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   成矿作用 在 石油天然气工业 分类中 的翻译结果: 查询用时:0.481秒
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成矿作用
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  mineralization
    Additionally, it is also helpful to discuss the fluid action in deep crust, the interaction between fluid and rock, as well as the mineralization of other energy mineral deposits such as sandstone-type uranium deposit according to basin fluids analyzing.
    并对探讨深部地壳流体作用、流体-岩石相互作用及其它能源矿产(如:砂岩型铀矿)的成矿作用等具有重要意义。
短句来源
    DSDP and ODP have revealed numerous paleoceanographic events and paleoenviron-mental changes which controlled the formation and distribution of marine mineral re-sources,and provided vast amount of scientific data for the study of marine mineralization.
    深海钻探与大洋钻探发现的许多古海洋事件和古环境变化,控制着海洋矿产的形成与分布,并为研究海底成矿作用提供了大量科学资料。
短句来源
    The geological practice has proven that there is an in- ner original relation between sequence boundaries,system tracts and mineralization of solid or liquid minerals.
    层序界面和体系域与固、液体矿产的成矿作用存在内在的、有机的成因联系。
短句来源
    This kind of cause and effect coupling relation with mineralization brings to light the real value of sequence stratigraphy,also gives a new challenge to sequence stratig- raphy.
    这种与成矿作用有关的因果耦合关系揭示了层序地层学应有的价值,反之学科的交叉又向层序地层学发出了新的挑战。
短句来源
  “成矿作用”译为未确定词的双语例句
    Formation of Carlin-Type Gold Deposit by Hydrocarbon Fluid and its Correlation to Accumulation and Dispersion of Petroleum in Youjiang Basin, South China
    有机流体成矿作用与古油藏成藏作用相互耦合——以右江盆地微细浸染型金矿为例
短句来源
    Geochemical Characteristics of Hydrocarbonearing Area Pb-Zn Ore Deposits in Jinding and Their Metallogenic Role
    金顶铅锌矿床油气地球化学特征及其成矿作用探讨
短句来源
    Large-scale metallogenesis and petroleum field formation in continental China——constraints from the lithosphere
    中国大陆大规模成矿作用油气田形成——来自岩石圈的约束
短句来源
    The formation of the Carlin-type gold deposit by the hydrocarbon fluid and its correlation to the accumulation and dispersion of petroleum in Youjiang basin, South China
    有机成矿流体成矿作用与古油藏成藏作用的相互耦合——以右江盆地微细浸染型金矿为例
    The present paper deals with the relationship of the evolution of sedhoentary basin andmineralhation during Mesozoic time.
    本文讨论了长江中下游地区中生代沉积盆地演化与成矿作用的关系。
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  mineralization
Potential rates of microbial P immobilization were greater than those of organic P mineralization in mineral soils for both forests.
      
The decomposition study showed that A450 exhibited significantly higher decomposition rate, mineralization rates of N, P and K as well as much shorter N and P net immobilization periods.
      
They show potential as carriers for drug controlled delivery and templates for biomimetic mineralization.
      
Effects of pH and initial Ca2+-H2PO4- concentration on fibroin mineralization
      
In the present study, the effects of pH and initial Ca2+-H2PO4- (Ca-P) concentration on fibroin mineralization were studied.
      
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DSDP and ODP have revealed numerous paleoceanographic events and paleoenviron-mental changes which controlled the formation and distribution of marine mineral re-sources,and provided vast amount of scientific data for the study of marine mineralization.ODP and other related studies have proved that the development AABM and up-welling , high siliceous bioproductivity,and hiatus during Eocene , Oligocene , Miocene andPliocene were favourable for the formation of polymetallic nodules , Co-rich crusts andphosphorites,Thus,DSDP...

DSDP and ODP have revealed numerous paleoceanographic events and paleoenviron-mental changes which controlled the formation and distribution of marine mineral re-sources,and provided vast amount of scientific data for the study of marine mineralization.ODP and other related studies have proved that the development AABM and up-welling , high siliceous bioproductivity,and hiatus during Eocene , Oligocene , Miocene andPliocene were favourable for the formation of polymetallic nodules , Co-rich crusts andphosphorites,Thus,DSDP and ODP have greatly contributed to the theory of marine min-eralization.

深海钻探与大洋钻探发现的许多古海洋事件和古环境变化,控制着海洋矿产的形成与分布,并为研究海底成矿作用提供了大量科学资料。大洋钻探及其他有关研究已经证明,南极底层水和上升流的发育,硅质生物的高生产力,以及始新世、渐新世、中新世与上新世的沉积间断,都有利于多金属结核、富钴结壳和磷灰石的形成。因此,深海钻探和大洋钻探对于海洋成矿理论有重大贡献。

The present paper deals with the relationship of the evolution of sedhoentary basin andmineralhation during Mesozoic time.During the Indo-Sinin tectonic movement,a series of downwarping basins were formedand those of the sediments of ore formation in a regression sequence were deposited. In theearly Middle Triassic, locally occurred a Sabkha circumstance and evaporite as well as hteh fer-ric carbonate and Pb-Zn deposits were formed,i. e. the Zhouchongcun group. In the MiddleTriassic, Cupreous sandstone formation...

The present paper deals with the relationship of the evolution of sedhoentary basin andmineralhation during Mesozoic time.During the Indo-Sinin tectonic movement,a series of downwarping basins were formedand those of the sediments of ore formation in a regression sequence were deposited. In theearly Middle Triassic, locally occurred a Sabkha circumstance and evaporite as well as hteh fer-ric carbonate and Pb-Zn deposits were formed,i. e. the Zhouchongcun group. In the MiddleTriassic, Cupreous sandstone formation was deposited in a front delta conditbo as tlie Huang-maqing group. Uraniferous Sandstones was formed below the Xiangshang formation by organ-ic processes. During the Cretaceous anhydrite (salt) beds were formed in the faulted basin thatresulted from tensional tectonism' As a whole, the basinal evolution and the brine fiuids arethe foundamental cause of the polycyclic ore formatfon.

本文讨论了长江中下游地区中生代沉积盆地演化与成矿作用的关系。印支旋回本区在挤压构造环境下,形成坳褶盆地和海退序列的含矿建造;早中三叠世在局限台地-萨布哈环境下形成周冲村组富铁碳酸盐、铅锌、膏(盐)等合矿建造;中三餐世与三角洲前线亚相有关的沉积环境下形成黄马青组含铜砂岩建造。南象运动是一次变格运动,其界面直接控制象山组砂岩铀矿。晚自垩世与拉伸引张构造有关,形成断陷盆地中的巨厚膏盐矿产.作者认为盆地演化及卤水流体是本区多旋回成矿作用最本质的因素。

After leaching blackshales with CHCL3, HaAc-NaAc buffer, HCl-H3PO4 mixture, HCl-HP mix-ture and heavy liquid sequentially, chloroform extracted bitumen-A, carbonate, ferromanganese oxide,silicate components and kerogen are obtained respectively-The recovery of standard addition for different components ranges 86%-104.3%. The sequential analysis is applicable to, besides the study of main components in oil shales, biomineralization research.

用三氯甲烷、醋酸-醋酸钠缓冲溶液、盐酸-磷酸混合液、盐酸-氢氨酸混合液和重液分离法,依次处理暗色泥质岩,分别得到氯仿沥青A、碳酸盐组分、铁锰氧化物组分、硅酸盐组分,最后得到生油母质干酪根。各组分的标准加入回收率为38%~104.3%。除用于油页岩中主要组分的赋存状态研究外,该分析方法亦适用于生物成矿作用研究。

 
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