Main Progress and Achievements of Bauxite Mineral Prospective Survey Project of Fusui-Chongzuo District,Guangxi
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摘要: 在龙州地区首次发现早石炭世的堆积型铝土矿矿源层,提出广西堆积型铝土矿至少存在早石炭世和晚二叠世两个时代的矿源层。探索运用高密度电阻率法寻找古风化壳沉积型铝土矿的有效性试验工作。提交新发现矿产地4处,探获新增铝土矿(3341)资源量5 289.15万吨。重新厘定区域地层岩性及岩相特征,系统总结区内铝土矿矿床(点)的时空分布特征、控矿地质条件、成矿规律及找矿标志,建立了区域成矿模式和预测找矿模型,圈定成矿远景区5处,找矿靶区6处,开展区域矿产预测,初步评价了本区铝土矿资源潜力。为该地区下一步地质调查、矿产勘查规划和开发提供了丰硕的基础资料和有益参考。Abstract: In this project, we discovered a new accumulation type bauxite source bed of early Carboniferous in Longzhou district, and proposed that there were at least two metallogenic epochs of accumulation type bauxite source beds in Guangxi which were early Carboniferous and late Permian. We tried to search for ancient weathering crust sedimentary bauxite by using the high density resistivity method of prospecting effectiveness test work. We submitted 4 newly discovered mineral lands, and figured out 52 891.5 kilotons of bauxite resources (3341). We redefined the regional stratigraphic lithology and facies characteristics, and summarized the bauxite deposits (occurrences) temporal and spatial distribution characteristics, controlling ore-forming geological conditions, metallogenic regularities and prospecting criteria. We established the regional metallogenic model and prospecting model, delineated 5 metallogenic prospective areas and determined 6 prospecting target areas. In addition, we forecasted the prospecting potential of bauxite in the Fusui-Chongzuo district,Guangxi. All these progress and achievements provide fruitful basic materials and beneficial reference for further geological survey, mineral exploration and development.
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Keywords:
- Fusui-Chongzuo district /
- bauxite /
- mineral prospective survey /
- progress and achievement /
- Guangxi
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[1] 广西壮族自治区地质局.广西壮族自治区区域地质志[M].北京:地质出版社,1985. [2] 广西壮族自治区地质矿产局.广西泥盆纪沉积相古地理及矿产[M].南宁:广西人民出版社,1987. [3] 广西壮族自治区地方志编纂委员会.广西通志——地质矿产志[M].南宁:广西人民出版社,1992 . [4] 广西壮族自治区地质矿产局.广西的泥盆系[M].武汉:中国地质大学出版社,1992. [5] 广西地质矿产勘查开发局.广西壮族自治区岩石地层[M].武汉:中国地质大学出版社,1997. [6] 广西壮族自治区地质矿产局.广西的石炭系[M].武汉:中国地质大学出版社,1999. [7] 广西壮族自治区地质矿产勘查开发局.广西壮族自治区数字地质图及说明书(1∶50万)[M].南宁:广西壮族自治区地质矿产局,2000. [8] 万兵,周文煊,杨承恪.广西铝土矿的物源探讨[J].地质与勘探,1981(1):25-32. [9] 李启津,侯正洪,吴成柳.广西原生铝土矿矿床成因探讨[J].轻金属,1981(10):1-3. [10] 曹信禹.试论桂西铝土矿的类型和成因[J].广西地质科技,1982(1):38-46. [11] 苏煜.广西平果铝土矿沉积环境和成因初探[J].桂林冶金地质学院学报,1985,5(4):315-321. [12] 万兵,周文宣,杨承格.广西上二叠统底部沉积铝土矿物源探讨[J].广西地质,1988,1(3):14-17. [13] 范长智.桂西平果铝土矿床成因探讨[J].矿产与勘查,1991(2):8-13. [14] 张起钻.桂西岩溶堆积型铝土矿床地质特征及成因[J].有色金属矿产与勘查,1999(6):486-489. [15] 罗允义.广西铝土矿遥感综合成矿预测及资源总量估算[J].地质与勘探,2003,39(3):58-62. [16] 李彩娟.桂西岩溶堆积型铝土矿床成矿作用及控矿因素[J].矿产与地质,2003,17(3):225-228. [17] 李镇梁.广西泥盆纪至早石炭世地层的平行不整合[J].南方国土资源,2005(11):24-29. [18] 王力,龙永珍,彭省临.桂西铝土矿成矿物质来源的地质地球化学分析[J].桂林工学院学报,2004,24(1):12-18. [19] 邓军.桂西岩溶堆积型铝土矿床地质特征及成矿模式[J].南方国土资源,2006(2):35-37. [20] 梁裕平,邓军,吴天生,等.扶绥-龙州一水铝土矿成矿条件及成矿预测[J].南方国土资源,2007(10):27-29. [21] 戴塔根,龙永珍,张起钻,等.桂西铝多金属矿床地质地球化学特征与成矿机理[J].地球科学与环境学报,2007,29(4):345-350. [22] 邓军.广西龙州县金龙铝土矿地质特征及成因初探[J].矿产与地质,2011,25(3):197-202. [23] 王瑞湖,李梅,蒙永坚.广西堆积型铝土矿成矿特征与资源潜力预测[J].地质通报,2010,29(10):1526-1532. [24] 王庆飞,邓军,刘学飞,等.铝土矿地质与成因研究进展[J].地质与勘探,2012,48(3):430-448.
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