| 1. | Corrensite forms networks of crinkled or folded sheets .
柯绿泥石呈卷曲网状或折迭片状。 |
| 2. | Of these minerals, kaolinite, illite and chlorite are commonest .
在这些矿物中，高岭石，伊利石和绿泥石最常见。 |
| 3. | Clay fraction is dominated by illite and kaolinite with small proportions of smectite , chlorite and vermiculite
粘粒组成主要为伊利石和高岭石，也有少量蒙皂石、绿泥石和蛭石。 |
| 4. | Fine - grained feldspar sandstone is the main oil - bearing rock and chlorite is the dominant kind of clay minerals
研究结果表明，长2油藏含油砂岩以细粒长石砂岩为主，粘土矿物中绿泥石含量较高。 |
| 5. | Group leading products for magnesium fertilizer products series , magnesium oxide product series , lingmei chemical products series , lu : nidan powder and powder series
集团的主导产品为镁肥料产品系列、氧化镁产品系列、菱镁化工产品系列、绿泥石粉及滑石粉系列。 |
| 6. | The cementation of laumonite , calcite and chlorite , compact and pressure solution , as well as the dissolution of laumontite , feldspar are also of main factors which affect reservoir properties
方解石、绿泥石、浊沸石的胶结作用、压实压溶作用和浊沸石、长石的溶解作用也是影响储集性能的主要因素。 |
| 7. | The ore ' s mineral component is simple , and its main association of minerals are leucocratic sphalerite - galenite ? iopsite ( epidot , chlorite ) . leucoratic sphalerite and diopsite are the guide minerals in the ore
主要矿物组合为浅色闪锌矿-方铅矿-透辉石(绿帘石、绿泥石) ，其中浅色闪锌矿和透辉石为该类矿石的标型矿物。 |
| 8. | The xrd and sem indicate that the types clay consists of i / s mixed layer , illite and kaolinite . the i / s mixed layer is the most abundant mineral in the clay samples . the chlorite clay mineral has not been detected in the formation
Xrd与sem综合分析证实，砂岩中粘土矿物由i s混层、伊利石与高岭石组成，其中以i s混层为主，样品中没有发现绿泥石矿物。 |
| 9. | Clay minerals are of illite , chlorite , kaolinite and smectite assemlblage . the content of illite is very high and its crystallinity index is high too , which indicate the cool and arid climate condition in the time of sediment conformation
粘土矿物组合为伊利石、绿泥石、高岭石和蒙皂石，伊利石含量占绝对优势，其结晶度指数( hw )较高，反映东海南部外陆架粘土形成于寒冷干燥的气候环境。 |
| 10. | With the intermittent activity of hot fluid containing cc ^ , ferrous carbonate minerals dissolved and precipitate repeatedly many times . in addition , dissolution of shells and feldspars , decrease of chlorite and increase of kaolinite could be found
随着富co _ 2热流体多次间歇性入侵导致了含铁碳酸盐矿物的反复多次溶解和沉淀、生物介壳大量溶蚀和长石铸模孔的形成以及绿泥石消失、高岭石增加等。 |
