2) Carbonate mineral
碳酸盐矿物
1.
An elementary description of carbonate mineral grownextensively in gold deposit;
浅谈金矿床广泛发育的碳酸盐矿物
2.
The cathodoluminescence and trace elements in carbonate minerals;
碳酸盐矿物的阴极发光性与微量元素的关系
3.
Controlling factors of cathodeluminescence of carbonate minerals
碳酸盐矿物阴极发光性的控制因素分析
3) carbonate minerals
碳酸盐矿物
1.
X-ray diffraction and petrography analysis showed that the burial depth from 2500 meters to 3000 meters was favorable to diagenetic evolution of clay and carbonate minerals in source rock.
粘土矿物和碳酸盐矿物的转化对烃源岩力学性质产生了影响,导致随埋藏深度的增加岩石由相对塑性向相对脆性转变。
2.
Mineralogical examination and stable isotope analyses for the Lake Qinghai sediments indicate that authigenic carbonate minerals are present either in the form of one type or several types in the sediments, and that large differences in δ18O of up to 6.
青海湖沉积岩芯的矿物学和稳定同位素研究结果显示自生碳酸盐矿物以单种或多种矿物形式保存在沉积物中;不同碳酸盐样品的δ18O值的变化范围为5。
4) carbonate
[英]['kɑ:bəneit] [美]['kɑrbə,net]
碳酸盐矿物
1.
Silicate minerals and carbonate are the main rock-forming minerals of the earth s crust.
硅酸盐矿物和碳酸盐矿物是构成地壳的主要造岩矿物,论述了两类矿物溶解动力学的研究现状与展望,指出两类矿物的溶解和沉积过程中CO2吸收和释放,对全球环境有重要影响。
2.
The relationship between the formation of some typical mineral (the authigenic pyrite and the ferruginous carbonate) and hydrocarbon is discussed in this paper, based on the correlation of stratigraphic features and diagenetic mineral in different structural belt in the Member 3 of Shahejie Formation from Dongying Depression.
针对自生黄铁矿-碳酸盐矿物-自生石英矿物组合,提出了示烃球的新认识并将其分为两大类,I型示烃球主要分布于含油性较好层段,II型示烃球主要分布于烃类活动相对较弱的非含油层段。
5) Genesis of carbonate minerals
碳酸盐矿物成因
6) authigenic carbonate mineral
自生碳酸盐矿物
1.
By means of thin-section analysis, cathodeluminecenme analysis, element analysis, isotope analysis and SEM examination, authigenic carbonate mineral in the early Tertiary sandstone of south-central XiHu depression was studied here.
论文运用阴极发光、扫描电子显微镜、偏光显微镜和化学分析等手段，对西湖凹陷中南部古近系砂岩储层中自生碳酸盐矿物的矿物学、岩石学、地球化学特征进行了综合分析，评价了碳酸盐胶结物对储层的影响，探讨了碳酸盐胶结物的形成机制。
补充资料：盐类矿物
分子式：
CAS号：
性质：碱金属、碱土金属的卤化物，硫酸盐，碳酸盐，重碳酸盐及少量硼酸盐、硝酸盐等矿物的总称。其主要种类如下。(1)氯化物：岩盐NaCl，钾盐KCl，光卤石KCl·MgCl2·6H2O。(2)硫酸盐类：无水钾镁矾K2SO4·2MgSO4，钾芒硝K2SO4·Na2SO4，杂卤石K25O4·MgSO4·2CaSO4·2H2O，芒硝Na2SO4·10H2O；硬石膏CaSO4、石膏CaSO4·2H2O。(3)碳酸盐：苏打Na2CO3·10H2O。(4)硼酸盐：硼钾镁石KMg2B11O19·9H2O。盐类矿物是由盐湖水分强烈蒸发，卤水浓度增高，先后从溶液中析出结晶而成。主要用于化工、食品和建筑材料工业等。
CAS号：
性质：碱金属、碱土金属的卤化物，硫酸盐，碳酸盐，重碳酸盐及少量硼酸盐、硝酸盐等矿物的总称。其主要种类如下。(1)氯化物：岩盐NaCl，钾盐KCl，光卤石KCl·MgCl2·6H2O。(2)硫酸盐类：无水钾镁矾K2SO4·2MgSO4，钾芒硝K2SO4·Na2SO4，杂卤石K25O4·MgSO4·2CaSO4·2H2O，芒硝Na2SO4·10H2O；硬石膏CaSO4、石膏CaSO4·2H2O。(3)碳酸盐：苏打Na2CO3·10H2O。(4)硼酸盐：硼钾镁石KMg2B11O19·9H2O。盐类矿物是由盐湖水分强烈蒸发，卤水浓度增高，先后从溶液中析出结晶而成。主要用于化工、食品和建筑材料工业等。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条