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- Foliation, bloom, and production became erratic. 萌芽、开花和结果变得很不正常。
- The deposits belong to altered cataclastic rock type. 金矿体受断裂构造的直接控制。
- On the surface of foliation there develops strong stretching lineation defined by alignment of elongated minerals. 在片理面上发育有强烈的拉伸线理，这些线理则是由拉长的矿物定向展布而显示。
- In addition, the presence and absence of foliation are an other factor to classify fault rocks. 除此之外，是否具有片理构造是划分断层岩的另一个因素。
- Let us keep walking perpendicular to the trend of foliation to get more details. 我们垂直这些片理化岩石的走向穿越一段并作详细观察。
- Fault rocks with a random fabric include fault breccia, fault gouge, pseudotachylyte and cataclastic rocks. 具有紊乱组构的断层岩包括断层角砾岩、断层泥、假玄武玻璃以及碎裂岩。
- There are neoformative foliation and lineation(stretching lineation) in the shear zone. 剪切带以出现新生的面理和线理（拉伸线理）为特征。
- The latter contains well-consolidated structural breccia, cataclastic and mylonitic rocks. 后者则包括固结较好的构造角砾岩，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. 具碎裂结构的翡翠硬度将略有降低，因而也会影响翡翠的质量。
- 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.
- The deposit is a medium-low temperature altered cataclastic rock type Au deposit. 金矿床属中低温热液构造蚀变岩型金矿。
- Based on the proven gold deposits,there are three ore-forming types: skarn, altered cataclastic rock and quartz veins. 在已探明的金矿床中,有矽卡岩型、破碎蚀变岩型、石英脉型三类。
- Base foliation is fascicular, cauline foliation each other is unripe, feather crack. 基生叶丛生,茎生叶互生,羽裂。
- Base foliation wraps around needle form provides long power, cauline foliation does not have form of handle, line. 基生叶倒披针形具长柄;茎生叶无柄.;线形。
- The Yinkengshan ore spot occurs in SN-trending cataclastic zones in rhyoignimbrites. 其中银坑山矿点受发育于流纹质熔结凝灰岩中的近SN向碎裂带控制。
- Based on the proven gold deposits, there are three ore-forming types: skarn, altered cataclastic rock and quartz veins. 在已探明的金矿床中，有矽卡岩型、破碎蚀变岩型、石英脉型三类。
- Look at this exposure. The rock has well-developed foliation defined by elongated quartz and feldspar parallel to each other. 快看这个露头，这个露头上的岩石具有很发育的片理，片理是由拉长的石英和长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. 强烈的片理、拉伸线理、a型褶皱、鞘褶皱以及糜棱岩，这些构造特征仅仅反映出宏观的证据。
- Steep mylonite foliation in the earlier shear belts strikes NE-NNE, and dips NW or SE; its stretching lineation is gentle. 早期剪切带糜棱面理走向NE-NNE,倾向NW或SE,面理倾角较陡,矿物拉伸线理水平或近水平;
- 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。
