Nanhuan (Cryogenian) Stratigraphic Sequence in Central-south China and Its Response for Major Geological Events
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摘要: 罗迪尼亚超大陆裂解、雪球地球、锰铁成矿作用耦合是南华纪重大地质事件。中南地区南华纪地层广泛分布，自北而南沉积类型丰富，本文以冰期沉积、锰矿层和铁矿层为标志，以同位素年龄为格架，厘定了南华纪岩石地层和年代地层序列，自北而南对比了超大陆裂解事件、斯图特冰期、马里诺冰期、成锰事件、成铁事件、火山事件和早期生命演化事件沉积的差异性。本文认为中南地区南华系表现为两次冰期和一次间冰期的沉积特征，下铁上锰、南铁北锰的时空格局揭示了裂谷的演化历程。建议进一步聚焦南华系存在的关键地质问题，加强锰铁成矿作用与全球重大地质事件的响应关系调查研究，为新一轮找矿突破战略行动提供理论支撑。Abstract: Breakup of the Rodinia Supercontinent, the Snowball Earth and manganese and iron mineralization coupling have been significant geological events during the Nanhuan (Cryogenian). The Nanhuan strata has been widely distributed in Central-south China, with variety sedimentation types being gradual transition from south to north. This review redefines the Nanhuan lithostratigraphy and chronostratigraphy sequence in Central-south China in the framework of regional glacial deposits, manganese deposits, iron deposits and isotopic ages. Regional geological events including breakup, Sturtian and Marinoan, manganization and iron-forming, volcanism activity, and early life evolution have been compared from north to south, focusing on the differences. This paper approved two glaciations with one interglaciation sedimentation preserved in Central-south China. And rifting evolution could be revealed by temporal and spatial distribution of iron and manganese. Further geological survey could be aimed at relationship between regional manganese-iron mineralization and global geological events to provide basic geological supports for the Prospecting Breakthrough Strategy Action.
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Key words:
- Nanhuan /
- Snowball Earth /
- manganese deposit /
- iron ore bed /
- supercontinent breakup
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[1] 安志辉,叶琴,胡军,童金南,田力.2021.神农架成冰纪宋洛生物群的赋存层位厘定[J/OL].地球科学.https://kns.cnki.net/kcms/detail/42.1874.P.20211125.1908.016.html
[2] 柏道远,陈迪,凌跃新,吴能杰,李彬,李银敏,杨俊.2021.湖南常德-安仁断裂及其控岩控矿特征[M].武汉:中国地质大学出版社.
[3] 蔡娟娟,崔晓庄,兰中伍,王剑,江卓斐,邓奇,卓皆文,陈风霖,江新胜.2018.华南扬子陆块成冰纪冰川作用的启动时限及其全球对比[J].古地理学报,20(1):65-86.
[4] 蔡志勇,罗洪,熊小林,吴德宽,吴贤亮,孙三才,杨军.2006.武当群上部变沉积岩组时代归属问题:单锆石U-Pb 年龄的制约[J].地层学杂志,30(1):60-63.
[5] 蔡志勇,熊小林,罗洪,吴德宽,孙三才,饶帮良,王寿琼.2007.武当地块耀岭河群火山岩的时代归属:单锆石U-Pb 年龄的制约[J].地质学报,81(5):620-625.
[6] 陈旭, 李朗田, 丛源, 曹景良, 黄飞, 雷玉龙, 肖德长, 李连支.2021.湘中地区成锰盆地内部聚锰槽盆结构初探[J].资源环境与工程,35(5):580-586.
[7] 陈建书,戴传固,彭成龙,王敏,卢定彪,王雪华,骆珊.2016.湘黔桂相邻区新元古代820~635 Ma 时期裂谷盆地充填序列与地层格架[J].中国地质,43(3):899-920.
[8] 邓乾忠,杨青雄,毛新武,孔令耀.2016.湖北武当—随枣地区中—晚南华世岩石地层序列与年代学研究[J].资源环境与工程,30(2):132-142.
[9] 杜秋定,汪正江,王剑,卓皆文,谢尚克,邓奇,杨菲.2013.湘中长安组碎屑锆石LA-ICP-MSU-Pb 年龄及其地质意义[J].地质论评,59(2):334-344.
[10] 杜远生,周琦,余文超,王萍,袁良军,齐靓,郭华,徐源.2015.Rodinia 超大陆裂解、Sturtian冰期事件和扬子地块东南缘大规模锰成矿作用[J].地质科技情报,34(6):1-7.
[11] 福建省地质调查研究院.2016.福建1∶5 万长汀县、南岩、策田、濯田幅区域地质调查报告[R].
[12] 福建省地质调查研究院.2017.中国区域地质志·福建志[M].北京:地质出版社.
[13] 付勇,郭川.2021.南华盆地新元古代成冰纪成锰作用及其成矿背景[J].地质论评,67(4):973-991.
[14] 付胜云,谢小青.2010.湘西及邻区早震旦世锰矿成矿规律探讨[J].中国锰业,28(3):30-33.
[15] 高林志,尹崇玉,丁孝忠,王泽九,张恒.2015.华南地区新元古代年代地层标定及地层对比[J]. 地球学报,36(5):533-545.
[16] 广东省地质矿产局.1996.广东省岩石地层[M].武汉:中国地质大学出版社.
[17] 广西壮族自治区区域地质调查院.2016.广西1∶5 万水口、林溪、龙额乡、良口幅区域地质调查报告[R].
[18] 海南省地质调查院.2017.中国区域地质志·海南志[M].北京:地质出版社.
[19] 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[J].地球科学——中国地质大学学报,39(8):929-953.
[20] 湖北省地质矿产局.1996.湖北省岩石地层[M].武汉:中国地质大学出版社.
[21] 湖北省地质调查院.2021.中国区域地质志·湖北志[M].北京:地质出版社.
[22] 湖南省地质矿产局.1997.湖南省岩石地层[M].武汉:中国地质大学出版社.
[23] 湖南省地质调查院.2013.湖南1∶25 万武冈幅、怀化幅区域地质调查报告[R].
[24] 湖南省地质调查院.2017.中国区域地质志·湖南志[M].北京:地质出版社.
[25] 江西省地质矿产勘查开发局.2017.中国区域地质志·江西志[M].北京:地质出版社.
[26] 旷红伟,柳永清,耿元生,白华青,彭楠,范正秀,宋换新,夏晓旭,王玉冲,陈骁帅.2019.中国中新元古代重要沉积地质事件及其意义[J].古地理学报,21(1):1-30.
[27] 兰中伍.2023.华南南华系年代地层学研究进展[J].沉积与特提斯地质,43(1):180-187.
[28] 李聪,陈世悦,张鹏飞,张跃,王玲,毕明威.2010.华南加里东期陆内构造属性探讨[J].中国石油大学学报(自然科学版),34(5):18-24.
[29] 李明龙,田景春,方喜林,郑德顺,许克元,陈林,曹文胜,赵军,冉中夏.2019.鄂西走马地区大塘坡组顶部泥岩碎屑锆石LA-ICP-MS U-Pb 年龄及其地质意义[J].沉积与特提斯地质,39(1):22-31.
[30] 林树基,卢定彪,肖加飞,熊小辉,李艳桃.2013.贵州南华纪冰期地层的主要特征[J].地层学杂志,37(4):542-557.
[31] 凌文黎,段瑞春,柳小明,程建萍,毛新武,彭练红,刘早学,杨红梅,任邦方,2010.南秦岭武当山群碎屑锆石U-Pb年代学及其地质意义[J].科学通报,55(12):1153-1161.
[32] 刘浩, 徐扬, 张维峰, 徐大良, 魏运许, 邓新, 金鑫镖, 彭练红.2023.西大别红安岩群含磷岩系的形成时代及物源分析[J].华南地质,39(2):278-291.
[33] 刘鸿允,郝杰,李曰俊.1999.中国中东部晚前寒武纪地层与地质演化[M].北京:科学出版社.
[34] 卢定彪,张德明,吴开彬,跃连红,黄文俊.2018.华南新元古代南华大冰期气候岩石地层对比[J].中国科技论文,13(9):1060-1067.
[35] 马国干,李华芹,张自超.1984.华南地区震旦纪时限范围的研究[J].中国地质科学院宜昌地质矿产研究所所刊,8:1-29.
[36] 马晓辉,刘阳,张向宁,李艳翔,张雪,任良良,赵亮亮.2022.湘西南大岩坳向斜“大塘坡式”锰矿成矿地质条件及成矿预测[J].华南地质,38(3):521-532.
[37] 牛志军,邓新,刘浩,李福林,宋芳,何垚砚,杨文强.2022.扬子陆块南北缘新元古代火山-沉积岩系研究现状与问题[J].华南地质,38(1):27-45.
[38] 牛志军,杨文强,宋芳,何垚砚,田洋.2020.湘桂地区新元古代地层序列物源分析构造演化[M].北京:科学出版社.
[39] 潘桂棠,陆松年,肖庆辉,张克信,尹福光,郝国杰,骆满生,任飞,袁四化.2016.中国大地构造阶段划分和演化[J].地学前缘,23(6):1-23.
[40] 彭学军,刘耀荣,吴能杰,陈建超,李建清.2004.扬子陆块东南缘南华纪地层对比[J].地层学杂志,28(4):354-359.
[41] 舒良树,陈祥云,楼法生.2020.华南前侏罗纪构造[J].地质学报,94(2):333-360.
[42] 宋芳,牛志军,刘浩,何垚砚,杨文强.2016.鄂东南地区南华系沉积特征与接触关系:扬子陆块内部与东南缘盆地对比的良好借鉴[J].地层学杂志,40(3):251-260．
[43] 孙海清,黄建中,杜远生,罗来,伍皓.2014.扬子地块东南缘南华系长安组同位素年龄及其意义[J].地质科技情报,33(2):15-20+27.
[44] 汤加富,符鹤琴,余志庆.1987.华南晚前寒武纪硅铁建造的层位、类型与形成条件[J].矿床地质,6(1):1-10.
[45] 唐晓珊,黄建中,张纯臣.1994.华南地体北缘(湖南部分)前寒武纪地层[J].中国区域地质,(4):303-310.
[46] 王剑,段太忠,谢渊,汪正江,郝明,刘伟.2012.扬子地块东南缘大地构造演化及其油气地质意义[J].地质通报,31(11):1739-1749.
[47] 王寿琼,周骏华,胡文虎.1989.湖北武当地区耀岭河群火山-冰川沉积及其地层意义[J].地层学杂志,13(1):14-21+81.
[48] 吴定金,龚光林,雷玉龙,曹景良.2020.扬子陆块东南缘早南华世大塘坡早期岩相古地理及锰矿床地质意义[J].中国锰业,38(2):6-12.
[49] 吴年文,江拓,徐琼,赵小明,赵龙,邱啸飞.2021.南秦岭随枣地块耀岭河组双峰式火山岩:对扬子克拉通北缘大陆裂解过程的约束[J].地质通报,40(6):920-929.
[50] 伍皓, 江新胜, 王剑, 汪正江, 杜秋定, 邓奇, 崔晓庄, 杨菲.2015.湘西托口地区南华系沉积地层学研究及其地质意义[J].地层学杂志,39(3):300-309.
[51] 武汉地质调查中心.2019a.湖北1∶5 万十堰市、吕家河、薛家村、土城幅区域地质调查报告[R].
[52] 武汉地质调查中心.2019b.1∶5 万郭镇市、白羊田、北港镇区域地质调查报告[R].
[53] 徐鹏,李欢,谢家涛,王球.2022.鄂西北地区海相火山岩型铁矿成矿规律及找矿方向[J].矿产勘查,13(5):548-566.
[54] 闫斌,朱祥坤,唐索寒,朱茂炎.2010.广西新元古代BIF 的铁同位素特征及其地质意义[J]. 地质学报,84(7):1080-1086.
[55] 杨明桂,王光辉.2020.华南新元古代晚期地层层序与南华间冰期—冰后期大规模沉积成矿作用[J].华东地质,41(3):197-208.
[56] 杨彦均,魏绪寿,陈文斌,张立志,侯东南,赵德星,朱鸿.1984.
[57] 湖南省石门县杨家坪上前寒武系剖面研究[J].湖南地质,3(4):1-96.
[58] 尹崇玉,高林志,刘鹏举,唐烽,王自强,陈寿铭.2015.中国新元古代生物地层序列与年代地层划分[M].北京:科学出版社.
[59] 余文超,杜远生,周琦,王萍,袁良军,徐源,潘文,谢小峰,齐靓,焦良轩.2016.黔东松桃地区大塘坡组LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质论评,62(3):539-549.
[60] 余志庆,汤家富,符鹤琴.1989“. 新余式”铁矿地质特征及其成因[J].矿床地质,8(4):1-10.
[61] 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[J].中国科学:地球科学,43(10):1553-1582.
[62] 张开毕,陈金良,林亨才,黄昌旗,罗志兴.2005.闽西南地区南华纪—震旦纪岩石地层的划分与对比[J].中国地质,32(3):363-369.
[63] 张克信,何卫红,徐亚东,翟刚毅,石万忠,陆永潮.2023.华南青白口纪—三叠纪构造-地层区划及特征[J].华南地质,39(1):1-23.
[64] 张启锐,储雪蕾.2006.扬子地区江口冰期地层的划分对比与南华系层型剖面[J].地层学杂志,30(4):306-314.
[65] 张启锐,黄晶,储雪蕾.2012.湖南怀化新路河地区的南华系[J].地层学杂志,36(4):761-763.
[66] 赵小明,张开明,毛新武,马铁球,黄友义,莫位仁,吴年文,王汉荣.2015.中南地区大地构造相特征与成矿地质背景研究[M].武汉:湖北人民出版社.
[67] 赵彦彦,郑永飞.2011.全球新元古代冰期的记录和时限[J].岩石学报,27(2):545-565.
[68] 中国冶金地质总局湖南地质勘查院.2018.扬子陆块东南缘南华系锰矿成矿预测与选区报告[R].
[69] 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[J].地球科学,41(2):177-188.
[70] 周传明.2016.扬子区新元古代前震旦纪地层对比[J].地层学杂志,40(2):120-135.
[71] Bao X J, Zhang S H, Jiang G Q, Wu H C, Li H Y, Wang X Q, An Z Z, Yang T S. 2018. Cyclostratigraphic constraints on the duration of the Datangpo Formation and the onset age of the Nantuo (Marinoan) glaciation in South China[J]. Earth and Planetary Science Letters, 483: 52-63.
[72] Cawood P A, Zhao G C, Yao J L, Wang W, Xu Y J, Wang Y J. 2018. Reconstructing South China in Phanerozoic and Precambrian supercontinents[J]. Earth-Science Reviews, 186(1): 173-194.
[73] Charvet J, Shu L S, Faure M, Choulet F, Wang B, Lu H F, Breton N L. 2010. Structural development of the Lower Paleozoic belt of South China: Genesis of an intracontinental orogen[J]. Journal of Asian Earth Science, 39(4): 309-330.
[74] Dong Y P, Liu X M, Santosh M, Zhang X N, Chen Q, Yang C, Yang Z. 2011. Neoproterozoic subduction tectonics of the northwestern Yangtze Block in South China: Constrains from zircon U-Pb geochronology and geochemistry of mafic intrusions in the Hannan Massif [J]. Precambrian Research, 189(1-2): 66-90.
[75] Du Q D, Wang Z J, Wang J, Qiu Y S, Jiang X S, Deng Q, Yang F. 2013. Geochronology and paleoenvironment of the pre-Sturtian glacial strata: Evidence from the Liantuo Formation in the Nanhua rift basin of the Yangtze Block, South China[J]. Precambrian Research, 233(3): 118-131.
[76] Faure M, Shu L S, Wang B, Charvet J, Choulet F, Monié P. 2009. Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China[J]. Terra Nova, 21(5): 360-368.
[77] Hoffman P F, Kaufman A J, Halverson G P, Schrag D P. 1998. A Neoproterozoic Snowball Earth[J]. Science, 281(5381): 1342-1346.
[78] Lan Z W, Huyskens M H, Le Hir G, Mitchell R N, Yin Q Z, Zhang G Y, Li X H. 2022. Massive volcanism may have foreshortened the Marinoan Snowball Earth [J]. Geophysical Research Letters, 49, e2021GL097156.
[79] Lan Z W, Li X H, Zhu M Y, Zhang Q R, Li Q L. 2015. Revisiting the Liantuo Formation in Yangtze Block, South China: SIMS U-Pb zircon age constraints and regional and global significance[J]. Precambrian Research, 263: 123-141.
[80] Li X H, Li Z X, Li W X. 2014. Detrital zircon U-Pb age and Hf isotope constrains on the generation and reworking of Precambrian continental crust in the Cathaysia Block, South China: A synthesis[J]. Gondwana Research, 25(3): 1202-1215.
[81] Li Z X, Li X H, Kinny P D, Wang J, Zhang S, Zhou H. 2003. Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China and correlations with other continents, evidence for a mantle superplume that broke up Rodinia[J]. Precambrian Research, 122(1-4): 85-109.
[82] Lin S F, Xing G F, Davis D W, Yin C Q, Wu M L, Li L M, Jiang Y, Chen Z H. 2018. Appalachian-style multi-terrane Wilson cycle model for the assembly of South China[J]. Geology, 46(4): 319-322.
[83] Ling W L, Ren B F, Duan R C, Liu X M, Mao X W, Peng L H, Liu Z X, Cheng J P, Yang H M. 2008. Timing of the Wudangshan, Yaolinghe volcanic sequences and mafic sills in South Qinling: U-Pb zircon geochronology and tectonic implication[J]. Chinese Science Bulletin, 53(14): 2192-2199.
[84] Liu H, Zhao J H, Cawood P A, Wang W. 2018. South China in Rodinia: Constrains from the Neoproterozoic Suixian volcano-sedimentary group of the South Qinling Belt[J]. Precambrian Research, 314: 170-193.
[85] Liu P J, Li X H, Chen S M, Lan Z W, Yang B, Shang X D, Yin C Y. 2015. New SIMS U-Pb zircon age and its constraint on the beginning of the Nantuo glaciation[J]. Science Bulletin, 60(10): 958-963.
[86] MacDonald F A, Schmitz M D, Crowley J L, Roots C F, Jones D S, Maloof A C, Strauss J V, Cohen P A, Johnston D T, Schrag D P. 2010. Calibrating the Cryogenian[J]. Sciences, 327(5970): 1241-1243.
[87] Qi L, Cawood P A, Xu Y J, Du Y S, Zhang H C, Zhang Z K. 2020. Linking South China to North India from the late Tonian to Ediacaran: Constraints from the Cathaysia Block[J]. Precambrian Research, 350: 105898.
[88] Qi L, Xu Y J, Cawood P A, Du Y S. 2018. Reconstructing Cryogenian to Ediacaran successions and paleogeography of the South China Block[J]. Precambrian Research, 314: 452-467.
[89] Qiu W J, Zhou M F, Li X C, Williams-Jones A E, Yuan H L. 2018. The genesis of the Giant Dajiangping SEDEX-type pyrite deposit, South China[J]. Economic Geology, 113(6): 1419-1446.
[90] Shu L S, Yao J L, Wang B, Faure M, Charvet J, Chen Y. 2021. Neoproterozoic plate tectonic process and Phanerozoic geodynamic evolution of the South China Block[J]. Earth-Science Reviews, 216: 103596.
[91] Song H Y, An Z H, Ye Q, Stüeken E E, Li J, Hu J, Algeo T J, Tian L, Chu D L, Song H J, Xiao S H, Tong J N, 2023. Mid-latitudinal habitable environment for marine eukaryotes during the waning stage of the Marinoan snowball glaciation[J]. Nature Communications, 14(1):1-9.
[92] Wang J, Li Z X. 2003. History of Neoproterozoic rift basins in South China: Implications for Rodinia break-up[J]. Precambrian Research, 122(1-4): 141-158.
[93] Wang W, Zeng M F, Zhou M F, Zhao J H, Zheng J P, Lan Z F. 2018. Age, provenance and tectonic setting of Neoproterozoic to early Paleozoic sequences in southeastern South China Block: Constraints on its linkage to western Australia-East Antarctica[J]. Precambrian Research, 309: 290-308.
[94] Yang F L, Zhou X F, Peng Y X, Song B W, Kou X H. 2020. Evolution of Neoproterozoic basins within the Yangtze Craton and its significance for oil and gas exploration in South China: An overview[J]. Precambrian Research, 337, 105563.
[95] Yao J L, Shu L S, Santosh M. 2011. Detrital zircon U-Pb geochronology, Hf-isotopes and geochemistry—New clues for the Precambrian crustal evolution of Cathaysia Block, South China[J]. Gondwana Research, 20(2-3): 553-567.
[96] Yao W H, Li Z X, Li W X, Li X H, Yang J H. 2014. From Rodinia to Gondwanaland: A tale of detrital zircon provenance analyses from the southern Nanhua Basin, South China[J]. American Journal of Science, 314(1): 278-313.
[97] Ye Q, Tong J N, Xiao S H, Zhu S X, An Z H, Tian L, Hu J. 2015. The survival of benthic macroscopic phototrophs on a Neoproterozoic snowball Earth[J]. Geology, 43(6): 507-510.
[98] Zhang Q R, Li X H, Feng L J, Huang J, Song B. 2008. A new age constraint on the onset of the Neoproterozoic glaciations in the Yangtze platform, South China[J]. Journal of Geology, 116(4): 423-429.
[99] Zhang S H, Jiang G Q, Han Y G. 2008. The age of the Nantuo Formation and Nantuo glaciation in South China[J]. Terra Nova, 20(4): 289-294.
[100] Zhang Y Y, Luo T Y, Gan T, Zhou M Z, Han X Q. 2021. Early Silurian Wuchuan-Sihui-Shaoguan exhalative sedimentary pyrite belt, South China: constraints from zircon dating for K-bentonite of the giant Dajiangping deposit[J]. Acta Geochimica, 40(1): 1-12.
[101] Zhou C M, Tucker R, Xiao S H, Peng Z X, Yuan X L, Chen Z. 2004. New constraints on the ages of Neoproterozoic glaciations in South China[J]. Geology, 32(5): 437-440.
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