Gejiu City, called Tin-Capital, has its long history of Tin mining and production.
个旧市又被称为“锡都”，拥有悠久的锡矿开采和生产历史。
Yunhai Artistic Gallery is located in Gejiu, one of the beautiful cities in Yunnan Province.
云海艺术家画廊位于美丽的云南省个旧市（锡都）。
These changes resulted in the differences of metallogenetic characteristics between east and west area of Gejiu.
这一变化导致个旧东、西区成矿特点的差异；
The Gejiu strata formation is the mainly mineral-hosting rock series, but not the main source for mineralization.
个旧组是矿床的主要赋矿岩系，但不是成矿物源的主要提供者。
The forest landscape patterns of Gejiu city of Yunnan province were analyzed by using the landscape index method.
采用景观指数法对个旧市城市森林5种景观类型的格局进行了分析。
Taking the two tin deposits-Gejiu and Yinyan as an example, the application of this model has been concretely illustrated.
并以个旧和银岩两个锡矿区的矿床为例，具体说明了该模型的应用。
Taking Gejiu area as an example, this paper utilizes regional geochemical data to evaluate regional geochemical environment for the first time.
在此基础上，以云南个旧地区为例，首次运用区域化探资料对该区域人居环境进行了初步评价。
Factors affecting environment include: Gejiu primary mineral is rich in multi-metal sulfide, which is easy to become acid as the result of oxidation.
影响环境的因素有：个旧原生矿床富含多金属硫化物，氧化后易生成酸；
According to the historical materials, the famous Gejiu Sn deposit was first exploited for Ag(Pb) Zn ore at Yindongkuang of Laochang orefield in 1290.
著名的个旧锡矿，据史料在元廿七年（12 90年） ，率先在老厂矿区银铜矿开始采银（铅）锌矿。
During Middle Triassic, the Gejiu area was in a special sedimental environment, i. e. in a restricted marginal sea basin within the continental rift system.
中三叠世，个旧矿区处于特殊的沉积环境—陆裂谷系中的局限边缘海盆。
The mechanism of rock-forming processes of infiltration vein-like skarn in Gejiu tin deposit is analyzed using multi-phase and multi-component equilibrium theory.
用多相多组分平衡理论分析了个旧锡矿区渗滤脉状矽卡岩形成的机理，以该理论为基础设计的计算机程序模拟了这类矽卡岩脉的成岩过程。
According to geographic environment, meteorological condition and industrial dust, lead and arsenic pollution model of the Gejiu area's soil is defined as atmospheric pollution type.
根据个旧地区的地理环境、气象条件及工业粉尘情况，确定个旧地区土壤中铅、砷污染模式为大气污染型。
This paper studies in the western part of GeJiu, Yunnan Province, using ETM multi-spectral data. finding out the spatial distribution of wall rock alterations and recognize structures.
以云南省个旧西区为研究区域，选用TM多光谱遥感数据为基本数据源，了解围岩蚀变分布情况和构造特征。
Gejiu Formation in Triassic was mainly comprised of dolomite, limestone and mudstone, belonging to the sedimentary sequences of Gejiu-Napo back-arc rift basin under the regime of thermal subsidence.
中三叠个旧组以白云岩、灰岩和泥岩为主，属于个旧-那坡弧后裂谷盆地热沉降背景下形成的沉积序列。
Gejiu Formation in Triassic was mainly comprised of dolomite, limestone and mudstone, belonging to the sedimentary sequences of Gejiu-Napo back-arc rift basin under the regime of thermal subsidence.
中三叠个旧组以白云岩、灰岩和泥岩为主，属于个旧-那坡弧后裂谷盆地热沉降背景下形成的沉积序列。
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