[1] 陈文一,王中刚,刘家仁. 2003. 贵州二叠纪岩相古地理与沉积矿产关系. 古地理学报, 5(1): 17-20. [Chen W Y,Wang Z G,Liu J R. 2003. Relationship between lithofacies palaeogeography and sedimentary mineral resources of the two fold strata in Guizhou. Journal of Palaeogeography(Chinese Edition), 5(1): 17-20] [2] 戴传固,郑启钤,陈建书,张慧,代雅然. 2014. 贵州海西—燕山构造旋回期成矿地质背景研究. 贵州地质, 31(2): 82-88. [Dai C G,Zheng Q Q,Chen J S,Zhang H,Dai Y R. 2014. Geological background study of metallogenic in Haixi-Yanshan tectonic cycle in Guizhou. Guizhou Geology, 31(2): 82-88] [3] 何斌,徐义刚,肖龙,王雅玫,王康明,沙绍礼. 2006. 峨眉山地幔柱上升的沉积响应及其地质意义. 地质论评, 6(1): 30-37. [He B,Xu Y G,Xiao L,Wang Y W,Wang K M,Shao S L. 2006. Sedimentary responses to uplift of Emeishan mantle plume and its implications. Geological Review, 6(1): 30-37] [4] 韩忠华,潘家州. 2007. 浅析贵州二叠系锰矿与峨眉山玄武岩之关系. 贵州地质, 24(3): 197-201. [Han Z H,Pan J Z. 2007. Relationship analysis on Permian manganese and Emeishan Basalt in Guizhou. Guizhou Geology, 24(3): 197-201] [5] 何登发,李德生,张国伟,赵路子,樊春,鲁人齐,文竹. 2011. 四川多旋回叠合盆地的形成与演化. 地质科学, 46(3): 589-606. [He D F,Li D S,Zhang G W,Zhao L Z,Fan C,Lu R Q,Wen Z. 2011. Formation and evolution of multi-cycle superposed Sichuan Basin,China. Chinese Journal of Geology, 46(3): 589-606] [6] 李旭兵,曾雄伟,王传尚,刘安,白云山. 2011. 东吴运动的沉积学响应: 以湘鄂西及邻区二叠系茅口组顶部不整合面为例. 地层学杂志, 35(3): 299-304. [Li X B,Zeng X W,Wang C S,Liu A,Bai Y S. 2011. Sedimentary response to the Dongwu Movement: A case of the unconformity on top of the Permian Maokou Formation in the western Hubei-Hunan and neighboring areas. Journal of Stratigraphy, 35(3): 299-304] [7] 刘红军. 2001. 扬子地块西缘古特提斯盆地演化与含锰建造盆控特征. 矿物岩石, 21(3): 109-117. [Liu H J. 2001. Paleo-Tethyan basin evolution and basin-bound feature of Mn-bearing formation in the west margin of Yangtze Plate. Journal of Mineralogy and Petrology, 21(3): 109-117] [8] 刘平,廖友常,殷科华,叶德书,朱华,韩忠华,杨光龙. 2008. 与火山活动有关的热水沉积锰矿: 以贵州二叠纪锰矿为例. 中国地质, 35(5): 992-998. [Liu P,Liao Y C,Yin K H,Ye D S,Zhu H,Han Z H,Yang G L. 2008. Hydrothermal sedimentary manganese deposits associated to volcanic activities: Permian manganese deposit in Guizhou. Geology in China, 35(5): 992-998] [9] 刘巽锋,王庆生,高兴基. 2001. 贵州锰矿地质. 贵阳: 贵州人民出版社. [Liu X F,Wang Q S,Gao X J. 2001. Guizhou Manganese Mine Geology. Guiyang: Guizhou People's Publishing House] [10] 刘志臣,张远国,陈登,刘金海,崔忠强,胡乐宇,钟月丽. 2013. 贵州遵义锰矿区“白泥塘层”硅质岩地球化学特征及其地质意义. 矿物学报, 33(4): 265-270. [Liu Z C,Zhang Y G,Chen D,Liu J H,Cui Z Q,Hu L Y,Zhong Y L. 2013. Geochemical characteristics and geological significance of “white muddy layer”siliceous rocks in Zunyi manganese deposit,Guizhou. Acta Mineralogica Sinica, 33(4): 265-270] [11] 刘志臣,王聪,张远国,范波,陈登,魏泽权,崔忠强. 2015. 贵州遵义锰矿床地球化学特征及成因分析. 矿物学报, 35(4): 481-488. [Liu Z C,Wang C,Zhang Y G,Fan B,Chen D,Wei Z Q,Cui Z Q. 2015. Geochemistry and ore genesis of Zunyi Mn Deposit,Guizhou Province,China. Acta Mineralogica Sinica, 35(4): 481-488] [12] 刘志臣,吴发刚,骆红星,孙远彬,周晓林,陈登,代璨怡. 2016a. CSAMT法在贵州遵义锰矿整装勘查中的运用. 物探与化探, 40(2): 342-348. [Liu Z C,Wu F G,Luo H X,Sun Y B,Zhou X L,Chen D,Dai C Y. 2016a. The application of CSAMT method to monoblock exploration in the Zunyi manganese deposit,Guizhou Province. Geophysical and Geochemical Exploration, 40(2): 342-348] [13] 刘志臣,颜佳新,陈登,钟月丽,骆红星,范耀宏,龙宣霖,李隆富. 2016b. 贵州遵义深溪大型隐伏锰矿床的发现及成因探讨. 地质论评,62(s): 217-218. [Liu Z C,Yan J X,Chen D,Zhong Y L,Luo H X,Fan Y H,Long X L,Li L F. 2016b. Discovery and ore genesis of Zunyi Shenxi large concealed Mn deposit,Guizhou Province,China. Geological Review,62(s): 217-218] [14] 刘志臣,颜佳新,陈登,钟月丽,汪洋,王劲松,崔忠强,龙宣霖,李隆富,魏泽权,秦先进,刘永坤,周晓林,戴文坤,时中越,陈蝶,刘柯,蔡嘉骅. 2017. 贵州遵义锰矿国家整装勘查区地质找矿主要进展及潜力预测. 贵州地质, 34(2): 63-70. [Liu Z C,Yan J X,Chen D,Zhong Y L,Wang Y,Wang J S,Cui Z Q,Long X L,Li L F,Wei Z Q,Qin X J,Liu Y K,Zhou X L,Dai W K,Shi Z Y,Chen D,Liu K,Cai J H. 2017. Main progress and potential prediction of geological prospecting of manganese ore in national fully equipped exploration area of Zunyi,Guizhou Province. Guizhou Geology, 34(2): 63-70] [15] 刘志臣,周琦,颜佳新,汪洋,陈登,钟月丽,秦先进. 2019. 二叠纪贵州遵义次级裂谷盆地结构及其对锰矿的控制作用. 古地理学报, 21(3): 517-526. [Liu Z C,Zhou Q,Yan J X,Wang Y,Chen D,Zhong Y L,Qin X J. 2019. Structure of Zunyi rift basin in Guizhou Province during the Permian and its controlling on manganese deposits. Journal of Palaeogeography(Chinese Edition), 21(3): 517-526] [16] 陶平,杜昌乾,马荣,朱华,杜芬应,韩中华,廖莉萍. 2005. 贵州及邻区二叠系锰矿地质特征及成矿作用探讨. 贵州地质, 22(2): 103-108. [Tao P,Du C Q,Ma R,Zhu H,Du F Y,Han Z H,Liao L P. 2005. Geological characteristics and mineralization of Permian manganese deposits in Guizhou and its adjacent areas. Guizhou Geology, 22(2): 103-108] [17] 王涛,计文化,胡建民,李建星,胡道功,童英. 2016. 专题地质填图及有关问题讨论. 地质通报, 35(5): 633-641. [Wang T,Ji W H,Hu J M,Li J X,Hu D G,Tong Y. 2016. Geological mapping for special issues and a discussion on related topics. Geological Bulletin of China, 35(5): 633-641] [18] 王砚耕. 2000. 贵州西南部红土型金矿. 贵州: 贵州科技出版社. [Wang Y G. 2000. Lateritic gold deposits in southwestern Guizhou. Guizhou: Guizhou Science and Technology Publishing House] [19] 王砚耕,陈建书,陈启飞. 2018. 贵州构造—建造划分及其意义. 贵州地质, 35(3): 167-170. [Wang Y G,Chen J S,Chen Q F. 2018. Structure-formation division and its significance of Guizhou. Guizhou Geology, 35(3): 167-170] [20] 汪洋,刘志臣,陈登,钟月丽,秦先进. 2018. 贵州遵义二叠纪锰矿气液喷口群的发现及地质意义. 贵州地质, 35(2): 81-87,95. [Wang Y,Liu Z C,Chen D,Zhong Y L,Qin X J. 2018. Discovery and geological significance of submarine hydrothermal vent in Zunyi manganese deposit,Guizhou. Guizhou Geology, 35(2): 81-87,95] [21] 杨炳南,胡祥云,周琦,沈小庆,何帅,谢小峰,王家俊. 2018. 华南南华纪古天然气渗漏沉积型锰矿AMT勘查技术方法研究. 贵州地质, 35(4): 105-111. [Yang B N,Hu X Y,Zhou Q,Shen X Q,He S,Xie X F,Wang J J. 2018. An audio-frequency magnetotellurics method study on the exploration technology of ancient natural gas seepage sedimentary-type manganese deposit of Nanhua Period in South China. Guizhou Geology, 35(4): 105-111] [22] 杨瑞东,程玛莉,魏怀瑞. 2009. 贵州水城二叠系茅口组含锰岩系地质地球化学特征与锰矿成因分析. 大地构造与成矿学, 32(4): 613-619. [Yang R D,Cheng M L,Wei H R. 2009. Geochemical characteristics and origin of a manganese deposit in the Middle Permian Maokou Formation in Shuicheng,Guizhou,China. Geotectonica et Metallogenia, 32(4): 613-619] [23] 杨瑞东,程玛莉,高军波,徐海,李军,陈军,刘坤. 2018. 贵州二叠系茅口组顶部锰矿沉积特征及矿床成因研究. 地质学报, 92(4): 804-816. [Yang R D,Cheng M L,Gao J B,Xu H,Li J,Chen J,Liu K. 2018. The sedimentary characteristics and origin of manganese deposit in the Middle Permian Maokou Formation in Guizhou,China. Acta Geologica Sinica, 92(4): 804-816] [24] 杨坤光,李学刚,戴传固,张慧,周琦. 2012. 断层调整与控制作用下的叠加构造变形: 以贵州地区燕山期构造为例. 地质科技情报, 31(5): 50-56. [Yang K G,Li X G,Dai C G,Zhang H,Zhou Q. 2012. Superimposition deformation controlled and adjusted by faults: An example from Yanshanian structural deformation in Guizhou Province. Geological Science and Technology Information, 31(5): 50-56] [25] 翟裕生,张湖,宋鸿林,邓军,程小久. 1997. 大型构造与超大型矿床. 北京: 地质出版社,1-175. [Zhai Y S,Zhang H,Song H L,Deng J,Cheng X J. 1997. Large Structure and Superlarge Deposit. Beijing: Geological Publishing House,1-175] [26] 张国伟,郭安林,王岳军,李三忠,董云鹏,刘少峰,何登发,程顺有,鲁如魁,姚安平. 2013. 中国华南大陆构造与问题. 中国科学: 地球科学, 43(10): 1553-1582. [Zhang G W,Guo A L,Wang Y J,Li S Z,Dong Y P,Liu S F,He D F,Cheng S Y,Lu R K,Yao A P. 2013. Tectonics of South China continent and its implications. Science China: Earth Sciences, 43(10): 1553-1582] [27] 张进,贺振宇,曲军峰,张庆龙,李锦轶,郑荣国,张北航,赵衡,解国爱,刘建峰. 2018. 基岩区构造地质填图方法思考、实践、探索. 地质通报, 37(2): 192-221. [Zhang J,He Z Y,Qu J F,Zhang Q L,Li J Y,Zheng R G,Zhang B H,Zhao H,Xie G A,Liu J F. 2018. The structural mapping in exposed bedrock areas: Methods,practice and exploration. Geological Bulletin of China, 37(2): 192-221] [28] 周琦,杜远生,覃英. 2013. 古天然气渗漏沉积型锰矿床成矿系统与成矿模式: 以黔湘渝毗邻区南华纪“大塘坡式”锰矿为例. 矿床地质, 32(3): 457-466. [Zhou Q,Du Y S,Qin Y. 2013. Ancient natural gas seepage sedimentary-type manganese metallogenic system and ore-forming model: A case study of‘Datangpo type’ manganese deposits formed in rift basin of Nanhua Period along Guizhou-Hunan-Chongqing border area. Mineral Deposits, 32(3): 457-466] [29] 周琦,杜远生,袁良军,张遂,余文超,杨胜堂,刘雨. 2016. 黔湘渝毗邻区南华纪武陵裂谷盆地结构及其对锰矿的控制作用. 地球科学, 41(2): 177-188. [Zhou Q,Du Y S,Yuan L J,Zhang S,Yu W C,Yang S T,Liu Y. 2016. The structure of the Wuling rift basin and its control on the manganese deposit during the Nanhua Period in Guizhou-Hunan-Chongqing border area,South China. Earth Science, 41(2): 177-188] [30] 周琦,杜远生,袁良军,张遂,杨炳南,潘文,余文超,王萍,徐源,齐靓,刘雨,覃永军,谢小峰. 2017. 古天然气渗漏沉积型锰矿床找矿模型: 以黔湘渝毗邻区南华纪“大塘坡式”锰矿为例. 地质学报, 91(10): 2285-2298. [Zhou Q,Du Y S,Yuan L J,Zhang S,Yang B N,Pan W,Yu W C,Wang P,Xu Y,Qi L,Liu Y,Qin Y J,Xie X F. 2017. Exploration models of ancient natural gas seep sedimentary-type manganese ore deposit: A case study of the Nanhua Period “Datangpo”type manganese ore in the conjunction area of Guizhou,Hunan and Chongqing. Acta Geologica Sinica, 91(10): 2285-2298] [31] 朱洪发,秦德余,刘翠章. 1989. 论华南孤峰组和大隆组硅质岩成因、分布规律及其构造机制. 石油实验地质, 11(4): 341-348. [Zhu H F,Qin D Y,Liu C Z. 1989. On the origin,distributive pattern and tectonic control of siliceous rocks in Gufeng and Dalong Formations,South China. Petroleum Geology & Experiment, 11(4): 341-348] [32] Attwa M,Henaish A. 2018. Regional structural mapping using a combined geological and geophysical approach: A preliminary study at Cairo-Suez district,Egypt. Journal of African Earth Sciences,144: 104-121. [33] Bernhard S,Olaf D. 2012. Dissolved reactive manganese at pelagic redox clines(part Ⅰ): A method for determination based on field experiments. Journal of Marine Systems, 90(1): 23-30. [34] Childs C, Nicol A,Walsh J J, Watterson J. 2003. The growth and propagation of synsedimentary faults. Journal of Structural Geology, 25(4): 633-648 [35] Edmond J M,von Damm K. 1983. Hot springs on the ocean floor. Scientific American, 248(4): 70-85. [36] Kuznetsov V G. 2017. Evolution of sedimentary rock formation of a rock association level. Doklady Earth Sciences, 475(1): 736-738. [37] He B,Xu Y G,Chung S L,Xiao L,Wang Y M. 2003. Sedimentary evidence for a rapid,kilometer scale crustal doming prior to the eruption of the Emeishan flood basalts. Earth Planet Science Letters, 213: 391-405. [38] Kruse F A,Perry S L. 2013. Mineral mapping using simulated world-view-3 short-wave-infrared imagery. Remote Sensing, 5(6): 2688-2703. [39] Maynard J B. 2003. Manganiferous sediments,rocks,and ores. In: Heinrich D H,Karl K T(eds). Treatise on Geochemistry. Oxford: Pergamon, 20(2): 289-308. [40] Shellnutt J G,Zhou M F. 2006. Rifting-related,Permian ferrosyenites in the Panxi region of the Emeishan large igneous province,SW China. Geochimica et Cosmochimica Acta,70(18,Supplement): A579. [41] Shellnutt J G,Zhou M F,Chung S L. 2010. The Emeishan large igneous province: Advances in the stratigraphic correlations and petrogenetic and metallogenic models. Lithos, 119(1-2): 34-46. [42] Wang X X,Wang T,Ke C H,Yang Y,Li J B,Li Y H,Qi Q J,Lü X Q. 2014. Nd-Hf isotopic mapping of Late Mesozoic granitoids in the East Qinling Orogen,Central China: Constraint on the basements of terranes and distribution of Mo mineralization. Journal of Asian Earth Sciences, 103: 169-183. [43] Zeng J W,Xu R,Gong X M. 2011. Hydrothermal activities and seawater acidification in the Late Devonian F-F transition: Evidence from geochemistry of rare earth elements. Science China: Earth Science, 54(2): 540-549. [44] Zhang Z C,Mao J W,Saunders A D,Ai Y,Li Y,Zhao L. 2009. Petrogenetic modeling of three mafic-ultramafic layered intrusions in the Emeishan large igneous province,SW China,based on isotopic and bulk chemical constraints.Lithos, 113(3-4): 369-392. |