Evaluation of Denudation Degree of Carlin-Type Gold Deposits in Southwest Guizhou Province
-
摘要: 对黔西南卡林型金矿集区开展矿田、矿床 (点) 剥蚀程度研究，能为新一轮找矿勘查布局提供有力支撑.以热液渗滤晕分带理论为指导，依据区内金矿床原生晕在空间中存在分带性以及次生异常与金矿床在地表呈现总体无偏特征，构建了大区域尺度量纲中能总体反映成矿元素分散流与原生晕共性特征的元素分带序列，计算了基于序列中元素区域化探扫面数据多重分形奇异性分析的前缘元素与尾部元素地球化学强度“对比值”，研制了矿田及其附近以“对比值”数据结构为主体的“低-浅-中-高”4个级别剥蚀程度定量评价指标，并结合实地地质特征开展综合评价工作.给出区内10个矿田和15个主要金矿床 (点) 的剥蚀程度评价结果，总体显示出右江区矿田剥蚀程度低于扬子区，泥堡、紫木凼、水银洞、丫他、烂泥沟等中-特大型金矿床剥蚀程度皆为低-浅剥蚀，而资源量相对较小的板其、戈塘、老万场等金矿床剥蚀程度普遍偏高.在此基础上，通过戈塘与水银洞金矿的进一步地质比对，论证了评价结果逼进了勘查事实并可以扩展到区内有一定勘查程度的地区.此外，对评价结果的分析表明，“对比值”异常是寻求找矿突破和现有矿床 (点) 深部成矿预测的主要评价指标之一，对找矿勘查有重要指示作用.据此初步提出水银洞金矿床及其以东的深部、戈塘金矿床北西二叠系与三叠系接触带附近、上大观矿点深部等14处深部找矿潜力较大的地区.Abstract: The study of the denudation degree of the Carlin-type gold deposits (ore fields-ore deposits-ore occurrences) in southwest Guizhou Province could facilitate future exploration. Present research is based on hydrothermal halo zoning percolation theory, the general unbiased feature of the space between gold deposits and secondary anomalies as well as the mineralization zoning of the ore-forming elements. The sequence of element zoning which could reflect the common features of ore-forming elements dispersed flow and primary halos in regional scale dimension is firstly constructed.Then, the contrast values of geochemical strength between the front and rear halo in zoning sequence are obtained on the basis of singularity analysis of stream sediment geochemical dataset collected in this region. The evaluating indicators of denudation degree are established and classified into four different levels as low-light-medium-high according to the data structures of contrast values.In addition, the evaluating indicators are applied to comprehensive evaluation combined with the geological characteristics of deposits, ore fields and their surroundings. In this paper, the results of denudation degree related to the ten ore fields and fifteen major gold deposits are presented. Our research reveals that the Youjiang ore fields have lower degree of denudation than the Yangtze one. Furthermore, the degree of denudation is apparently positively correlated with the amount of resources.The medium to superlarge sized gold deposits such as Nibao deposit, Zimudang deposit, Shuiyindong deposit, Yata deposit and Lannigou deposit are characterized with the low-to light-denudation degree.While the relatively small sized deposits such as Banqi deposit, Getang deposit, Laowanchang deposit are with the high degree of denudation. The evaluation results are consistent with those of the previous exploration work and may be extended to the areas undergone basic prospection.In addition, it is found that the anomalies of the contrast value are the main sign of the evaluation for obtaining prospecting breakthrough and deep area ore-prospecting of existing deposits. Fourteen districts of deep ore with high prospecting potential are proposed in this study, including the Shuiyindong deposits and its eastern deep area, the contact zone between Permian and Triassic strata in the northwestern part of Getang deposit and the deep part of the Shangdaguan ore occurrence.
-
图 1 黔西南卡林型金矿集区大地构造位置
A-Ⅰ.黔西南扬子区；A-Ⅱ.黔西南右江区；据马丽芳等 (2002)编制
Fig. 1. Tectonic location of Carlin-type gold deposits concentrated area in southwest Guizhou Province
图 2 黔西南卡林型金矿集区矿产地质图
据马丽芳等 (2002)、韩至钧等 (1999)、王砚耕等 (1995)、王亮等 (2009)、吴德超等 (2003)和贵州地矿局 (兴仁、安龙、罗甸和盘县4个1:20万图幅矿调资料，1980) 综合编制
Fig. 2. Geological sketch of the Carlin-type gold deposits concentrated area in southwest Guizhou Province
图 3 黔西南地区典型卡林型金矿床勘探线剖面
a.烂泥沟金矿8号勘探线剖面；b.丫他金矿32号勘探线剖面；c.板其金矿27号勘探线剖面；d.紫木凼金矿32号勘探线剖面；e.水银洞金矿勘探线剖面；f.戈塘金矿勘3号探线剖面；g.泥堡金矿二龙抢宝段勘探线剖面；P1m.下二叠统茅口组；P2w-c.上二叠统吴家坪-长兴组；P2β.上二叠统峨眉山玄武岩组；P2dc.上二叠统大厂组；Sbt.构造蚀变体；P2l1-3.上二叠统龙潭组1~3段；T1y.下三叠统夜郎组；T2g.中三叠统关岭组；T2xm.中三叠统许满组；T2nl.中三叠统尼罗组；T2by.中三叠统边阳组；图e据刘建中等(2006)修编；图a,b,c,d和f据韩至钧等(1999)修编
Fig. 3. Prospecting line profile sketch of typical Carlin-type gold deposits in southwest Guizhou Province
图 4 黔西南卡林型金矿集区地形地貌
数字高程模型及剖面通过Global Mapper软件在线获取的黔西南地区高程数据创建；矿田位置及其范围据吴德超等 (2003)和韩至钧等 (1999)
Fig. 4. Topography sketch of the Carlin-type gold deposits concentrated area in southwest Guizhou Province
图 5 通过遥感影像获取的水系 (a) 与Au元素次生异常叠合 (b)
Fig. 5. Spatial superimposed sketchs of the river systems obtained by remote sensing images (a) and Au secondary anomaly (b)
图 6 次生晕分带评价值综合结果
a.前缘晕 (As-Hg-Sb) 奇异指数第一主成分得分；b.矿体晕 (Au) 奇异指数；c.矿尾晕 (Wo-Sn-Mo) 奇异指数第一主成分得分；d.次生晕分带评价值 (前缘晕/矿尾晕)
Fig. 6. Comprehensive results of evaluation values of secondary halo zoning
图 7 典型矿床次生晕分带评价值投点对比
Fig. 7. Comparison of evaluation values of secondary halo zoning among typical ore deposits
图 8 前缘元素异常中的次生晕分带评价值异常
Ⅰ.灰家堡；Ⅱ.戈塘；Ⅲ.泥堡；Ⅳ.雄武；Ⅴ.大厂；Ⅵ.归顺；Ⅶ.芹菜坪；Ⅷ.赖子山；Ⅸ.丫-板-百；Ⅹ.望谟
Fig. 8. Anomaly evaluation values of secondary halo zoning of the front halo elements anomalies
表 1 成矿元素最大方差旋转因子解
Table 1. Varimax rotated factor solution of the ore-forming elements
元素 主成分 F1 F2 F3 Co 0.948 0.062 0.149 Cu 0.938 -0.059 0.195 Cr 0.903 0.158 0.145 Ni 0.901 0.260 0.209 Zn 0.666 0.441 0.399 Sn 0.539 0.532 0.229 Mo 0.503 0.418 0.461 Ba 0.403 -0.538 -0.152 Pb 0.381 0.770 0.293 As 0.338 0.416 0.711 Sb 0.264 0.244 0.811 F 0.259 0.762 0.099 Au 0.248 -0.122 0.666 W 0.130 0.549 0.586 Hg 0.048 0.215 0.718 Bi 0.044 0.817 0.294 Ag -0.006 0.275 0.452 注：KMO=0.910;对应特征值8.006、2.684、1.291. 
下载: 导出CSV
表 2 黔西南卡林型金矿集区矿田和主要金矿床 (点) 剥蚀程度评价结果汇总统计
Table 2. Evaluation of denudation degree of the ore fields and the main gold deposits (occurrences) in Carlin-type gold deposits concentrated area in southwest Guizhou Province
构造位置 矿田 主体级别 剥蚀程度 低-浅剥蚀区 矿床 (点) 所在级别 剥蚀程度 矿体剥离程度 前缘晕 矿体晕 矿尾晕 评价值 数据指标 综合推断 存在 前缘晕 矿体晕 矿尾晕 评价值 数据指标 综合推断 扬子地台 灰家堡 西区 10~13 10~13 8~11 10~11 浅 浅 √ 紫木凼 9 12 6 10 浅 浅 小部分 东区 9~12 7~9 8~10 10~13 低 低 √ 水银洞 12 7 11 10 低 低 隐伏 戈塘 9~12 10~13 9~12 3~8 中-高 中-高 √ 戈塘 12 13 12 3 高 高 大部分 泥堡 9~10 10~11 7~9 9~11 中-浅 浅 √ 泥堡 8 11 6 9 中 浅 部分 铁厂坳 13 8 8 13 低 低 半隐伏 雄武 10~12 9~12 9~11 4~7 中-高 中-高 √ 雄武 11 7 6 12 低 低 半隐伏 大厂 9~12 10~13 10~11 4~8 中-高 高 老万场 12 12 11 7 中 高 大部分 归顺 9~11 10~12 8~11 6~11 中-浅 中-浅 √ 砂锅场 9 11 7 9 中 中 部分 芹菜坪 9~12 10~11 8~10 7~10 中-浅 中-浅 芹菜坪 10 11 7 10 浅 浅 少量 右江褶皱带 赖子山 西区 8~11 9~11 7~9 8~11 中-低 中-低 √ 庆坪 9 11 6 11 浅 浅 中区 9~10 10~12 10~12 2~5 中-高 高 东区 10~11 11~13 5~9 10~12 浅 浅-低 √ 烂泥沟 12 12 9 12 浅 浅-低 少量 丫-板-百 丫他矿区 10~11 12~13 5~7 10~12 浅 浅 √ 丫他 11 13 5 12 浅 浅 部分 板其北区 11~12 10~13 7~9 10~12 浅 浅 √ 板其南区 9~11 11~13 8~10 6~8 中 中 板其 11 13 10 8 中 中 大部分 百地矿区 10~13 11~13 9~11 10~13 浅 浅 √ 百地 12 12 10 10 浅 浅 小部分 望谟 岜赖地区 7~10 10~11 10~12 2~4 高 高 乐康地区 7~9 10~11 6~9 9~13 中-浅 中-浅 上大观地区 10~13 8~12 8~11 11~13 浅-低 浅-低 √ 上大观 13 8 8 13 低 低 隐伏 注：“矿体剥离程度”列中为矿体被剥蚀的可能性.
下载: 导出CSV
-
Chen, H.D., Zeng, Y.F., 1990.Nature and Evolution of the Youjiang Basin.Sedimentary Geology and Tethyan Geology, (1):28-37 (in Chinese with English abstract). https://www.researchgate.net/publication/293088175_The_characteristics_and_evolution_of_youjiang_terrace_Bose_Basin Chen, L.A., 1999.Geochemistry of Macroelements and Lateritization of Laowanchang Lateritic Gold Deposits in Qinglong, Guizhou.Guizhou Geology, 16(4):307-314 (in Chinese with English abstract). doi: 10.1007/s11631-015-0055-5 Chen, L.A., 2000.Geochemistry in the Mineralizing Process of Laowanchang Lateritic-Type Gold Deposits of Southwest Guizhou.Guizhou Geology, 17(1):18-26 (in Chinese with English abstract). https://www.journals.elsevier.com/journal-of-geochemical-exploration/recent-articles/ Chen, M.H., Mao, J.W., Qu, W.J., et al., 2007.Re-Os Dating of Arsenian Pyrites from the Lannigou Gold Deposit, Zhenfeng, Guizhou Province, and Its Geological Significances.Geological Review, 53(3):371-382 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_OA000004743 Chen, M.H., Zhang, W., Yang, Z.X., et al., 2009.Zircon SHRIMP U-Pb Age and Hf Isotopic Composition of Baiceng Ultrabasic Dykes in Zhenfeng County, Southwestern Guizhou Province.Mineral Deposits, 28(3):240-250 (in Chinese with English abstract). http://www.oalib.com/paper/4573388 Cheng, Q.M., 1999.Multifractality and Spatial Statistics.Computers & Geosciences, 25(9):949-961.doi: 10.1016/0098-3004(99)00060-6 Cheng, Q.M., 2003.GeoData Analysis System (GEODAS) for Mineral Exploration and Environmental Assessment, User's Guide.York University, Toronto. doi: 10.1007/s10653-012-9483-x Cheng, Q.M., 2004.Quantify the Generalized Self-Similarity of Spatial Patterns for Mineral Resources Assessment.Earth Science, 29(6):733-744 (in Chinese with English abstract). Cheng, Q.M., 2006.Singularity-Generalized Self-Similarity-Fractal Spectrum (3S) Models.Earth Science, 31(3):337-348 (in Chinese with English abstract). https://www.researchgate.net/publication/285728797_Singularity-generalized_self-similarity-fractal_spectrum_3S_models Cheng, Q.M., 2007.Mapping Singularities with Stream Sediment Geochemical Data for Prediction of Undiscovered Mineral Deposits in Gejiu, Yunnan Province, China.Ore Geology Reviews, 32(1):314-324.doi: 10.1016/j.oregeorev.2006.10.002 Cheng, Q.M., 2007.Singular Mineralization Processes and Mineral Resources Quantitative Prediction: New Theories and Methods.Earth Science Frontiers, 14(5):42-53 (in Chinese with English abstract). https://www.researchgate.net/profile/Qiuming_Cheng/publication/251701965_Singularity_theories_and_methods_for_characterizing_mineralization_processes_and_mapping_geo-anomalies_for_mineral_deposit_prediction/links/549353700cf22d7925da2f18.pdf?origin=publication_list Cheng, Q.M., 2008.Singularity of Mineralization and Multifractal Distribution of Mineral Deposits.Bulletin of Mineralogy, Petrology and Geochemistry, 27(3):298-305 (in Chinese with English abstract). https://www.researchgate.net/publication/289701679_Singularity_of_mineralization_and_multifractal_distribution_of_mineral_deposits Cheng, Q.M., 2010.Singularity Modeling of Geo-Anomalies and Recognition of Anomalies Caused by Buried Sources.Earth Science, 36(2):307-316.(in Chinese with English abstract). https://www.researchgate.net/publication/279562174_Singularity_modeling_of_geo-anomalies_and_recognition_of_anomalies_caused_by_buried_sources Cheng, Q.M., Agterberg, F.P., Ballantyne, S.B., 1994.The Separation of Geochemical Anomalies from Background by Fractal Methods.Journal of Geochemical Exploration, 51(2):109-130.doi: 10.1016/0375-6742(94)90013-2 China University of Geosciences, Bureau of Geology and Mineral Exploration and Development of Guizhou Province, 2013.Metalllogenic Laws and Metalllogenic Prediction of the Fine-Disseminated Gold Deposits in Southwest Guizhou Province, Guiyang (in Chinese). Compile Council of A Dictionary of Earth Sciences, 2006.Earth Science Dictionary.Geological Publishing House, Beijing (in Chinese). Fang, W.X., Hu, R.Z., Su, W.C., et al., 2006.Features of Metallogenic System of Compound Continental Dynamics in Yunnan-Guizhou-Guangxi-Hunan Provinces.Geotectonica et Metallogenia, 30(4):470-480 (in Chinese with English abstract). doi: 10.1007/s11631-014-0665-3 Feng, X.S., Wang, S.Y., 2004.Minerogenetic Series and Minerogenetic Law in Guizhou Provice, China.Geological Publishing House, Beijing (in Chinese). Guo, Z.C., Zhou, Z.F., 2006.Exploration Practice of Huijiabao-Anticline Gold Deposit, Southwest Guizhou and Establishment on Two-Story-Building Model.Guizhou Geology, 23(3):176-181 (in Chinese with English abstract). https://www.researchgate.net/publication/285743062_Exploration_practice_of_Huijiabao-anticline_gold_deposit_Southwest_Guizhou_and_establishment_on_two-storybuilding_model Han, Z.J., Wang, Y.G., Feng, J.Z., et al., 1999.Geology and Exploration of the Gold Deposits in Southwest Guizhou.Guizhou Science and Technology Press, Guiyang (in Chinese). He, S.L., Zeng, Z.G., Luo, M.X., et al., 2008.A Review of Thirty Years' Gold Geochemical Exploration in Southwestern Guizhou and a Prospect for Future Work.Geophysical and Geochemical Exploration, 32(5):461-464(in Chinese with English abstract). https://www.hindawi.com/journals/geofluids/2017/2417209/ref/ Hu, R.Z., Peng, J.T., Ma, D.S., et al., 2007.Epoch of Large-Scale Low-Temperature Mineralizations in Southwestern Yangtze Massif.Mineral Deposits, 26(6):583-596 (in Chinese with English abstract). https://www.researchgate.net/publication/284470454_Epoch_of_large-scale_low-temperature_mineralizations_in_southwestern_Yangtze_massif Huang, J.G., Li, H.J., Li, W.J., et al., 2012.Trace Element Characteristics of Fluorite and Its Sm-Nd Isotopic Dating in Getang Gold Deposit, Guizhou Province.Advances in Earth Science, 27(10):1087-1093 (in Chinese with English abstract). http://www.adearth.ac.cn/EN/abstract/abstract10971.shtml Li, H., Zhang, W.H., Liu, B.L., et al., 1999.The Study on Axial Zonality Sequence of Primary Halo and Some Criteria for the Application of this Sequence for Major Types of Gold Deposits in China.Geology and Prospecting, 35(1):32-35 (in Chinese with English abstract). https://www.researchgate.net/publication/285813174_The_application_of_Mapgis_combining_RGMap_in_analysis_of_the_geochemical_primary_halos Li, X.Z., 2001.Evolution of Karst Geomorphology of Upper-Cenozoic and Its Influential Factors in Guizhou Plateau.Guizhou Geology, 18(2):29-36 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGYR198704014.htm Lin, S.J., 1993.The Main Features of Tectonic Movement of Late-Cenozoic Era in Guizhou.Guizhou Geology, 1(1):10-17 (in Chinese with English abstract). doi: 10.1007/BF00160738 Lin, S.J., Zhou, Q.Y., Chen, P.Y., et al., 1992.Upper Cenozoic in Guizhou.Guizhou Science and Technology Press, Guiyang (in Chinese). Liu, C.M., 2006.Progress in Studies on Primary Halos of Ore Deposit.Acta Geological Sinica, 80(10):1528-1538 (in Chinese with English abstract). doi: 10.1007/BF02872261 Liu, C.M., Ma, S.M., 2007.The Main Achievements of the Study on Primary Halo in the Past 50 Years in China.Computing Techniques for Geophysical and Geochemical Exploration, 29(Suppl.1):215-222 (in Chinese with English abstract). Liu, J.Z., Deng, Y.M., Liu, C.Q., et al., 2006.Metallogenic Conditions and Model of the Superlarge Shuiyindong Stratabound Gold Deposit in Zhenfeng County, Guizhou Province.Geology in China, 33(1):169-177 (in Chinese with English abstract). https://www.researchgate.net/publication/279699448_Metallogenic_conditions_and_model_of_the_superlarge_Shuiyindong_stratabound_gold_deposit_in_Zhenfeng_County_Guizhou_Province Liu, J.Z., Deng, Y.M., Liu, C.Q., et al., 2006.Metallogenic Conditions and Model of the Superlarge Shuiyindong Stratabound Gold Deposit in Zhenfeng County, Guizhou Province.Geology in China, 33(1):169-177 (in Chinese with English abstract). https://www.researchgate.net/publication/279699448_Metallogenic_conditions_and_model_of_the_superlarge_Shuiyindong_stratabound_gold_deposit_in_Zhenfeng_County_Guizhou_Province Luo, M.S., Lu, L.Q., Jia, J., et al., 2014.Evolution of Sedimentary Basins in China during Mesozoic.Earth Science, 8(8):954-976 (in Chinese with English abstract). https://www.researchgate.net/publication/287500542_Evolution_of_sedimentary_basins_in_China_during_Mesozoic Ma, L.F., Qiao, X.F., Min, L.R., et al., 2002.Geological Atlas of China.Geological Publishing House, Beijing (in Chinese). Su, W.C., Hu, R.Z., Xia, B., et al., 2009.Calcite Sm-Nd Isochron Age of the Shuiyindong Carlin-Type Gold Deposit, Guizhou, China.Chemical Geology, 258(3-4):269-274.doi: 10.1016/j.chemgeo.2008.10.030 Tao, P., 1999.Geological Feature of Nibao Carlin Type Gold Deposit and Relationship with Nearby Lateritic Gold Deposit in Southwestern Guizhou.Guizhou Geology, 16(3):213-220 (in Chinese with English abstract). doi: 10.1007/s12517-015-2077-z Tao, P., Ma, R., Lei, Z.Y., et al., 2007.Review of Gold Mineralization System in the Southwestern Guizhou Province, Yangtze Block.Geology and Prospecting, 43(4):24-28 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GZDZ602.006.htm Wang, L., Zhang, Y.W., Liu, S.G., 2009.The Application of Regional Gravity and Magnetic Data to Delineaing Intrusivie Bodies and Local Geological Structures in Guizhou Province.Geophysical and Geochemical Exploration, 33(3):245-249 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-WTYH904.006.htm Wang, Y.G., Wang, L.T., Zhang, M.F., et al., 1995.Texture of the Upper Crust and Pattern of the Disseminated Gold Deposits Distributed in Nanpangjiang Area.Guizhou Geology, 12(2):91-183 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GZDZ199502000.htm Wei, Y., Zhang, Z.Y., He, W.H., et al., 2014.Evolution of Sedimentary Basins in the Upper Yangtze during Mesozoic.Earth Science, 39(8):1065-1078 (in Chinese with English abstract). https://www.researchgate.net/publication/287780575_Evolution_of_sedimentary_basins_in_the_Upper_Yangtze_during_Mesozoic Wu, D.C., Liu, J.D., Liu, X.F., et al., 2003.The Superposed Folds and the Importance of Mine Field Tectonic in Southwestern Guizhou.Geology and Exploration, 39(2):16-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX198402012.htm Zeng, Y.F., Liu, W.J., Chen, H.D., et al., 1995.Evolution of Sedimentation and Tectonics of the Youjiang Composite Basin, South China.Acta Geological Sinica, 69(2):113-124 (in Chinese with English abstract). Zhai, Y.S., 1999.On the Metallogenic System.Earth Science Frontiers, 6(1):13-27 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY901.002.htm Zhang, K.X., Pan, G.T., He, W.H., et al., 2015.New Division of Tectonic-Strata Superregion in China.Earth Science, 40(2):206-233 (in Chinese with English abstract). Zhu, L.M., Jin, J.F., He, M.Y., et al., 1997.A Discussion about the Genesis of Fine-Grained Dissemination Gold Deposits in Southwestern Guizhou Province.Volcanology and Mineral Resources, 18(2):117-126 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ198703006.htm Zou, G.H., Ouyang, Z.Q., Li, H., et al., 1996.Prospecting Models of Major Types of Gold Deposits in China.Geological Publishing House, Beijing (in Chinese). 陈洪德, 曾允孚, 1990.右江沉积盆地的性质及演化讨论.岩相古地理, (1):28-37. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199001003.htm 陈履安, 1999.晴隆老万场红土型金矿常量元素地球化学特征及其红土化作用.贵州地质, 16(4):307-314. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199904006.htm 陈履安, 2000.老万场红土型金矿成矿过程的地球化学作用.贵州地质, 17(1):18-26. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ200001003.htm 陈懋弘, 毛景文, 屈文俊, 等, 2007.贵州贞丰烂泥沟卡林型金矿床含砷黄铁矿Re-Os同位素测年及地质意义.地质论评, 53(3):371-382. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200703009.htm 陈懋弘, 章伟, 杨宗喜, 等, 2009.黔西南白层超基性岩墙锆石SHRIMP U-Pb年龄和Hf同位素组成研究.矿床地质, 28(3):240-250. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200903003.htm 成秋明, 2004.空间模式的广义自相似性分析与矿产资源评价.地球科学, 29(6):733-744. http://earth-science.net/WebPage/qk.aspx?id=73# 成秋明, 2006.非线性成矿预测理论:多重分形奇异性-广义自相似性-分形谱系模型与方法.地球科学, 31(3):337-348. http://earth-science.net/WebPage/qk.aspx?id=78# 成秋明, 2007.成矿过程奇异性与矿产预测定量化的新理论与新方法.地学前缘, 14(5):42-53. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200705006.htm 成秋明, 2008.成矿过程奇异性与矿床多重分形分布.矿物岩石地球化学通报, 27(3):298-305. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200803014.htm 成秋明, 2010.地质异常的奇异性度量与隐伏源致矿异常识别.地球科学, 36(2):307-316. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201102017.htm 中国地质大学 (武汉), 贵州地矿局, 2013.贵阳:黔西南微细浸染型金矿构造控矿与成矿规律. 《地球科学大辞典》编委会, 2006.地球科学大辞典.北京:地质出版社. 方维萱, 胡瑞忠, 苏文超, 等, 2006.滇黔桂湘地区中生代复合大陆动力成矿系统特征.大地构造与成矿学, 30(4):470-480. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200604008.htm 冯学仕, 王尚彦, 2004.贵州省区域矿床成矿系列与成矿规律.北京:地质出版社. 郭振春, 周忠赋, 2006.黔西南灰家堡背斜金矿勘查实践及"两层楼"模式的建立.贵州地质, 23(3):176-181. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ200603002.htm 韩至钧, 王砚耕, 冯济舟, 等, 1999.黔西南金矿地质与勘查.贵阳:贵州科技出版社. 何邵麟, 曾昭光, 罗明学, 等, 2008.黔西南金矿勘查地球化学30年:回顾与展望.物探与化探, 32(5):461-464. http://www.cnki.com.cn/Article/CJFDTOTAL-WTYH200805004.htm 胡瑞忠, 彭建堂, 马东升, 等, 2007.扬子地块西南缘大面积低温成矿时代.矿床地质, 26(6):583-596. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200706002.htm 黄建国, 李虎杰, 李文杰, 等, 2012.贵州戈塘金矿萤石微量元素特征及钐钕测年.地球科学进展, 27(10):1087-1093. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201210008.htm 李惠, 张文华, 刘宝林, 等, 1999.中国主要类型金矿床的原生晕轴向分带序列研究及其应用准则.地质与勘探, 35(1):32-35. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT901.008.htm 李兴中, 2001.晚新生代贵州高原喀斯特地貌演进及其影响因素.贵州地质, 18(1):29-36. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ200101006.htm 林树基, 1993.贵州晚新生代构造运动的主要特征.贵州地质, 1(1):10-17. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199301001.htm 林树基, 周启永, 陈佩英, 等, 1992.贵州的上新生界.贵阳:贵州科技出版社. 刘崇民, 2006.金属矿床原生晕研究进展.地质学报, 80(10):1528-1538. doi: 10.3321/j.issn:0001-5717.2006.10.006 刘崇民, 马生明, 2007.我国原生晕研究50年的主要成果, 物探化探计算技术, 29(增刊1):215-222. http://www.cnki.com.cn/Article/CJFDTOTAL-WTHT2007S1050.htm 刘建中, 邓一明, 刘川勤, 等, 2006.贵州省贞丰县水银洞层控特大型金矿成矿条件与成矿模式.中国地质, 33(1):169-177. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200601018.htm 刘平, 李沛刚, 李克庆, 等, 2006.黔西南金矿成矿地质作用浅析.贵州地质, 23(2):83-92, 97. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ200602000.htm 骆满生, 卢隆桥, 贾建, 等, 2014.中国中生代沉积盆地演化.地球科学, 8(8):954-976. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201408003.htm 马丽芳, 乔秀夫, 闵隆瑞, 等, 2002.中国地质图集.北京:地质出版社. 陶平, 1999.黔西南泥堡卡林型金矿地质特征及其与附近"红土型"金矿的关系.贵州地质, 16(3):213-220. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199903006.htm 陶平, 马荣, 雷志远, 等, 2007.扬子区黔西南金矿成矿系统综述.地质与勘探, 43(4):24-28. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200704006.htm 王亮, 张应文, 刘盛光, 2009.区域重磁资料圈定贵州境内侵入岩体及局部地质构造.物探与化探, 33(3):245-249. http://www.cnki.com.cn/Article/CJFDTOTAL-WTYH200903002.htm 王砚耕, 王立亭, 张明发, 等, 1995.南盘江地区浅层地壳结构与金矿分布模式.贵州地质, 12(2):91-183. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199502000.htm 韦一, 张宗言, 何卫红, 等, 2014.上扬子地区中生代沉积盆地演化.地球科学, 39(8):1065-1078. http://earth-science.net/WebPage/qk.aspx?id=128# 吴德超, 刘家铎, 刘显凡, 等, 2003.黔西南地区叠加褶皱及其对金矿成矿的意义.地质与勘探, 39(2):16-20. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200302004.htm 曾允孚, 刘文均, 陈洪德, 等, 1995.华南右江复合盆地的沉积构造演化.地质学报, 69(2):113-124. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199502001.htm 翟裕生, 1999.论成矿系统.地学前缘, 6(1):13-27. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201104004.htm 张克信, 潘桂棠, 何卫红, 等, 2015.中国构造-地层大区划分新方案.地球科学, 40(2):206-233. http://earth-science.net/WebPage/qk.aspx?id=134# 朱赖民, 金景福, 何明友, 等, 1997.黔西南微细浸染型型金矿床成因讨论:矿床时空分布及同位素证据.火山地质与矿产, 18(2):117-126. http://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ199702008.htm 邹光华, 欧阳宗圻, 李惠, 等, 1996.中国主要类型金矿床找矿模型.北京:地质出版社. -
点击查看大图
图(8) / 表(2)
计量
- 文章访问数: 3978
- HTML全文浏览量: 2279
- PDF下载量: 70
- 被引次数: 0
