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整体有机质
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  “整体有机质”译为未确定词的双语例句
     ( 3 ) According to the genetic relationship between soluble and insoluble organic matter in the source rocks, coupled with data of kerogen, organic matter in continental source rocks is classified into 5 types: the sapropel type, the humus-sapropel type, the sapropel-humus type, the humus type and kerogen coal.
     其母质类型除腐殖型外,还发育了大量腐泥型等多类型生油岩。 3.依据生油岩中可溶与不溶有机质成因联系,将可溶有机质视为整体有机质的一个“碎片”,结合干酪根等资料,将陆相生油岩有机质类型划分为五种类型即:腐泥型、腐殖-腐泥型、腐泥-腐殖型、腐殖型和腐煤型。
短句来源
     ORGANIC GEOCHEMISTRY OF THE BIJIASHAN LEAD-ZINC DEPOSIT (Ⅱ) - FEATURES OF BULK ORGANIC MATTER AND SOURCES OF ORE-FORMING MATERIALS
     毕家山铅锌矿床有机地球化学研究(Ⅱ):整体有机质特征与成矿物质来源探讨
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     The average of the total organic carbon (TOC) is only 0.4%. The type of organic matter is main sapropel-type kerogen. The hydrocarbon source rock is in evolution stage of high maturation-over maturation.
     剖面上该组碳酸盐岩整体有机质丰度不高,有机碳均值仅为0.4%,有机质类型以腐泥型占绝对优势,烃源岩处在高成熟热演化阶段。
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  相似匹配句对
     On Entirety Enterprise Planning
     整体企划
     The Concept of Western Literature Structure: From Entirety to Fragment
     从整体到碎片
短句来源
     (3) organic matter.
     (3) 有机质
短句来源
     organic matter content is low;
     有机质含量低;
短句来源
     Studies have shown that soluble and insoluble organic matter are organically connected in the sedimentary rock, both contributing to hydrocarbon generation.
     研究表明,沉积岩中可溶和不溶有机质,是一个有机联系的整体,共同参与了油气的生成。
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  bulk organic matter
The chronology is constructed from six AMS radiocarbon dates on the bulk organic matter.
      
This may cause an underestimation of the terrigenous proportion of bulk organic matter when assessments are based on bulk carbon isotopic signatures alone.
      
In contrast to the variety of changes evident in molecular compositions, neither σ13C values nor C/N ratios differ significantly in the bulk organic matter of modern and aged spruce components.
      
To obtain information about the fate of DOC leached from the O horizon into the mineral soil, 14C measurements were made on bulk organic matter and DOC.
      
Organic geochemistry of the Japan Sea sediments-1: Bulk organic matter and hydrocarbon analyses of Core KH-79-3, C-3 from the Ok
      
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The subject is treated on the basis of field experiences and large amount of geochemical data. It is proposed that (1) the content and distribution of organic matter in continental source rocks are something related to the types of lake sediments deposited, generally expressed by the presence of organic carbon, chloroform extract asphalt "A" and hydrocarbons content (2) From the study of the types of organic matter by means of chromatogram, infrared spectrum, chromatogrammass spectrogram, it has been found that...

The subject is treated on the basis of field experiences and large amount of geochemical data. It is proposed that (1) the content and distribution of organic matter in continental source rocks are something related to the types of lake sediments deposited, generally expressed by the presence of organic carbon, chloroform extract asphalt "A" and hydrocarbons content (2) From the study of the types of organic matter by means of chromatogram, infrared spectrum, chromatogrammass spectrogram, it has been found that in addition to the above, sedimentary facies zone also plays a part and that the source rocks contain kerogen of many types. ( 3 ) According to the genetic relationship between soluble and insoluble organic matter in the source rocks, coupled with data of kerogen, organic matter in continental source rocks is classified into 5 types: the sapropel type, the humus-sapropel type, the sapropel-humus type, the humus type and kerogen coal.

本文依据陆相石油勘探实践及大量的地球化学分析资料,对陆相生油岩有机质的丰度及类型进行了探讨。研究认为:1.陆相生油岩有机质含量及分布与湖相沉积类型和相带有关。一般采用有机碳、氯仿沥青“A”及烃含量来表示。2.应用色谱、红外、元素、色谱—质谱联用技术、扫描电子显微镜等分析资料,研究了有机质类型认为:陆相生油岩类型及分布受沉积相带的控制。其母质类型除腐殖型外,还发育了大量腐泥型等多类型生油岩。3.依据生油岩中可溶与不溶有机质成因联系,将可溶有机质视为整体有机质的一个“碎片”,结合干酪根等资料,将陆相生油岩有机质类型划分为五种类型即:腐泥型、腐殖-腐泥型、腐泥-腐殖型、腐殖型和腐煤型。

The Xixia formation in Lower Permian is one of the main segments that contain hydrocarbon source rock. The organic enrichment of carbonate in this formation is not high as a whole in the profile. The average of the total organic carbon (TOC) is only 0.4%. The type of organic matter is main sapropel-type kerogen. The hydrocarbon source rock is in evolution stage of high maturation-over maturation. The organic geochemical analysis of the dense rock samples qurried in profile indicates that: There are 5 organic-rich...

The Xixia formation in Lower Permian is one of the main segments that contain hydrocarbon source rock. The organic enrichment of carbonate in this formation is not high as a whole in the profile. The average of the total organic carbon (TOC) is only 0.4%. The type of organic matter is main sapropel-type kerogen. The hydrocarbon source rock is in evolution stage of high maturation-over maturation. The organic geochemical analysis of the dense rock samples qurried in profile indicates that: There are 5 organic-rich members in upright profile. The average of total organic carbon (TOC) is over 0.4% and the total thickness is about 42 m. They are the segments that consisted of effective hydrocarbon source rock in Xixia formation.

下二叠统栖霞组是南陵—无为地区主要的烃源岩层位之一。剖面上该组碳酸盐岩整体有机质丰度不高,有机碳均值仅为0.4%,有机质类型以腐泥型占绝对优势,烃源岩处在高成熟热演化阶段。剖面上密集采样分析表明,垂向上存在3个有机质相对富集的小层段,其有机碳平均值均超过0.4%,累计厚度为42m左右,它们为该组有效生烃层段。

 
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