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1)  Xinwuli rock body
新屋里岩体
1.
Based on geochemical prospecting data on the Xinwuli rock body in the Fenghuangshan deposit at Tongling,Anhui Province,origin and mineralizing signification of the rock body is preliminarily ascertained,and intrusive mechanism of the body is analyzed.
通过对铜陵凤凰山新屋里岩体化探样测试数据的系统分析研究,初步确定了岩体的成因、成矿意义,并对其侵位机制进行了探讨。
2)  Shiwu intrusion
石屋岩体
1.
The Censhan intrusion is much similar to the Shiwu intrusion in field occurrence,formation time and petrological characteristic.
安徽省石屋岩体和岑山岩体在地质产状、形成时代及岩石学特征上十分相似 ,前人将其划为同一单元 ,并一直将其定名为黑云母斜长花岗斑岩。
3)  poetry of White Cottage Style
白屋体新诗
4)  Qianlishan pluton
千里山岩体
1.
The Indosinian Wangxianling pluton is close to the Early Yanshanian Qianlishan pluton,and the geochemical diagrams and regional tectonic evolutional settings suggest that Wangxianling granites were formed in a post-collisional tectonic setting while Qianlishan granites were formed .
区内,印支期王仙岭岩体与燕山早期千里山岩体紧密相邻,前者成矿差,后者则发育多个大型、超大型矿床。
5)  Yejili intrusion
野芨里岩体
1.
Yejili intrusion in Inner Mongolia is situated at the 100 km northeast of Jinchuan Cu-Ni-PGE sulfide deposit.
野芨里岩体分布于金川铜镍(铂)硫化物矿床北偏东约100 km处,位于内蒙古境内。
6)  intrusion at the 128 km sign
128公里岩体
1.
The intrusion at the 128 km sign of the Xinjiang-Tibet highway is representative for the Caledonian western Kunlun tectonic belt.
新藏公路128公里岩体是西昆仑加里东构造带内一个具有代表性的岩体。
补充资料:新屋
【诗文】:
耳顺何为土木勤,叔孙墙屋有前闻。
纵然一世如红叶,犹得十年吟白云。
性逸且图称野客,才难非敢傲明君。
清甜数尺沙泉井,平与邻家昼夜分。



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【出处】:
全唐诗:卷709-32
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