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含丰富
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  contain abundant
    the Gaojiashan Formation, 16—46.5 m thick, consists of sandstone and siltstone and is unconformably overlain by Upper Silurian clastic rocks. Both the above-mentioned two formations contain abundant plant microfossils, including 10 genera (26 species), e. g. : Pseudozonos phaera, Trachys phaeridium, Leiopsophos phaera, Leiafusa, Lophosphos phaeridium and Monotromatos phaeridium.
    上部曹家山组以砂岩,粉砂岩为主,厚度16~46.5m,含丰富的微古植物化石,共计有10属26种,其中的许多属、种是晚震旦世的特征分子,其层位相当华中区的陡山沱组一灯影组。
短句来源
    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”。
短句来源
    The rock association of the Carboniferous Yunzhug Formation consists of fine quartzose sandstone, shale and siltstone with several bioclastic limestonebeds, which contain abundant fossils, mainly including brachiopods, bivalves, conodonts, corals,bryozoans,ammonites and trilobites.
    石炭系永珠组岩石组合特征为细粒石英砂岩、页岩、粉砂岩,夹多层生物碎屑灰岩,含丰富的生物化石,主要有腕足类、双壳类、牙形刺、珊瑚、苔藓虫、菊石、三叶虫。
短句来源
  aboundant
    Magnetostratigraphy has been used to study the typical sections, where aboundant mammalian faunas were found, in North China since 5.30Ma B.P. . And the relation between mammalian faunas and magnetostratigraphic sequence has been established.
    通过中国北方5.30Ma以来含丰富哺乳动物化石的典型剖面的磁性地层研究,建立5.30Ma以来中国北方陆相哺乳动物群与磁性地层序列对比。
短句来源
  “含丰富”译为未确定词的双语例句
    (3 ) Carried abundant water, H2O + ≥4% or more than 12%.
    (3)含丰富的结构水,H2O+含量≥4%,大者可达12%以上。
    (4)the copper minerals in ores are rich,the degree of Cu in sulfide is high, indicating that porphyry Cu (Au) mineralization may exist in the depth.
    4矿石含丰富的铜矿物 ,其他硫化物矿物中含铜量大 ,指示深部可能存在斑岩型 Cu(Au)矿化。
短句来源
    The fossil plants include: Sublepidodendron sp., Lepidodendron gansuense sp. nov., Lepidodendron volkmannianum, Lep.
    含丰富的植物化石,主要分子有:Sublepidodendron sp., Lepidodendron ciyaoense sp. nov., Lep jingyuanense sp.nov.
短句来源
    Abundant late Carboniferous fusulinids are found in this section including Eostaffella,Pseudoendothyra,Milleralla,Ozawainella,Pseudostaffella,Profusulinella,Fusulina,Fusulinella,Triticites,and Protricites. The base of the section is not exposed .
    碳酸盐岩中含丰富的Eostaffella、Pseudoendothyra、Milleralla、Ozawainella、Pseudostaffella、Profusulinella、Fusulina、Fusulinella、Triticites、Protricites等,属于典型的石炭纪分子。
短句来源
    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
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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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  aboundant
In the ethyl acetate extract, low molecular weight phenols were identified, the most aboundant being hydroxytyrosol, which is present in the olive pulp.
      
A germanium Low Energy Photon Detector (LEPD) is used for radioassaying which allows the relatively aboundant X-rays from123mTe to be measured.
      
An aboundant literature on vehicle routing problems is available.
      
Some resources, once thought to be aboundant, are becoming alarmingly scarce or polluted and devoid of their original characteristics.
      


In the year 1985, coal balls discovered by authors in No. 14 aud No. 16 coal seam of Taiyuan fromation in Tao Zao coalfield located in Shandong province are of mixed type, they consist mainly of pyritic and calcareous permineralized fossils , of plants and small amount of Marine animals. Fossils in the coal balls include cordaites, lycopodiales, psaronius,lyginopteris sphenophyllum, calamites and animal fossils of gastoopocla. In some pyritic coal balls, abundant bacteria and algae are eontained. The discovery...

In the year 1985, coal balls discovered by authors in No. 14 aud No. 16 coal seam of Taiyuan fromation in Tao Zao coalfield located in Shandong province are of mixed type, they consist mainly of pyritic and calcareous permineralized fossils , of plants and small amount of Marine animals. Fossils in the coal balls include cordaites, lycopodiales, psaronius,lyginopteris sphenophyllum, calamites and animal fossils of gastoopocla. In some pyritic coal balls, abundant bacteria and algae are eontained. The discovery of coal balls is of geological importance to the study of the coal-forming plant materials, the origin of macerals and the envirooment in which coal is formed.

作者于1985年在山东省陶枣煤田太原组的14号和16号煤层中发现了煤核,主要为黄铁质和钙质煤核,煤核属混合型,为矿化的植物化石和少量的海相动物化石所组成,包括科达类、石松类、辉木类、皱羊凿、楔叶、芦木和腹足类动物化石,一些黄铁质的煤核中含丰富的菌藻类化石。煤核的发现对深入研究成煤植物、显微组分成因和煤的形成环境具有重要地质意义。

This paper deals chiefly with the facies changes and controlling factors of theChangxing Limestone in the Changxing area, Zhejiang province. There are apparentdifferences in thickness and lithology of the Changxing Limestone. Over a distanceof about 10 km from Meishan of Changxing county to Niutoushan of Guangdecounty, the thickness dramatically decreases from over 50 m to zero; whereas tothe east of Meishan, at the sections of Huangzishan of Huzhou and Xishan of theTaihu Lake, the thickness increases to over...

This paper deals chiefly with the facies changes and controlling factors of theChangxing Limestone in the Changxing area, Zhejiang province. There are apparentdifferences in thickness and lithology of the Changxing Limestone. Over a distanceof about 10 km from Meishan of Changxing county to Niutoushan of Guangdecounty, the thickness dramatically decreases from over 50 m to zero; whereas tothe east of Meishan, at the sections of Huangzishan of Huzhou and Xishan of theTaihu Lake, the thickness increases to over 100m. The Changxing Limestone in thevicinity of Meishan, Changxing, is dark--coloured, bituminous, flatly stratified, mostlymedium--to thick--bedded, and contains abundant layer--like or lenticular chert;whereas the limestone in Huangzishan and Xishan is light--coloured, mostly thick--to very thick--bedded, and contains rare chert. There are also appreciable differen-ces in fossil appearance between the Changxing Limestone of Meishan and that of Huangzishan and Xishan. The factors causing these differences within such alimited extent are: (1) After the deposition of the alternating marine and continentalLongtan Formation the time when the Changxing Formation began to be depositedwas not synchronous in different places. There was a sea-wall in the western partof the study area, and the Changxing Formation sediments overlapped westwards.In other words, there was a depositional break between the Longtan Formationand the Changxing Formation in some places; for example, at the Qiaomaigang andTuzishan sections. (2) Sedimentary environments varied from area to area. TheHuangzishan--Xishan area is marked by a carbonate rock platform, while theMeishan area by a depression in front of a platform. Some geologists consider thatthe upper part of the Changxing Formation is absent and that there was a deposi-tional break between the Permian and Triassic deposits. The authors, however, holdthat the break does not lie in the upper part of the Changxing Formation but insome local places in the lower part of the formation and that the depositionbetween the Permian and Triassic was continuous in most areas. The ChangxingFormation is wholly lacking at Niutoushan; the Triassic Yingken Formation directlyoverlies the Longtan Formation and is characterized by a weathering crust and aconglomerate bed.

本文主要讨论浙江省长兴地区长兴组灰岩的变化及控制因素。长兴组灰岩在厚度及岩性方面有明显的变化,从长兴县的煤山向西到广德县的牛头山,大约在10km距离内、厚度从50m逐渐减少,甚至完全消失。而从煤山向东到湖洲黄芝山,厚度增加到大于100m。煤山长兴灰岩呈灰黑色,含沥青,成层平整,含丰富的透镜状燧石。而黄芝山等剖面的长兴灰岩呈浅色,很少含沥青和燧石,厚-巨厚层,成层不清楚。在化石群方面也有明显差别。控制这些变化的因素有两个,一是在海陆交互相的龙潭期沉积后,在研究区的西部有一海堤,长兴期沉积由煤山向西超覆,长兴灰岩的下部在一些剖面上缺失.另一个因素是沉积环境不同,湖州-苏州一带为碳酸盐岩台地,而在煤山-广德的独山一带为台前凹陷。

Tongziyian Formation deposited during the late Early Permian in Fujian consists of shallow marine and coal-bearing littoral logoonal fascies and co~ ntiental deposit with a total thickness of 419-870 m. It may be subdivided into three members. The first and third members contain many coal seams and are abundant in fossil plants. The second member is composed of shallow marine claystone which has animal fossils as follows.Altudoceras,Shan-graoceras, Shouchangoceras, Unicisteges crenulata, Pygmochonetes jingxianensis,...

Tongziyian Formation deposited during the late Early Permian in Fujian consists of shallow marine and coal-bearing littoral logoonal fascies and co~ ntiental deposit with a total thickness of 419-870 m. It may be subdivided into three members. The first and third members contain many coal seams and are abundant in fossil plants. The second member is composed of shallow marine claystone which has animal fossils as follows.Altudoceras,Shan-graoceras, Shouchangoceras, Unicisteges crenulata, Pygmochonetes jingxianensis, Neoplicatifera huangi, etc. Studying systematically on the fossil plants from Tianhushan coalfield, Longyian, and Yingting areas the writers have analysed the pattern of feature and the botanical characters of the flora. It consists of 33 genera 80 species distributed separately in Lycopsida, Sphenopsida,Noeg-gerathiales, Filices Pteridospermopsida, Cordaitopsida, Seeds and Plantae insertae sedis. Summarizing the characteristics of the flora it may be called as Gigantonoclea spp.-Tingia carbonica Flora and further divided into two assemblages. The lower is represented by Gigantonoclea spp.and the upper the Cathaysiopteridium fasciculatum (gen. et sp. nov. )-Cordaites principalis

本文论述了福建早二叠世晚期含煤地层,即童子岩组,它是福建省的主要含煤地层,一种典型的海陆交互相沉积。它不仅发育完整,含煤层数多,也含丰富的动植物化石。笔者通过对采自天湖山煤田、龙岩、永定等地植物化石系统研究,总结了早二叠世晚期植物群的面貌和特征。该植物群组成共计33属80种,分属于九大类群,其中以真蕨纲和种子蕨纲的大羽羊齿类和栉羊齿类最丰富为特征,并称之为Cigantonoclea spp.—Tingia carbonica Flora。此外,笔者将该植物群进一步划分为上、下两个植物组合,对早二叠世晚期古气候和古地理作了简要的分析和讨论。

 
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