延吉盆地白垩纪地层序列及盆地演化
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摘要
本文在野外地质调查和前人资料的综合分析对比基础上,对延吉盆地的岩石地层序列、生物地层特征做了详细总结,并对各组时代归属进行了讨论;将延吉盆地白垩纪地层与松辽盆地、鸡西盆地进行对比,提出延吉盆地上下白垩统界线应置于大拉子组之顶;并对延吉盆地的白垩纪岩相古地理进行分析,认为延吉盆地早白垩世为温暖潮湿气候条件下的一套河湖相、泥炭沼泽相夹火山碎屑岩沉积,晚白垩世干旱气候条件下的河流相红色粗碎屑岩沉积;在系统查证延吉盆地各断裂的基本特征基础上,提出延吉盆地并没有单独的控盆断裂,其构造分区为两隆两坳;并将延吉盆地演化分为两个盆地演化旋回,确立延吉盆地为早白垩世断陷盆地和晚白垩世坳陷盆地叠加的复合盆地性质。
Yanbian region located in the junction parts of Paleao-Asian Ocean tectonic domain and Pacific tectonic domain, it belongs to the eastern parts of Xinan-Mongolia Orogenic belt and an important composition of Mesozoic volcanic belt circling west Pacific ocean. The main strata of Yanji Basin are composed of Cretaceous, it has clearly two basin evolution stages, namely: the early Cretaceous rifting basin stage and the late Cretaceous depression basin stage.
Based on systematically geological survey and comprehensively analyzing and comparing the previous data, the author discussed the rock strata sequences of Yanji basin, biostratigraphic characteristics and regional comparison, and then analyzed its litho-palaeogeography and discussed its basin evolution cycle. The scientific achievements as follow:
1. Summarized each of the Cretaceous litho-stratigraphic units of Yanji Basin, and rectified its standards, and then established the strata sequences of Yanji Basin.
2. Through comprehensive isotopic chronologic and biostratigraphic discussions, the age of the Tuntianying formation of Yanji Basin is amended from the middle Jurassic to early Cretaceous.
3. Through analyzing the typical elements of Dalazi Fauna, and after discussing its evolution sequence with the Jehol Fauna and the Songhuajiang Fauna, it is clear that the Dalazi Fauna is a transitional fauna between the Jehol Fauna and the Songhuajiang Fauna, and its age should be late Early Cretaceous.
4. After discussing the Cretaceous lithostratigraphic sequence of Yanji basin and its evolution of litho-paleaogeography, the author reckons that the Yanji basin in early Cretaceous is a set of stream facies, lacustrine facies, and peat facies with volcanic pyroclastic rocks deposition, however, the late Cretaceous is stream facies red coarse grain clastic deposition under dry climate condition.
5. The author proposes that the Yanji basin should not be independent controlling basin faults, and its tectonic division is two uplifts and two depressions, and divides the Yanji basin evolution into two cycles, namely early Cretaceous rift basin and late Cretaceous depression basin.
Yanbian region located in the junction parts of Paleao-Asian Ocean tectonic domain and Pacific tectonic domain, it belongs to the eastern parts of Xinan-Mongolia Orogenic belt and an important composition of Mesozoic volcanic belt circling west Pacific ocean. The main strata of Yanji Basin are composed of Cretaceous, it has clearly two basin evolution stages, namely: the early Cretaceous rifting basin stage and the late Cretaceous depression basin stage.
Based on systematically geological survey and comprehensively analyzing and comparing the previous data, the author discussed the rock strata sequences of Yanji basin, biostratigraphic characteristics and regional comparison, and then analyzed its litho-palaeogeography and discussed its basin evolution cycle. The scientific achievements as follow:
1. Summarized each of the Cretaceous litho-stratigraphic units of Yanji Basin, and rectified its standards, and then established the strata sequences of Yanji Basin.
2. Through comprehensive isotopic chronologic and biostratigraphic discussions, the age of the Tuntianying formation of Yanji Basin is amended from the middle Jurassic to early Cretaceous.
3. Through analyzing the typical elements of Dalazi Fauna, and after discussing its evolution sequence with the Jehol Fauna and the Songhuajiang Fauna, it is clear that the Dalazi Fauna is a transitional fauna between the Jehol Fauna and the Songhuajiang Fauna, and its age should be late Early Cretaceous.
4. After discussing the Cretaceous lithostratigraphic sequence of Yanji basin and its evolution of litho-paleaogeography, the author reckons that the Yanji basin in early Cretaceous is a set of stream facies, lacustrine facies, and peat facies with volcanic pyroclastic rocks deposition, however, the late Cretaceous is stream facies red coarse grain clastic deposition under dry climate condition.
5. The author proposes that the Yanji basin should not be independent controlling basin faults, and its tectonic division is two uplifts and two depressions, and divides the Yanji basin evolution into two cycles, namely early Cretaceous rift basin and late Cretaceous depression basin.
引文
[1]孙革,郑少林,中国东北中生代地层划分对比之新见,JOURNAL OF STRATIGRAPHY,2000,24(1):60-64
[2]王义刚,1983.黑龙江省东部的几种Bathonian菊石.见:黑龙江省东部中、上侏罗统与下白垩统化石(上册),哈尔滨:黑龙江科技出版社.100-104.
[3]王东方,刁乃昌,1984.辽西侏罗-白垩系火山岩系统的同位素年龄测定-兼测侏罗系与白垩系的底界年龄.国际交流地质学术论文集(5).北京:地质出版社.1-12.
[4]周志炎,李佩娟,1980,从古植物学观点讨论中国中生代陆相地层的划分、对比和时代.见:国际交流地质学术论文集(4)地层古生物.北京:地质出版社.82-91.
[5]陈丕基,1988.热河生物群的分布与迁移——兼论中国陆相侏罗-白垩系的界线划分.古生物学报,27(6):659-683.
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[8]顾知微,陈金华,沙金庚,1984.黑龙江省东部侏罗纪和白垩纪双壳类的初步研究.见:黑龙江省东部中、上侏罗统与下白垩统化石(下册).哈尔滨:黑龙江科技出版社.49-220.
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[10]乔秀云,万传彪,徐衍彬,焦玉国,孔惠,金玉东,2003.吉林延吉盆地早白垩世沟鞭藻类及其它藻类.微体古生物学报,20(3):309-317.
[11]周志炎,陈丕基,厉宝贤等,1980.吉林东部延边地区晚中生代陆相地层.中国科学院南京地质古生物研究所丛刊,第1号:1-21
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[13]张光富,2005.中国吉林大拉子组的时代探讨.JOURNAL OF STRATIGRAPHY,29(4)381-386
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[19]陈丕基.2000.陆相白垩系.见:中国科学院南京地质古生物研究所编.中国地层研究二十年(1979—1999).合肥:中国科学技术大学出版社.329-345.
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[22]周志炎,李佩娟.1980.从古植物学观点讨论中国中生代陆相地层的划分、对比和时代.见:地质部书刊编辑室编.国际交流地质学术论文集——为二十六届国际地质大会撰写.北京:地质出版社.82-91.
[23]周志炎,陈丕基,厉宝贤,文世宣,黎文本,张璐瑾,叶美娜,刘兆生,李再平,杨学林.1980.吉林东部延边地区中生代陆相地层.中国科学院南京地质古生物研究所丛刊,1:1-21.
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[25]陶君容,张川波.1990.吉林省延吉盆地早白垩世被子植物化石.植物学报,32(3):220-229.
[26]陶君容,杨永.2003.吉林延边早白垩世大拉子组植物化石新类型——星学异麻黄.古生物学报,42(2):208-215.
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[28]斯行健,周志炎,1962.中国中生代陆相地层.北京:科学出版社.40-60.
[29]殷鸿福.1988.中国古生物地理学.武汉:中国地质大学出版社.1-329.
[30]李超文,郭锋,2005.延吉地区晚中生代火山岩的Ar—Ar年代学格架及其 大地构造学意义.
[31]靳克、许文良,2003.延吉地区中生代火山岩的岩石学和地球化学:对构造体制转换与岩石圈深部物质组成的制约.
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[33]周志炎,李佩娟,1980.从古植物学观点讨论中国中生代陆相地层的划分、对比和时代.国际交流地质学术论文集—为二十六届国际地质大会撰写(地质部书刊编辑室编写).北京:地质出版社.82-91.
[34]余静贤,苗淑娟,1984.延边地区早白垩世孢粉组合,中国地质科学院天津地质矿产研究所所刊,8:55-80.
[35]程裕祺等,中国地层典,白垩系,2000
[36]Swisher C C,Wang Yuan-qing,Wang Xiao-lin,Xu Xing,Wang Yuan,1999.Cretaceous age for the feathered dinosaurs of Liaoning,China.Nature,400:58-61.
[37]CHENG Jinhu,HE Chengquan,2001.Early Cretaceous dinoflagel-lates from the Didao Formation in the Jixi Basin,eastern Hei-longjiang Province,NE China.Acta Palaeontologica Sinica.42(1):127-133
[38]GAO Ruiqi,HE Chengquan,QIAO Xiuyun,1992.A new genus and species of Cretaceous dinoflagellates from two transgressive beds in Songliao basin,NE China.Acta Palaeontologica Sinica,31(1):17-29
[39]LI Wenben,2001.An earliest Cretaceous Palynological Assembal-age from the Tuntianyin Formation in Antu,Jilin Province.Acta Palaeontologica Sinica,40(4):450-456
[40]MAO Shaozhi,WAN Chuanbiao,QIAO Xiuyun,1999:Cretaceous nonmarine dinoflagellates from northeast China.Grana,38:144-161
[41]Chen Pei-ji.1994.Cretaceous conchostracan faunas of China.Cretaceous Research,15:259-269.
[42]Doyle J A &Hickey L J.1976.Pollen and leaves from the Mid-Cretaceous Potomac Group and their bearing on early angiosperm evolution.In:Beck C B ed.Origin and early evolution of angiosperms.New York:Columbia University Press.139-206.
[43]Krassilov V A.1967.Early Cretaceous flora of South Primorje and its significance for stratigraphy.Moscow:Nauka.1-364(in Russian).
[44]Krassilov V A. 1982. Early Cretaceous flora of Mongolia. Palaeontographica,Abt. B181: 1-43.
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[2]王义刚,1983.黑龙江省东部的几种Bathonian菊石.见:黑龙江省东部中、上侏罗统与下白垩统化石(上册),哈尔滨:黑龙江科技出版社.100-104.
[3]王东方,刁乃昌,1984.辽西侏罗-白垩系火山岩系统的同位素年龄测定-兼测侏罗系与白垩系的底界年龄.国际交流地质学术论文集(5).北京:地质出版社.1-12.
[4]周志炎,李佩娟,1980,从古植物学观点讨论中国中生代陆相地层的划分、对比和时代.见:国际交流地质学术论文集(4)地层古生物.北京:地质出版社.82-91.
[5]陈丕基,1988.热河生物群的分布与迁移——兼论中国陆相侏罗-白垩系的界线划分.古生物学报,27(6):659-683.
[6]斯行健,周志炎,1962.中国中生代陆相地层.北京:科学出版社:1-180.
[7]顾知微,1962.中国的侏罗系和白垩系.北京:科学出版社.1-84.
[8]顾知微,陈金华,沙金庚,1984.黑龙江省东部侏罗纪和白垩纪双壳类的初步研究.见:黑龙江省东部中、上侏罗统与下白垩统化石(下册).哈尔滨:黑龙江科技出版社.49-220.
[9]吉林省地矿局,吉林省地质志,1985
[10]乔秀云,万传彪,徐衍彬,焦玉国,孔惠,金玉东,2003.吉林延吉盆地早白垩世沟鞭藻类及其它藻类.微体古生物学报,20(3):309-317.
[11]周志炎,陈丕基,厉宝贤等,1980.吉林东部延边地区晚中生代陆相地层.中国科学院南京地质古生物研究所丛刊,第1号:1-21
[12]王友勤,刘尔义,1996.中国东北区中生代生物群特征简述.吉林地质,15(3、4):111-117.
[13]张光富,2005.中国吉林大拉子组的时代探讨.JOURNAL OF STRATIGRAPHY,29(4)381-386
[14]王友勤,苏养正,刘尔义.1997.东北区区域地层.武汉:中国地质大学出版社.1-175.
[15]勾韵娴.1983.吉林省延边地区白垩纪介形类.古生物学报,22(1):42-54.
[16]瓦赫拉梅耶夫B A.1988.侏罗—白垩纪全球植物群及气候.孙革,张志诚,郑少林译.1990.南京:南京大学出版社.1-169.
[17]孙革,曹正尧,李浩敏等.1995.白垩纪植物群.见:李星学主编冲国地质时期植物群.广州:广东科技出版社.310-344.
[18]孙革,郑少林.2000.中国东北中生代地层划分对比之新见.地层学杂志,24(1):60-64.
[19]陈丕基.2000.陆相白垩系.见:中国科学院南京地质古生物研究所编.中国地层研究二十年(1979—1999).合肥:中国科学技术大学出版社.329-345.
[20]余静贤,苗淑娟.1983.延边地区早白垩世孢粉组合.中国地质科学院天津地质矿产研究所所刊,8:55-76.
[21]张川波.1986.吉林省延吉盆地早白垩世中晚期地层.长春地质学院学报,(2):15-27.
[22]周志炎,李佩娟.1980.从古植物学观点讨论中国中生代陆相地层的划分、对比和时代.见:地质部书刊编辑室编.国际交流地质学术论文集——为二十六届国际地质大会撰写.北京:地质出版社.82-91.
[23]周志炎,陈丕基,厉宝贤,文世宣,黎文本,张璐瑾,叶美娜,刘兆生,李再平,杨学林.1980.吉林东部延边地区中生代陆相地层.中国科学院南京地质古生物研究所丛刊,1:1-21.
[24]陶君容.2000.中国晚白垩至新生代植物区系发展演变.北京:科学出版社.1-183.
[25]陶君容,张川波.1990.吉林省延吉盆地早白垩世被子植物化石.植物学报,32(3):220-229.
[26]陶君容,杨永.2003.吉林延边早白垩世大拉子组植物化石新类型——星学异麻黄.古生物学报,42(2):208-215.
[27]黄嫔,张光富.2002.吉林延边智新盆地大拉子组孢粉组合.微体古生物学报,19(3):263-275.
[28]斯行健,周志炎,1962.中国中生代陆相地层.北京:科学出版社.40-60.
[29]殷鸿福.1988.中国古生物地理学.武汉:中国地质大学出版社.1-329.
[30]李超文,郭锋,2005.延吉地区晚中生代火山岩的Ar—Ar年代学格架及其 大地构造学意义.
[31]靳克、许文良,2003.延吉地区中生代火山岩的岩石学和地球化学:对构造体制转换与岩石圈深部物质组成的制约.
[32]余静贤,苗淑娟,1983.延边地区早白垩世孢粉组合.中国地质科学院天津地质矿产研究所所刊,8:55-79.
[33]周志炎,李佩娟,1980.从古植物学观点讨论中国中生代陆相地层的划分、对比和时代.国际交流地质学术论文集—为二十六届国际地质大会撰写(地质部书刊编辑室编写).北京:地质出版社.82-91.
[34]余静贤,苗淑娟,1984.延边地区早白垩世孢粉组合,中国地质科学院天津地质矿产研究所所刊,8:55-80.
[35]程裕祺等,中国地层典,白垩系,2000
[36]Swisher C C,Wang Yuan-qing,Wang Xiao-lin,Xu Xing,Wang Yuan,1999.Cretaceous age for the feathered dinosaurs of Liaoning,China.Nature,400:58-61.
[37]CHENG Jinhu,HE Chengquan,2001.Early Cretaceous dinoflagel-lates from the Didao Formation in the Jixi Basin,eastern Hei-longjiang Province,NE China.Acta Palaeontologica Sinica.42(1):127-133
[38]GAO Ruiqi,HE Chengquan,QIAO Xiuyun,1992.A new genus and species of Cretaceous dinoflagellates from two transgressive beds in Songliao basin,NE China.Acta Palaeontologica Sinica,31(1):17-29
[39]LI Wenben,2001.An earliest Cretaceous Palynological Assembal-age from the Tuntianyin Formation in Antu,Jilin Province.Acta Palaeontologica Sinica,40(4):450-456
[40]MAO Shaozhi,WAN Chuanbiao,QIAO Xiuyun,1999:Cretaceous nonmarine dinoflagellates from northeast China.Grana,38:144-161
[41]Chen Pei-ji.1994.Cretaceous conchostracan faunas of China.Cretaceous Research,15:259-269.
[42]Doyle J A &Hickey L J.1976.Pollen and leaves from the Mid-Cretaceous Potomac Group and their bearing on early angiosperm evolution.In:Beck C B ed.Origin and early evolution of angiosperms.New York:Columbia University Press.139-206.
[43]Krassilov V A.1967.Early Cretaceous flora of South Primorje and its significance for stratigraphy.Moscow:Nauka.1-364(in Russian).
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