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1)  Shangmanggang
滇西上芒岗
2)  Shangmanggan
上芒岗
1.
The Shangmanggang gold deposit is characterized by occurring as the upper red clay type and lower Carlin type.
上芒岗金矿由下部原生卡林型和上部红色粘土型金矿体所组成 ,赋矿地层为侏罗系勐戛组砂泥质岩、白云质灰岩和二叠系沙子坡组泥硅质灰岩、白云岩。
2.
The extensive red clayization of the Shangmanggang Carlin type gold deposit is responsible for the upper red clay type ore bodies and the widespread secondary geochemical anomalies.
上芒岗卡林型金矿床的强烈红土化作用 ,形成了上部红色粘土型金矿体 ,产生了一定范围的次生地球化学异常。
3)  Shangmanggang gold deposit
上芒岗金矿
1.
Typomorphism of pyrite and their prospecting implications of Shangmanggang gold deposit in western Yunnan province
滇西上芒岗金矿黄铁矿标型特征及其找矿意义
2.
The Shangmanggang gold deposit is located in Gaoli-Gongshan tectonic-magmatic metallogenic belt,western Nujiang river within the "Three-River region".
云南潞西上芒岗金矿位于西南“三江”地区怒江以西高黎贡山构造-岩浆-变质-成矿带上,是近年在“滇(中国云南)缅(缅甸联邦)”相邻地区首次发现的一个卡林型金矿床。
4)  western Yunnan
滇西
1.
Genetic types and framework model of Beiya gold ore district in western Yunnan;
滇西北衙金矿矿床类型与结构模型
2.
Cenozoic coupled basin-mountain and prospecting direction for sandstone-type uranium deposits in western Yunnan;
滇西新生代盆山耦合与砂岩型铀矿找矿方向
3.
Paleoelevation reconstruction of Red River drainage areas in Western Yunnan Plateau since Miocene;
中新世以来滇西高原内红河流域区的古高程反演
5)  west Yunnan
滇西
1.
On ecological adaptability to spatial construction in mountain cities: a case study of West Yunnan;
山地城市空间格局建构的生态适应性——以滇西地区为例
2.
Depths of Discontinuity Surfaces in Crust and Upper Mantle beneath West Yunnan Determined by Stacking Receiver Function;
用接收函数叠加技术研究滇西上地幔间断面埋深
3.
Using surface wave and receiver function to jointly inverse the crust-mantle velocity structure in the West Yunnan area;
利用面波和接收函数联合反演滇西地区壳幔速度结构
6)  Longgang area in central Yunnan
滇中龙岗
补充资料:满江红 清明与诸生登西*柏岗
【诗文】:
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