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1)  facies tract of diage-netic minerals
成岩矿物相带
2)  metallogenic magmatic rock belt
成矿岩带
3)  diagenetic facies band
成岩相带
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。
5)  magmatic metallogenetic belt
岩浆成矿带
6)  middle Yunnan sandrock minerlization area
滇中砂岩成矿带
补充资料:造岩矿物
见“矿物”(996页)。
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