首页|吉林省东南部白山市金英金矿床金赋存状态及流体包裹体特征

吉林省东南部白山市金英金矿床金赋存状态及流体包裹体特征

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金英金矿床位于中朝准地台北缘东段,铁岭—靖宇隆起与太子河—浑江陷褶断束接触界面凹陷侧.通过野外实际调查、矿相学、电子探针和流体包裹体测试综合研究发现:该矿床矿物组成简单,矿石类型为硅化构造角砾岩型,金矿物种类有自然金、含银自然金和银金矿,载金矿物主要为石英,主要以裂隙金形式赋存,其次以粒间金和包裹金形式赋存;石英中包裹体多为气液两相包裹体,形态以椭圆形、菱形和不规则形为主,成矿温度139.6 ℃~253.1 ℃,盐度1.74%~4.65%,密度0.79~0.94 g/cm3,成矿压力33.6~65.6 MPa,成矿深度1.2~2.4 km,属中低温低盐度低密度流体.
Occurrence state of gold and characteristics of fluid inclusions in Jinying Gold Deposit,Baishan City,southeast Jilin Province
Jinying Gold Deposit is situated on the eastern section of the northern margin of China-Korea quasi-platform.It lies on the depression side of the contact interface between Tieling-Jingyu uplift and Taizihe-Hunjiang depression fold fault bundle.Through field investigation,mineralogical analysis,electron probe,and fluid inclusion testing,it has been determined that the deposit's mineral composition is uncomplicated and consists of siliceous struc-tural breccia-type ore.The gold mineral species include native gold,silver-bearing native gold,and electrum,with quartz being the primary host for gold which occurs mainly as fissure gold,followed by intergranular and encased gold.The inclusions within quartz consist primarily of gas-liquid two-phase fluids,which take on a predominantly oval,diamond and irregular form.Ore formation occurs at temperatures ranging from 139.6 ℃ to 253.1 ℃,with salinity levels between 1.74%and 4.65%,densities ranging from 0.79 g/cm3 to 0.94 g/cm3,pressures between 33.6 MPa and 65.6 MPa,and depths of formation spanning from 1.2 km to 2.4 km;these characteristics classify the fluid as medium-low tempera-ture,low salinity,and low density.

occurrence stateore-forming fluidfluid inclusionsedimentation mechanismJinying Gold Deposit

汪徽、温守钦、李敏、朱恩静

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东北大学资源与土木工程学院

赋存状态 成矿流体 流体包裹体 沉淀机理 金英金矿床

国家重点研发计划项目

2016YFC0801603

2024

黄金
长春黄金研究院

黄金

CSTPCD
影响因子:0.446
ISSN:1001-1277
年,卷(期):2024.45(2)
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