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   含丰富 在 石油天然气工业 分类中 的翻译结果: 查询用时:0.059秒
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含丰富
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  contain abundant
    In the past several decades,the marine origin of Paleozoic oil and gas in China has long been an important problem to which petroleum geologists pay great attention. A major breakthrough was made in 1984 when well Shacan 2 encountered Paleozoic oil of marine origin in the Tarim basin,which for the first time demonstrates that "the Paleozoic marine deposits in China contain abundant oil".
    几十年来,中国古生代海相成油一直是国内外石油地质学家关注的大问题,1984年塔里木盆地沙参2井实现古生代海相油气重大突破,首次证明“中国古生界海相含丰富的石油”。
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  “含丰富”译为未确定词的双语例句
    Biomarkers compounds studies show that there are low Pr/Ph ratios, abundant gammacerane and >C30 hopanes and dibenzothiophenes for the western Qaidam oils, reflecting an anoxic and saline-hypersaline environment for their source-rocks.
    原油生物标志化合物研究发现,西部原油Pr/Ph比值较低,含丰富的伽玛蜡烷、>C_(30)藿烷和硫芴,反映了它们形成于强还原超咸水—咸水环境;
短句来源
    The northern Qaidam oils have high Pr/Ph ratios, low abundance of gammacerane and >C3o hopanes and abundant dibenzofurans which are indicative of a suboxic and freshwater environment.
    北部原油Pr/Ph比值较高,伽玛蜡烷和>C_(30)藿烷丰度极低,含丰富的氧芴,说明它们形成于弱氧化淡水环境;
短句来源
    The terpanedistributions of heavy oil are also rich in gammacerane and sterane distributions are rich indinosteranes and 4-methyl steranes, triaromatic dinosteranes and 4-methyl triaromaticdinosteranes.
    重质稠油含丰富的甲藻甾烷和 4-甲基甾烷,三芳甲藻甾烷和 4-甲基三芳甲藻甾烷明显富集,伽玛蜡烷含量高。
短句来源
    Chinese Devonian coals are dominated by the cutinitic liptobiolith, and their unique organic geochemical characteristics,specially the molecular geochemical features are determined by their unique coal petrological naturPs- By use of modernanalytical instruments, authors have discussed the biomarker composition of Chinese Devonian coals, analyzed the genesis oftetracyclic diterpenoid hydrocarbons from the Devonian coals and pointed out that tetracyclic diterpenoids detected out ofChinese Devonian coals originated from the pteridophyta.
    中国泥盆纪煤主要为角质残植煤,由其独特的煤岩组成特征决定了其独特的有机地球化学特征,特别是分子有机地球化学特征。 运用现代分析仪器,首次详细探讨了中国犯企纪煤的烷烃生物标志物组成特征:含丰富的四环二该烷及其它萜类化合物,不合甾族类化合物;
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    The Mid-Pleistocene Series grows multi-layer organic material layer and gray mud-rock abundance of herbal plant, the depth ranging from 200-800 meters; the light solidifying, natural porosity from 25% to 30%,The saturation of water reaching 90%, been in low temperature climate and semi-salt water condition in a long term, which is benefit for the growing and breeding of methane bacterium.
    中更新统发育多层含丰富草本植物的有机质和暗色泥岩,埋深约200~800m,沉积物固结程度低,原生孔隙度25%~30%,含水饱和度高达90%,并长期处于低温气候和富盐半咸水介质环境中,非常有利于甲烷菌的生长和繁殖,类比柴达木盆地第四系生物气田成藏地质特征,该区具备生物气成藏地质条件;
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  contain abundant
They contain abundant chlorite that replaces globular and platy Al-glauconite to a variable extent.
      
The lakes under study contain abundant SRBs not only in bottom sediments (from 103 to 107 cells/dm3) but also in the water column (from 102 to 106 cells/ml).
      
The rocks contain abundant buchia fauna of Volgian-Valanginian age, as well as carbonized plant detritus and flora of the Early Cretaceous habit.
      
The results indicate that sinking particulate materials contain abundant isoprenoid ketone, aldehyde and alcohol lipid compounds which take part in marine chemical cycling.
      
Spermatogenesis is initiated in summer (February-March), when the seminiferous tubules contain abundant undifferentiated spermatozoids, which are transformed to spermatozoa as fall advances (MayJune).
      
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The Shiwu Formation in Shiwu half-graben developed well and widely spread. In well-SN 10 near Shiwu township in Gongzhuling City, its sequence is complete and the boundaries of top and bottom are clear, and its lithological character, sporopollen assemblage and thickness are distinct, thus the stratum is named Shiwu Formation. The sporopollen assemblage of the formation is characterized by abundant Classopollis, Cyathidites and a few Tricolpopollenites, Clavatipollenites etc. Therefore, it is called as Classopollis-Cyathidites-...

The Shiwu Formation in Shiwu half-graben developed well and widely spread. In well-SN 10 near Shiwu township in Gongzhuling City, its sequence is complete and the boundaries of top and bottom are clear, and its lithological character, sporopollen assemblage and thickness are distinct, thus the stratum is named Shiwu Formation. The sporopollen assemblage of the formation is characterized by abundant Classopollis, Cyathidites and a few Tricolpopollenites, Clavatipollenites etc. Therefore, it is called as Classopollis-Cyathidites- Thicolpopollenites assemblage, which could compare with that of the Guantao and Gecun Formations in South China. Its age should belong to Aptian of Early Cretaceous.

十屋断陷十屋组十分发育,分布稳定,顶底界线、岩性特征、沉积旋回和厚度清楚,含丰富的孢粉化石,具备建组条件。十屋组的建立必将有助于松辽地区深部地层划分对比。十屋组产Classopollis-Cyathidites-Tricolpopollenites孢粉组合,可与我国南方馆头组、葛村组对比,时代为早白垩世阿普第期

Chinese Devonian coals are dominated by the cutinitic liptobiolith, and their unique organic geochemical characteristics,specially the molecular geochemical features are determined by their unique coal petrological naturPs- By use of modernanalytical instruments, authors have discussed the biomarker composition of Chinese Devonian coals, analyzed the genesis oftetracyclic diterpenoid hydrocarbons from the Devonian coals and pointed out that tetracyclic diterpenoids detected out ofChinese Devonian coals originated...

Chinese Devonian coals are dominated by the cutinitic liptobiolith, and their unique organic geochemical characteristics,specially the molecular geochemical features are determined by their unique coal petrological naturPs- By use of modernanalytical instruments, authors have discussed the biomarker composition of Chinese Devonian coals, analyzed the genesis oftetracyclic diterpenoid hydrocarbons from the Devonian coals and pointed out that tetracyclic diterpenoids detected out ofChinese Devonian coals originated from the pteridophyta.

中国泥盆纪煤主要为角质残植煤,由其独特的煤岩组成特征决定了其独特的有机地球化学特征,特别是分子有机地球化学特征。运用现代分析仪器,首次详细探讨了中国犯企纪煤的烷烃生物标志物组成特征:含丰富的四环二该烷及其它萜类化合物,不合甾族类化合物;着重分析了煤中大量检出的四环二萜烷的生源,指出我国泥企纪煤中检出的四环二萜烷未源于应类植物。

A set of fan-delta bodies formed as an alluvial fan prograded into a lake at hundd climate in Jurassic of Bayinbuluk area, Hejing, Xinjiang. Complete fan-delta sequence shows clearly lakeward progradation sequence. Fan-delta plain is dondnated by massive sandy conglomerae of debris flow origin, interbedded with lenticular pebbly sandstone or medium to coaree-graned sandstone and medium to flaggy sediments of sheet now origin. Fan-delta front is dondnated by massive sandy conglomerate of debris flow origin, with...

A set of fan-delta bodies formed as an alluvial fan prograded into a lake at hundd climate in Jurassic of Bayinbuluk area, Hejing, Xinjiang. Complete fan-delta sequence shows clearly lakeward progradation sequence. Fan-delta plain is dondnated by massive sandy conglomerae of debris flow origin, interbedded with lenticular pebbly sandstone or medium to coaree-graned sandstone and medium to flaggy sediments of sheet now origin. Fan-delta front is dondnated by massive sandy conglomerate of debris flow origin, with occasional lenticular sandstone of distribuop channel facies. Dedelta mainly consists of blackgray shale and silty shale, interbedded with sandstone formed by turbidity current. Abundant plant fossils are found in fan-delta, with local carbonaceous shale and thin coal seam. Mudstone in prodelta is a good source rock.

新疆和静巴音布鲁克地区侏罗系中发育一套在潮湿气候条件下形成的冲积角进积至内陆湖泊中而形成的扇三角洲沉积体。三角洲层序完整,清楚显示向湖进积序列:扇三角洲平原部分主要以泥石流成因的块状砂砾岩为主,夹扇面河道沉积的含砾砂岩、中粗粒砂岩透镜体及中落层状漫流沉积;扇三角洲前缘以碎屑流沉积的块状砂砾岩为主,夹水下分流河道沉积的砂岩透镜体;前扇三角洲以深灰色页岩、粉砂质页岩为主,夹浊流成因的砂岩,沉积体中含丰富的植物化石,局部见碳质页岩及薄煤层,前扇三角洲泥岩为好的烃源岩。

 
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