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- Foliation, bloom, and production became erratic. 萌芽、開花和結果變得很不正常。
- The deposits belong to altered cataclastic rock type. 金礦體受斷裂構造的直接控制。
- On the surface of foliation there develops strong stretching lineation defined by alignment of elongated minerals. 在片理面上發育有強烈的拉伸線理,這些線理則是由拉長的礦物定向展布而顯示。
- 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岩的另一個因素。
- Let us keep walking perpendicular to the trend of foliation to get more details. 我們垂直這些片理化岩石的走向穿越一段並作詳細觀察。
- Fault rocks with a random fabric include fault breccia, fault gouge, pseudotachylyte and cataclastic rocks. 具有紊亂組構的斷層岩包括斷層角礫岩、斷層泥、假玄武玻璃以及碎裂岩。
- 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)為特徵。
- The latter contains well-consolidated structural breccia, cataclastic and mylonitic rocks. 後者則包括固結較好的構造角礫岩,碎裂岩和糜棱岩。
- The jadeite's quality with cataclastic texture is also poor because its hardness with this texture will decrease. 具碎裂結構的翡翠硬度將略有降低,因而也會影響翡翠的質量。
- 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;然後延遲葉狀結構.
- The deposit is a medium-low temperature altered cataclastic rock type Au deposit. 金礦床屬中低溫熱液構造蝕變岩型金礦。
- Based on the proven gold deposits,there are three ore-forming types: skarn, altered cataclastic rock and quartz veins. 在已探明的金礦床中,有矽卡岩型、破碎蝕變岩型、石英脈型三類。
- Base foliation is fascicular, cauline foliation each other is unripe, feather crack. 基生葉叢生,莖生葉互生,羽裂。
- Base foliation wraps around needle form provides long power, cauline foliation does not have form of handle, line. 基生葉倒披針形具長柄;莖生葉無柄.;線形。
- The Yinkengshan ore spot occurs in SN-trending cataclastic zones in rhyoignimbrites. 其中銀坑山礦點受發育於流紋質熔結凝灰岩中的近SN向碎裂帶控制。
- Based on the proven gold deposits, there are three ore-forming types: skarn, altered cataclastic rock and quartz veins. 在已探明的金礦床中,有矽卡岩型、破碎蝕變岩型、石英脈型三類。
- Look at this exposure. The rock has well-developed foliation defined by elongated quartz and feldspar parallel to each other. 快看這個露頭,這個露頭上的岩石具有很發育的片理,片理是由拉長的石英和長石相互平行排列而成,
- Strong foliation, stretching lineation, a-type folds, sheath folds and mylonite, these structural characteristics only reflect macroscopic evidence. 強烈的片理、拉伸線理、a型褶皺、鞘褶皺以及糜棱岩,這些構造特徵僅僅反映出宏觀的證據。
- Steep mylonite foliation in the earlier shear belts strikes NE-NNE, and dips NW or SE; its stretching lineation is gentle. 早期剪切帶糜棱面理走向NE-NNE,傾向NW或SE,面理傾角較陡,礦物拉伸線理水平或近水平;
- 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. 后兩種岩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,並在葉理面上顯示一種銀色光澤。