贵州中坪地区上三叠统二桥组砂岩粒度分析及其沉积环境意义

doi:10.13686/j.cnki.dzyzy.2023.04.004

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Abstract Through the grain size analysis of 16 sandstone samples from the Upper Triassic Erqiao Formation in Zhongping area of Guizhou Province, combined with the regional geological setting, the paper studies the sedimentary environment and hydrodynamic conditions during the formation of the sandstone. The analysis on the probability cumulative grain size curves, C-M diagram, grain size characteristic parameters and scatter diagram of structure parameters of the sandstone indicates that the probability cumulative grain size curves of the sandstone from Erqiao Formation show good normal distribution, and the frequency histograms mostly show single-peak curves. The normal probability cumulative curves are mainly multi-bouncing population-one suspension population, one bouncing population-one suspension population, and one bouncing population-one suspension population-transitional zone patterns, mainly composed of suspended and jumping components, but lack of rolling components. The Upper Triassic Erqiao Formation in Zhongping area from the lower to the upper part is in a sedimentary environment transitioning from delta plain and delta front facies to shallow lake facies.

Key words： Upper Triassic Erqiao Formation grain size analysis sedimentary environment Guizhou Province

Received: 27 April 2022

PACS:

P585.2

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	Articles by authors
	WANG Ning-zu
	ZHANG Wen-bin
	HE Bi
	TAO Gang
	ZHAO Fei
	SUN Ping-yuan
	ZHANG Zhi-xi
	ZHAO Zhen-guan

Cite this article:

WANG Ning-zu,ZHANG Wen-bin,HE Bi等. SANDSTONE GRAIN SIZE ANALYSIS OF UPPER TRIASSIC ERQIAO FORMATION IN ZHONGPING AREA, GUIZHOU PROVINCE: Implication of Sedimentary Environment[J]. GEOLOGY AND RESOURCES, 2023, 32(4): 406-417.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2023.04.004 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2023/V32/I4/406

[1]	刘宝珺, 张锦泉. 沉积成岩作用[M]. 北京:科学出版社, 1992:65-92. Liu B J, Zhang J Q. Sedimentary diagenesis[M]. Beijing:Science Press, 1992:65-92. (in Chinese)
[2]	赵澄林. 沉积学原理[M]. 北京:石油工业出版社, 2001:1-214. Zhao C L. Principles of sedimentology[M]. Beijing:Petroleum Industry Press, 2001:1-214.
[3]	姜在兴. 沉积学[M]. 北京:石油工业出版社, 2003:136-152. Jiang Z X. Sedimentology[M]. Beijing:Petroleum Industry Press, 2003:136-152. (in Chinese)
[4]	成都地质学院陕北队. 沉积岩(物)粒度分析及其应用[M]. 北京:地质出版社, 1978:1-133. Shanbei Team of Chengdu College of Geology. Grain size analysis and application for sediments[M]. Beijing:Geological Publishing House, 1978:1-133. (in Chinese)
[5]	张帅军. 西藏岗玛日地区下三叠统康鲁组砂岩粒度分析及环境意义[D]. 北京:中国地质大学, 2013. Zhang S J. Sandstone grain size analysis and environmental significance of Lower Triassic Kanglu Formation, Gangmari region, Tibet[D]. Beijing:China University of Geosciences, 2013.
[6]	丁旭林. 粒度分析与重矿物组合的地质应用[J]. 科学技术与工程, 2012, 12(14):3439-3442. Ding X L. Geologic application of grain size analysis and heavy mineral assemblage[J]. Science Technology and Engineering, 2012, 12(14):3439-3442.
[7]	Weiss E L, Frock H N. Rapid analysis of particle size distributions by laser light scattering[J]. Powder Technology, 1976, 14(2):287-293.
[8]	肖晨曦. 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 C X. 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.
[9]	贵州省地质矿产局. 贵州省区域地质志[M]. 北京:地质出版社, 1987:76-135. Guizhou Bureau of Geology and Mineral Resources. Regional geology of Guizhou Province[M]. Beijing:Geological Publishing House, 1987:76-135. (in Chinese)
[10]	贵州省地质矿产局. 贵州省岩石地层[M]. 北京:地质出版社, 1997:136-201. Guizhou Bureau of Geology and Mineral Resources. Stratigraphy (lithostratic) of Guizhou Province[M]. Beijing:Geological Publishing House, 1997:136-201.
[11]	孙平原, 何碧, 赵飞, 等. 贵州乌蒙山黔西地区二叠系玄武岩地球化学特征及其地质意义[J]. 科学技术与工程, 2019, 19(12):41-51. Sun P Y, He B, Zhao F, et al. Geochemical characteristics and their geological significance of Permian basalt rocks in Qianxi area, Wumengshan of Guizhou Province[J]. Science Technology and Engineering, 2019, 19(12):41-51.
[12]	何碧, 张向文, 赵飞, 等. 贵州黔西官坝地区二叠系-三叠系地质界面黏土岩的火山岩特征、LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 现代地质, 2020, 34(5):1028-1042. He B, Zhang X W, Zhao F, et al. Volcanic characteristics, LA-ICP-MS zircon U-Pb ages of claystone at the Permian-Triassic boundary, Guanba area in Guizhou Province, South China and the geological implications[J]. Geoscience, 2020, 34(5):1028-1042.
[13]	王宁祖, 张向文, 何碧, 等. 贵州省黔西县大寨地区中三叠统关岭组绿豆岩锆石U-Pb年代学、地球化学特征及地质意义[J]. 矿物岩石, 2019, 39(1):82-91. Wang N Z, Zhang X W, He B, et al. Zircon U-Pb geochronology and geochemistry of the mung bean rocks of the Middle Triassic Guanling Formation in Dazhai area of Qianxi County, Guizhou Province[J]. Journal of Mineralogy and Petrology, 2019, 39(1):82-91.
[14]	乔卫涛, 陈仁, 胡歆睿, 等. 贵州开阳地区澄江组第二段砂岩粒度分析与沉积环境[J]. 贵州地质, 2020, 37(1):59-65. Qiao W T, Chen R, Hu X R, et al. Grain-size analysis and depositional environment of the second member of Chengjiang Formation at Kaiyang area of Guizhou Province[J]. Guizhou Geology, 2020, 37(1):59-65.
[15]	陈逵. 元坝地区须家河组储层岩石学特征和图像法粒度分析研究[D]. 成都:成都理工大学, 2014. Chen K. Reservoir petrology characteristics study and image method grain-size analysis of Xujiahe Formation in Yuanba area[D]. Chengdu:Chengdu University of Technology, 2014.
[16]	Folk R L, Ward W C. Brazos River bar:A study in the significance of grain size parameters[J]. Journal of Sedimentary Petrology, 1957, 27(1):3-26.
[17]	Visher G S. Grain size distributions and depositional processes[J]. Journal of Sedimentary Petrology, 1969, 39(3):1074-1106.
[18]	王立亭. 试论黔西北及邻区非海相三叠系/侏罗系界线[J]. 贵州地质, 2002, 19(3):175-178, 162. Wang L T. Initial discussion on the boundary of the Triassic-Jurassic of the non-marine facies in Northwest Guizhou and its adjacent areas[J]. Guizhou Geology, 2002, 19(3):175-178, 162.
[19]	周冰洋, 赵兵, 孙剑, 等. 贵州大方地区二桥组地层特征及沉积相分析[J]. 地质学刊, 2017, 41(1):46-53. Zhou B Y, Zhao B, Sun J, et al. Stratigraphic features and sedimentary facies analysis of the Erqiao Formation in the Dafang area of Guizhou Province[J]. Journal of Geology, 2017, 41(1):46-53.
[20]	周冰洋. 贵州大方地区中-晚三叠世地层划分对比及沉积相分析[D]. 成都:成都理工大学, 2017. Zhou B Y. Stratigraphic division and comparison and sedimentary facies analysis of Middle-Late Triassic in Dafang County of Guizhou Province[D]. Chengdu:Chengdu University of Technology, 2017.
[21]	胡阳, 龚晓波, 廖阮颖子. 重庆长寿地区上三叠统地层特征研究[J]. 四川有色金属, 2020, 29(4):29-32. Hu Y, Gong X B, Liao R Y Z. Stratigraphic characteristics of upper Triassic in Changshou area of Chongqing[J]. Sichuan Nonferrous Metals, 2020, 29(4):29-32.
[22]	孙建勋, 吴亮, 肖长源, 等. 黔北普宜地区晚三叠世二桥组砂岩碎屑锆石U-Pb年龄、重矿物分析及地质意义[J]. 地质学报, 2022, 96(3):824-839. Sun J X, Wu L, Xiao C Y, et al. Implications of detrital zircon U-Pb ages and analysis of heavy minerals from sandstone of the Late Triassic Erqiao Formation in Puyi area, North Guizhou[J]. Acta Geologica Sinica, 2022, 96(3):824-839.
[23]	王云飞. 抚仙湖现代湖泊沉积物中海绿石的发现及成因的初步研究[J]. 科学通报, 1983(22):1388-1392. Wang Y F. the Discovery and Preliminary study on genesis of glauconite in modern lake sediments of Fuxian Lake[J]. Chinese Science Bulletin, 1983(22):1388-1392. (in Chinese)
[24]	朱政源, 董凌峰, 于航, 等. 海绿石的成因与应用[J]. 科技创新与应用, 2015(33):16-18. Zhu Z Y, Dong L F, Yu H, et al. Genesis and application of glauconite[J]. Technology Innovation and Application, 2015(33):16-18. (in Chinese)
[25]	吴龙, 宗维, 杜小峰, 等. 鄂西恩施白垩纪盆地跑马岗组砂砾岩粒度分析[J]. 资源环境与工程, 2019, 33(2):164-169. Wu L, Zong W, Du X F, et al. Grain size analysis of sand-conglomerate of Paomagang Formation in Enshi Cretaceous basin, western Hubei Province[J]. Resources Environment & Engineering, 2019, 33(2):164-169.
[26]	Friedman G M. Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands[J]. Journal of Sedimentary Petrology, 1967, 37(2):327-354.
[27]	Passega R. Grain size representation by CM patterns as a geologic tool[J]. Journal of Sedimentary Petrology, 1964, 34(4):830-847.