1.The form of secondary minerals is schistose aggregated and spherical.
次生矿物形态主要呈片状集合体和球状体。
2.These secondary pores formed the main accumulative interspace of semi deep reservoir. The throat shape is point and schistose.
同时这些次生溶孔构成了储层的主要储集空间，而连通孔隙的喉道多为点-片状；
3.Typically the rock is massive , but commonly it is flaggy or schistose .
这类岩石典型地呈块状，但常呈薄板状或片理化。
4.The latter two rock types have a slaty to schistose structure, they are green in fresh state and show a silvery lustre on foliation planes.
后两种岩类有着从板状构造向片状构造的发展趋势，在清新状态下呈绿色，并在叶理面上显示一种银色光泽。
5.Grasslands on mountain slopes, stony or pebbly calcareous or schistose mountain slopes, steppes, roadsides, or as a field weed;
多石子的山坡草地，石质或石灰或山坡，干草原，路旁，作为田野杂草的或；
6.Characters of schistose structure of Nanjing's sand and seismic liquefaction of subsoil of a metro section
南京砂的结构特性与地铁地基液化判别