1) monomineralic rock
单矿物岩
2) anchimonomineralic rock
近单矿物岩
3) monomineralic topaz rock
黄玉单矿物岩
1.
Experimental study on the system granite-H2O-RF(R = Li, Na, K, Rb, Cs and H+ ) indicates that monomineralic topaz rock can crystallize from an F-rich magma.
业已在自然界发现中深成相、超浅成相和良好封闭相的岩浆成因黄玉单矿物岩,拥有宏观、微观岩浆成因标志,得到有关富挥发分酸性岩体成岩、成矿实验成果的有力佐证,属一类新的岩浆岩。
4) monomineralic rock
单矿岩
5) 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。
补充资料：造岩矿物
见“矿物”(996页)。
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