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n.生叶，发叶；叶形装饰；绿叶的状态；编张数号
1、floriation───n.花饰
2、exfoliation───n.剥落；剥落物；表皮脱落
3、volitation───n.飞翔，飞行
4、defoliation───n.落叶，去叶；[植]脱叶
5、spoliation───n.强夺；毁弃
6、filiations───n.父子关系；起源；私生子父亲之鉴定；分支
7、ciliation───n.具有睫毛；具有纤毛；睫毛
8、filiation───n.父子关系；起源；私生子父亲之鉴定；分支
9、foliations───n.生叶，发叶；叶形装饰；绿叶的状态；编张数号
1、The oil shale on the surface show opening foliation , abundant pore volume and low density because of less overburden pressure.───地表油页岩由于覆压减小等影响，页理张开、孔隙增加、密度减小。
2、The contact relationship of the two rock sections is structural foliation which have no upper and lower relationship in sequence.───两个岩段之间没有层序上的上下关系，为构造面理接触。
3、There are neoformative foliation and lineation(stretching lineation) in the shear zone.───剪切带以出现新生的面理和线理（拉伸线理）为特征。
4、In particular, the space is characterized by horizontal distribution of projective sphere bundle to have flat foliation.───特别地，这个空间可以由摄影球丛具有平坦的叶状结构的水平分布来刻划。
5、whereas foliation attitude of gneiss type exerts a relatively weak role in controlling attitude of miniature faults in gneiss type rocks.───而片麻岩类岩石叶理产状对发育于该类岩石内的微断层产状控制作用相对较弱。
6、If cherimoyas do not receive enough chilling, the trees will go dormant slowly and then experience delayed foliation .───集散地，如果没有得到足够的严冬，将树木休眠去慢慢体会，然后延迟叶状结构。
7、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。
8、In addition, the presence and absence of foliation are an other factor to classify fault rocks.───除此之外，是否具有片理构造是划分断层岩的另一个因素。
9、Foliated fault rocks are characterized by well-developed foliation which is resulted from the preferred orientation of mineral grains in the rock.───理化断层岩石具有发育良好的面理构造，这些面理是岩石中矿物颗粒优选定向而造成的。
1、Foliation, bloom, and production became erratic.
2、B1 and B2: carbon-free, no foliation, saturated with electrolyte and distilled water respectively.
3、The magnetic lineation and magnetic foliation study of the ore area show that the magnetic fabric study can proclaim the stress field of rock deformation as the petrofabric analysis.
4、In the north Dabieshan domain, early foliation and N-S-trending compressional lineation are deformed by N-verging folds coeval to the syn-exhumation ductile structures of the central Dabieshan domain.
5、B1: carbon-free, no foliation, saturated with electrolyte.
6、Base foliation is fascicular, cauline foliation each other is unripe, feather crack.
7、On the surface of foliation there develops strong stretching lineation defined by alignment of elongated minerals.
8、Using the group foliation method to solve the nonlinear wave equation.
9、Foliation is particularly pronounced.