吉林白山地区新元古界碳酸盐岩沉积演化规律及沉积事件探讨:以青沟子剖面为例
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摘要
吉林白山地区新元古界碳酸盐岩在青沟子剖面上出露连续,发育多种沉积事件。笔者通过实测剖面资料及碳酸盐岩镜下特征分析,研究白山地区万隆组—青沟子组碳酸盐岩的沉积演化规律和典型事件的沉积模式。结果表明,白山地区新元古界碳酸盐岩具有缓坡型台盆体系—镶边型台盆体系动态演化的特征,海平面变化是控制碳酸盐岩沉积演化的重要因素。结合碳酸盐岩沉积相发育类型,提出"封闭性镶边缓坡台地"沉积模式。分析沉积事件特征与沉积环境的联系,证实臼齿构造集中发育于中缓坡相,叠层石集中发育于礁核和礁后滩相。
The Neoproterozoic carbonate rocks outcrop continuously in Qinggouzi section,in Baishan area of Jilin Province,with abundant of sedimentary events indicated. Based on field measurements and microscope observation of the carbonate rocks,the sedimentary evolution of Wanlong Formation and Qinggouzi Formation carbonate rocks in Qinggouzi section and the sedimentary models of typical events are analyzed. The results show that the dynamic evolution of Neoproterozoic carbonate rocks in Baishan area is from gentle slope platform basin system to rimmed platform basin system,and the fluctuation of sea level is an important factor controlling the sedimentary evolution of carbonate rocks. In combination with the sedimentary facies of carbonate rocks,the deposition model of"closed rimmed gentle slope platform"is put forward. Analysis of the relationship between sedimentary event characteristics and sedimentary environment confirms that the molar-tooth structures mainly occurr in the medium-gentle slope facies while stromatolites in the reef core and the back-reef beach facies.
The Neoproterozoic carbonate rocks outcrop continuously in Qinggouzi section,in Baishan area of Jilin Province,with abundant of sedimentary events indicated. Based on field measurements and microscope observation of the carbonate rocks,the sedimentary evolution of Wanlong Formation and Qinggouzi Formation carbonate rocks in Qinggouzi section and the sedimentary models of typical events are analyzed. The results show that the dynamic evolution of Neoproterozoic carbonate rocks in Baishan area is from gentle slope platform basin system to rimmed platform basin system,and the fluctuation of sea level is an important factor controlling the sedimentary evolution of carbonate rocks. In combination with the sedimentary facies of carbonate rocks,the deposition model of"closed rimmed gentle slope platform"is put forward. Analysis of the relationship between sedimentary event characteristics and sedimentary environment confirms that the molar-tooth structures mainly occurr in the medium-gentle slope facies while stromatolites in the reef core and the back-reef beach facies.
引文
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[3]刘燕学,旷红伟,孟祥化,等.吉辽徐淮地区新元古代地层对比格架[J].地层学杂志,2005,29(4):387-396.LIU Yan-xue,KUANG Hong-wei,MENG Xiang-hua,et al.The Neoproterozoic stratigraphic correlation framework in the Jilin-Liaoning-Xuzhou-Huaiyang area[J].Journal of Stratigraphy,2005,29(4):387-396.
[4]杜凤芝,纪春华,刘大业.吉林通化地区元古代岩石地层研究[J].吉林地质,2015,34(1):7-11.DU Feng-zhi,JI Chun-hua,LIU Da-ye.Study of Paleoproterozoic strata in Tonghua area of Jilin Province[J].Jilin Geology,2015,34(1):7-11.
[5]曲鹏展,程日辉,宋立斌,等.柳河盆地中生代充填特征与盆地演化[J].世界地质,2018,37(1):185-198.QU Peng-zhan,CHENG Ri-hui,SONG Li-bin,et al.Mesozoic filling characteristics and evolution of Liuhe Basin[J].Global Geology,2018,37(1):185-198.
[6]吉林省地质矿产局.吉林省区域地质志[M].北京:地质出版社,1989:72-77,518-519.Bureau of Geology and Mineral Resources of Jilin Province.Regional geology of Jilin Province[M].Beijing:Geological Publishing House,1989:72-77,518-519.
[7]孟祥化,葛铭,刘燕学.中朝板块新元古代微亮晶(臼齿构造)碳酸盐事件、层序地层和建系研究[J].地层学杂志,2006,30(3):211-222.MENG Xiang-hua,GE Ming,LIU Yan-xue.Study of the Neoproterozoic microspar(molar tooth)carbonate events,sequence stratigraphy of the Sino-Korean Plate and the establishment of the beihuan system[J].Journal of Stratigraphy,2006,30(3):211-222.
[8]王德海.吉辽徐淮新元古代层序地层和岩相古地理及海相烃源岩发育特征:博士学位论文[D].北京:中国地质大学,2007.WANG De-hai.Sequence stratigraphy and lithofacies paleogeography and marine source rocks of Ji-Liao-Xu-Huai area Neoproterozoic:doctor's degree thesis[D].Beijing:China University of Geosciences,2007.
[9]刘燕学,蔡国印,旷红伟,等.吉林南部震旦纪万隆组与八道江组之间风化壳的发现[J].岩石矿物学杂志,2005,24(1):47-52.LIU Yan-xue,CAI Guo-yin,KUANG Hong-wei,et al.The discovery of paleo-weathering crusts between Sinian Wanlong Formation and Badaojiang Formation in southern Jilin Province[J].Acta Petrologica et Mineralogica,2005,24(1):47-52.
[10]Wilson J L.Carbonate facies in geologic history[M].New York:Springer Verlag,1975:292-301.
[11]关士聪.中国海相、陆相和海洋油气地质[M].北京:地质出版社,1999:1-10.GUAN Shi-cong.Marine-facies,terrestrial and offshore petroleum geology of China[M].Beijing:Geological Publishing House,1991:1-10.
[12]Tucker M E,Wright V P.Carbonate sedimentology[M].Oxford:Blackwell Science Company Limited,1990:33-34.
[13]徐文礼.缓斜坡碳酸盐台地沉积模式:以土库曼斯坦阿姆河盆地中-上侏罗统卡洛夫-牛津阶为例:博士学位论文[D].成都:成都理工大学,2013.XU Wen-li.Sedimentary mode of glacis carbonate platform:taking Callovian-Oxfordian of Upper Middle Jurassic in Amu-Darya Basin of Turkmenistan as an example:doctor's degree thesis[D].Chengdu:Chengdu University of Technology,2013.
[14]金振奎,石良,高白水,等.碳酸盐岩沉积相及相模式[J].沉积学报,2013,31(6):965-979.JIN Zhen-kui,SHI Liang,GAO Bai-shui,et al.Carbonate facies and facies models[J].Acta Sedimentologica Sinica,2013,31(6):965-979.
[15]高志前,樊太亮,李岩,等.塔里木盆地寒武-奥陶纪海平面升降变化规律研究[J].吉林大学学报(地球科学版),2006,36(4):549-556.GAO Zhi-qian,FAN Tai-liang,LI Yan,et al.Study on Eustatic sea level change rule in Cambrian-Ordovician in Tarim Basin[J].Journal of Jilin University(Earth Science Edition),2006,36(4):549-556.
[16]Bauerman H.Report on the geology of the country near the forth-ninth parallel of North latitude West of the Rocky Mountains[R].Ottawa:Geological Survey Report Programme of Canada,1885:1-42.
[17]葛铭,孟祥化,旷红伟,等.微亮晶(臼齿)碳酸盐岩:21世纪全球地学研究的新热点[J].沉积学报,2003,21(1):81-89.GE Ming,MENG Xiang-hua,KUANG Hong-wei,et al.Molar tooth carbonates:carbonate research highlight of the world in the 21st century[J].Acta Sedimentologica Sinica,2003,21(1):81-89.
[18]Winston D.Evidences for intracratonic,fluvial and lacustrine setting of Middle to Late Proterozoic LaurentiaBaltica[J].Geological Association of Canada Special Paper,1990,38(1):535-564.
[19]Knoll A H.Microbiotas of the Late Precambrian Hunnberg Formation,Nordaustlandet,Svalbard[J].Journal of Paleontology,1984,58(1):131-162.
[20]Pratt B R.Shrinkage feature(molar tooth structure)in Proterozoic limestrone:new model for their origin through synsedimentary earthquake-induced dewatering[C]//Programs-Geological Society of America.Geological Society of America 1992 Annual Meeting Abstracts,1992,24(7):53.
[21]乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J].地质学报,1994,68(1):16-34.QIAO Xiu-fu,SONG Tian-rui,GAO Lin-zhi,et al.Seismic sequence in carbonate rocks by vibrational liquefaction[J].Acta Geologica Sinica,1994,68(1):16-34.
[22]Furniss G,Rittle J F,Winston D.Gas bubble and expansion crack origin of“molar tooth”calcite structures in the Middle Proterozoic Belt Supergroup,western Montana[J].Journal of Sedimentary Research,1998,68(1):104-114.
[23]孟祥化,葛铭.中朝板块层序、事件、演化[M].北京:科学出版社,2004:147-150.MENG Xiang-hua,GE Ming.Sequence,events and evolution of Sino-Korea Plate[M].Beijing:Science Press,2004:147-150.
[24]Kahl C,Knoll A H.Microbenthic distribution of Proterozoic tidal flats:environmental and taphonomic considerations[J].Geology,1996,24(1):79-82.
[25]Bartley J K,Knoll A H.Lithification and fabric genesis in precipitated stromatolites and associated peritidal carbonates,Mesoproterozoic Billyakh Group,Siberia[C]//Grotzinger J P,James N P,eds.Carbonate sedimentation and diagenesis in the evolving Precambrian world.SEPM,Special Publication,2000,67:59-73.
[26]Hofmann H J.The mid-Proterozoic Little Dal macrobiota,Mackenzie mountains,Northwest Canada[J].Palaeontology,1985,28(2):31-54.
[27]赵彦彦,郑永飞.全球新元古代冰期的记录和时限[J].岩石学报,2011,27(2):545-565.ZHAO Yan-yan,ZHENG Yong-fei.Record and time of Neoproterozoic glaciations on Earth[J].Acta Petrologica Sinica,2011,27(2):545-565.
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