斑岩矿床,porphyry deposit
1)porphyry deposit斑岩矿床
1.The views on the metallogenetic series of Chinaporphyry deposits;中国斑岩矿床成矿系列的几点认识
2)Porphyry deposits斑岩矿床
1.It won" t do to neglect the relations epithermal gold deposits and the porphyry deposits.从具体资料出发，认为扩大浅成低温热液作用的范围，摒弃中温热液和高温热液矿床，以及否定它们与斑岩矿床的关系是不妥当的；认为斑岩成矿系列是建立成矿模式、划分有关矿床的基础。
3)Porphyry molybdenum deposit斑岩钼矿床
1.Geological features and origin of Xiaodonggou porphyry molybdenum deposit in Hexigten Banner,Inner Mongolia;内蒙古小东沟斑岩钼矿床地质特征及成因探讨
英文短句/例句
1.Ore-forming time of the Jiguanshan porphyry molybdenum deposit, northern margin of North China Craton and the Indosinian mineralization.华北克拉通北缘鸡冠山斑岩钼矿床成矿年代及印支期成矿事件
2.Isotopic and element geochemical study of Jinduicheng superlarge porphyry Mo deposit in East Qinling area东秦岭金堆城大型斑岩钼矿床同位素及元素地球化学研究
3.Re-Os Dating of Molybdenite from the Sharang Porphyry Molybdenum Deposit in Gongbo"gyamda County,Tibet and Its Geological Significance西藏工布江达县沙让斑岩钼矿床辉钼矿铼-锇同位素年龄及其地质意义
4.Mineralization characteristics and prospective forecasting of Qulong porphyry copper(molybdenum) deposit in Tibet西藏驱龙斑岩型铜(钼)矿床矿化特征及远景预测
5.Geological characteristics and molybdenite Re-Os isotopic dating of Yuchiling porphyry Mo deposit in western Henan Province豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄
6.The Machangqing Porphyry Cu-Mo-Au Deposit in Yunnan Province: Magmatism and Mineralization云南省马厂箐斑岩型铜钼金矿床岩浆作用及矿床成因
7.A Study on the Enrichment of Pt and Pd in the Fengshan Porphyry Cu-Mo Deposits,Hubei丰山斑岩型铜(钼)矿床中铂、钯的富集特征研究
8.Space-Time Framework of Structure-Magma-Mineralization of Alkali-Rich Porphyry Mo-Cu-Au Polymetallic Deposit in Boxingchang, Yunnan Province云南宝兴厂富碱斑岩型铜钼金多金属矿床构造—岩浆—成矿时空结构
9.Host-rocks and alteration characters of the Baogutu porphyry copper-molybdenum deposit in Xinjiang, NW China.新疆包古图斑岩型铜钼矿床容矿岩石及蚀变特征
10.The Study on Metallogeny and Localizing Forecast of Yulong Porphyry Copper-Molybdenum Mineralization, Xizang (Tibet);西藏玉龙斑岩铜（钼）矿成矿作用与矿床定位预测研究
11.Machangqing Porphyry-type Cu-Mo-Au Deposit,Yunnan Province:Geological Characteristics and Its Genesis云南马厂箐斑岩型铜钼(金)矿床地质特征与矿床成因
12.Geological characteristics and prospecting mark of the Baishan porphyry Mo deposit, East Tianshan东天山白山斑岩型钼矿床的地质特征及找矿标志
13.Molybdenite Re-Os and SHRIMP zircon U-Pb dating of Duobuza porphyry copper deposit in Tibet and its geological implications西藏多不杂斑岩铜矿床辉钼矿Re-Os和锆石U-Pb SHRIMP测年及地质意义
14.Geology and Metallogenetic Setting of the Habo Porphyry Cu(Mo-Au) Deposit,Yunnan云南哈播斑岩型铜(-钼-金)矿床地质与成矿背景研究
15.Geology and ore-forming fluids of Xilekuduke porphyry Cu-Mo deposit in nothern Junggar.准噶尔北部希勒库都克斑岩钼铜矿床地质与成矿流体
16.The Tuwu and Yandong large porphyry copper (molybdenum) deposits were discovered recently in south-eastern Xinjiang, form the Eastern Tianshan porphyry copper belt.新疆哈密南部发现的土屋、延东大型斑岩铜(钼)矿床,构成了东天山斑岩铜矿带。
17.THE GEOCHEMICAL EVOLUTION OF HYDROTHERMAL FLUIDS IN PORPHYRY MOLYBDENUM DEPOSIT--TAKE THE AMERICAN HENDERSON PORPHYRY MOLYBDENUM DEPOSIT AS AN EXAMPLE斑岩钼矿热液流体的地球化学演化——以美国亨德森斑岩钼矿为例
18.Re-Os Isotopic Chronology of Molybdenite from the Taipinggou Porphyry-type Molybdenum Deposit in Inner Mongolia and Its Geological Significance内蒙古太平沟斑岩型钼矿床Re-Os等时线年龄及其地质意义
相关短句/例句
Porphyry deposits斑岩矿床
1.It won" t do to neglect the relations epithermal gold deposits and the porphyry deposits.从具体资料出发，认为扩大浅成低温热液作用的范围，摒弃中温热液和高温热液矿床，以及否定它们与斑岩矿床的关系是不妥当的；认为斑岩成矿系列是建立成矿模式、划分有关矿床的基础。
3)Porphyry molybdenum deposit斑岩钼矿床
1.Geological features and origin of Xiaodonggou porphyry molybdenum deposit in Hexigten Banner,Inner Mongolia;内蒙古小东沟斑岩钼矿床地质特征及成因探讨
4)porphyry copper deposit斑岩铜矿床
1.Three-dimensional metallogenic prediction of Pulangporphyry copper deposit in Yunnan Province by using GIS technology;基于GIS的云南普朗斑岩铜矿床三维成矿预测
2.Molybdenite Re-Os and SHRIMP zircon U-Pb dating of Duobuzaporphyry copper deposit in Tibet and its geological implications西藏多不杂斑岩铜矿床辉钼矿Re-Os和锆石U-Pb SHRIMP测年及地质意义
3.One of them,the Xuejiping medium-scaleporphyry copper deposit,lies in western porphyry belt;and in eastern porphyry belt the Pulang superlarge-scaleporphyry copper deposit lies.位于义敦岛弧南端的中甸岛弧已成为我国又一重要的斑岩铜矿产地,其中雪鸡坪中型斑岩铜矿床产于西斑岩带,普朗超大型斑岩铜矿床产于东斑岩带。
5)porphyry deposit斑岩型矿床
1.In addition, evidence is provided for the presence of volatile phase in skarn andporphyry deposits.通过总结多年来对夕卡岩型和斑岩型矿床的研究所获得的成果 ,作者认识到挥发相在这些矿床形成过程中的重要地位和意义。
6)porphyry Cu ore deposit斑岩Cu矿床
延伸阅读
斑脱岩 分子式 mAl2O3·nSiO2·xH2O CAS号 1302-78-9 性质 膨润土是一种以蒙脱石为主要矿物成分（可达85%～ 90%)的粘土岩、亦称蒙脱石粘土岩，常含少量伊利石、高岭石、埃 洛石、绿泥石、沸石、石英、长石、方解石等。一般为白色、淡黄 色，因含铁量变化又旦浅灰、浅绿、粉红、褐红、砖红、灰黑色等 。具蜡状、土状或油脂光泽。膨润土有的松散如土，也有的致密坚 硬；主要化学成分是二氧化硅、三氧化二铝和水，还含有铁、镁、 钙、钠、钾等元素，Na2O和CaO含量对膨润土的物理化学性质和工艺 技术性能影响颇大。蒙脱石矿物属单斜晶系，通常呈土状块体，白 色，有时带浅红、浅绿、淡黄等色。光泽暗淡。硬度1～2，密度2～ 3g/cm3。按蒙脱石可交换阳离子的种类、含量和层电荷大小，膨润 土可分为钠基膨润土（碱性土）、钙基膨润土（碱土性土）、天然 漂白土（酸性土或酸性白土），其中钙基膨润土又包括钙钠基和钙 镁基等。膨润土具有强的吸湿性和膨胀性，可吸附8～15倍于自身体 积的水量，体积膨胀可达数倍至30倍；在水介质中能分散成胶凝状 和悬浮状，这种介质溶液具有一定的粘滞性、能变性和润滑性；有 较强的阳离子交换能力；对各种气体、液体、有机物质有一定的吸 附能力，最大吸附量可达5倍于自身的重量；它与水、泥或细沙的掺 合物具有可塑性和粘结性；具有表面活性的酸性漂白土能吸附有色 离子。 用途 膨润土可作为粘结剂、吸附剂、填充剂、触变剂、絮 凝剂、洗涤剂、稳定剂、增稠剂等，用作化肥、杀菌剂和农药的载 体，橡胶和塑料的填料，合成树脂和油墨的防沉降助剂，颜料和原 浆涂料的触变和增稠，日用化工品的添加剂，医药的吸着剂和粘结 剂等，还广泛用于石油、冶金、铸造、机械、陶瓷、建筑、轻工、 造纸、纺织和食品等部门。
