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geochemistry characters
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  地球化学特征
     ore-forming geochemistry characters of metallogenic and trace elements, REE and lead, sul-fur, hydrogen and oxygen isotope are Studied in rather detuils.
     本文校系统地研究了成矿元素及微星元素.稀土元素和铅、硫、氢、氧同位素等成矿地球化学特征.研究结果表明,研究区内成矿物质来源是多方面的;
短句来源
     Through the analysis of petroleum geology, geochemistry and testing data and the study of oil/gas formation, hydrochemical , hydrodynamic, fluid potential field, migration passages, geochemistry characters, migration directions and control factors , the numerical stimulation of migration pathway ,migration mode, how to control oil/gas distribution ,we can know the oil/gas migration directions, period and pathway along reservoir beds.
     本文通过对研究区油气地质、地化和测试资料分析,对西斜坡区油气生成、水化学场与动力场、流体势场、运移通道、油气运移的地球化学特征、油气运移方向及控制因素、油气运移路径的模拟及运移模式、油气运移对油气成藏与分布的控制作用系统全面的研究,搞清油气沿储层运移的方向、时期、通道路径。
短句来源
     Based on the characteristics of rock association and multielement quantitative analysis results of Precambrian metamorphic rocks in Northern Fujian,the paper represents to the discussion of geochemistry characters of trace elements and abundance characteristics of such metallogenic elements as gold,silver,tin and tantalum of Precambrian metamorphic rocks in Northern Fujian.
     通过闽北前寒武纪变质岩地层岩石共生组合特点以及各层组岩石多元素定量分析结果的研究,阐述了闽北前寒武纪变质岩地层微量元素地球化学特征和金、银、锡、钽等成矿元素丰度特征。
短句来源
     According to analysis of sedimentary characters and geochemistry characters of Luanchuan Group of New Proterozoic Era.
     通过对新元古代栾川群地层沉积特征及地球化学特征分析,栾川群形成于被动大陆边缘构造环境。
短句来源
     Geochemistry Characters and Oil and Gas Source Correlation in the Reservoirs of West Slope in Dongpu Depression
     东濮凹陷西斜坡油藏地球化学特征与油气源对比
短句来源
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  “geochemistry characters”译为未确定词的双语例句
     Study on Geochemistry Characters of Agricultural Soil Around Xi'an City
     西安市郊农田土壤环境地球化学研究
短句来源
     Based on the traditional ore geochemistry studies, in this paper, we use modern analysis technologies (GC-MS, ESEM) to explore the organic geochemistry characters and ore-forming environment of the witherite deposits.
     本文在传统地球化学分析的基础上,借助GC—MS、ESEM等现代测试技术,对矿床有机地球化学问题进行探讨。
短句来源
     Geochemistry characters of oceanic island basalt suggest that the slab which descend into the mantle may be mixed with the source area of plume .
     大洋岛玄武岩地化特征上的多样性提示,沉入下地幔的板片可能从深部卷入地幔柱的源区。
短句来源
     The sequence patterns of these 2 sets of source rocks are studied by using Sinian and Cambrian systems for example,and based on sequence analysis,the source rocks are studied and evaluated by using geochemistry characters as reference,thus beneficial areas of source rocks are pointed out.
     以中扬子区震旦系、寒武系为例,对2套烃源岩所在的层序样式进行了研究,以层序分析为基础,参考地化特征对2套烃源岩进行了研究及评价,指出了有利烃源岩区。
短句来源
  相似匹配句对
     Geochemistry characters of inorganic natural gas
     无机成因天然气的地球化学特征
短句来源
     Geochemistry Characters of Base Element in Tibet Soils
     西藏土壤盐基元素的地球化学特征
短句来源
     The Characters of Eggshell
     鸡蛋壳的性状
短句来源
     ANALYTICAL GEOCHEMISTRY
     《分析地球化学》
短句来源
     the distortion of characters;
     人物形象发生了严重的扭曲和变形;
短句来源
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This paper adopts the methods of existing form analysis of element, simulate experiments and mathematical statistics etc. to carry on systematic research on environmental geochemistry character of shallow layer ground water system in Hangzhou City and its effect on chemical composition formation. To combine with the conditions of geology and hydrogeology in this area, a series of important conclusions are obtained.

本文采用元素的存在形态分析,模拟试验以及数理统计等方法,首次对杭州市浅部含水系统的环境地球化学特征及其对地下水化学成分形成的影响进行了系统的研究,并结合本区的地质和水文地质条件,得出了一系列重要的结论。

ore-forming geochemistry characters of metallogenic and trace elements, REE and lead, sul-fur, hydrogen and oxygen isotope are Studied in rather detuils. The results of studies above showthat ore-forming materials are from many sources in discussed area, and that the water medium inore-forming process is the mixture of atmospheric water and magmatic water in main metallogenicStuge and is chiefly the atmospheric water in the late stage, and that ore sort further wil1 be empha-sised depending on the minerallization...

ore-forming geochemistry characters of metallogenic and trace elements, REE and lead, sul-fur, hydrogen and oxygen isotope are Studied in rather detuils. The results of studies above showthat ore-forming materials are from many sources in discussed area, and that the water medium inore-forming process is the mixture of atmospheric water and magmatic water in main metallogenicStuge and is chiefly the atmospheric water in the late stage, and that ore sort further wil1 be empha-sised depending on the minerallization degree of certain stages in the area.

本文校系统地研究了成矿元素及微星元素.稀土元素和铅、硫、氢、氧同位素等成矿地球化学特征.研究结果表明,研究区内成矿物质来源是多方面的;成矿过程中的介质水在成矿主要阶段是大气降水与再平衡岩浆水的混会,在成矿晚期则主要来自大气降水;成矿是多阶段的,可依据各阶段的矿化程度来确定今后应侧重的矿种.

According to the lithology and geochemistry characters of the iron horizons ofthe Longqiao iron deposit, stratigraphic correlation with Middle TriassicZhouchongcunian gypsum-bearing rock series in the Nanjing area, coupled withthe distribution of the ore horizons and regional tectonics and a tectonic analysisof volcanic basin, it has been shown that iron horizons would be originallyiron-rich sedimentary (siderite, ankerite, magnetite, hematite) source beds, in theMiddle Triassic Ma'anshan'an (Zhouchoncunan)...

According to the lithology and geochemistry characters of the iron horizons ofthe Longqiao iron deposit, stratigraphic correlation with Middle TriassicZhouchongcunian gypsum-bearing rock series in the Nanjing area, coupled withthe distribution of the ore horizons and regional tectonics and a tectonic analysisof volcanic basin, it has been shown that iron horizons would be originallyiron-rich sedimentary (siderite, ankerite, magnetite, hematite) source beds, in theMiddle Triassic Ma'anshan'an (Zhouchoncunan) stage deposited in the lagoonal-sabkh sedimentary environmet. The source beds might have played an importantrole as embryo beds which have caused the preference of thermometamorphismand hydrothermal superimposition on such ?particular beds during the magmaticintrusion at the Yanshanian.

根据龙桥铁矿层位岩性、地球化学特征及其与南京地区中三叠世周冲村期含膏岩系的对比,结合含矿层位的展市与区域构造及火山岩盆地的构造分析。论证龙桥铁矿含矿层位是中三叠世东马鞍山期(周冲村期)萨布哈-泻湖沉积环境下,含铁沉积(菱铁矿、钱白云石、磁铁矿及赤铁矿)矿源层。经燕山期岩浆侵入的热变质和热液叠加构造,成矿作用经历多阶段演化。

 
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