青年中文青年中文

foliation的意思

foliation中文翻譯:

n.生葉,發葉;葉形裝飾;綠葉的狀態;編張數號

相似詞語短語

foliations───n.生葉,發葉;葉形裝飾;綠葉的狀態;編張數號

filiation───n.父子關系;起源;私生子父親之鑒定;分支

defoliation───n.落葉,去葉;[植]脫葉

exfoliation───n.剝落;剝落物;表皮脫落

filiations───n.父子關系;起源;私生子父親之鑒定;分支

floriation───n.花飾

spoliation───n.強奪;毀棄

volitation───n.飛翔,飛行

ciliation───n.具有睫毛;具有纖毛;睫毛

雙語使用場景

Foliated fault rocks are characterized by well-developed foliation which is resulted from the preferred orientation of mineral grains in the rock.───理化斷層巖石具有發育良好的面理構造,這些面理是巖石中礦物顆粒優選定向而造成的。

In addition, the presence and absence of foliation are an other factor to classify fault rocks.───除此之外,是否具有片理構造是劃分斷層巖的另一個因素。

In particular, the space is characterized by horizontal distribution of projective sphere bundle to have flat foliation.───特別地,這個空間可以由攝影球叢具有平坦的葉狀結構的水平分布來刻劃。

The contact relationship of the two rock sections is structural foliation which have no upper and lower relationship in sequence.───兩個巖段之間沒有層序上的上下關系,為構造面理接觸。

If cherimoyas do not receive enough chilling, the trees will go dormant slowly and then experience delayed foliation .───集散地,如果沒有得到足夠的嚴冬,將樹木休眠去慢慢體會,然后延遲葉狀結構。

The oil shale on the surface show opening foliation , abundant pore volume and low density because of less overburden pressure.───地表油頁巖由于覆壓減小等影響,頁理張開、孔隙增加、密度減小。

whereas foliation attitude of gneiss type exerts a relatively weak role in controlling attitude of miniature faults in gneiss type rocks.───而片麻巖類巖石葉理產狀對發育于該類巖石內的微斷層產狀控制作用相對較弱。

There are neoformative foliation and lineation(stretching lineation) in the shear zone.───剪切帶以出現新生的面理和線理(拉伸線理)為特征。

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.───后兩種巖類有著從板狀構造向片狀構造的發展趨勢,在清新狀態下呈綠色,并在葉理面上顯示一種銀色光澤。

英語使用場景

Foliation is particularly pronounced.

Using the group foliation method to solve the nonlinear wave equation.

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.

B1 and B2: carbon-free, no foliation, saturated with electrolyte and distilled water respectively.

Base foliation is fascicular, cauline foliation each other is unripe, feather crack.

Foliation, bloom, and production became erratic.

B1: carbon-free, no foliation, saturated with electrolyte.

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.

On the surface of foliation there develops strong stretching lineation defined by alignment of elongated minerals.