这种变化反映了埋藏成岩作用对原来沉积的粘土矿物组合的影响。
These changes reflect the effects of burial diagenesis on the originally deposited clay mineral assemblage.
根据自生矿物与粘土矿物组合，在塔里木中新生界碎屑岩中可以识别出两种成岩环境。
Based on the authigenic and clay mineral assemblage, two types of diagenetic ambient have been recognized in the meso - cainozoic detrital rocks in tarim basin.
利用断面沟扇体系及基底形态、地震反射结构、粘土矿物组合、岩屑类型、重矿物组合明确古流向和物源。
Source orientation was studied by using Basement and fractured surface form, Seismic Reflection structure, Clay mineral Assemblages, cuttings type and heavy mineral Combination.
粘土矿物的组合类型以伊利石-蒙皂石-高岭石-绿泥石型为主，伊利石-高岭石-蒙皂石-绿泥石型次之；
The research results show that the content of the illite in this area is the highest, the smectite or kaolinite are the second and chlorite is the lowest;
粘土矿物的组合类型以伊利石-蒙皂石-高岭石-绿泥石型为主，伊利石-高岭石-蒙皂石-绿泥石型次之；
The research results show that the content of the illite in this area is the highest, the smectite or kaolinite are the second and chlorite is the lowest;
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