealed.

塔中奥陶系碳酸盐岩的勘探始于1989年,直至2005年发现塔中Ⅰ号坡折带奥陶系碳酸盐岩凝析气田,探明加控制石油地质储量1.5×108t(油当量),是我国目前发现的第一个奥陶系生物礁型大油气田。油气的主力产层位于上奥陶统良里塔格组上部,储层为受坡折带控制的陆棚边缘礁滩体石灰岩。油气沿坡折带呈带状展布,为整体含油的大型准层状岩性油气藏。论述了塔中碳酸盐岩大油气田的勘探历程、主要地质特征,以及对海相碳酸盐岩勘探的启示。

 
<< 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生物礁型的内容
在知识搜索中查有关生物礁型的内容
在数字搜索中查有关生物礁型的内容
在概念知识元中查有关生物礁型的内容
在学术趋势中查有关生物礁型的内容
 
 

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