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geochemical parameter
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  地球化学参数
     The time of hydrocarbon generation from exinite is later than coal according to the geochemical parameter of hopanes,such as occurrence of 17β(H)trisnorhopane and C_ 29βα-hopanes as peak carbon,C_ 31αβ22S/22(S+R)index.
     壳质组萜烷系列化合物的地球化学参数(以17β(H)三降藿烷、C29βα-藿烷、C31αβ22S/22(S+R))表明壳质组热演化史比煤岩有迟豫效应。
短句来源
     IDEAL MODEL AND PRINCIPLE OF STACHING STRUCTURE OF AXIAL GEOCHEMICAL PARAMETER OF GOLD DEPOSIT
     金矿床轴向地球化学参数叠加结构的理想模式及其应用准则
短句来源
     Based on summarization of change regulation of axial geochemical parameter for gold deposits, the characteristics of multi-stage stacking mineralization of gold deposit are used to establish the ideal model of axial geochemical parameter with different stacking structures. Finally, the criteria for prediction of concealed ore bodies have been determined.
     在研究和总结金矿床轴向地球化学参数变化规律的特性和共性的基础上,用金矿具有多期多阶段叠加矿成晕观点,建立了不同叠加结构地化参数轴向变化的理想模式,确定了其用于盲矿预测的准则
短句来源
     It will be a good prospecting for deep orebodies according to the analysis to the features of microelements geochemical parameter axial variation of the trench,transverse drift and drilling samples.
     通过对探槽、穿脉、钻孔样品微量元素地球化学参数轴向变化特征的分析,认为矿体的深部找矿前景较好。
短句来源
     Some geochemical parameter changes caused by sequential gas washing are modeled by PR state equation,and the relationship betw een the parameters and mode of gas washing is analyzed.
     用PR状态方程定量计算和分析了部分常用地球化学参数随气洗次数的变化规律及这些参数与气洗方式之间的关系;
短句来源
  地化参数
     : This paper introduces gas chromalographic analysis technique for cutting head space gas and establishes light alkaneratio method and Pixler method to distinguish oil and gas source,oil and gas bed and organic geochemical parameter evaluation criteria of oil and gas productivity prediction.
     本文介绍了岩屑罐顶气气相色谱分析技术,确立了轻烷烃比值法、皮克斯莱尔法判别油气源岩、油气层和油气产能预测的有机地化参数评价标准;
短句来源
     After an analysis of geochemical parameter s i.e. carbon isotopic composition and R/Ra value of CO2, etc, plus a combination of the geological features of the related pools, the paper proposed that except those in Yingge marine basin, which have a metamorphic origin, the rest of CO2 fields (pools) in east China can be attributed to predominantly an origin of mantle-derived volcano-magma.
     本文通过二氧化碳碳同位素组成,R/Ra值等地化参数分析,并结合相关气藏地质特征,指出除莺歌海盆地CO2气田(藏)为变质成因外,中国东部其它CO2气田(藏)主要为幔原火山─—岩浆成因。
短句来源
     Based on summarization of change regulation of axial geochemical parameter for gold deposits, the characteristics of multi-stage stacking mineralization of gold deposit are used to establish the ideal model of axial geochemical parameter with different stacking structures. Finally, the criteria for prediction of concealed ore bodies have been determined.
     在研究和总结金矿床轴向地球化学参数变化规律的特性和共性的基础上,用金矿具有多期多阶段叠加矿成晕观点,建立了不同叠加结构地化参数轴向变化的理想模式,确定了其用于盲矿预测的准则
短句来源
     Starting with the correction to the geochemical parameter, the paper set up the correction relations between geochemical parameters of cuttings, sidewall core, core and sealing core, derivated updating formulas of oil saturation, thus, correcting oil saturation data of cuttings, core, sidewall core into laboratory state of sealing core.
     该文从地化录井参数ST的校正入手,建立岩屑、井壁取心、岩心与密闭取心的地化参数校正关系,导出含油饱和度的校正公式,将岩屑、岩心、井壁取心含油饱和度数据校正到密闭取心实验室状态下。
短句来源
  “geochemical parameter”译为未确定词的双语例句
     Elements of different indicating significance are concentrated in different positions of mineralization, exhibiting zonation. Such zonation is an important geochemical parameter for evaluating denudation extent of mineralization and ore hunting prospects.
     具有不同指示意义的元素组合于矿化的不同部位聚集而出现的分带 ,是用于评价矿化剥蚀程度及其成矿远景的重要地球化学参量
短句来源
     The analyses of synthesizing geochemical parameter characteristics indicate that deposition of the manganese-bearing sequences was the consequence of episodic, multi-cycle activities of hydrothermal solution.
     综合地球化学各参数特征分析表明本区孤峰组含锰岩系的沉积是热水活动间歇式、多次活动的结果。
短句来源
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  geochemical parameter
Near the transform which bounds the AAD to the east, there is a marked change in the morphology of the spreading center, as well as in virtually every measured geochemical parameter.
      
The focus of this study is placed on the application of geochemical parameter and signature analyses related with the aforementioned geological units, which are of subcontinental extension into South America.
      


Classification of kerogen,maturation of organic matters,source correlation, and migration of hydrocarbons are discussed in this paper based on geochemical parameters,ie.steranes and terpanes,and some suggestions for further petroleum exploration in Erlian Basin are presented also. The classification of kerogen is based on the ratio:ΣC_(27)steranes/ΣC_(29)ster- anes,with which degree of oil generation can be divided relatively. The threshold parameters of oil generation in the two depressions has...

Classification of kerogen,maturation of organic matters,source correlation, and migration of hydrocarbons are discussed in this paper based on geochemical parameters,ie.steranes and terpanes,and some suggestions for further petroleum exploration in Erlian Basin are presented also. The classification of kerogen is based on the ratio:ΣC_(27)steranes/ΣC_(29)ster- anes,with which degree of oil generation can be divided relatively. The threshold parameters of oil generation in the two depressions has been determined by using a lot of multiple molecular parameters of maturity and the parameters related to the biochemical markers of observed the crude oils. The correlative method of GC map and the method of mean squar difference has been used to interprete the oil source in both Ehebaolige and Saihantala depression of the basin. The relative hydrocarbons migration in two depressions is illustrated in the light of using the corresponding molecular parameters based on principle of geoch- romatography. Finally,this paper indicates that the sample of A_3-118 is more mature, with a better type of kerogen,and more promising prospects would be expected.

本文应用甾烷、萜烷地球化学参数,研究了生油母质类型、有机质成熟度、油源对比及烃类相对运移等问题,并提出对二连盆地石油勘探的一些建议。

This paper expounds the petrogeno-minerogenetic conditions of Tangquan monzonitic granite-the transitional type granite between granitic rocks of the two genetic series in South China from geological and physico-chemical angle.It shows that the transitional type granite has the demarcational characteristics between granitic rocks of the two genetic series, provides another basis for research in granitic rocks of two genetic series. The Tangquan monzonitic granitic body is situated on the contraction-close boundary...

This paper expounds the petrogeno-minerogenetic conditions of Tangquan monzonitic granite-the transitional type granite between granitic rocks of the two genetic series in South China from geological and physico-chemical angle.It shows that the transitional type granite has the demarcational characteristics between granitic rocks of the two genetic series, provides another basis for research in granitic rocks of two genetic series. The Tangquan monzonitic granitic body is situated on the contraction-close boundary of ancient plate. The rock body has both characteristics of the syntexis type granite and of the transformation type granite. Because the rock body had the function of "Welding" deep fault it made the rock body a type of deep fault zone granite which had a specific implication of structure. According to the geologo-geochemical research and thermody-namic calculation, the emplacemental depth of the rock body is about 6.6KM. Its original and final formation temperatures are about 720—750℃ and about 640—680℃ respectively. Its oxidation coefficient f~* and other geochemical parameters show almost intermediate between the characteristic parametersof syntexis type and transformation type. The origin of the rock body is considered as follows. The geological body with the embryo of the transformation type granite was transformated and was superimposed by the magma of syntexis type granite. This paper provides an example of quantitative physicochemical calculation to study the petrogeno-minerogenetie and alteration conditions of the transitional type granite.

汤泉二长花岗岩位于闽西南永梅海西——印支拗陷东北缘,政和——大埔断裂带中段。岩体K—Ar法同位素年龄为110百万年,是燕山晚期的产物。据热力学计算的结果,岩体侵位深度为6.6Km±的中深成相。成岩初始温度为720—750℃,终了温度为640—680℃。根据多种地质地球化学特征,初步认为汤泉岩体是两种成因系列花岗岩之间过渡类型岩体。其对深断裂的“焊接”作用,使之成为具特定构造含义的深断裂带花岗岩的典型。文章为研究深断裂带过渡类型花岗岩的成岩成矿及交代蚀变条件,提供了一个运用物理化学方法定量计算的实例。

This paper expounds the petrogeno-minerogenetic conditions of Tangquan monzonitic granite-the transitional type granite between granitic rocks of the two genetic series in South China from geological and physico-chemical angle.It shows that the transitional type granite has the demarcational characteristics between granitic rocks of the two genetic series, provides another basis for research in granitic rocks of two genetic series. The Tangquan monzonitic granitic body is situated on the contraction-close boundary...

This paper expounds the petrogeno-minerogenetic conditions of Tangquan monzonitic granite-the transitional type granite between granitic rocks of the two genetic series in South China from geological and physico-chemical angle.It shows that the transitional type granite has the demarcational characteristics between granitic rocks of the two genetic series, provides another basis for research in granitic rocks of two genetic series. The Tangquan monzonitic granitic body is situated on the contraction-close boundary of ancient plate. The rock body has both characteristics of the syntexis type granite and of the transformation type granite. Because the rock body had the function of "Welding" deep fault it made the rock body a type of deep fault zone granite which had a specific implication of structure. According to the geologo-geochemical research and thermodynamic calculation,the emplacemental depth of the rock body is about 6.6KM. Its original and final formation temperatures are about 720—750℃ and about 640—680℃ respectively. Its oxidation coefficient f and other geochemical parameters show almost intermediate between the characteristic parameters of syntexis type and transformation type. The origin of the rock body is considered as follows: The geological body with the embryo of the transformation type granite was transformated and was superimposed by the magma of syntexis type granite. This paper provides an example of quantitative physicochemical calculation to study the petrogeno-minerogenetic and alteration conditions of the transitional type granite.

汤泉二长花岗岩位于闽西南永梅海西——印支拗陷东北缘,政和——大埔断裂带中段。岩体K—Ar法同位素年龄为110百万年,是燕山晚期的产物。据热力学计算的结果,岩体侵位深度为6.6Km±的中深成相。成岩初始温度为720—750℃,终了温度为640—680℃。根据多种地质地球化学特征,初步认为汤泉岩体是两种成因系列花岗岩之间过渡类型岩体。其对深断裂的“焊接”作用,使之成为具特定构造含义的深断裂带花岗岩的典型。文章为研究深断裂带过渡类型花岗岩的成岩成矿及交代蚀变条件,提供了一个运用物理化学方法定量计算的实例。

 
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