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陆相     
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  continental
     Recognition and Application of Remained Accommodation in Continental Basin
     陆相盆地中残留可容纳空间的识别与应用
短句来源
     CHARACTERISTICS OF ~1H_(NMR),~(13)C_(NMR) AND INFRARED SPOCTRUMS OF THE HEAVY FRACTIONS OF CONTINENTAL HEAVY OIL IN CHINA AND THEIR APPLICATIONS
     我国陆相重质原油及重质组分的~1H_(NMR),~(13)C_(NMR)谱和红外光谱特征及应用
短句来源
     Evolvement law and mechanism of microcosmic flow field in continental faulted basin
     陆相断陷湖盆油藏微观流场演化规律及演变机理
短句来源
     Subtle Hydrocarbon Reservoir Exploration Method in Continental Basin
     陆相盆地隐蔽油气藏勘探方法——以金湖凹陷戴南组为例
短句来源
     3D AVO Analysis for Identifying Thin Continental Sandstone Interbeds and Deep Volcanic Rocks
     利用3-D AVO分析识别陆相薄互层砂岩气藏和深层火成岩(英文)
短句来源
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  continental facies
     Low temperature ore\|forming fluid is generally sulfate brine and mainly contains sulfate with Ba 2+ , Sr 2+ , Ca 2+ , and this type of fluid widely occurs in all kinds of environment in sea facies and continental facies.
     低温成矿流体一般为硫酸盐型卤水 ,主要是Ba2 +,Sr2 +,Ca2 +的硫酸盐化合物 ,在海陆相各环境中广泛存在。
短句来源
     DISCUSSION ON THE GEOLOGICAL CHARACTERISTICS AND THE EVOLUTION OF XUPU RED BASIN OF CONTINENTAL FACIES
     溆浦陆相红盆地质特征及其演化探讨
短句来源
     JURASSIC-CRETACEOUS BOUNDARY OF CONTINENTAL FACIES IN NORTHEAST CHINA
     中国东北地区陆相侏罗、白垩系界线
短句来源
     Feasibility of time-lapse seismic monitoring in long-period water-drive continental facies clastic rock reservoir.
     陆相碎屑岩油藏长期水驱时移地震监测的可行性
短句来源
     Geological Characteristics of Iron—ore in Volcanic Rocks of Continental Facies in Late Triassic,South Fujian
     闽南晚三叠世陆相火山岩铁矿地质特征
短句来源
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  terrestrial
     There are obvious differences between two analytical methods named classic sequence stratigraphy and Cross' high-resolution sequence stratigraphy on identification method, applicability, inner structure and the knowledge of formation distribution of the sequence in the terrestrial rift basin.
     陆相断陷盆地高精度层序地层研究常采用经典层序地层学和Cross高分辨率层序地层学两种分析方法,这两种方法存在明显的差别,主要体现在层序识别方法与适用范围、层序结构与对地层分布的认识等方面。
短句来源
     Identification and significance of Δ~5-stenols in salty terrestrial sediments
     在陆相咸水沉积物中检出Δ~5-甾醇化合物及其生源意义探索
短句来源
     STRUCTURAL LITHOLOGICAL LITHOFACIES MAPPING METHOD—A New Method for 1∶50,000 Geological Mapping of the Terrestrial Red Basin
     陆相红色盆地1∶5万填图的一种新方法———构造—岩性—岩相填图法
短句来源
     EXPERT SYSTEM OF SINGLE WELL CORE FACIES ANALYSIS IN TERRESTRIAL DOWN-FAULTED BASIN
     陆相断陷盆地单井岩心相分析专家系统
短句来源
     The paper describes the isotopic characters of hydrogen, oxygen, sulfur, and fluid inclusion characters in geology, and discusses the metallogeny, metallogenic regularities and prospecting indicators for subvolcanic copper-silver-gold-lead-zinc polymetallic deposits in the Mesozoic terrestrial volcanic region of east China.
     本文阐述了中国东部中生代陆相火山岩地区次火山岩铜银金铅锌多金属矿床(以下简称铜银多金属矿床)地质特征,氢、氧、硫同位素地质特征,流体包裹体地质特征,讨论了成矿作用、成矿规律和找矿标志。 提出了次火山岩型矿床的理念,认为次火山岩型矿床基于:矿化集中区常发育次火山岩;
短句来源
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  terrigenous
     1∶50 000 regional economical-geological survey of terrigenous red basins in Jiangxi Province
     江西陆相红盆地1∶5万区调中的经济地质调查
短句来源
     According to the facies migration characteristics and superimposing patterns of system tracts in the reference well, the standards for identifying two types of terrigenous sequences (type Ⅰand Ⅱ) and for their system tracts have been established.
     根据参照井处的沉积相迁移特征及体系域叠置样式 ,建立了在参照井的背景下 ,Ⅰ型与Ⅱ型陆相层序划分及其层序界面判识标准 ,以及低水位体系域 (LST)、水进体系域 (TST)、高水位体系域 (HST)及水退体系域 (RST)的识别模式。
短句来源
     But terrigenous sequence of type Ⅱ lacks LST.
     而Ⅱ型陆相层序缺失LST。
短句来源
     While terrigenous sequence of type Ⅱ lacks LST.
     而Ⅱ型陆相层序缺失LST。
短句来源
     Basic principle of Milankovitch cycle and it's prospect in terrigenous lake basin analysis
     米氏旋回基本原理及其在陆相湖盆分析中的应用前景
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  continental
With a temperate continental monsoon climate, the mountain area belongs to the warm temperate deciduous broad-leaved forest region.
      
Comparison of element abundance between the exposed crust of the continent of China and the global averaged upper continental cr
      
Distribution, migration and derivation of Mesozoic-Cenozoic regional fault systems in the central continental margin of eastern
      
Deep-large faults in the central continental margin of eastern China are well developed.
      
The geochemistry of chert from the Zhongpu Group reveals that all cherts coexisting with island-arc volcanic rocks formed in a continental margin basin environment.
      
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  continental facies
The locally distributed continental facies (group 1) is characterized by the development of uranium and REE mineralization.
      
This is the most accurate correlation of the PTB in continental facies with that in the marine GSSP.
      
The association of the investigated ophiolites with volcanoclastic metasedimentary rocks of marine to continental facies is a further confirmation of their ensialic evolution.
      
The top of the sequence is represented by an alternating complex of marine to continental facies with carbonaceous sediments.
      
  terrestrial
In terrestrial ecosystems, soil nutrient regimes at a plant's living site generally represent the plant's "nutrition habitat".
      
Fine root turnover is a major pathway for carbon and nutrient cycling in terrestrial ecosystems and is most likely sensitive to many global change factors.
      
There is a crucial need in the study of global change to understand how terrestrial ecosystems respond to the climate system.
      
Research results of the rare earth elements reveal that these cherts formed in a relatively deep-water basin with no significant terrestrial interference.
      
Some original results of flight and terrestrial experiments are presented.
      
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  terrigenous
The grain size and element (including redox sensitive elements and terrigenous elements) concentration of surface sediments from the Changjiang Estuary hypoxia zone and its adjacent sea area were measured in this research.
      
The organic matter sources are dominated by marine input in the silt flat, artemisia schrenkiana flat, and the transition zone between silt and spartina alterniflora flat, and are controlled by terrigenous input in spartina alterniflora flat.
      
Certified reference materials of bottom sediments-terrigenous clay (SDO-1), volcanic-terrigenous mud (SDO-2), and lime mud (SDO-3)-were used as model samples.
      
The low quality of OM is partly related to its intense anaerobic decomposition in anoxic environments with terrigenous sedimentation.
      
The Nile River plays the leading role in terrigenous sedimentation in the southeastern Mediterranean, especially in deep-sea areas.
      
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