White mica formed at earlier fluid_rich stage is dominantly phengite with atom number of Si varying between 6.5 and 7.2 pfu .

富流体阶段早期的 白色 云母主要为多硅白云母，其Si原子数介于6.5pfu和7.2pfu之间；

Structural characteristics of thin films of white mica

四川 白云 母薄膜的结构特性

( 3 ) With increasing Li and ( Al + Ti ) white mica evolves from siderophyllite in zone a b and c to zinnwaldite in zone d ;

随着Li和（Al+Ti）含量的增加， 白色 云母成份从a，b，c带的铁叶云母演化到d带的铁锂云母；

The fluid_bearing stage proceeded at high temperatures and pressures and is characterized by the participation of minor fluids . White mica formed at this stage is dominated by phengite .

弱流体阶段有少量流体参与，并且其压力、温度较高，形成的 白色 云母主要为多硅白云母；

Calcined clay / LEE white slippery powder / PY ⅱ water white mica powder / titanium white powder 105 ~ 115 phr ;

补强填充剂为煅烧陶土、LEE白滑粉、PY－Ⅱ型水 白云 母粉和钛白粉并用体系（105～115份）；

Multifunctional materials prepared by means of the surface treatment about crude white mica

天然 白云 母表面改性制备多功能材料

Compositions of detrital white mica grains from early Mesozoic sedimentary rocks in the eastern Jianghan basin : constraints on the exhumation of the HP-UHP rocks in Dabie orogen

江汉盆地东部早中生代沉积地层碎屑 云母成分：对大别高压-超高压岩石暴露作用的约束