‘Qianzhong Uplift’ and evolution of the Late Paleozoic palaeogeography and its control on formation of bauxite in Guizhou Province
Deng Xu-Sheng1,2, Du Yuan-Sheng2,3, Yu Wen-Chao2,3, Wu Kai-Bin1, Lu Shu-Fan1, Zhang Han-Bin1
1 Guizhou Geological Survey,Guiyang 550081,China; 2 Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones,Ministry of Natural Resources,Guiyang 550081,China; 3 School of Earth Sciences,China University of Geosciences(Wuhan),Wuhan 430074,China
Abstract The Early Paleozoic regional uplift(e.g.,the Qianzhong Uplift)and sea-level changes had obviously controlled the evolution of the Late Paleozoic palaeogeography and paleogeomorphology in Guizhou Province. However,the formation time and evolution of the Qianzhong Uplift is still in debate,which limits the understanding of the Permo-Carboniferous paleogeographic and paleogeomorphologic evolution that formed bauxite in Guizhou. In this paper,based on field surveys and data collection,we established the palaeogeography of several important geological periods from the Late Cambrian to Permian in Guizhou,and re-recognized the formation time and evolution of the Qianzhong Uplift,and revealed the coupling relationship between the Qianzhong Uplift and Guizhou bauxite formation. During the Cambrian to early-middle Early Silurian,the continent-marine transitional facies were missed in the northern margin of the Qianzhong Uplift,central Guizhou Province,such as Bijie,Jinsha and Zunyi. The large-scale uplift of the central Guizhou Province should begin with the tidal flat deposits of the Hanchiatien Formation in the Early Silurian. Because of the Qianzhong Uplift,the central Guizhou and Zunyi areas experienced long-lasting and intense weathering and erosion,forming karst depressions,funnels,and canyons in the Early Carboniferous. The karst landform provided material conditions and location for the formation of bauxite deposits in the Early Carboniferous. The bauxite ore formed under intense chemical wreathing and leaching induced by the glacio-eustasy and paleoclimate fluctuations. The early long-lasting and intense weathering and erosion occurred in the northern Guizhou along with the Permo-Carboniferous glacio-eustasy,had leaded to the formation of coastal wetland and depressions,which were favorable places for the Early Permian bauxite formation. The Early Permian bauxite ores in Guizhou Province have an obvious coupling relationship with the Late Paleozoic Ice Age.
Fund:Co-funded by the National Natural Science Foundation of China(Nos. U1812402,41802116)and the Guizhou Scientific and Technology Planning Project(QKHPTRC[2018]5626)
About author: Deng Xu-Sheng,born in 1986,doctor of philosophy,is an engineer. Now he is mainly engaged in sedimentology. E-mail: dengxs86@163.com.
Cite this article:
Deng Xu-Sheng,Du Yuan-Sheng,Yu Wen-Chao et al. ‘Qianzhong Uplift’ and evolution of the Late Paleozoic palaeogeography and its control on formation of bauxite in Guizhou Province[J]. JOPC, 2020, 22(5): 872-892.
Deng Xu-Sheng,Du Yuan-Sheng,Yu Wen-Chao et al. ‘Qianzhong Uplift’ and evolution of the Late Paleozoic palaeogeography and its control on formation of bauxite in Guizhou Province[J]. JOPC, 2020, 22(5): 872-892.
[1] 陈庆刚,陈群,戴晓燕. 2016. 黔中地区铝土矿成矿时代探讨. 贵州地质, 33(2): 101-107. [Chen Q G,Chen Q,Dai X Y. 2016. Discussion of metallogenic epoch of bauxite deposit in central Guizhou. Guizhou Geology, 33(2): 101-107] [2] 陈群,戴晓燕,梁鹏,蒋建文. 2019. 贵州省修文县石炭系小山坝铝土矿矿床地质特征. 贵州地质, 36(4): 316-323. [Chen Q,Dai X Y,Liang P,Jiang J W. 2019. Geological characteristics of Xiaoshanba bzuxite deposit in Carboniferous system of Xiuwen,Guizhou. Guizhou Geology, 36(4): 316-323] [3] 陈旭,戎嘉余,周志毅,张元动,詹仁斌,刘建波,樊隽轩. 2001. 上扬子区奥陶—志留纪之交的黔中隆起和宜昌上升. 科学通报, 46(12): 1052-1056. [Chen X,Rong J Y,Zhou Z Y,Zhang Y D,Zhan R B,Liu J B,Fan J X. 2001. The Qianzhong and Yichang Uplift of the Ordocician-Silurian in the Upper Yangtze Region. Chinese Science Bulletin, 46(12): 1052-1056] [4] 崔金栋. 2013. 黔中隆起及其周缘构造演化的沉积响应. 中南大学博士学位论文,13. [Cui J D. 2013. Sedimentary response to tectonic evolution of the Central Guizhou Uplift and its adjacent areas. Doctoral dissertation of Central South University,13] [5] 崔滔,焦养泉,杜远生,计波,雷志远,翁申富,金中国,赵爽. 2013. 黔北务正道铝土矿沉积特征及分布规律. 地质科技情报, 32(1): 52-56. [Cui T,Jiao Y Q,Du Y S,Ji B,Lei Z Y,Weng S F,Jin Z G,Zhao S. 2013. Sedimentary characteristics and distribution features of bauxite in Wuchuan-Zheng'an-Daozhen Area,Northern Guizhou Province. Geological Science and Technology Information, 32(1): 52-56] [6] 崔滔,焦养泉,杜远生,汪小妹,雷志远,翁申富,金中国. 2014. 黔北务正道地区早二叠世铝土矿沉积古地理及其控矿意义. 古地理学报, 16(1): 9-18. [Cui T,Jiao Y Q,Du Y S,Wang X M,Lei Z Y,Weng S F,Jin Z G. 2014. Sedimentary palaeogeography and its mineralization significance of the Early Permian bauxite in Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province. Journal of Palaeogeography(Chinese Edition), 16(1): 9-18] [7] 戴传固,王敏,陈建书,王雪华. 2013. 贵州构造运动特征及其地质意义. 贵州地质, 30(2): 119-124. [Dai C G,Wang M,Chen J S,Wang X H. 2013. Tectonic movement characteristic and its geological significance of Guizhou. Guizhou Geology, 30(2): 119-124] [8] 戴新春,黄友庄. 1998. 刍议黔中隆起及其形成过程中的均衡沉陷作用. 贵州工业大学学报, 27(2): 23-26. [Dai X C,Huang Y Z. 1998. On the Central Guizhou Uplift and the isostatic subsidence in the process of its formation. Journal of Guizhou University of Technology, 27(2): 23-26] [9] 邓新,杨坤光,刘彦良,佘振兵. 2010. 黔中隆起性质及其构造演化. 地学前缘, 17(3): 79-89. [Deng X,Yang K G,Liu Y L,She Z B. 2010. Characteristics and tectonic evolution of Qianzhong Uplift. Earth Science Frontiers, 17(3): 79-89] [10] 杜远生,周琦,金中国,凌文黎,张雄华,喻建新,汪小妹,余文超,黄兴,崔滔,雷志远,翁申富,吴波,覃永军,曹建州,彭先红,张霞,邓虎. 2013. 黔北务正道地区铝土矿基础地质与成矿作用研究进展. 地质科技情报, 32(1): 1-5. [Du Y S,Zhou Q,Jin Z G,Ling W L,Zhang X H,Yu J X,Wang X M,Yu W C,Huang X,Cui T,Lei Z Y,Weng S F,Wu B,Qin Y J,Cao J Z,Peng X H,Zhang X,Deng H. 2013. Advances in basic geology and metallogenic regularity study of bauxite in Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province. Geological Science and Technology Information, 32(1): 1-5] [11] 杜远生,周琦,金中国,凌文黎,汪小妹,余文超,崔滔,雷志远,翁申富,吴波,覃永军,曹建州,彭先红,张霞,邓虎. 2014. 黔北务正道地区早二叠世铝土矿成矿模式. 古地理学报, 16(1): 1-8. [Du Y S,Zhou Q,Jin Z G,Ling W L,Wang X M,Yu W C,Cui T,Lei Z Y,Weng S F,Wu B,Qin Y J,Cao J Z,Peng X H,Zhang X,Deng H. 2014. Mineralization model for the Early Permian bauxite deposits in Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province. Journal of Palaeogeography(Chinese Edition), 16(1): 1-8] [12] 杜远生,周琦,金中国,焦养泉,凌文黎,汪小妹,喻建新,张雄华,顾松竹,余文超,黄兴,崔滔,张莹华,史骁,雷志远,莫光员,翁申富,赵远由,李沛刚,覃永军. 2015. 黔北务正道地区二叠系铝土矿沉积地质学. 武汉: 中国地质大学出版社,35-67. [Du Y S,Zhou Q,Jin Z G,Jiao Y Q,Ling W L,Wang X M,Yu J X,Zhang X H,Gu S Z,Yu W C,Huang X,Cui T,Zhang Y H,Shi X,Lei Z Y,Mo G Y,Weng S F,Zhao Y Y,Li P G,Qin Y J. 2015. Sedimentary Geology of the Permian Bauxite Deposit in Wuchuan-Zheng'an-Daozhen Area,Northern Guizhou Province. Wuhan: China University of Geosciences Press,35-67] [13] 范广慧,王永标,孟峥,李国山. 2016. 贵州紫云晚二叠世—早三叠世初火山作用与生物礁的沉积演化. 沉积学报, 35(1): 24-34. [Fan G H,Wang Y B,Meng Z,Li G S. 2016. The Relationship between volcanism and reef sedimentary evolution from Late Permian to the beginning of Early Triassic in Ziyun,Guizhou Province. Acta Sedimentologica Sinica, 35(1): 24-34] [14] 高道德. 1996. 黔中沉积型铝土矿成矿模式. 贵州地质, 13(2): 166-171. [Gao D D. 1996. A genetic model for sedimentary type of bauxite deposits in central Guizhou. Guizhou Geology, 13(2): 166-171] [15] 贵州省地质调查院. 2017. 中国区域地质志·贵州志. 北京: 地质出版社,709-728. [Guizhou Geological Survey. 2017. The Regional Geology of China,Guizhou Province. Beijing: Geological Publishing House,709-728] [16] 韩忠华. 2008. 贵州道真县大塘铝土矿沉积相特征. 矿产与地质, 22(5): 428-432. [Han Z H. 2008. Sedimentary facies characteristics of the Datang bauxite deposit in Daozhen County,Guizhou. Mineral Resources and Geology, 22(5): 428-432] [17] 何熙琦,肖加飞,王尚彦,刘爱民,黎超,白平. 2005. 黔中隆起研究. 贵州地质, 22(2): 83-89. [He X Q,Xiao J F,Wang S Y,Liu A M,Li C,Bai P. 2005. The study on the Qianzhong Upheaval. Guizhou Geology, 22(2): 83-89] [18] 胡华蕊,刑凤存,侯明才,段金宝,张殿伟. 2019. 上扬子奥陶纪层序岩相古地理重建及油气勘探启. 地球科学, 44(3): 798-809. [Hu H R,Xing F C,Hou M C,Duan J B,Zhang D W. 2019. Ordovician sequence and lithofacies paleogeography reconstruction in Upper Yangtze region and its implication for oil and gas exploration. Earth Science, 44(3): 798-809] [19] 黄兴,张雄华,杜远生,郄文昆,杨兵,段先锋. 2013. 黔北务正道地区及邻区石炭纪—二叠纪之交海平面变化对铝土矿的控制. 地质科技情报, 32(1): 80-86. [Huang X,Zhang X H,Du Y S,Qie W K,Yang B,Duan X F. 2013. Control of sea-level changes over the forming of bauxite between Carboniferous and Permian in northern Guizhou and adjacent regions. Geological Science and Technology Information, 32(1): 80-86] [20] 焦大庆,马永生,邓军,孟庆芬,李东海. 2003. 黔桂地区石炭纪层序地层格架及古地理演化. 现代地质, 17(3): 294-302. [Jiao D Q,Ma Y S,Deng J,Meng Q F,Li D H. 2003. The sequence-stratigraphic framework and the evolution of paleogeography for Carboniferous of the Guizhou and Guangxi areas. Geoscience, 17(3): 294-302] [21] 金中国,刘辰生,邹林,郑明泓,张力,韩英. 2018. 贵州务—正—道地区二叠纪铝土矿沉积环境地球化学证据. 地质学报, 92(4): 817-827. [Jin Z G,Liu C S,Zou L,Zheng M H,Zhang L,Han Y. 2018. Geochemical evidence of sedimentary environment of Permian bauxite in the Wuchuan-Zheng'an-Daozhen area,Guizhou Province. Acta Geologica Sinica, 92(4): 817-827] [22] 鞠天吟. 1999. 黔中隆起之窥见. 贵州地质, 16(2): 180-184. [Ju T Y. 1999. Discussion on Central Guizhou Uplift. Guizhou Geology, 16(2): 180-184] [23] 雷志远,廖友常. 2007. 黔北大竹园铝土矿矿床地质特征及成因浅析. 西部探矿工程, 18(2): 94-97. [Lei Z Y. 2007. Geological characteristics and genetic analysis of Dazhuyuan bauxite deposit in northern Guizhou Province. West-China Exploration Engineering, 18(2): 94-97] [24] 雷志远,翁申富,陈强,熊星,潘忠华,和秀林,陈海. 2013. 黔北务正道地区早二叠世大竹园期岩相古地理及其对铝土矿的控矿意义. 地质科技情报, 32(1): 8-12. [Lei Z Y,Weng S F,Chen Q,Xiong X,Pan Z H,He X L,Chen H. 2013. Lithofacies paleogeography of the Dazhuyuan Age,Early Permian in the Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province and its implication for bauxitisation. Geological Science and Technology Information, 32(1): 8-12] [25] 廖士范. 1990. “遵义隆起”的发生发展与古风化壳铝土矿的形成问题. 贵州工学院学报, 19(1): 81-82. [Liao S F. 1990. Problems of happening and developing of the Central Guizhou Upwarping and forming of ancient weathering-crust bauxite deposit. Journal of Guizhou Institute of Teghnology, 19(1): 81-82] [26] 李儒峰,刘本培,赵澄林. 1997. 扬子板块石炭纪沉积层序及其全球性对比研究. 沉积学报, 15(3): 23-28. [Li R F,Liu B P,Zhao C L. 1997. Correlation of Carboniferous depositional sequences on the Yangtze plate with others on a global scale. Acta Sedimentologica Sinica, 15(3): 23-28] [27] 刘宝珺,许效松. 1994. 中国南方岩相古地理图集(震旦纪—三叠纪). 北京: 科学出版社,58-75. [Liu B J,Xu X S. 1994. Atlas of the Palaeogeography of South China(Sinian-Triassic). Beijing: Science Press, 58-75] [28] 刘本培,李儒峰,尤德宏. 1994. 黔南独山石炭系层序地层及麦粒?带冰川型全球海平面变化. 地球科学, 19(5): 553-564. [Liu B P,Li R F,You D H. 1994. Carboniferous sequences stratigraphy and glacio-eustasy of Triticites Zone in Southern Guizhou,China. Earth Science-Journal of China University of Geosciences, 19(5): 553-564] [29] 刘平. 1993. 三论贵州之铝土矿: 贵州北部铝土矿成矿时代、物质来源及成矿模式. 贵州地质, 10(2): 105-113. [Liu P. 1993. An additional discussion on bauxite deposits of Guizhou(Ⅲ)—Their metallogenetic epoch,material source and metallogenetic model. Geology of Guizhou, 10(2): 105-113] [30] 刘平,廖友常. 2013. 试论遵义高铁铝土矿与低铁铝土矿的分带性及形成机制. 中国地质, 40(3): 949-966. [Liu P,Liao Y C. 2013. The zonation and genetic mechanism of Zunyi high-and low-ferrous bauxites. Geology in China, 40(3): 949-966] [31] 刘平,廖友常. 2014. 黔中—渝南沉积型铝土矿区域成矿模式及找矿模型. 中国地质, 41(6): 2063-2082. [Liu P,Liao Y C. 2014. Regional metallogenic model and prospecting criteria of sedimentary bauxite deposits in central Guizhou-southern Chongqing region. Geology in China, 41(6): 2063-2082] [32] 刘平,廖友常,张雅静. 2015. 黔中—渝南石炭纪铝土矿含矿岩系中的海相沉积特征. 中国地质, 42(2): 641-654. [Liu P,Liao Y C,Zhang Y J. 2015. Characteristics of marine deposits of the bauxite-bearing rock series in central Guizhou-southern Chongqing area. Geology in China, 42(2): 641-654] [33] 刘平,廖友常,张雅静. 2016. 沉积型铝土矿及其含矿岩系在岩溶洼地中的沉积特征: 以遵义后槽矿区为例. 中国地质, 43(2): 546-563. [Liu P,Liao Y C,Zhang Y J. 2016. Sedimentary characteristics of sedimentary bauxite and ore-bearing rock series in corroded depression: A case study of the Houcao mining area in Zunyi. Geology in China, 43(2): 546-563] [34] 刘特明. 1987. 黔中何时隆起. 贵州地质, 4(1): 65-71. [Liu T M. 1987. Further discussion about Central Guizhou Upwarping. Geology of Guizhou, 4(1): 65-71] [35] 刘特明. 1989. 再论“黔中隆起”. 贵州工学院学报, 19(1): 87-88. [Liu T M. 1989. When Central Guizhou rose. Journal of Guizhou Institute of Teghnology, 19(1): 87-88] [36] 刘伟,许效松,余谦. 2011. 探讨黔中古隆起形成机制及演化. 沉积学报, 29(4): 658-664. [Liu W,Xu X S,Yu Q. 2011. Discussion on forming mechanism and evolution of the Central Guizhou Palaeouplift. Acta Sedimentologica Sinica, 29(4): 658-664] [37] 刘巽锋,秦典燮. 1988. 贵州中部早石炭世古喀斯特特征及铝铁矿成矿作用. 贵州地质, 5(1): 11-24. [Liu X F,Qin D X. 1988. The Early Carboniferous palaeokarst feature and minerogenesis of alumino-ferric deposits in the center of Guizhou. Geology of Guizhou, 5(1): 11-24] [38] 刘幼平,周文龙,程国繁,崔滔,龙汉生. 2016. 贵州铝土矿含矿岩系特征与成矿规律研究. 矿物学报, 36(2): 289-294. [Liu Y P,Zhou W L,Chen G F,Cui T,Long H S. 2003. A research on characteristics of ore-bearing rock series and mineralization principles of bauxite from Guizhou Province,China. Acta Mineralogica Sinica, 36(2): 289-294] [39] 梅冥相. 1991. 试论贵州早石炭世铝土铁质岩系的沉积环境及物质来源. 贵州地质, 8(4): 322-328. [Mei M X. 1991. A preliminary discussion on material resources and depositional environment of bauxite rock system of Early Carboniferous epoch in Guizhou Province. Geology of Guizhou, 8(4): 322-328] [40] 梅冥相. 1994. 论“黔中古陆”. 贵州地质, 11(3): 199-206. [Mei M X. 1994. On the central Guizhou“Old Land”. Geology of Guizhou, 11(3): 199-206] [41] 梅冥相,高金汉,李东海,孟庆芬,易定红. 2003. 黔桂地区泥盆系层序地层格架及相对海平面变化. 沉积学报, 21(2): 297-306. [Mei M X,Gao J H,Li D H,Meng Q F,Yi D H. 2003. Devonian sequence stratigraphy and relative sea-level changes in Guizhou and Guangxi area,South China. Acta Sedimentologica Sinica, 21(2): 297-306] [42] 梅冥相,高金汉,易定红,孟庆芬,李东海. 2002. 黔桂地区二叠系层序地层格架及相对海平面变化研究. 高校地质学报, 8(3): 318-333. [Mei M X,Gao J H,Yi D H,Meng Q F,Li D H. 2002. Study on sequence stratigraphic framework and relative sea-level changes of the Permian in Guizhou and Guangxi area,South China. Geological Journal of China Universities, 8(3): 318-333] [43] 梅冥相,马永生,邓军,张海,孟晓庆,陈永红,聂瑞贞,张从. 2005. 上扬子区下古生代界层序地层格架的初步研究. 现代地质, 19(4): 551-562. [Mei M X,Ma Y S,Deng J,Zhang H,Meng X Q,Chen Y H,Nie R Z,Zhang C. 2005. Sequence-stratigraphic framework for the Early Palaeozoic of the Upper-Yangtze region. Geoscience, 19(4): 551-562] [44] 梅冥相,孟庆芬,易定红,李东海. 2004. 黔桂地区石炭系层序地层格架及海平面变化. 地球学报, 25(1): 39-46. [Mei M X,Meng Q F,Yi D H,Li D H. 2004. Devonian sequence stratigraphy and relative sea-level changes in Guizhou and Guangxi area,South China. Acta Geoscientica Sinica, 25(1): 39-46] [45] 孟庆芬,邓军. 2003. 贵州南部二叠系层序地层格架. 现代地质, 17(1): 68-74. [Meng Q F,Deng J. 2003. The Permian sequence-stratigraphic framework in southern Guizhou. Geoscience, 17(1): 68-74] [46] 孟琦,黄恒,颜佳新,陈发垚. 2018. 黔南地区中二叠世碳酸盐台地边缘沉积演化及古海洋意义. 古地理学报, 20(1): 87-103. [Meng Q,Huang H,Yan J X,Chen F Y. 2018. Sedimentary evolution of the Middle Permian carbonate platform margin in southern Guizhou and its palaeo-oceanographic implications. Journal of Palaeogeography(Chinese Edition), 20(1): 87-103] [47] 莫江平,郦今敖. 1991. 黔中铝土矿的成矿环境. 地质与勘探,(11): 12-18. [Mo J P,Li J A. 1991. Metallogenic environment of bauxite in central Guizhou. Geology and Exploration,(11): 12-18] [48] 牛新生,冯常茂,刘进. 2007. 黔中隆起的形成时间及形成机制探讨. 海相油气地质, 12(2): 46-50. [Niu X S,Feng C M,Liu J. 2007. Formation mechanism and time of Qianzhong Uplift. Marine Origin Petroleum Geology, 12(2): 46-50] [49] 潘忠华,葛辰悦,翁申富,陈强,李克庆,朱成林. 2013. 务川县岩风阡铝土矿地质特征及成矿环境研究. 贵州地质, 30(3): 192-197. [Pan Z H,Ge C Y,Weng S F,Chen Q,Li K Q,Zhu C L. 2013. Geological characters and metallogenic environment of Yanfengqian bauxite deposit in Wuchuan. Guizhou Geology, 30(3): 192-197] [50] 郄文昆,张雄华,蔡雄飞,张扬. 2007. 华南地区石炭纪—早二叠世早期成冰期的地球生物学过程与烃源岩的形成. 地球科学—中国地质大学学报, 32(6): 803-810. [Qie W K,Zhang X H,Cai X F,Zhang Y. 2007. Geobiological processes and the formation of hydrocarbon source rocks in the Carboniferous-Early Permian glacial period in South China. Earth Science-Journal of China University of Geosciences, 32(6): 803-810] [51] 郄文昆,张雄华,杜远生,张扬. 2010. 华南地区下石炭亚系碳同位素记录及对晚古生代冰期的响应. 中国科学: 地球科学, 40(11): 1533-1542. [Qie W K,Zhang X H,Du Y S,Zhang Y. 2010. Lower Carboniferous carbon isotope stratigraphy in South China: Implications for the Late Paleozoic glaciation. Science China Earth Sciences, 40(11): 1533-1542] [52] 戎嘉余,陈旭,王怿,詹仁斌,刘建波,黄冰,唐鹏,吴荣昌,王光旭. 2011. 奥陶—志留纪之交黔中古陆的变迁: 证据与启示. 中国科学: 地球科学, 41(10): 1407-1415. [Rong J Y,Chen X,Wang Y,Zhan R B,Liu J B,Huang B,Tang P,Wu R C,Wang G X. 2010. Northward expansion of Central Guizhou Oldland through the Ordovician and Silurian transition: Evidence and implications. Science China Earth Sciences, 41(10): 1407-1415] [53] 沈志达,梅冥相,曾羽. 1990. 贵州太康运动的地层学效应: 兼论“黔中隆起”的形成. 贵州地质, 7(2): 91-97. [Shen Z D,Mei M X,Zeng Y. 1990. The stratigraphic effect of the Taconic Movement in Guizhou-A discussion on the formation of Palaeoland of Central Guizhou. Geology of Guizhou, 7(2): 91-97] [54] 王成善,李祥辉,陈宏德,覃建雄. 1999. 中国南方二叠纪海平面变化及升降事件. 沉积学报, 17(4): 536-541. [Wang C S,Li X H,Chen H D,Qin J X. 1999. Permian sea-level changes and rising-falling events in South China. Acta Sedimentologica Sinica, 17(4): 536-541] [55] 王俊达,李华梅. 1998. 贵州石炭纪古纬度与铝土矿. 地球化学, 27(6): 572-578. [Wang J D,Li H M. 1998. Carboniferous Paleo-Latitude and bauxite deposit of central Guizhou Province. Geochimica, 27(6): 572-578] [56] 翁申富,雷志远,赵爽,冉英,汪小妹,朱成林. 2011. 遵义仙人岩铝土矿赋存富集与古岩溶地貌的关系. 贵州地质, 28(4): 260-264. [W S F,Lei Z Y,Zhao S,Ran Y,Wang X M,Zhu C L. 2011. Relation between richening,preserving and paleokarst landform of Xianrenyan bauxite deposit in Zunyi. Geology of Guizhou, 28(4): 260-264] [57] 武国辉,金中国,鲍淼,毛佐林. 2008. 黔北务正道铝土矿成矿规律探讨. 地质与勘探, 44(6): 31-35. [Wu G H,Jin Z G,Bao M,Mao Z L. 2008. Relation between richening,preserving and paleokarst landform of Xianrenyan bauxite deposit in Zunyi. Geology and Prospecting, 44(6): 31-35] [58] 武思琴,颜佳新,刘柯,严雅娟. 2016. 黔西南二叠纪早期陆源碎屑沉积体系对冈瓦纳冰川发育的响应. 地学前缘, 23(6): 299-311. [Wu S Q,Yan J X,Liu K,Yan Y J. 2016. Response of early Permian silisiclastic depositional system to the advance of Gondwana glaciation in southwestern Guizhou. Earth Science Frontiers, 23(6): 299-311] [59] 严雅娟,颜佳新,武思琴. 2015. 黔南地区早二叠世大幅度冰川性海平面下降的沉积学新证据. 地球科学, 40(2): 372-380. [Yan Y J,Yan J X,Wu S Q. 2015. Sedimentary records of Early Permian major glacial sea-level falls in southern Guizhou Province,China. Earth Science-Journal of China University of Geosciences, 40(2): 372-380] [60] 杨瑞东. 1993. 华南地区石炭纪海平面波动与沉积效应. 云南地质, 12(2): 177-182. [Yang R D. 1993. Sea-level fluctuations and sedimentary effect of Carboniferous in Southern China. Yunnan Geology, 12(2): 177-182] [61] 杨明德. 1989. 黔中铝土矿矿床沉积环境及成矿作用. 矿产地质, 3(13): 27-33. [Yang M D. 1989. Sedimentation environment and mineralization of bauxite deposits in central Guizhou Province. Mineral Resources and Geology, 3(13): 27-33] [62] 尹琼. 2013. 黔中隆起及其周缘奥陶系沉积相研究. 中南大学硕士学位论文: 52-53. [Yin Q. 2013. Ordovician sedimentary facies of Central Guizhou Uplift and its adjacent areas. Masteral dissertation of Central South University: 52-53] [63] 尹赞勋. 1949. 中国南部志留纪地层之分类与对比. 中国地质学会志,29︰1-62. [Yin Z X. 1949. Silurian stratigraphic classification and comparison in South China. The Bulletin of Geological Society of China, 29: 1-62] [64] 殷科华,叶德书,沈大兴,王林,罗本利. 2009. 息烽—遵义早石炭世大唐期岩相古地理特征. 沉积学报, 27(4): 606-613. [Yin K H,Ye D S,Shen D X,Wang L,Luo B L. 2009. Characteristics of lithofacies paleogeography during Datangian Age(Early Carboniferous)in Xifeng and Zunyi,Guizhou. Acta Sedimentologica Sinica, 27(4): 606-613] [65] 余文超,杜远生,顾松竹,崔涛,黄兴,喻建新,覃永军,雷志远,翁申富,曹建州. 2013. 黔北务正道地区早二叠世铝土矿多期淋滤作用及其控矿意义. 地质科技情报, 32(1): 34-39. [Yu W C,Du Y S,Gu S Z,Cui T,Huang X,Yu J X,Qin Y J,Lei Z Y,Weng S F,Cao J Z. 2013. Multiperiod leaching process of Early Permian bauxite in Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province and its significance of ore-control. Geological Science and Technology Information, 32(1): 34-39] [66] 余文超,杜远生,周琦,金中国,汪小妹,覃永军. 2012. 黔北务川—正安—道真地区铝土矿系中生物标志物及其地质意义. 古地理学报, 14(5): 651-662. [Yu W C,Du Y S,Zhou Q,Jin Z G,Wang X M,Qin Y J. 2012. Biomarkers of bauxite-bearing strata and its geological significance in Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province. Journal of Palaeogeography(Chinese Edition), 14(5): 651-662] [67] 余文超,杜远生,周琦,金中国,汪小妹,覃永军,崔滔. 2014. 黔北务正道地区下二叠统铝土矿层物源研究: 来自碎屑锆石年代学的证据. 古地理学报, 16(1): 19-29. [Yu W C,Du Y S,Zhou Q,Jin Z G,Wang X M,Qin Y J,Cui T. 2014. Provenance of bauxite beds of the Lower Permian in Wuchuan-Zheng'an-Daozhen area,northern Guizhou Province: Evidence from detrital zircon chronology. Journal of Palaeogeography(Chinese Edition), 16(1): 19-29] [68] 于鑫,杨江海,刘建中,杜远生,柴嵘. 2017. 黔西南晚二叠世龙潭组物源分析及区域沉积古地理重建. 地质学报, 91(6): 1374-1385. [Yu X,Yang J H,Liu J Z,Du Y S,Chai R. 2017. Provenance of the Late Permian Longtan Formation in SW Guizhou Province and implication for reconstruction of regional sedimentation and paleogeography. Acta Geologica Sinica, 91(6): 1374-1385] [69] 张启明,江新胜,秦建华,崔晓庄,刘才泽. 2012. 黔北—渝南地区中二叠世早期梁山组的岩相古地理特征和铝土矿成矿效应. 地质通报, 31(4): 558-568. [Zhang Q M,Jiang X S,Qin J H,Cui X Z,Liu C Z. 2012. Lithofacies palaeogeography of the early Middle Permian Liangshan Formation in northern Guizhou-southern Chongqing area and its bauxite ore-forming effect. Geological Bulletin of China, 31(4): 558-568] [70] 张莹华,凌文黎,吴慧,张亚男,丁晓英,崔涛,杜远生,雷志远,翁申富. 2013. 黔北铝土矿不同类型矿石地球化学特征及其对成矿作用的指示. 地质科技情报, 32(1): 71-79. [Zhang Y H,Ling W L,Wu H,Zhang Y N,Ding X Y,Cui T,Du Y S,Lei Z Y,Weng S F. 2013. Geochemistry of varied type ores of northern Guizhou bauxites and its implication for mineralization. Geological Science and Technology Information, 32(1): 71-79] [71] 周恳恳. 2015. 中上扬子及其东南缘中奥陶世—早志留世沉积特征与岩相古地理演化. 中国地质科学院博士学位论文: 81-86. [Zhou K K. 2015. Middle Ordovician-Early Silurian lithofacies paleogeography of Middle-Upper Yangtze and its southeastern margin. Doctoral dissertation of Chinese Academy of Geological Sciences: 81-86] [72] 周明辉. 2005. 论“黔中隆起”的形成与演化. 南方油气, 18(2): 6-9. [Zhou M H. 2005. Discussion about the formation and evolution of Central Guizhou Upwarping. Southern China Oil and Gas, 18(2): 6-9] [73] 周希云. 1990. 对“黔中隆起”的几点初步认识. 贵州工业大学学报, 19(1): 84-85. [Zhou X Y. 1990. Tentative knowledge of Central Guizhou Upwarping. Journal of Guizhou Institute of Teghnology, 19(1): 84-85] [74] 朱永红,翁申富,李沛刚,赵爽,韩忠华,陈强,杨时强. 2018. 贵州遵义铝土矿(带)成矿条件及成因分析. 地质科技情报, 37(1): 177-183. [Zhu Y H,Weng S F,Li P G,Zhao S,Han Z H,Chen Q,Yang S Q. 2018. Metallogenic factor and origin in Zunyi bauxite belt,Guizhou. Geological Science and Technology Information, 37(1): 177-183] [75] Bárdossy G,Alev G J J. 1990. Lateritic Bauxites. Amsterdam: Elsevier,1-624. [76] Buggisch W,Joachimski M M,Sevastopulo G,Morrow J R. 2008. Mississippian δ13Ccarb and conodont apatite δ18O records-Their relation to the Late Palaeozoic Glaciation. Palaeogeography,Palaeoclimatology,Palaeoecology, 268(3): 273-292. [77] Buggisch W,Wang X,Alekseev A S,Joachimski M M. 2011. Carboniferous-Permian carbon isotope stratigraphy of successions from China(Yangtze platform),USA(Kansas)and Russia(Moscow Basin and Urals). Palaeogeography,Palaeoclimatology,Palaeoecology, 301: 18-38. [78] Chen B,Joachimski M M,Shen S Z,Lambert L L,Lai X L,Wang X D,Chen J,Yuan D X. 2013. Permian ice volume and palaeoclimate history: Oxygen isotope proxies revisited. Gondwana Research, 24(1): 77-89. [79] Cohen K M,Finney S C,Gibbard P L,Fan J X. 2013. The ICS international chronostratigraphic Chart. Episodes, 36(3): 199-204. [80] Deng X,Yang J,Cawood P A,Wang X C,Du Y S,Huang Y,Lu S F,He B. 2020. Detrital record of late-stage silicic volcanism in the Emeishan large igneous province. Gondwana Research, 79: 197-208. [81] Frakes L A,Francis J E,Syktus J I. 1992. Climate Modes of the Phanerozoic. London: Cambridge University Press, 7-54. [82] Hao X,Leung K,Wang R,Sun W,Li Y. 2010. The geomicrobiology of bauxite deposits. Geoscience Frontiers, 1(1): 81-89. [83] Haq B U,Schutter S R. 2008. A chronology of Paleozoic sea-level changes. Science, 322(5898): 64-68. [84] He B,Xu Y,Chung S,Xiao L,Wang Y. 2003. Sedimentary evidence for a rapid,kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts. Earth and Planetary Science Letters, 213: 391-405. [85] Huang X,Aretz M,Zhang X,Du Y,Qie W,Wen Q,Wang C,Luan T. 2017. Pennsylvanian-early Permian palaeokarst development on the Yangtze Platform,South China,and implications for the regional sea-level history. Geological Journal, 53(4): 1241-1262. [86] Isbell J L,Miller M F,Wolfe K L,Lenaker P A. 2003. Timing of late Paleozoic glaciation in Gondwana: Was glaciation responsible for the development of Northern Hemisphere cyclothems?Geological Society of America Special Paper, 370: 5-24. [87] Koch J T,Frank T D. 2011. The Pennsylvanian-Permian transition in the low-latitude carbonate record and the onset of major Gondwanan glaciation. Palaeogeography,Palaeoclimatology,Palaeoecology,308(3/4): 362-372. [88] Kofukuda D,Isozaki Y,Igo H. 2014. A remarkable sea-level drop and relevant biotic responses across the Guadalupian-Lopingian(Permian)boundary in low-latitude mid-Panthalassa: Irreversible changes recorded in accreted paleo-atoll limestones in Akasaka and Ishiyama,Japan. Journal of Asian Earth Sciences, 82: 47-65. [89] Li P,Yu W,Du Y,Lai X,Weng S,Pang D,Xiong G,Lei Z,Zhao S,Yang S. 2020. Influence of geomorphology and leaching on the formation of Permian bauxite in northern Guizhou Province,South China. Journal of Geochemical Exploration, 210: 106446. [90] Ling K Y,Zhu X Q,Tang H S,Li S X. 2017. Importance of hydrogeological conditions during formation of the karstic bauxite deposits,Central Guizhou Province,Southwest China: A case study at Lindai deposit. Ore Geology Reviews, 82: 198-216. [91] Liu C,Jarochowska E,Du Y,Vachard D,Munnecke A. 2017. Stratigraphical and δ13C records of Permo-Carboniferous platform carbonates,South China: Responses to late Paleozoic icehouse climate and icehouse-greenhouse transition. Palaeogeography,Palaeoclimatology,Palaeoecology, 474: 113-129. [92] Nicholls R J,Cazenave A. 2010. Sea-level rise and its impact on coastal zones. Science, 328(5985): 1517-1520. [93] Poulsen C J,Pollard D,Montañez I P,Rowley D. 2007. Late Paleozoic tropical climate response to Gondwanan deglaciation. Geology, 35(9): 771-774. [94] Price G D,Valdes P J,Sellwood B D. 1997. Prediction of modern bauxite occurrence: Implications for climate reconstruction. Palaeogeography,Palaeoclimatology,Palaeoecology, 131(1-2): 1-13. [95] Retallack G J. 2008. Cool-Climate or Warm-Spike lateritic bauxites at high latitudes?The Journal of Geology, 116(6): 558-570. [96] Rotzoll K,Fletcher C H. 2012. Assessment of ground water inundation as a consequence of sea-level rise. Nature Climate Change, 3(5): 477-481. [97] Shi G R,Waterhouse J. 2010. Late Palaeozoic global changes affecting high-latitude environments and biotas: An introduction. Palaeogeography,Palaeoclimatology,Palaeoecology, 298(1): 1-16. [98] Ueno K,Hayakawa N,Nakazawa T,Wang Y,Wang X. 2013. Pennsylvanian-Early Permian cyclothemic succession on the Yangtze Carbonate Platform,South China. Geological Society,London,Special Publications, 376(1): 235-267. [99] Wang X,Qie W,Sheng Q,Qi Y,Wang Y,Liao Z,Shen S Z,Ueno K. 2013. Carboniferous and Lower Permian sedimentological cycles and biotic events of South China. Geological Society,London,Special Publications, 376(1): 33-46. [100] Weng S,Yu W,Algeo T J,Du Y,Li P,Lei Z,Zhao S. 2019. Giant bauxite deposits of South China: Multistage formation linked to Late Paleozoic Ice Age(LPIA)eustatic fluctuations. Ore Geology Reviews, 104: 1-13. [101] Yang J,Cawood P A,Du Y. 2015. Voluminous silicic eruptions during late Permian Emeishan igneous province and link to climate cooling. Earth and Planetary Science Letters, 432: 166-175. [102] Yu W,Algeo T J,Yan J,Yang J,Du Y,Huang X,Weng S. 2019. Climatic and hydrologic controls on upper Paleozoic bauxite deposits in South China. Earth-Science Reviews, 189: 159-176. [103] Zhu R,Yang Z,Wu H,Ma X,Huang B,Meng Z,Fang D. 1998. Paleomagnetic constraints on the tectonic history of the major blocks of China duing the Phanerozoic. Science China(Series D),41(S2): 1-19.
