地槽

dì cáo
  • geosyncline
地槽地槽
  1. 华北地台与秦岭地槽构造关系初探

    Preliminary study of relationship between North China platform and Qinling geosyncline

  2. 新疆西准噶尔地槽多旋回发展及其迁移特征

    Property of the polycyclic development and migration of West Junggar geosyncline

  3. 应用PH3发生器地槽熏蒸杀虫试验报告

    Test report of ph_3 generator application in underground aeration passage

  4. 地槽褶皱带钙碱性安山流纹质火山岩有关的AgSnCuPbZn(Au)成矿亚系列;

    Ag-Sn-Cu-Pb-Zn - ( Au ) subseries related to calc - alkaline basaltic - rhyolitic volcanic rocks of geosyncline (ⅳ);

  5. 介绍了利用电容液位计和DCS控制系统的比值仪表模块的结合,成功地对成品碱地槽液位测量实施改进的工作内容。

    Combing capacitance-type level meter and ratio instrument module of DCS controlling system level determination of product caustic soda ground bunker was successfully innovated .

  6. 综合研究表明,W-Sb-Au型金矿床的赋矿层位形成于地壳强烈活动期(地槽期、地洼期)。

    The synthetic study shows that the host-rock layers of the W-Sb-Au type gold deposits were formed during the strongly active stages of the crust evolution ;

  7. 该成矿带位于北祁连加里东优地槽的东南缘。这里是向南俯冲敛合板块残留的岛弧。CAB插槽42和地、CAB插槽5。

    Being the residual island are of the convergent plate subducted to the south , the central Baiyin Minerogenetic Belt is located at the southeast edge of the north Qilian Caledonian eugeosyncline .

  8. 在Blatt等(1972)图解中,落入优地槽区。

    Fall into slot in Blatt etc. ( 1972 ) map .

  9. 下扬子区中上元古界,可以分为四个构造层次.中元古界早期构造层,为一套巨厚的地槽型火山碎屑岩及砂泥质复理石建造,形成于1900-1400Ma;

    The middle-upper Proterozoic of lower Yangtze area can be divided into four structural layers : the first one , formed at early stage of middel Proterozoic ( 1900-1400Ma ), was characterized by a suit of geosyncline pyroclastic rocks and flysch formation ;

  10. 矿区经历了地槽-地台-地洼三个构造发展阶段;

    Baoshan area has passed three geotectonic stages which are geosyncline-platform-geodepression .

  11. 从板块构造观点论地槽

    On the subject of geosynclines from the viewpoint of plate tectonics

  12. 川西盐边群的优地槽岩石组合

    Eugeosyncline rock association of Yanbian group in Western sichuan , China

  13. 秦岭地槽汞锑资源成矿探讨

    Research on hg , sb mineralization in Qinling geosyncline , China

  14. 两种地槽风道通风性能的比较

    Comparison of ventilation characteristics of two kinds of land groove air DUT

  15. 对扬子地台与秦岭地槽的边界作了新的推断;

    The boundary between Yangzi platform and Qinling geosyncline has been reinterpreted .

  16. 新疆阿尔泰地槽成矿元素分布特征

    Distribution characteristics of mineralization elements in Altay geosynclinal , xinjiang

  17. 秦岭地槽褶皱系的多旋回成矿作用

    A preliminary study on the polycyclic mineralization in Qinling geosynclinal fold system

  18. 大兴安岭地槽褶皱系岩金找矿远景分析

    Gold prospecting in Da Xing'anling geosynclinal folded system , China

  19. 边界问题或构造关系问题,一直是地质学家最为关心的问题之一。华北地台与秦岭地槽构造关系的实质是洋壳与陆壳的矛盾统一和相互转化。

    The Problem of boundary or tectonic relation has been interesting to geologists .

  20. 广东大地构造位于华南加里东地槽褶皱系。

    Tectonically , Guangdong is located in the south China Caledonian Geosynclinal Folded System .

  21. 得克萨斯海湾有一海岸在墨西哥湾海岸地槽中。

    One , the Texas Gulf Coast , is in the Gulf Coast geosyncline .

  22. 钦州残余地槽回返时期的思考

    Consideration on inversion period of Qinzhou residual geosyncline

  23. 地槽常受深断裂控制。

    Geosyncline is always controlled by deep fractures .

  24. 东苏旗南部处于内蒙古中部地槽褶皱系。

    The south Dongsuqi is located in the geosynclinal fold system of Middle Inner Mongolia .

  25. 中华地台与兴蒙古生代地槽褶皱区界线的重新厘定

    Redetermination of the boundary between Chinese platform and Da Hinggan Ling-Mongolian Paleozoic geosynclinal folded belt

  26. 地槽学说与板块构造

    Geosyncline theory and plate tectonics

  27. 祁连优地槽区块状硫化物矿床形成地质环境的初步对比研究和探讨

    A preliminary investigation into the ore forming environment of the massive sulfide deposits in the Qilian eugeosyncline

  28. 作者认为地槽学说与板块构造没有矛盾。

    In the author 's opinion , geosyncline theory should not be in contradiction with plate tectonics .

  29. 露天囤套膜高水分小麦地槽通风安全储藏试验

    Safe storage of wheat at high moisture content stored in the open air with aeration through ground passage

  30. 对中国大地构造特点的一些认识并着重讨论地槽褶皱带的多旋回发展问题

    On some of the tectonic characteristics of China with special discussion on the polycyclic development of geosynclinal FOLDBELTS