首页|湘中稻草湾锑矿区矿体空间分布规律及深边部找矿预测

湘中稻草湾锑矿区矿体空间分布规律及深边部找矿预测

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稻草湾锑矿区位于湘中锡矿山锑矿田的北部,是近年来新发现的隐伏锑矿床,通过钻孔和坑探工程控制,锑矿资源规模已达到中型,是近年老矿山边部找矿的重要突破.通过对该矿床矿体空间分布特征以及控矿条件进行分析预测找矿靶区.经研究表明,锡矿山矿田各矿床的矿体自特定的层位产出,具有方向性、成群性、等距性等特征;矿体呈层状、似层状产出于上泥盆统佘田桥组(D3s2)硅化灰岩和层间破碎带中;矿体受构造控制明显,稻草湾背斜为矿体富集提供虚脱空间;矿体的成矿有利岩性组合为佘田桥组(D3s2)灰岩+佘田桥组(D3s3)钙质页岩(总屏蔽层).
Spatial distribution characteristics of ore bodies and prospecting prediction in the deep and edge area of Daocaowan antimony mining area,Central Hunan
The Daocaowan antimony mining area is located in the north of the tin mines of antimony ore field in central Hunan,which is a newly discovered concealed antimony deposit in recent years.Through drilling and pit exploration engineering control,the scale of antimony resources has reached medium-sized,which is an important breakthrough in the prospecting of old mines in recent years.Through the analysis of the spa-tial distribution characteristics of the ore body and the ore-controlling conditions,the prospecting target area is predicted.The research shows that the ore bodies of each deposit in the tin mines of ore field are produced from a specific horizon,with the characteristics of directivity,grouping and equidistant.The layered and stratoid orebodies occur in the silicified limestone and interlayer fracture zone of the Upper Devonian Shetian-qiao Formation(D3s2).The ore body is obviously controlled by the structure,and the Daocaowan anticline provides the detachment space for the enrichment of the ore body.The favorable lithology combination of ore body is Shetianqiao Formation(D3s2)limestone+Shetianqiao Formation(D3s3)calcareous shale(total shielding layer).

antimony depositspatial distribution of ore bodiesprospecting prediction at the deep and edge placeDaocaowanCentral Hunan

赵志坚、雷洁、徐昊、曾昆仑

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湖南科技大学地球科学与空间信息工程学院,湖南湘潭 411201

湖南省国土空间调查监测所 湖南长沙 410129

冷水江市狮子山锑业有限公司 湖南娄底 417501

锑矿 矿体空间分布 深边部找矿预测 稻草湾 湘中地区

中国地质调查局老矿山深部和外围找矿项目

12120113083200

2024

矿产与地质
桂林矿产地质研究院

矿产与地质

CSTPCD
影响因子:0.42
ISSN:1001-5663
年,卷(期):2024.38(2)
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