碳酸盐风化壳

  • 【土】carbonated weathering crust
碳酸盐风化壳碳酸盐风化壳
  1. 下奥陶统马家沟组为低渗透率碳酸盐岩风化壳气藏;

    Low-permeability carbonate gas reservoirs of Majiagou Formation , Lower Ordovician ;

  2. 碳酸盐岩风化壳及喀斯特成土作用研究

    Weathering Crust of Carbonate Rocks and Process of Karst Soil Formation

  3. 锌硼硅-氧化铝微晶玻璃的制备及性能硅铝碳酸盐型风化壳

    PREPARATION AND PROPERTIES OF ZBS-Al_2O_3 GLASS-CERAMICS siallite-carbonate weathered crust

  4. 碳酸盐岩风化壳界面土层的结构和矿物学特征

    Characteristics of structure and mineralogy of interface laterite in weathering crust of carbonate rocks

  5. 拆去空气净化器外壳。硅铝碳酸盐型风化壳

    Remove air cleaner housing . siallite-carbonate weathered crust

  6. 酸不溶物对碳酸盐岩风化壳发育程度的影响

    Impact of Acid-Insoluble Residua of Carbonate Rocks on Developing Intensities of Their Weathering Crusts

  7. 石灰土(碳酸盐岩风化壳)形成地球化学过程研究

    Study on geochemical processes in limestone soil profiles

  8. 高海拔山地碳酸盐岩风化壳的发育特征及其地貌意义

    The developing features and the geomorphic significance of carbonate rocks weathering crust on high mountains

  9. 碳酸盐岩风化壳岩-土界面地球化学特征及其形成过程&以贵州花溪灰岩风化壳剖面为例

    Geochemical characteristics and formation mechanism of rock-soil interface in limestone weathering crust at huaxi , Guizhou Province

  10. 碳酸盐岩风化壳母岩的不均一性:来自粒度分析的证据

    The inhomogeneity of the basement carbonate rock developing weathering crust : the evidence from grain size analysis

  11. 碳酸盐岩风化壳储层空间分布预测与油气疏导格架的匹配关系研究

    Study on the Distribution Prediction of Carbonate Weathering Crust Reservoir Space and Its Relationship with Oil-gas Grooming Framework

  12. 贵州碳酸盐岩风化壳中晶体石英的硅同位素组成及硅质来源探讨

    Silicon Isotopic Composition and Silica Source of Quartz Crystals in the Weathering Crusts of Carbonate Rocks , Guizhou Province

  13. 混合铵盐用于风化壳淋积型稀土矿浸取稀土的动力学研究硅铝碳酸盐型风化壳

    Kinetics of leaching rare earth from a weathered crust elution-deposited rare earth ore in South China with mixed ammonium salt

  14. 贵州碳酸盐岩风化壳中的晶体石英具有较强的测年潜力,其成因判别是年代学研究的前提和基础。

    The ages of crystal quartz determined by the fission track method are well feasible and credible , while the origin of crystal quartz is the precondition and groundwork of the method .

  15. 本文通过对稀土赋存状态的实验研究,结合稀土元素质量迁移系数,系统的分析了稀土元素在碳酸盐岩风化壳中的迁移、转化行为,探讨了稀土发生富集和分异的机理。

    This paper through the studies about the combining states of REE and the mass transport coefficient , analyses the behavior of REE systematically and provides the mechanism about the enrichment and fractionation of REE .

  16. 如何综合利用钻井、地质、测井、地震资料进行碳酸盐岩风化壳储层评价是鄂尔多斯盆地下古生界天然气勘探中亟须解决的问题。

    Using all available information ( drilling , geology , well-logging and seismic data ) to evaluate carbonate weathering crust reservoir is a hard job in gas exploration in lower Paleozoic reservoirs in the Erdos basin .

  17. 碳酸盐岩红色风化壳Ce异常特征及形成机理

    The charateristics of CE anomalies in weathering crusts of carbonate rocks and its formation mechanism

  18. 在碳酸盐岩红色风化壳上部Ce显示正异常,底部富集层显示强烈负异常。

    Ce shows positive anomalies in the upper and intense negative anomalies at the bottom .

  19. 碳酸盐岩红色风化壳中的氧化铁矿物

    Iron oxide minerals in red weathering crust of carbonate rocks

  20. 黎塘碳酸盐岩红土风化壳形成的地球化学过程演绎

    Deduction of geochemical forming process of carbonate laterite weathering crust at Litang in Guangxi

  21. 微地域搬运&碳酸盐岩红色风化壳形成过程的一种方式

    Micro-Area Transportation of Residues : A Style of Forming the Red Weathering Crusts of Carbonate Rocks

  22. 贵州碳酸盐岩红色风化壳稀土富集与分异的机理研究

    The Mechanism about the Enrichment and the Fractionation of Ree of the Red Residua in Karst Terrains of Guizhou Province

  23. 堆山造景工程是一项利用建筑渣土,在坑塘上进行堆载的市政工程。黎塘碳酸盐岩红土风化壳形成的地球化学过程演绎

    The construction waster of the city was gathered to fill the pond . DEDUCTION OF GEOCHEMICAL FORMING PROCESS OF CARBONATE LATERITE WEATHERING CRUST AT LITANG IN GUANGXI

  24. 通过对白云岩和灰岩风化壳稀土赋存状态的对比,发现在碳酸盐岩红色风化壳中稀土具有相同的赋存和转化规律。

    Through comparing the REE combining states between the dolomite and the limestone weathering profiles , we find that REE has the similar combing states and transformation characters .

  25. 弄清碳酸盐岩红色风化壳中稀土富集和分异的机理,有助于丰富稀土表生地球化学知识,同时也为喀斯特地区风化成土地球化学过程和土壤物质来源的示踪提供了重要依据。

    Studying the mechanism about the enrichment and fractionation of REE , will help to enrich the knowledge about the geochemistry and provide the important evidences about weathering and pedogenesis of carbonate rocks and the provenance of the red residue .