Structure of Zunyi rift basin in Guizhou Province during the Permian and its controlling on manganese deposits
Liu Zhi-Chen1,2, Zhou Qi3, Yan Jia-Xin1, Wang Yang2, Chen Deng1,2, Zhong Yue-Li2, Qin Xian-Jin2
1 Faculty of Earth Sciences,China University of Geosciences(Wuhan),Wuhan 430074,China; 2 The 102 Geological Team,Bureau of Geology and Mineral Exploration and Development;Guizhou Province,Guizhou Zunyi 553003,China; 3 Bureau of Geology and Mineral Exploration and Development Guizhou Province,Guiyang 550003, China
Abstract：As the earliest discovered manganese mine with industrial value in Guizhou Province,Zunyi manganese deposit is one of the important manganese resource bases in China. According to the detailed division of the Permian Maokou-Longtan Formations,the Zunyi secondary rift basin is considered to be composed of three 3rd-order faulted basins and two 3rd-order uplifts,which could be classified into at least 13 4th-order faulted basins. The 3rd-order faulted basins controlled the formation of the Tongluojing-Shenxi,Zhuanlongmiao-Xiejiaba,Zhangjiawan-Xinglong,and Heshangchang-Wulongxi manganese sub-belts. The Tongluojing-Shenxi manganese sub-belt is the center of the Zunyi rift basin with strong manganese mineralization,forming three large manganese beds in Tongjing,Shenxi,and Yongan. The 4th-order faulted basins controlled the formation of various manganese beds in the study area. Moreover,14 synsedimentary faults have been identified,which are believed to be the ascending channel of the deep fluids rich in silicon and manganese gas and play a key role on the formation of Zunyi Permian manganese deposit. Therefore,the formation of Zunyi rift basin has a significant controlling on the manganese deposit. Results of this research are of great significance for searching hidden deposits and guiding the full-scale exploration of Zuiyi Manganese deposit.
Liu Zhi-Chen,Zhou Qi,Yan Jia-Xin et al. Structure of Zunyi rift basin in Guizhou Province during the Permian and its controlling on manganese deposits[J]. JOPC, 2019, 21(3): 517-526.
[1] 蔡学林,曹家敏,朱介寿,程先琼. 2008. 中国大陆岩石圈壳幔韧性剪切带系统. 地学前缘, 15(3): 36-54. [Cai X L,Cao J M,Zhu J S,Cheng X Q.2008. The system of crust-mantle ductile shear zones in China continental lithosphere. Earth Science Frontiers, 15(3): 36-54] [2] 陈文一,王立亭,叶念曾,蔡英,马忠魏. 1984. 贵州早二叠世岩相古地理研究. 贵州地质, 1(1): 9-63. [Chen W Y,Wang L T,Ye N Z,Cai Y, Ma Z W.1984. Lithofacies palaeogeographic characteristics of Early Permian in Guizhou. Guizhou Geology, 1(1): 9-63] [3] 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] [4] 何卫红,唐婷婷,乐明亮,邓晋福,潘桂棠,邢光福,骆满生,徐亚东,韦一,张宗言,肖异凡,张克信. 2014. 华南南华纪—二叠纪沉积大地构造演化. 地球科学, 39(8): 929-953. [He W H,Tang T T,Yue M L,Deng J F,Pan G T,Xing G F,Luo M S,Xu Y D,Wei Y,Zhang Z Y,Xiao Y F,Zhang K X.2014. Sedimentary and tectonic evolution of Nanhuan-Permian in South China. Earth Science, 39(8): 929-953] [5] 侯忠林,薛友智. 1997. 扬子地台周边锰矿. 北京: 冶金工业出版社. [Hou Z Q,Xue Y Z.1997. Manganese Ore Around the Yangtze Platform. Beijing: Metallurgical Industry Press] [6] 李维波,李江海,王洪浩,塔斯肯. 2015. 二叠纪古板块再造与岩相古地理特征分析. 中国地质, 42(2): 685-694. [Li W B,Li J H,Wang H H,Ta S K.2015. Characteristics of the reconstruction of Permian paleoplate and lithofacies paleogeography. Geology in China, 42(2): 685-694] [7] 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] [8] 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] [9] 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] [10] 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] [11] 刘志臣,颜佳新,陈登,钟月丽,骆红星,范耀宏,龙宣霖,李隆富. 2016. 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.2016. Discovery and ore genesis of Zunyi Shenxi large concealed Mn deposit,Guizhou Province,China. Geological Review,62(s): 217-218] [12] 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] [13] 刘志臣,周琦,颜佳新,陈登,汪洋,秦先进,钟月丽. 2018. 贵州遵义二叠纪成矿时代及锰矿成因探讨. 第十四届全国矿床学会会议论文,943-944. [Liu Z C,Zhou Q,Yan J X,Chen D,Wang Y,Qin X J,Zhong Y L.2018. Exploration of the Permian Mineralization Ore and the Genesis of Manganese Ore in Zunyi,Guizhou Province. Paper presented at the 14th National Association of Mineral Deposits Conference,943-944] [14] 王鸿祯. 1990. 中国及邻区构造古地理和生物古地理. 北京: 中国地质大学出版社. [Wang H Z.1990. Tectonics,Palaeogeography and Paleogeography of China and Its Adjacent Areas. Beijing: China University of Geosciences Press] [15] 肖传桃,丁静,胡望水,唐友军,吕炳全,柴华,焉飞. 2009. 下扬子地区中二叠世上升流相区古生态学研究. 沉积学报, 27(2): 319-325. [Xiao C T,Ding J,Hu W S,Tang Y J,Lü B Q,Chai H,Yan F.2009. A study on palaeoecology in upwelling phase region of Middle Permian in the Lower Yangtze area. Sedimentologica, 27(2): 319-325] [16] 薛友智. 2012. 中国锰矿地质特征与勘查评价. 四川地质学报,32(s): 14-19. [Xue Y Z.2012. Geological characteristics and exploration evaluation of manganese deposits in China. Sichuan Journal of Geology,32(s): 14-19] [17] 颜佳新,赵坤. 2002. 二叠—三叠纪东特提斯地区古地理、古气候和古海洋演化与地球表层多圈层事件耦合. 中国科学, 32(9): 751-759. [Yan J X,Zhao K.2002. The coupling of palaeogeography palaeoclimate paleooceanic evolution and multi circle events of the earth's surface layer in the two fold-Triassic East Tethys region. China Science, 32(9): 751-759] [18] 杨海生,周永章,杨志军,张澄博,杨小强. 2003. 热水沉积硅质岩地球化学特征及意义: 以华南地区为例. 中山大学学报(自然科学版), 42(6): 111-115. [Yang H S,Zhou Y Z,Yang Z J,Zhang C B,Yang X Q.2003. Geochemical characteristics and significance of hydrothermal cherts: A case study of South China. Acta Scientiarum Naturalium Universitatis Sunyatseni, 42(6): 111-115] [19] 杨怀宇,陈世悦,郝晓良,郭桦,李聪,杨勇. 2010. 南盘江坳陷晚古生代隆林孤立台地沉积特征与演化阶段. 中国地质, 37(6): 1638-1646. [Yang H Y,Chen S Y,Hao X L,Guo H,Li C,Yang Y.2010. Sedimentary characteristics and evolutionary stages of Late Paleozoic Longlin isolated platform in Nanpanjiang depression. Geology in China, 37(6): 1638-1646] [20] 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] [21] 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 sesimentary characteristics and origin of manganese deposit in the Middle Permian Maokou Formation in Guizhou,China. Acta Geologica Sinica, 92(4): 804-816] [22] 杨玉卿,冯增昭. 2000. 中国南方二叠纪沉积体系. 古地理学报, 2(1): 11-18. [Yang Y Q,Feng Z Z.2000. Permian deposional systems in South China. Journal of Palaeogeography(Chinese Edition), 2(1): 11-18] [23] 姚敬劬. 1995. 扬子地台南缘及其邻区锰矿研究. 北京: 冶金工业出版社. [Yao J Q.1995. Study on Manganese Deposits in the Southern Margin of Yangtze Platform and Its Adjacent Areas. Beijing: Metallurgical Industry Press] [24] 姚旭,周瑶琪,李素,李斗. 2013. 硅质岩与二叠纪硅质沉积事件研究现状及进展. 地球科学进展, 11(2): 1-3. [Yao X,Zhou Y Q,Li S,Li D.2013. Research status and advances in chert and Permian chert event. Advances in Earth Science, 11(2): 1-3] [25] 殷鸿福,吴顺宝. 1999. 华南是特提斯多岛洋体系的一部分. 地球科学, 24(1): 1-12. [Yin H F,Wu S B.1999. South China defined as part of Tethyan Archipelagic ocean system. Erath Science, 24(1): 1-12] [26] 周琦,杜远生,王家生,彭家强. 2007. 黔东北地区南华系大塘坡组冷泉碳酸盐岩及其意义. 地球科学, 32(3): 339-346. [Zhou Q,Du Y S,Wang J S,Pen J Q.2007. Characteristics and significance of the Cold Seep Carbonates from the Datangpo Formation of the Nanhua Series in the northeast Guizhou. Earth Science, 32(3): 339-346] [27] 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] [28] 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] [29] 周新平,何幼斌,杜红权,李华. 2009. 四川宣汉地区二叠系硅岩地球化学特征及成因研究. 古地理学报, 11(6): 670-680. [Zhou X P,He Y B,Du H Q,Li H.2009. Geochemical characteristics and origin of the Permian siliceous rocks in Xuanhan region of Sichuan Province. Journal of Palaeogeography(Chinese Edition), 11(6): 670-680] [30] 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] [31] Bernhard S,Olaf D.2012. Dissolved reactive manganese at pelagic redoxclines(part Ⅰ): A method for determination based on field experiments. Journal of Marine Systems, 90(1): 23-30. [32] Golonka J,Ford D.2001. Pangean(LateCarboniferous-MiddleJurassic)paleoenvironment and lithofacies. Palacogeography,Palacoelimatology,Palaeoecology, 16(1): 1-34. [33] He B,Xu Y G,Guan J P,Zhong Y T.2010. Paleokarst on the top of the Maokou Formation: Further evidence for domal crustal uplift prior to the Emeishan flood volcanism. Lithos, 119(1-2): 1-9. [34] Liu H J.1999. Sedimentology of Triassic Dounan type manganese deposits,western margin,Yangtze Platform,China. Lore Geology Reviews, 15(2): 165-176. [35] Murray R W.1994. Chemical criteria to identify the depositional environment of chert: General principles and applications. Sedimentary Geology, 90(3): 213-232. [36] 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. [37] Maynard J B.2010. The chemistry of manganese ores through time: A signal of increasing diversity of earth-surface environments. Economic Geology, 105(3): 535-552. [38] Roy S.2006. Sedimentary manganese metallogenesis in response to the evolution of the Earth system. Earth-Science Reviews, 77(4): 273-305. [39] Sheng J Z,Jin Y G.1994. Correlation of Permian deposits in China. Palaeoworld, 4(1): 14-113. [40] 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.
