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
   海进-海退旋回 的翻译结果: 查询用时:0.286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
 

海进海退旋回
相关语句
  “海进-海退旋回”译为未确定词的双语例句
     Compared with the transgressive regressive cycles of the Late Devonian Frasnian in the southern Guizhou Province in China and the globe, the cyclic sequences were well developed in Wangguangou formation of upper Devonian in Shangnan area, And meantime, on the basis of the regional stratigraphy correlation, it is suggested that the upper part of Wangguangou Formation be absent.
     通过详细的旋回层序研究以及与中国黔南和世界晚泥盆世弗拉斯阶海进-海退旋回进行比较研究,并结合区域地层对比研究,商南地区上泥盆统王冠沟组旋回发育不完整,推测可能地层发育不全。
短句来源
  相似匹配句对
     Quaternary Transgressions in Shanghai Region
     论上海地区的第四纪海进
短句来源
     A new transgressive model
     一种新的海进模式
短句来源
     HOLOCENE TRANSGRESSIVE-REGRESSIVE SEQUENCE IN YANGTZE DELTA AREA
     全新世长江三角洲地区的海进海退层序
短句来源
     Trimsgression,Regression and Ancient Climatic Environment in the Littoral of Bohai Sea since Pleistocene Epoch.
     晚更新世以来渤海湾沿岸的海进海退及古气候环境
短句来源
     Holocene Ostracoda Assemblages and Marine Transgression-Regression Cycle in the Northwestern Coastal Area of the Bohai Gulf
     渤海湾西北岸全新世介形类组合特征及海进海退旋回
短句来源
查询“海进-海退旋回”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。
  transgressive-regressive cycle
The sediments accumulated in the distal part of the epiplatformal basin as a symmetrical transgressive-regressive cycle.
      
The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by Middle Pleistocene rocks belonging to a transgressive-regressive cycle.
      


This report relates to some branch of learning, e. g. biostratigraphy, petrostratigraphy, petrography of fossil, palaeoecology, sedimentology , palaeoclimatology, palaeomagnetism, minerology etc. It is a acadomic and synthetical study.

根据岩石组合,古生物组合,沉积构造及剖面结构,将贵州早二叠世沉积相划分为四个相区、九个相带,它们是: 1.滨岸漫滩沼泽相 Ⅰ.陆地边缘相区 2.潮汐泥坪相 3.潮坪沼泽相 4.半局限台地相带 Ⅱ.碳酸盐台地相区 5.开阔台地相带 6.较深水台沟相带 7.碳酸盐合地边缘生物滩相带 Ⅲ .碳酸盐台地边缘相区8.碳酸盐台地边缘生物礁相带   Ⅳ.浅海盆地相区 9.浅海陆棚相带。 贵州早二叠世经历了一个完整的海进海退旋回,茅口早期是最大的海侵期,就沉积的演化而言,它大体经历了两个阶段。即第一阶段(栖霞早期)系清水和浊水混合的缓坡型沉积,其特征是:1.碳酸岩与碎屑岩共同发育;2.碳酸盐台地边缘礁滩相不发育。第二阶段(栖霞晚期至茅日晚期)为清水碳酸盐台地沉积,特征是:1.主要为碳酸盐岩,2.碳酸盐台地边缘生物滩礁带发育。

Mizhi intra-platform depression developed on the broad shallow water carbonateplatform in Ordos epeiric sea during Early Ordovician.The area of the depression is about 70000 km~2.It was formd by the combined effect of both the differential subsidence of theplatform interior and the rise of sea level.The evolution process can be divided into threeperiods(lower Majiagou,upper Majiagou and Fengfeng).Each period can be subdividedinto three stages.The first stage differential subsidence occurred in the platform interior,and...

Mizhi intra-platform depression developed on the broad shallow water carbonateplatform in Ordos epeiric sea during Early Ordovician.The area of the depression is about 70000 km~2.It was formd by the combined effect of both the differential subsidence of theplatform interior and the rise of sea level.The evolution process can be divided into threeperiods(lower Majiagou,upper Majiagou and Fengfeng).Each period can be subdividedinto three stages.The first stage differential subsidence occurred in the platform interior,and sea level rose;the second stage,intense differential subsidence and evident rise of sealevel resulted in formation of Mizhi intra-platform depression;the third stage,differentialsubsidence weakened gradually,the sea level fell,and the depression was filled.Theevolution of Mizhi depression underwent three large-scale transgressive-regressive changesand formed three supercycles and three stratigraphic sequences corresponding respectivelyto lower Majiagou,upper Majiagou and Fengfeng Formations.Three perfect source-reservoir-cap assemblages were formed from the dark organic-rich micrite at the top ofthe transgressive limb of each supercycle to the evaporite at the upper part of the regres-sive branch.Mizhi intra-platform depression is a gas-bearing sag because of high organicmaturation.Recently,the significant discovery of gas in Fengfeng sequence indicatesthat intra-platform depression has great potential to accumulate gas.The gas accumulatedin porous dolomite reservoirs related closely to palaeokarst.A geological model shows thatfour types of stratigraphic traps existed in the depression.

早奥陶世在广阔的鄂尔多斯浅水陆表海碳酸盐台地内发育了米脂内台地坳陷。它是由台地内部差异沉降和海平面上升的共同作用下形成的。坳陷经历了三次主要的海进—海退旋回,构成了三套生储盖组合。坳陷的构造稳定性决定了其圈闭型式以地层圈闭为主。作者建立了该坳陷发育的地质模型,并提出其可能存在的四种地层圈闭类型。

The 3-D pattern on sequential stratigraphy proposed by Vail et. al (1988, 1989) can be considered as a basis on which their new idea of sequential stratigraphy is established. It is the same pattern relying on which they make stratigraphic and lithologic interpretations. As a matter of fact, such a pattern does not go beyond the scope of the conventional geological concepts yet, and it also does not substantially differ from the classic cycle sequence pattern of marine onlap and regression with the exception...

The 3-D pattern on sequential stratigraphy proposed by Vail et. al (1988, 1989) can be considered as a basis on which their new idea of sequential stratigraphy is established. It is the same pattern relying on which they make stratigraphic and lithologic interpretations. As a matter of fact, such a pattern does not go beyond the scope of the conventional geological concepts yet, and it also does not substantially differ from the classic cycle sequence pattern of marine onlap and regression with the exception of terminology.

维尔等人(1988,1989)提出的层序地层立体模式,可以说是他们的层序地层学新概念立论的基础,也是他们赖于进行地层和岩相解释的依据。然而,这一模式的实质,仍未超越传统地质概念的范畴。除了术语上的差别外,它与经典的海进-海退旋回性层序模式没有根本的差别。

 
<< 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海进-海退旋回的内容
在知识搜索中查有关海进-海退旋回的内容
在数字搜索中查有关海进-海退旋回的内容
在概念知识元中查有关海进-海退旋回的内容
在学术趋势中查有关海进-海退旋回的内容
 
 

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