湘鄂西下寒武统牛蹄塘组黑色页岩发育特征及沉积环境

doi:10.12108/yxyqc.20230410

Lithologic Reservoirs ›› 2023, Vol. 35 ›› Issue (4): 102-114.doi: 10.12108/yxyqc.20230410

• PETROLEUM EXPLORATION • Previous Articles Next Articles

Development characteristics and sedimentary environment of black shale of Lower Cambrian Niutitang Formation in western Hunan and Hubei

LIANG Xiaocong¹, NIU Xing¹, HU Mingyi¹, LI Yang², HU Zhonggui¹, CAI Quansheng¹

1. School of Geosciences, Yangtze University, Wuhan 430100, China;
2. Research Institute of Exploration and Development, PetroChina Southwest Oil and Gas Field Company, Chengdu 610000, China

Received:2022-08-31 Revised:2022-09-15 Online:2023-07-01 Published:2023-07-01

Abstract

Abstract: The Lower Cambrian Niutitang Formation in the western Hunan and Hubei is an important target for shale gas exploration in southern China. Two profiles，Guchengcun in western Hubei and Yanwutan in western Hunan，were selected to carry out petrological and geochemical analysis of the black shale series of Lower Cambrian Niutitang Formation，so as to find out the provenance and tectonic background of the black shale，and analyze the sedimentary environment. The results show that：（1）The black shale deposits of Niutitang Formation in the two profiles are obviously different. The shale of Niutitang Formation in Guchengcun profile is mainly argillaceous shale with small thickness，and a small amount of siliceous shale is developed at the bottom，while the shale of Niutitang Formation in Yanwutan profile is mainly siliceous shale with large thickness，and the bottom is rich in silicophosphorous nodules，nickel，cobalt，vanadium and other metals. The quartz content of Yanwutan profile is much higher than that of Guchengcun profile，and pyrite is also more abundant.（2）There are obvious differences in the sedimentary environment，provenance background and tectonic background between the black rock series in the two profiles. The provenance of Guchengcun profile is mainly felsic igneous rocks and quartz sedimentary rocks，which were deposited in a weak reduction and weak oxidation environment on the continental shelf of the passive continental margin. The provenance of Yanwutan profile is mainly felsic igneous rocks， quartzitic sedimentary rocks and continental tholeiites， and with the input of hydrothermal provenance， it was deposited in a reducing environment on the continental slope of the passive continental margin.（3）In the Early Cambrian，the sediments of Hefeng Guchengcun in western Hubei were mainly black carbonaceous shale and limestone，with low contents of organic matters and silica，the water body was relatively shallow，and it was obviously affected by sea level fluctuations，so it was a shelf environment. However，the sedimentary thickness in western Hunan was large，with high content of organic matters，and it was close to deep faults，the source of hydrothermal silicon was abundant， which is a continental slope environment.

Key words: shelf, continental slope, geochemistry, hydrothermal silicon, black shale, Niutitang Formation, Lower Cambrian, Guchengcun profile, Yanwutan profile, western Hunan and Hubei

CLC Number:

TE121.1

LIANG Xiaocong, NIU Xing, HU Mingyi, LI Yang, HU Zhonggui, CAI Quansheng. Development characteristics and sedimentary environment of black shale of Lower Cambrian Niutitang Formation in western Hunan and Hubei[J].Lithologic Reservoirs, 2023, 35(4): 102-114.

References

[1] 李娟,于炳松,郭峰.黔北地区下寒武统底部黑色页岩沉积环境条件与源区构造背景分析[J].沉积学报, 2013, 31(1):20-31. LI Juan, YU Bingsong, GUO Feng. Depositional setting and tectonic background analysis on Lower Cambrian black shales in the north of Guizhou province[J]. Acta Sedimentologica Sinica, 2013, 31(1):20-31.
[2] 刘炳辰,齐永安,代明月,等.寒武纪生物大爆发之后的底栖生态系统工程建造者:以河南地区为例[J].地球科学, 2021, 46(1):148-161. LIU Bingchen, QI Yongan, DAI Mingyue, et al. Benthic ecosystem engineer after the Cambrian explosion:An example from Henan province[J]. Earth Science, 2021, 46(1):148-161.
[3] 余江浩,王登,王亿,等.湖北西部上二叠统大隆组页岩气资源潜力评价[J].岩性油气藏, 2018, 30(4):84-90. YU Jianghao, WANG Deng, WANG Yi, et al. Evaluation of shale gas resource potential of Late Permian Dalong Formation in western Hubei province[J]. Lithologic Reservoirs, 2018, 30(4):84-90.
[4] 徐祖新,韩淑敏,王启超.中扬子地区陡山沱组页岩储层中黄铁矿特征及其油气意义[J].岩性油气藏, 2015, 27(2):31-37. XU Zuxin, HAN Shumin, WANG Qichao. Characteristics of pyrite and its hydrocarbon of shale reservoir of Doushantuo Formation in Middle Yangtze area[J]. Lithologic Reservoirs, 2015, 27(2):31-37.
[5] 徐增连,张博,里宏亮,等.松辽盆地开鲁坳陷钱家店地区姚家组砂岩地球化学特征及物源和构造背景分析[J].矿物岩石地球化学通报, 2019, 38(3):572-586. XU Zenglian, ZHANG Bo, LI Hongliang, et al. Geochemistry of the Yaojia Formation sandstone in the Kailu Depression, Songliao Basin:Implications for its provenance and tectonic setting[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2019, 38(3):572-586.
[6] 王登,周豹,冷双梁,等.鄂西咸丰地区五峰组-龙马溪组硅质岩地球化学特征及地质意义[J].岩性油气藏, 2022, 34(1):52-62. WANG Deng, ZHOU Bao, LENG Shuangliang, et al. Geochemical characteristics and geological significance of siliceous rocks of Wufeng Formation-Longmaxi Formation in Xianfeng area, western Hubei[J]. Lithologic Reservoirs, 2022, 34(1):52-62.
[7] 谢环羽,姜在兴,王培玺,等.中-上扬子地区寒武系层序地层格架[J].石油学报, 2021, 42(7):865-884. XIE Huanyu, JIANG Zaixing, WANG Peixi, et al. Cambrian sequence stratigraphic framework in the Middle-Upper Yangtze area[J]. Acta Petrologica Sinica, 2021, 42(7):865-884.
[8] 赵建华,金之钧,林畅松,等.上扬子地区下寒武统筇竹寺组页岩沉积环境[J].石油与天然气地质, 2019, 40(4):701-715. ZHAO Jianhua, JIN Zhijun, LIN Changsong, et al. Sedimentary environment of the Lower Cambrian Qiongzhusi Formation shale in the Upper Yangtze region[J]. Oil&Gas Geology, 2019, 40(4):701-715.
[9] 刘忠宝,高波,冯动军,等.上扬子地区下寒武统黑色页岩矿物组成特征及其油气勘探意义[J].天然气工业, 2017, 37(4):21-26. LIU Zhongbao, GAO Bo, FENG Dongjun, et al. Mineral composition of the Lower Cambrian black shale in the Upper Yangtze region and its significance in oil and gas exploration[J]. Natural Gas Industry, 2017, 37(4):21-26.
[10] AWAN R S, LIU Chenglin, GONG Hongwei, et al. Paleo-sedimentary environment in relation to enrichment of organic matter of Early Cambrian black rocks of Niutitang Formation from Xiangxi area China[J]. Marine and Petroleum Geology, 2020, 112(C):104057-104057.
[11] 吴育平,刘成林,龚宏伟,等.湘西下寒武统牛蹄塘组地球化学特征及其对沉积-构造环境的响应[J].地质与勘探, 2021, 57(5):1065-1076. WU Yuping, LIU Chenglin, GONG Hongwei, et al. Geochemical characteristics and sedimentary tectonic setting of Lower Cambrian Niutitang Formation in western Hunan province[J]. Geology and Exploration, 2021, 57(5):1065-1076.
[12] 张国涛,陈孝红,王保忠,等.雪峰山地区震旦系-寒武系之交黑色岩系地球化学特征:物源、气候与构造背景[J].矿物岩石地球化学通报, 2022, 41(2):414-428. ZHANG Guotao, CHEN Xiaohong, WANG Baozhong, et al. Geochemical characteristics of black rock series in the transition zone between Sinian and Cambrian in the Xuefengshan area:Implications for their provenance, paleoclimate and tectonic setting[J]. Bulletin of Mineralogy Petrology and Geochemistry, 2022, 41(2):414-428.
[13] PI Daohui, LIU Congqiang, GRAHAM A, et al. Trace and rare earth element geochemistry of black shale and kerogen in the early Cambrian Niutitang Formation in Guizhou province, South China:Constraints for redox environments and origin of metal enrichments[J]. Precambrian Research, 2013, 225:218-229.
[14] FAN Haifeng, WEN Hanjie, ZHU Xiangkun, et al. Hydrothermal activity during Ediacaran-Cambrian transition:Silicon isotopic evidence[J]. Precambrian Research, 2013, 224:23-35.
[15] 李海,陈孝红,彭中勤,等.湘鄂西地区下寒武统牛蹄塘组页岩气储层特征[J].地质学报, 2022, 96(4):1421-1433. LI Hai, CHEN Xiaohong, PENG Zhongqin, et al. Shale gas reservoir characteristics of the Lower Cambrian Niutitang Formation in the western Hunan and Hubei areas[J]. Acta Geologica Sinica, 2022, 96(4):1421-1433.
[16] 李红敬,林正良,解习农.下扬子地区古生界硅岩地球化学特征及成因[J].岩性油气藏, 2015, 27(5):232-239. LI Hongjing, LIN Zhengliang, XIE Xinong. Geochemical characteristics and origin of Paleozoic siliceous rocks in Lower Yangtze area[J]. Lithologic Reservoirs, 2015, 27(5):232-239.
[17] 陈玉明,高星星,盛贤才.湘鄂西地区构造演化特征及成因机理分析[J].石油地球物理勘探, 2013, 48(增刊1):157-162. CHEN Yuming, GAO Xingxing, SHENG Xiancai. Tectonic evolution characteristics and mechanism in western Hunan-Hubei[J]. Oil Geophysical Prospecting, 2013, 48(Suppl 1):157-162.
[18] 张琳婷,郭建华,焦鹏,等.湘西北地区牛蹄塘组页岩气有利地质条件及成藏区带优选[J].中南大学学报(自然科学版), 2015, 46(5):1715-1722. ZHANG Linting, GUO Jianhua, JIAO Peng, et al. Geological conditions and favorable exploration zones of shale gas in Niutitang Formation at northwest Hunan[J]. Journal of Central South University (Science and Technology), 2015, 46(5):1715-1722.
[19] 黄俨然,杨荣丰,肖正辉,等.湘西北下寒武统牛蹄塘组页岩含气性影响因素分析[J].岩性油气藏, 2015, 27(4):11-16. HUANG Yanran, YANG Rongfeng, XIAO Zhenghui, et al. Influencing factors of shale gas-bearing property of Lower Cambrian Niutitang Formation in northwestern Hunan[J]. Lithologic Reservoirs, 2015, 27(4):11-16.
[20] 胡忠贵,秦鹏,胡明毅,等.湘鄂西地区下寒武统水井沱组页岩储层分布及非均质性特征[J].中国石油勘探, 2018, 23(4):39-50. HU Zhonggui, QIN Peng, HU Mingyi, et al. The distribution and heterogeneity characteristics of shale reservoirs in Lower Cambrian Shuijingtuo Formation in western Hunan-Hubei region[J]. China Petroleum Exploration, 2018, 23(4):39-50.
[21] TAYLOR S R, MCLENNAN S M. The continental crust:Its composition and evolution[J]. Geology, 1986, 94(4):57-72.
[22] ROLLINSON H R. A terrane interpretation of the Archaean Limpopo Belt[J]. Geological Magazine, 1993, 130(6):755-765.
[23] LAZAR R O, BOHACS K M, MACQUAKER J H S, et al. Capturing key attributes of fine-grained sedimentary rocks in outcrops, cores, and thin sections:Nomenclature and description guidelines[J]. Journal of Sedimentary Research, 2015, 85(3):230-246.
[24] 张梦琳,李郭琴,何嘉,等.川西南缘天宫堂构造奥陶系五峰组-志留系龙马溪组页岩气富集主控因素[J].岩性油气藏, 2022, 34(2):141-151. ZHANG Menglin, LI Guoqin, HE Jia, et al. Main controlling factors of Ordovician Wufeng-Silurian Longmaxi shale gas enrichment in Tiangongtang structure, southwestern margin of Sichuan Basin[J]. Lithologic Reservoirs, 2022, 34(2):141-151.
[25] 夏鹏,付勇,杨镇,等.黔北镇远牛蹄塘组黑色页岩沉积环境与有机质富集关系[J].地质学报, 2020, 94(3):947-956. XIA Peng, FU Yong, YANG Zhen, et al. The relationship between sedimentary environment and organic matter accumulation in the Niutitang black shale in Zhenyuan, northern Guizhou[J]. Acta Geologica Sinica, 2020, 94(3):947-956.
[26] ELDERFIELD H, PAGETT R. Rare earth elements in ichthyoliths:Variations with redox conditions and depositional environment[J]. Science of the Total Environment, 1986, 49:175-197.
[27] KIMURA H, WATANABE Y. Oceanic anoxia at the PrecambrianCambrian boundary[J]. Geology, 2001, 29(11):995-998.
[28] 何庆,高键,董田,等.鄂西地区下寒武统牛蹄塘组页岩元素地球化学特征及沉积古环境恢复[J].沉积学报, 2021, 39(3):686-703. HE Qing, GAO Jian, DONG Tian, et al. Elemental geochemistry and Paleo-environmental conditions of the Lower Cambrian Niutitang Shale in western Hubei province[J]. Acta Sedimentologica Sinica, 2021, 39(3):686-703.
[29] ALGEO T J, TRIBOVILLARD N. Environmental analysis of paleoceano-graphic systems based on molybdenum-uranium covariation[J]. Chemical Geology, 2009, 268(3/4):211-225.
[30] LIU Z H, ZHUANG X G, TENG G E, et al. The Lower Cambrian Niutitang formation at Yangtiao (Guizhou, SW China):Organic matter enrichment, source rock potential, and hydrothermal influences[J]. Journal of Petroleum Geology, 2015, 38(4):411-432.
[31] 贾智彬,侯读杰,孙德强,等.热水沉积区黑色页岩稀土元素特征及其地质意义:以贵州中部和东部地区下寒武统牛蹄塘组页岩为例[J].天然气工业, 2018, 38(5):44-51. JIA Zhibin, HOU Dujie, SUN Deqiang, et al. Characteristics and geological implications of rare earth elements in black shale in hydrothermal sedimentation areas:A case study from the Lower Cambrian Niutitang Fm shale in central and eastern Guizhou[J]. Natural Gas Industry, 2018, 38(5):44-51.
[32] 孟凡洋,陈科,包书景,等.湘西北复杂构造区下寒武统页岩含气性及主控因素分析:以慈页1井为例[J].岩性油气藏, 2018, 30(5):29-39. MENG Fanyang, CHEN Ke, BAO Shujing, et al. Gas-bearing property and main controlling factors of Lower Cambrian shale in complex tectonic area of northwestern Hunan province:A case of well Ciye 1[J]. Lithologic Reservoir, 2018, 30(5):29-39.
[33] 刘安,李旭兵,王传尚,等.湘鄂西寒武系烃源岩地球化学特征与沉积环境分析[J].沉积学报, 2013, 31(6):1122-1132. LIU An, LI Xubing, WANG Chuanshang, et al. Analysis of geochemical feature and sediment environment for hydrocarbon source rocks of Cambrian in west Hunan-Hubei area[J]. Acta Sedimentologica Sinica, 2013, 31(6):1122-1132.
[34] 祝庆敏,卢龙飞,潘安阳,等.湘西地区下寒武统牛蹄塘组页岩沉积环境与有机质富集[J].石油实验地质, 2021, 43(5):797-809. ZHU Qingmin, LU Longfei, PAN Anyang, et al. Sedimentary environment and organic matter enrichment of the Lower Cambrian Niutitang Formation shale, western Hunan province, China[J]. Petroleum Geology&Experiment, 2021, 43(5):797-809.
[35] 陈平,林卫兵,龚大建,等.贵州岑巩区块下寒武统变马冲组黑色页岩沉积地球化学特征及其沉积环境意义[J].地质科学, 2020, 55(4):1025-1043. CHEN Ping, LIN Weibing, GONG Dajian, et al. Sedimentary geochemical characteristics and its sedimentary environment significance of the black shale of the Lower Cambrian Bianmachong Formation in the Cen'gong block, Guizhou Province[J]. Chinese Journal of Geology, 2020, 55(4):1025-1043.
[36] ROSER B P, KORSCH R J. Provenance signatures of sandstonemudstone suites determined using discriminant function analysis of major-element data[J]. Chemical Geology, 1988, 67(1/2):119-139.
[37] ROBERT C L. Implications of elemental concentrations for provenance, redox conditions, and metamorphic studies of shales and limestones near Pueblo, CO, USA[J]. Chemical Geology, 2002, 191(4):305-327.
[38] FLOYD P A, LEVERIDGEB E. Tectonic environment of the Devonian Gramscatho basin, south Cornwall:framework mode and geochemical evidence from turbiditic sandstones[J]. Journal of the Geological Society, 1987, 144(4):531-542.
[39] ALLÈGRE C J, MINSTER J F. Quantitative models of trace element behavior in magmatic processes[J]. Earth and planetary science letters, 1978, 38(1):1-25.
[40] RONA P A. Criteria for recognition of hydrothermal mineral deposits in oceanic crust[J]. Economic Geology, 1978, 73(2):135-160.
[41] ZHANG Kun, JIA Chengzao, SONG Yan, et al. Analysis of Lower Cambrian shale gas composition, source and accumulation pattern in different tectonic backgrounds:A case study of Weiyuan block in the Upper Yangtze region and Xiuwu Basin in the Lower Yangtze region[J]. Fuel, 2020, 263:115978.
[42] DENG Tao, LI Yong, WANG Zhengjiang, et al. Geochemical characteristics and organic matter enrichment mechanism of black shale in the Upper Triassic Xujiahe Formation in the Sichuan basin:Implications for paleoweathering, provenance and tectonic setting[J]. Marine and Petroleum Geology, 2019, 109:698-716.
[43] 陈代钊,汪建国,严德天,等.中扬子地区早寒武世构造-沉积样式与古地理格局[J].地质科学, 2012, 47(4):1052-1070. CHEN Daizhao, WANG Jianguo, YAN Detian, et al. Tectonodepositional patterns and palaeogeography in the Middle Yangtze River region during the Early Cambrian[J]. Chinese Journal of Geology, 2012, 47(4):1052-1070.
[44] 周江羽,陈建文,张玉玺,等.下扬子地区幕府山组古环境和构造背景:来自细粒混积沉积岩系元素地球化学的证据[J].地质学报, 2021, 95(6):1693-1711. ZHOU Jiangyu, CHEN Jianwen, ZHANG Yuxi, et al. Paleoenvironment and tectonic background of Mufushan Formation in Lower Yangtze area:Evidence from geochemistry of fine-grained mixed-siliciclastic-calcareous deposits[J]. Acta Geologica Sinica, 2021, 95(6):1693-1711.
[45] 宋芳,牛志军,何垚砚,等.中扬子地区南华纪早期碎屑锆石U-Pb年龄及其对物源特征和古地理格局的约束[J].地质学报, 2016, 90(10):2661-2680. SONG Fang, NIU Zhijun, HE Yaoyan, et al. U-Pb Age of Detrital zircon and its restriction of provenance&paleogeographic characteristics of early Nanhua period in Middle Yangtze[J]. Acta Geologica Sinica, 2016, 90(10):2661-2680.
[46] ARMSTRONG J S, VERMA S P. Critical evaluation of six tectonic setting discrimination diagrams using geochemical data of Neogene sediments from known tectonic settings[J]. Sedimentary Geology, 2005, 177(1):115-129.
[47] BHATIA M R, CROOK K A. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J]. Contributions to Mineralogy and Petrology, 1986, 92(2):181-193.
[48] BHATIA M R. Plate Tectonics and geochemical composition of sandstones[J]. The Journal of Geology, 1983, 91(6):81-84.
[49] RICHARD M W. Chemical criteria to identify the depositional environment of chert:General principles and applications[J]. Sedimentary Geology, 1994, 90(3/4):213-232.
[50] RAHMAN M J, SUZUKI S. Geochemistry of sandstones from the Miocene Surma Group, Bengal Basin, Bangladesh:Implications for Provenance, tectonic setting and weathering[J]. Geochemical Journal, 2007, 41(6):415-428.
[51] 刘早学,许露露,温雅茹,等.湖北寒武系牛蹄塘组页岩气成藏条件与综合评价[J].地球科学, 2022, 47(5):1586-1603. LIU Zaoxue, XU Lulu, WEN Yaru, et al. Accumulation characteristics and comprehensive evaluation of shale gas in Cambrian Niutitang Formation, Hubei[J]. Earth Science, 2022, 47(5):1586-1603.
[52] ZHOU Lei, WANG Zongxiu, GAO Wanli, et al. Provenance and tectonic setting of the Lower Cambrian Niutitang Formation shales in the Yangtze platform, south China:Implications for depositional setting of shales[J]. Geochemistry, 2019, 79(2):984-398.
[53] 邱小松,胡明毅,胡忠贵.中扬子地区下寒武统岩相古地理及页岩气成藏条件分析[J].中南大学学报(自然科学版), 2014, 45(9):3174-3185. QIU Xiaosong, HU Mingyi, HU Zhonggui. Lithofacies palaeogeographic characteristics and reservoir-forming conditions of shale gas of Lower Cambrian in middle Yangtze region[J]. Journal of Central South University (Science and Technology), 2014, 45(9):3174-3185.
[54] 应维华.湘西北慈利-保靖深大断裂的演化及煤化沥青产出的地质意义[J].石油勘探与开发, 1991, 18(1):7-13. YING Weihua. Evolution of Cili-Baojing deep large faulting zone, northwestern Hunan and geological significance of he occurrence of carbonaceous asphaltenes[J]. Petroleum Exploration and Development, 1991, 18(1):7-13.
[55] 段太忠,曾允孚,高振中.根据沉积历史分析华南古大陆边缘的构造演化[J].石油与天然气地质, 1988, 9(4):410-420. DUAN Taizhong, ZENG Yunfu, GAO Zhenzhong. Analysis of tectonic evolution of paleo-continental margin in south China[J]. Oil&Gas Geology, 1988, 9(4):410-420.
[56] 叶亚培,唐书恒,郗兆栋,等.黔北地区牛蹄塘组页岩矿物组成特征与脆性评价[J].岩性油气藏, 2019, 31(4):62-71. YE Yapei, TANG Shuheng, XI Zhaodong, et al. Mineral compositions and brittleness evaluation of shale of Niutitang Formation in northern Guizhou[J]. Lithologic Reservoir, 2019, 31(4):62-71.

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[6]	HAN Chunyuan,ZHAO Xianzheng,JIN Fengming,WANG Quan,LI Xianping,WANG Suqing. “Multi-factor controlling, four-factor entrapping and key-factor enrichment”of stratigraphic-lithologic reservoirs and exploration practice in Erlian Basin (Ⅳ)———Exploration practice[J]. Lithologic Reservoirs, 2008, 20(1): 15 -20 .
[7]	DAI Chaocheng, ZHENG Rongcai, WEN Huaguo, ZHANG Xiaobing. Sequence-based lithofacies and paleogeography mapping of Paleogene in Lvda area, Liaodongwan Basin[J]. Lithologic Reservoirs, 2008, 20(1): 39 -46 .
[8]	YIN Yanshu, ZHANG Shangfeng, YIN Taiju. High resolution sequence stratigraphy framework and the distribution of sandbodies in salt lake of Qianjiang Formation in Zhongshi Oilfield[J]. Lithologic Reservoirs, 2008, 20(1): 53 -58 .
[9]	SHI Xuefeng, DU Haifeng. Study on the sedimentary facies of the member 3 and 4+5 of Yanchang Formation in Jiyuan area[J]. Lithologic Reservoirs, 2008, 20(1): 59 -63 .
[10]	YAN Shibang, HUWangshui, LI Ruisheng, GUAN Jian, LI Tao, NIE Xiaohong. Structural features of contemporaneous thrust faults in Hongche fault belt of Junggar Basin[J]. Lithologic Reservoirs, 2008, 20(1): 64 -68 .

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Development characteristics and sedimentary environment of black shale of Lower Cambrian Niutitang Formation in western Hunan and Hubei

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