1) Mudstone minerals
泥岩矿物
2) mud mineral
泥状矿物
1.
The relationship of aim mineral in ores fluorite and crypto-crystal quartz is very close ,the content of quartz is high,over 50%,its partical very fine,and there are some mud minerals in the ores.
矿石目的矿物萤石与细粒隐晶质石英关系极为密切,石英含量高,达50%以上,且呈极细粒状产出在萤石中,另外还含有泥状矿物(高岭土),提高萤石品位,降低精矿中硅含难度较大。
3) cement mineral
水泥矿物
4) diagenetic mineral
成岩矿物
1.
Based on generation relation of diagenetic minerals, fluid inclusion and fluorescence detection,the history of fluid activity and oil charging is reconstructed for reservoirs of Shasi Member located at depth of 1 600 m~2 700 m and 2 700 m~3 000 m.
通过成岩矿物的世代关系、流体包裹体研究和荧光检测,重现了研究区沙四段深部(2700m～3000m)和浅部(1600m～2700m)流体活动和油气充注历史。
2.
The accumulation properties of the reservoirs are mainly controlled by diagenetic mineral facies belts.
川西坳陷中段沙溪庙组砂岩储层极具非均质性,现今砂岩储集物性的优劣主要受成岩矿物相带的控制,其中以绿泥石-沸石成岩矿物相带为主体,高岭石成岩矿物相带为次,是研究区内有利于次生孔隙发育的成岩相标志,而板状碳酸盐成岩矿物相带以及石英增生成岩矿物相带则是砂岩致密化的重要标志。
3.
Its applications were discussed in the analyses and research of basin fluid diagenetic mineralogical age, fluid field character, evolution of formation water origin, reservoir heterogeneity, fluid movement trace, temperature and salinity of ancient fluid, distinguishing between sea facies and lake facies, diagenetic environment.
该文从原理出发,综合前人的研究,论述了其在盆地流体成岩矿物年代学分析、流体场特征分析、地层水成因演化研究、储层非均质性研究、流体活动示踪、古流体温度、盐度分析、海相、湖相区分、成岩环境分析等方面的应用。
6) rock-forming mineral
造岩矿物
1.
Application of X-ray crystallology on studying rock-forming mineral;
X射线晶体学对造岩矿物研究的应用
2.
Features of rock-forming minerals of Yanshanian mineralized granite in the polymetallic deposit concentration zone in southern Hunan and their implications for granite generation;
湘南多金属矿集区燕山期成矿花岗岩的造岩矿物特征及其成因意义
3.
In this paper, the chemical compositions of 105 rock-forming minerals of the volcanic rocks in Tengchong have been determined by the microprobe and systematically studied.
通过电子探针分析 ,系统研究了腾冲火山岩 10 5个造岩矿物的化学成分。
补充资料：泥岩
| 泥岩 mudstone 一种层理或页理不明显的粘土岩。矿物成分复杂，主要由粘土矿物（如水云母、高岭石、蒙脱石等）组成，其次为碎屑矿物（石英、长石、云母等）、后生矿物（如绿帘石、绿泥石等）以及铁锰质和有机质。质地松软，固结程度较页岩弱，重结晶不明显。常见类型有：①钙质泥岩。含适量碳酸钙，常见于大陆红色岩系和海洋、潟湖相的沉积岩层。②铁质泥岩。含较多的铁矿物，如赤铁矿、褐铁矿、针铁矿等，多见于红色岩层。③硅质泥岩。SiO2含量较高，不含或极少含铁质和碳酸盐质物，常与铁质岩、硅质岩、锰质岩相伴生。泥岩具吸水、粘结、耐火等性能，可用于制砖瓦、制陶等工业。
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参考词条