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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第42卷

期数:

2020年第01期

页码:

120-131

栏目:

基础地质与矿产地质

出版日期:

2020-01-15

文章信息/Info

Title:

Sedimentary Characteristics of the Shore Facies of Cambrian Upper Mingxinsi Formation in Sanqiutian Profile of Zhenyuan Area, the Northern Guizhou, China and Their Geological Significance

文章编号:

1672-6561(2020)01-0120-12

作者:

王萌¹; 2; 牟传龙^2*; 梁薇¹; 2; 郑斌嵩²; 3; 侯乾²

(1. 山东科技大学 地球科学与工程学院,山东 青岛 266590; 2. 中国地质调查局成都地质调查中心, 四川 成都 610081; 3. 中国地质大学(武汉)地球科学学院,湖北 武汉 430074)

Author(s):

WANG Meng¹; 2;  MOU Chuan-long^2*;  LIANG Wei¹; 2;  ZHENG Bin-song²; 3;  HOU Qian²

(1. College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, Shandong, China; 2. Chengdu Center, China Geological Survey, Chengdu 610081, Sichuan, China; 3. School of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China)

关键词:

岩相古地理;  明心寺组;  粒度分析;  沉积构造;  冲洗交错层理;  滨岸相;  陆棚相;  贵州

Keywords:

lithofacies paleogeography;  Mingxinsi Formation;  particle size analysis;  sedimentary structure;  washing cross-bedding;  shore facies;  shelf facies;  Guizhou

分类号:

P512.2; P531

DOI:

10.19814/j.jese.2019.08030

文献标志码:

A

摘要:

沉积环境分析是古地理重建的核心内容,黔北地区寒武系明心寺组沉积环境研究存在较大争议,以致对中上扬子地区明心寺组沉积期古地理格局的认识不能统一。选取寒武系明心寺组发育齐全、出露良好的黔北镇远地区三丘田剖面为研究对象,通过野外剖面观察、室内薄片鉴定及碎屑岩粒度分析等方法对三丘田剖面明心寺组岩石学特征、沉积构造、沉积演化序列、沉积相类型进行了详细分析。结果表明:黔北镇远地区三丘田剖面寒武系明心寺组上段发育大套的石英粉—细砂岩,沉积构造以低角度冲洗交错层理为主,碎屑颗粒的成分和结构成熟度均较高; 三丘田剖面明心寺组上段砂岩以双次跳跃组分为主,悬浮组分含量较少,纵向剖面自下而上显示为浅水陆棚→临滨→前滨→后滨演化序列,呈典型的陆棚相向滨岸相变化。综上所述,黔北镇远地区三丘田剖面寒武系明心寺组上段的沉积相为滨岸相。黔北镇远地区明心寺组滨岸相沉积的出现,指示了黔北地区区域上重新认识明心寺组沉积相的必要性,将直接影响对黔北地区乃至中上扬子地区寒武纪古地理格局及其大地构造背景的认识。

Abstract:

The analysis of depositional environment is the core content of paleogeographic reconstruction. There is greet disputes on the study of the sedimentary environment of Cambrian Mingxinsi Formation in the northern Guizhou, which leads to the different opinions on understanding of paleogeographic pattern of the middle-upper Yangtze region during Mingxinsi Formation sedimentary period. The succession of Cambrian Mingxinsi Formation from the well-developed Sanqiutian Profile in Zhenyuan area, the northern Guizhou was measured, and the lithological characteristics, sedimentary structure, sedimentary evolution sequence and sedimentary facies types of Mingxinsi Formation in Sanqiutian profile were analyzed in detail by outcrop observation, thin section identification and particle size analysis of clastic rocks. The results show that Cambrian upper Mingxinsi Formation in Sanqiutian profile of Zhenyuan area, the northern Guizhou develops a large set of quartz silty-fine sandstone, the sedimentary structure is dominated by low-angle washing cross-bedding, and the clastic particle is well sorted and rounded; the sandstones of upper Mingxinsi Formation in Sanqiutian profile are mainly composed of double jump components with a small amount of suspended components, and the vertical profile sequence shows a typical variation of shelf facies to shore facies, and the evolution sequence from bottom to up is shallow shelf→shoreface→foreshore→backshore. In conclusion, the sedimentary facies of Cambrian upper Mingxinsi Formation in Sanqiutian profile of Zhenyuan area, the northern Guizhou belongs to shore facies. The appearance of shore facies deposit in Zhenyuan area indicates the necessity of re-understanding the sedimentary facies of Mingxinsi Formation in the northern Guizhou, which will directly affect the understanding of Cambrian paleogeographic pattern and geotectonic background in the northern Guizhou and even the middle-upper Yangtze region.

参考文献/References:

[1] 王鹏万,斯春松,张润合,等.滇黔北坳陷寒武系碳酸盐岩古海洋环境特征及地质意义[J].沉积学报,2016,34(5):811-818. WANG Peng-wan,SI Chun-song,ZHANG Run-he,et al.Characteristic of the Cambrian Carbonate Paleo-ocean Environment in the Dianqianbei Depression and Its Geological Significance[J].Acta Sedimentologica Sinica,2016,34(5):811-818.
[2] 林文洲.贵州寒武系沉积体系及层序地层学研究[D].成都:成都理工大学,2001. LIN Wen-zhou.Depositional System and Sequence Stra-tigraphy Research of Cambrian in Guizhou Province[D].Chengdu:Chengdu University of Technology,2001.
[3] 冯增昭,彭勇民,金振奎,等.中国南方寒武纪岩相古地理[J].古地理学报,2001,3(1):1-14. FENG Zeng-zhao,PENG Yong-min,JIN Zhen-kui,et al.Lithofacies Palaeogeography of the Cambrian in South China[J].Journal of Palaeogeography,2001,3(1):1-14.
[4] 李 皎,何登发.四川盆地及邻区寒武纪古地理与构造-沉积环境演化[J].古地理学报,2014,16(4):441-460. LI Jiao,HE Deng-fa.Palaeogeography and Tectonic-depositional Environment Evolution of the Cambrian in Sichuan Basin and Adjacent Areas[J].Journal of Palaeogeography,2014,16(4):441-460.
[5] 牟传龙,梁 薇,周恳恳,等.中上扬子地区早寒武世(纽芬兰世—第二世)岩相古地理[J].沉积与特提斯地质,2012,32(3):41-53. MOU Chuan-long,LIANG Wei,ZHOU Ken-ken,et al.Sedimentary Facies and Palaeogeography of the Middle-upper Yangtze Area During the Early Cambrian(Terreneuvian-Series 2)[J].Sedimentary Geology and Tethyan Geology,2012,32(3):41-53.
[6] 梅冥相,马永生,张 海,等.上扬子区寒武系的层序地层格架:寒武纪生物多样性事件形成背景的思考[J].地层学杂志,2007,31(1):68-78. MEI Ming-xiang,MA Yong-sheng,ZHANG Hai,et al.Sequence-stratigraphic Frameworks for the Cambrian of the Upper Yangtze Region:Ponder on the Sequence Stratigraphic Background of the Cambrian Biological Diversity Events[J].Journal of Stratigraphy,2007,31(1):68-78.
[7] 梅冥相,张 丛,张 海,等.上扬子区下寒武统的层序地层格架及其形成的古地理背景[J].现代地质,2006,20(2):195-208. MEI Ming-xiang,ZHANG Cong,ZHANG Hai,et al.Sequence-stratigraphic Frameworks and Their Forming Backgrounds of Paleogeography for the Lower Cambrian of Upper Yangtze Region[J].Geoscience,2006,20(2):195-208.
[8] 徐鹏辉.黔北及其邻区牛蹄塘组—明心寺组岩相古地理及演化[D].北京:中国地质大学,2016. XU Peng-hui.Lithofacies Paleogeography and Evolution of Niutitang and Mingxinsi Formations in North Guizhou and Its Adjacent Areas[D].Beijing:China University of Geosciences,2016.
[9] 李 进.黔北下寒武统牛蹄塘组页岩古环境恢复与有机质富集研究[D].北京:中国地质大学,2018. LI Jin.Study on Paleo-environmental Reconstruction and Organic Matter Accumulation of the Lower Cambrian Niutitang Formation in the Northern Guizhou[D].Beijing:China University of Geosciences,2018.
[10] 久 凯,丁文龙,李玉喜,等.黔北地区构造特征与下寒武统页岩气储层裂缝研究[J].天然气地球科学,2012,23(4):797-803. JIU Kai,DING Wen-long,LI Yu-xi,et al.Structural Features in Northern Guizhou Area and Reservoir Fracture of Lower Cambrian Shale Gas[J].Natural Gas Geoscience,2012,23(4):797-803.
[11] 赵 松.黔北地区构造特征及其下古生界黑色页岩裂缝发育特征和分布规律研究[D].北京:中国地质大学,2013. ZHAO Song.The Structural Features and Lower Paleozoic of Black Shale Fracture Characteristics and Distribution in Qianbei Area[J].Beijing:China University of Geosciences,2013.
[12] 花友仁.扬子板块的地壳演化与地层对比[J].地质与勘探,1995,31(2):15-22. HUA You-ren.Crust Evolution and Stratigraphic Correlation of Yangtze Plate[J].Geology and Exploration,1995,31(2):15-22.
[13] 张国伟,郭安林,王岳军,等.中国华南大陆构造与问题[J].中国科学:地球科学,2013,43(10):1553-1582. ZHANG Guo-wei,GUO An-lin,WANG Yue-jun,et al.Tectonics of South China Continent and Its Implications[J].Science China:Earth Sciences,2013,43(10):1553-1582.
[14] 张鹏飞.中扬子地区古生代构造古地理格局及其演化[D].青岛:中国石油大学,2009. ZHANG Peng-fei.Pattern and Evolution of Paleozoic Tectono-palaeogeography in the Middle Yangtze Region[D].Qingdao:China University of Petroleum,2009.
[15] 门玉澎,许效松,牟传龙,等.中上扬子寒武系蒸发岩岩相古地理[J].沉积与特提斯地质,2010,30(3):58-64. MEN Yu-peng,XU Xiao-song,MOU Chuan-long,et al.Sedimentary Facies and Palaeogeography of the Eva-porates in the Middle-upper Yangtze Area[J].Sedimentary Geology and Tethyan Geology,2010,30(3):58-64.
[16] 蒲心纯,周浩达,王熙林,等.中国南方寒武纪岩相古地理与成矿作用[M].北京:地质出版社,1993. PU Xin-chun,ZHOU Hao-da,WANG Xi-lin,et al.Cambrian Lithofacies and Mineralization in South China[M].Beijing:Geological Publishing House,1993.
[17] 张玲华,李正祥,POWELL C M.扬子古大陆与澳大利亚古大陆新元古代层序对比和古大陆再造[J].地球科学,1995,20(6):657-666. ZHANG Ling-hua,LI Zheng-xiang,POWELL C M.Correlation of the Neoproterozoic Sequences Between the Yangtze and the Australian Paleocontinents,and a Paleocontinental reconstruction[J].Earth Science,1995,20(6):657-666.
[18] LI X H,SU L,CHUNG S L,et al.Formation of the Jinchuan Ultramafic Instrusion and the World's Third Largest Ni-Cu Sulfide Deposit:Associated with the ～825 Ma South China Mantle Plume?[J].Geochemistry,Geophysics,Geosystems,2005,DOI:org/10.1029/2005GC001006.
[19] LI Z X,BOGDANOVA S V,COLLINS A S,et al.Assembly,Configuration,and Break-up History of Rodinia:A Synthesis[J].Precambrian Research,2008,160(1/2):179-210.
[20] 李三忠,李玺瑶,赵淑娟,等.全球早古生代造山带(Ⅲ):华南陆内造山[J].吉林大学学报(地球科学版),2016,46(4):1005-1025. LI San-zhong,LI Xi-yao,ZHAO Shu-juan,et al.Glo-bal Early Paleozoic Orogens(Ⅲ):Intracontinental Orogen in South China[J].Journal of Jilin University(Earth Science Edition),2016,46(4):1005-1025.
[21] ZHAO G C,WANG Y J,HUANG B C,et al.Geolo-gical Reconstructions of the East Asian Blocks:From the Breakup of Rodinia to the Assembly of Pangea[J].Earth-science Review,2018,186:262-286.
[22] 王 頔.川中地区晚震旦世—早寒武世构造古地理演化及油气地质意义[D].武汉:长江大学,2017. WANG Di.Tectonic Paleogeographic Evolution and Petroleum Geological Significance During Late Sinian-Early Cambrian in Central Sichuan Basin[D].Wuhan:Yangtze University,2017.
[23] 段金宝,梅庆华,李毕松,等.四川盆地震旦纪—早寒武世构造-沉积演化过程[J].地球科学,2019,44(3):738-755. DUAN Jin-bao,MEI Qing-hua,LI Bi-song,et al.Sinian-Early Cambrian Tectonic-sedimentary Evolution in Sichuan Basin[J].Earth Science,2019,44(3):738-755.
[24] 汪泽成,姜 华,王铜山,等.四川盆地桐湾期古地貌特征及成藏意义[J].石油勘探与开发,2014,41(3):305-312. WANG Ze-cheng,JIANG Hua,WANG Tong-shan,et al.Paleo-geomorphology Formed During Tongwan Tectonization in Sichuan Basin and Its Significance for Hydrocarbon Accumulation[J].Petroleum Exploration and Development,2014,41(3):305-312.
[25] 武赛军,魏国齐,杨 威,等.四川盆地桐湾运动及其油气地质意义[J].天然气地球科学,2016,27(1):60-70. WU Sai-jun,WEI Guo-qi,YANG Wei,et al.Tongwan Movement and Its Geologic Significances in Sichuan Basin[J].Natural Gas Geoscience,2016,27(1):60-70.
[26] 唐 娜.四川盆地下寒武统岩相古地理研究[D].武汉:长江大学,2017. TANG Na.Study on Lithofacies Palaeogeography of the Lower Cambrian in the Sichuan Basin[D].Wuhan:Yangtze University,2017.
[27] 周小进,杨 帆.中国南方新元古代—早古生代构造演化与盆地原型分析[J].石油实验地质,2007,29(5):446-451. ZHOU Xiao-jin,YANG Fan.Tectonic Evolution and Prototypes Analysis from Neoproterozoic to Early Paleozoic in South China[J].Petroleum Geology and Experiment,2007,29(5):446-451.
[28] 杨 剑.黔北地区下寒武统黑色岩系形成环境与地球化学研究[D].西安:长安大学,2009. YANG Jian.Study on the Formation Environment and Geochemistry of Lower Cambrian Black Shale Series,Northern Guizhou Province,China[D].Xi'an:Chang'an University,2009.
[29] 孟晓庆.贵州及邻区下寒武统层序地层格架及其古地理演化[D].北京:中国地质大学,2007. MENG Xiao-qing.Sequence-stratigraphic Framework and Its Palaeogeographical Evolution of the Lower Cambrian Series in Guizhou and Its Adjacent Areas[D].Beijing:China University of Geosciences,2007.
[30] 李 伟,余华琪,邓鸿斌.四川盆地中南部寒武系地层划分对比与沉积演化特征[J].石油勘探与开发,2012,39(6):681-690. LI Wei,YU Hua-qi,DENG Hong-bin.Stratigraphic Division and Correlation and Sedimentary Characteristics of the Cambrian in Central-southern Sichuan Basin[J].Petroleum Exploration and Development,2012,39(6):681-690.
[31] 冯伟明,谢 渊,李 嵘,等.川东南—黔西北桐湾Ⅲ幕岩溶古地貌恢复[J].地质论评,2017,63(5):1270-1280. FENG Wei-ming,XIE Yuan,LI Rong,et al.Restoration of Karst Palaeotopography on the Tongwan Movement Period in the Southeastern Sichuan and Northwestern Guizhou[J].Geological Review,2017,63(5):1270-1280.
[32] 杨 帅,陈洪德,钟怡江,等.川西南地区晚震旦世微生物岩及其对桐湾运动Ⅰ幕的响应[J].岩石学报,2017,33(4):1148-1158. YANG Shuai,CHEN Hong-de,ZHONG Yi-jiang,et al.Microbolite of Late Sinian and Its Response for Tongwan Movement Episode Ⅰ in Southwest Sichuan,China[J].Acta Petrologica Sinica,2017,33(4):1148-1158.
[33] 曾 楷,李 飞,龚峤林,等.寒武系第二统仙女洞组混合沉积特征及古环境意义:以川北旺苍唐家河剖面为例[J].沉积学报,2019,DOI:10.14027/j.issn.1000-0550.2019.015. ZENG Kai,LI Fei,GONG Qiao-lin,et al.Characteristics and Paleoenvironmental Significance of the Mixed Siliciclastic-carbonate Sedimentation in the Xiannvdong Formation,Cambrian(Series 2):A Case Study from the Tangjiahe Section,Wangcang,Northern Sichuan[J].Acta Sedimentologica Sinica,2019,DOI:10.14027/j.issn.1000-0550.2019.015.
[34] 梁 薇,牟传龙,周恳恳,等.中上扬子地区寒武纪第三世—芙蓉世古地理[J].古地理学报,2015,17(2):172-185. LIANG Wei,MOU Chuan-long,ZHOU Ken-ken,et al.Palaeogeography of the Cambrian Epoch 3-Furongian in the Middle and Upper Yangtze Region[J].Journal of Palaeogeography,2015,17(2):172-185.
[35] 朱茂炎,杨爱华,袁金良,等.中国寒武纪综合地层和时间框架[J].中国科学:地球科学,2019,49(1):26-65. ZHU Mao-yan,YANG Ai-hua,YUAN Jin-liang,et al.Cambrian Integrative Stratigraphy and Timescale of China[J].Science China:Earth Sciences,2019,49(1):26-65.
[36] 贵州省地质矿产局.贵州省区域地质志[M].北京:地质出版社,1987. Bureau of Geology and Mineral Exploration and Deve-lopment,Guizhou Province.Regional Geology of Guizhou Province[M].Beijing:Geological Publishing House,1987.
[37] 葛东升,刘玉明,柳雪青,等.粒度分析在致密砂岩储层及沉积环境评价中的应用[J].特种油气藏,2018,25(1):41-45,72. GE Dong-sheng,LIU Yu-ming,LIU Xue-qing,et al.Application of Grain Size Analysis in Tight Sandstone Reservoir and Sedimentary Environment Evaluation[J].Special Oil and Gas Reservoirs,2018,25(1):41-45,72.
[38] 周 蒂.利用沉积物粒度数据反演沉积水动力参数[J].地质科学,1999,34(1):49-58. ZHOU Di.The Estimation of Sedimentary HydrodynamicParameters from Sediment Grain-size Data [J].Scientia Geologica Sinica,1999,34(1):49-58.
[39] 操应长,王 健,刘惠民.利用环境敏感粒度组分分析滩坝砂体水动力学机制的初步探讨:以东营凹陷西部沙四上滩坝砂体沉积为例[J].沉积学报,2010,28(2):274-284. CAO Ying-chang,WANG Jian,LIU Hui-min.Preli-minary Study on the Hydrodynamic Mechanism of Beach-bar Sandbodies with Environmentally Sensitive Grain Size Components:A Case Study from Beach-bar Sandbody Sediments of the Upper Part of the Fourth Member of the Shahejie Formation in the Western Dongying Depression[J].Acta Sedimentologica Sinica,2010,28(2):274-284.
[40] 袁红旗,王 蕾,于英华,等.沉积学粒度分析方法综述[J].吉林大学学报(地球科学版),2019,49(2):380-393. YUAN Hong-qi,WANG Lei,YU Ying-hua,et al.Review of Sedimentary Grain Size Analysis Methods[J].Journal of Jilin University(Earth Science Edition),2019,49(2):380-393.
[41] 肖晨曦,李志忠.粒度分析及其在沉积学中应用研究[J].新疆师范大学学报(自然科学版),2006,25(3):118-123. XIAO Cheng-xi,LI Zhi-zhong.The Research Summary of Grain Size Analysis and Its Application in the Sedimentation[J].Journal of Xinjiang Normal University(Natural Sciences Edition),2006,25(3):118-123.
[42] 袁 静,杜玉民,李云南.惠民凹陷古近系碎屑岩主要沉积环境粒度概率累积曲线特征[J].石油勘探与开发,2003,30(3):103-106. YUAN Jing,DU Yu-min,LI Yun-nan.Probability Cumulative Grain Size Curves in Terrigenous Depositional Environments of the Paleogene in Huimin Sag[J].Petroleum Exploration and Development,2003,30(3):103-106.
[43] 赵鲁阳,吕大炜,刘海燕,等.安徽巢北地区五通组沉积环境分析[J].沉积学报,2015,33(3):470-479. ZHAO Lu-yang,LU Da-wei,LIU Hai-yan,et al.The Analysis on the Depositional Environment of Wutong Formation in Northern Chaohu Area,Anhui[J].Acta Sedimentologica Sinica,2015,33(3):470-479.
[44] 丁喜桂,叶思源,高宗军.粒度分析理论技术进展及其应用[J].世界地质,2005,24(2):203-207. DING Xi-gui,YE Si-yuan,GAO Zong-jun.Development and Applications of Grain Size Analysis Technique[J].Global Geology,2005,24(2):203-207.
[45] 孙 诗,王 峰,陈洪德,等.鄂尔多斯盆地东北缘府谷剖面中二叠统盒8段沉积相特征[J].地球科学与环境学报,2019,41(2):225-240. SUN Shi,WANG Feng,CHEN Hong-de,et al.Sedimentary Facies Characteristics of He-8 Member of Middle Permian in Fugu Section,the Northeastern Margin of Ordos Basin,China[J].Journal of Earth Sciences and Environment,2019,41(2):225-240.
[46] 李增学,常象春,赵秀丽.岩相古地理学[M].北京:地质出版社,2010. LI Zeng-xue,CHANG Xiang-chun,ZHAO Xiu-li.Lithofacies Paleogeography[M].Beijing:Geological Publishing House,2010.
[47] FRIEDMAN G M.Distribution Between Dune,Beach,and River Sands from Their Textural Characteristics[J].Journal of Sedimentary Petrology,1961,31(4):514-529.
[48] 罗顺社,时 德,张存善,等.塔里木盆地西南缘上震旦统克孜苏胡木组有障壁海岸沉积体系[J].石油天然气学报,2005,27(1):24-25. LUO Shun-she,SHI De,ZHANG Cun-shan,et al.Beach-barrier Coast Deposit System in Upper Sinian Kezisuhumu Formation in the Southwest Margin of Tarim Basin[J].Journal of Oil and Gas Technology,2005,27(1):24-25.
[49] 杨奇铮,李 萍,高 伟,等.东海岛东北部典型岸段短期冲淤变化及影响因素分析[J].海洋科学进展,2016,34(4):532-541. YANG Qi-zheng,LI Ping,GAO Wei,et al.Short-term Coastal Erosion-deposition Variation Analysis of Northeastern Donghai Island[J].Advances in Marine Science,2016,34(4):532-541.
[50] 唐佐其,马义波,谯文浪,等.贵州省独山江寨地区下泥盆统碎屑岩物性、粒度特征及沉积环境讨论[J].贵州地质,2015,32(1):21-26. TANG Zuo-qi,MA Yi-bo,QIAO Wen-lang,et al.Discussion of Physical Property,Grading Features and Sedimentary Environment of Clastic Rock in Low Devonian of Jiangzhai Area in Dushan,Guizhou[J].Guizhou Geology,2015,32(1):21-26.
[51] 夏 鹏,王甘露,曾凡桂,等.黔北地区牛蹄塘组高—过成熟页岩气富氮特征及机理探讨[J].天然气地球科学,2018,29(9):1345-1355. XIA Peng,WANG Gan-lu,ZENG Fan-gui,et al.The Characteristics and Mechanism of High-over Matured Nitrogen-rich Shale Gas of Niutitang Formation,Northern Guizhou Area[J].Natural Gas Geoscience,2018,29(9):1345-1355.
[52] 牟传龙,许效松.华南地区早古生代沉积演化与油气地质条件[J].沉积与特提斯地质,2010,30(3):24-29. MOU Chuan-long,XU Xiao-song.Sedimentary Evolution and Petroleum Geology in South China During the Early Palaeozoic[J].Sedimentary Geology and Tethyan Geology,2010,30(3):24-29.

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备注/Memo

备注/Memo:

收稿日期:2019-08-28; 修回日期:2019-11-08; 网络首发日期:2019-12-31投稿网址:http:∥jese.chd.edu.cn/
基金项目:中国地质调查局地质调查项目(12120115004301)
作者简介:王 萌(1993-),男,安徽宿松人,山东科技大学工程硕士研究生,E-mail:329431441@qq.com。
*通讯作者:牟传龙(1965-),男,四川达县人,研究员,博士研究生导师,理学博士,E-mail:cdmchuanlong@163.com。

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更新日期/Last Update: 2020-01-07