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1)  Sidingheishan area
四顶黑山
1.
Discovery of layered mafic-ultramafic intrusives formed in 545Ma in the Sidingheishan area,eastern Tianshan,China and its significances for tectonics and Cu-Ni mineralization;
东天山四顶黑山地区545Ma层状镁铁质-超镁铁质岩体的发现及其大地构造学和成矿学意义
2)  Sidingshan Formation
四顶山组
1.
The gravel stone of Fengtai Formation is characterized by lower psephicity, no sorting, and the predominance of carbonates in stramatolith limestone, sandyclastic limestone, gravels and cements coming from the underlying Sidingshan Formation.
凤台砾岩的特征是砾石磨圆差、无分选,主要来自下伏四顶山组叠层石灰岩、砂屑灰岩,砾石和胶结物均以碳酸盐岩为主。
3)  No.4 Mine of Pingdingshan Coal Mine
平顶山四煤矿
4)  Sidingshan in Hefei
合肥市四顶山
5)  Jiuding Mountain Nature Reserve
四川九顶山自然保护区
1.
According to the relative parameters, the population dynamics of the black bears in the Jiuding Mountain Nature Reserve were simulated by a simulation modal-vortex 8.
41),对四川九顶山自然保护区野生黑熊的种群动态进行了模拟分析。
6)  Dingshan
顶山
1.
Dingshan area is the first class propecting area that was affirmed while small scale (1:1000000-1:500000) regional propecting for sandstone uranium deposit.
顶山地区是1992-1994年在准噶尔盆地开展的小比例(1:100万-1:50万)砂岩型铀矿区域预测工作中,划分出的一级远景区,并于1998-2002年进行的1:25万~1:20万带钻铀矿区域预测评价工作进一步落实的砂岩型铀成矿远景区,在主要目的层乌伦古河组的W-1旋回中已发现3个工业铀矿化孔。
补充资料:捱三顶四
1.亦作"捱三顶五"。 2.形容人群拥挤,接连不断。
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