演化中的裂谷带——五大连池火山岩带
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摘要
小古里河—科洛—五大连池—二克山新生代火山岩带是一条富钾火山岩带。文中重点论述了以下4点内容:(1)火山岩及其包体中存在典型的地幔交代作用;(2)根据火山岩K2O/Na2O比值勾画出富钾火山岩带范围;(3)地幔气体的绝热膨胀导致"冷泉和冻土现象";(4)地震活动的现状。论证了NNW走向的五大连池火山岩带是新生代初始的大陆裂谷,它们切穿了大兴安岭北北东向构造带。进一步从岩浆演化的趋势认为五大连池裂谷带将持续演化而不会夭折。
The Xiaogulihe-Keluo-Wudalianchi-Erkeshan Cenozoic volcanic rock belt is one rich in potassium.Four facts about this belt are analyzed in this work:(1)typical mantle metasomatism existing in the volcanic rocks and in their inclusions,(2)the distribution range of the K-rich volcanic belt estimated according to the K2O/Na2O ratio of the volcanic rocks,(3)the "cold spring and taele phenomenon" caused by adiabatic expansion of the mantle gases,and(4)the current situation of seismic activities.It is inferred from those facts that the NNW-strike Wudalianchi volcanic rock belt is a Cenozoic primal continental rift cutting through the NNE-strike Da-Hinggan-Mt.tectonic belt.The evolution tendency of its magma suggests that the Wudalianchi rift belt is still in a course of continuing evolution without a sign of coming to an end.
The Xiaogulihe-Keluo-Wudalianchi-Erkeshan Cenozoic volcanic rock belt is one rich in potassium.Four facts about this belt are analyzed in this work:(1)typical mantle metasomatism existing in the volcanic rocks and in their inclusions,(2)the distribution range of the K-rich volcanic belt estimated according to the K2O/Na2O ratio of the volcanic rocks,(3)the "cold spring and taele phenomenon" caused by adiabatic expansion of the mantle gases,and(4)the current situation of seismic activities.It is inferred from those facts that the NNW-strike Wudalianchi volcanic rock belt is a Cenozoic primal continental rift cutting through the NNE-strike Da-Hinggan-Mt.tectonic belt.The evolution tendency of its magma suggests that the Wudalianchi rift belt is still in a course of continuing evolution without a sign of coming to an end.
引文
[1]黑龙江省区测一队.龙镇公社幅1∶20万区域地质调查报告.1978.
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[2]Zhang M.Petrological characteristics of Shihlunite of Laohe-ishan and Huoshaoshan of Wudalianchi,Heilongjiang Prov-ince[J].Earth Science,1984,24:87-99(in Chinese).
[3]Wang C Q,Du X R,Liu J X.Keruo-Wudalianchi-Erkeshan volcanic clusters[J].Journal of East China College of Geolo-gy,1987,10(2):1-262(in Chinese).
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[25]Liu Z Y,Li HY.The genesis of thelow-temperature mineral water inthe Wudalianchi Volcanic Area[J].Heilongjiang Ge-ology,1997,8(3):55-62(in Chinese)
[26]Sun R B,Du J G.The hydro-geochemical background of the Wudalianchi volcanic area[J].Bulletin of Mineralogy,Petrol-ogy and Geochemistry,1998,17(3):150-155(in Chinese).
[27]Han Y W,Ma Z D.Geochemistry[M].Beijing:Geological Publishing House,2003:259-264(in Chinese).
[28]Dai J X,Wen HF,Song Y.Natural gas of the mantle origin in Wudalianchi[J].Experi mental Petroleum Geology,1992,14(2):200-203(in Chinese).
[29]Du J G,Li S Q.Geochemical characteristics of gases from the Wudalianchi volcanic area,Northeastern China[J].Acta Geologica Sinica,1999,73(2):225-229.
[30]Shang Guan Z G.Study of fluids and their stable isotope compositions fromvolcanic areas[M]∥Liu R X.Human,en-vironment and volcanic action.Beijing:Seismological Press,1995:98-100(in Chinese).
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[32]Fan Q C,Liu R X,Wei H Q,et al.Petrogeochemical char-acteristics of Holocene eruption of the Tianchi volcano,Changbai Mountains[J].Geological Review,1999,45(Sup-pl):263-271(in Chinese).
[33]Zhou X H,Armstrong R L.Cenozoic volcanic rock of eastern China—secular and geographic trendin chemistry and stronti-umisotop composition[J].Earth Planet Sci Lett,1982,53:301-329.
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[1]Hu S L,Wang S S,Liu J Q,et al.K-Ar ages and Sr and Oisotope characteristics[M]∥Petrological Research(2).Bei-jing:Geological Publishing House,1983:22-29(in Chinese).
[2]Zhang M.Petrological characteristics of Shihlunite of Laohe-ishan and Huoshaoshan of Wudalianchi,Heilongjiang Prov-ince[J].Earth Science,1984,24:87-99(in Chinese).
[3]Wang C Q,Du X R,Liu J X.Keruo-Wudalianchi-Erkeshan volcanic clusters[J].Journal of East China College of Geolo-gy,1987,10(2):1-262(in Chinese).
[4]Qiu J X,Liao Q A,Du X R.Petrological characteristics and genetic analysis of the belt of potassium-rich volcanic rocks from Erkeshan,Wudalianchi and Keluo of Heilongjiang[J].Acta Petrologica et Mineralogica,1988,7(2):92-108(in Chinese).
[5]Qiu J X,Liao Q A,Liu M H,et al.The K-rich volcanic rocks in Wudalianchi-Keluo-Erkeshan[M].Wuhan:China University of Geosciences Press,1991:204-207(in Chinese).
[6]Liu M H.Petrology study ontheinclusion of ijolite andleuci-tite[J].Journal of East China College of Geology,1990,13(2):41-50(in Chinese).
[7]Mu Z G,Liu C,Huang B L,et al.K-Ar ages and geochem-istry of the Late-Cenozoic rocksin Keluo,Heilongjiang Prov-ince[J].Acta Scientiarum Naturalium Universitatis Pekinen-sis,1992,28(6):733-744(in Chinese).
[8]Xia L Q.Onthe evolution of volcanic magma from Wudalian-chi[J].Acta Petrologica Sinica,1990(1):13-29(in Chinese).
[9]Wang J W,Xie G H,et al.Sr,Nd,Pbisotope geochemistry and magma evolution of potash volcanic rocks at Wudalianchi[J].Geochi mica,1988(4):310-318(in Chinese).
[10]Zhang J B.Source s characteristics of ultra-potassiumbasaltic rocks from northeast China and research on regional mantle geochemistry[D].Beijing:Institute of Geology,Chinese A-cademy of Sciences,1992:3-29(in Chinese).
[11]Fan Q C,Liu R X,Sui J L.Petrology and geochemistry of rift type Wudalianchi K-rich volcanic rock zone[J].Geolog-ical Review,1999,45(Suppl):358-368(in Chinese).
[12]Li Q,Chen WJ,Li D M,et al.Achronological research on volcanic rocks fromthe Wudalianchi area[J].Geological Re-view,1999,45(Suppl):393-399(in Chinese).
[13]Qu C Z,Cui J W.The features of Cenozoic K-rich basalt of the Keluo volcanic group and its formed tectonic setting and discussion on the cause of K-rich[J].Heilongjiang Geology,1991,2(3):50-57(in Chinese).
[14]Gong J S.Xiaogulihe-Keluo-Wudalianchi volcanic belt[J].Heilongjiang Geology,1997,8(4):29-39(in Chinese).
[15]Zhao WF.Continental rift valley systemand seismic-activi-ties in Northeast China[J].Geological Review,1981,3(2):23-39(in Chinese).
[16]Liu J Q.On the origin evolution of continental rift systemin Northeast China[J].Chinese Journal of Geology,1989,(3):209-216(in Chinese).
[17]Zhou X H,Zhu B Q.Study on the isotopic systemand man-tle chemical zonation of Cenozoic basalt in China[M]∥Liu R X.The age and geochemistry of Cenozoic volcanic rock in China.Beijing:Seismological Press,1992:366-391(in Chi-nese).
[18]Lu F X,Zheng J P,Zhang R S,et al.Phanerozoic mantle secular evolution beneath the eastern North China craton[J].Earth Science Frontiers,2005,12(1):61-67(in Chinese).
[19]Bureau of Geology and Mineral Resources of Heilongjiang Province.Regional geology of Heilongjiang Province[M].Beijing:Geological Publishing House,1993:519-520(in Chi-nese).
[20]Du S Z,Du X R.The research of Cenozoic basalts and spinel buchnerite enclaves Heilongjiang Province[J].Heilongjiang Geology,1983,5:9-19(in Chinese).
[21]LüZ W,Yang S L.Wudalianchi volcano and volcanic hazard prediction[J].Seismological and Geomagnetic Observation and Research,1996,17(6):45-53(in Chinese).
[22]Zhan Y,Zhao G Z,Bai D H.Preli minary study of Wudalian-chi volcanic cluster in Heilongjiang Province by MT measure-ment[J].Geological Review,1999,45(Suppl):400-407(in Chinese).
[23]Wu Z C(Qing dynasty).Record about the Ninggu pagoda[M].Shanghai:The Commercial Press,1936(in Chinese).
[24]Chen HZ,Ren J Z,Wu XJ.Volcanic eruptive processes and characteristics of the current volcanoes in the Wudalianchi volcano clusters known from manchurian-language historical archives discovered at present[J].Geological Review,1999,45(Suppl):409-413(in Chinese).
[25]Liu Z Y,Li HY.The genesis of thelow-temperature mineral water inthe Wudalianchi Volcanic Area[J].Heilongjiang Ge-ology,1997,8(3):55-62(in Chinese)
[26]Sun R B,Du J G.The hydro-geochemical background of the Wudalianchi volcanic area[J].Bulletin of Mineralogy,Petrol-ogy and Geochemistry,1998,17(3):150-155(in Chinese).
[27]Han Y W,Ma Z D.Geochemistry[M].Beijing:Geological Publishing House,2003:259-264(in Chinese).
[28]Dai J X,Wen HF,Song Y.Natural gas of the mantle origin in Wudalianchi[J].Experi mental Petroleum Geology,1992,14(2):200-203(in Chinese).
[29]Du J G,Li S Q.Geochemical characteristics of gases from the Wudalianchi volcanic area,Northeastern China[J].Acta Geologica Sinica,1999,73(2):225-229.
[30]Shang Guan Z G.Study of fluids and their stable isotope compositions fromvolcanic areas[M]∥Liu R X.Human,en-vironment and volcanic action.Beijing:Seismological Press,1995:98-100(in Chinese).
[31]Chen Y,Zhang Y X,David G,et al.Geochemistry of Ceno-zoic basalts and mantle xenoliths in Northeast China[J].Lithos,2007,95:108-126.
[32]Fan Q C,Liu R X,Wei H Q,et al.Petrogeochemical char-acteristics of Holocene eruption of the Tianchi volcano,Changbai Mountains[J].Geological Review,1999,45(Sup-pl):263-271(in Chinese).
[33]Zhou X H,Armstrong R L.Cenozoic volcanic rock of eastern China—secular and geographic trendin chemistry and stronti-umisotop composition[J].Earth Planet Sci Lett,1982,53:301-329.
[1]胡世玲,王松山,刘嘉麒,等.五大连池新生代玄武岩的K-Ar年龄和锶、氧同位素特征[M]∥岩石学研究:第2辑.北京:地质出版社,1983:22-29.
[2]张明.黑龙江省老黑山、火烧山石龙岩岩石学特征[J].地球科学——中国地质大学学报,1984,24:87-99.
[3]王承祺,杜向荣,刘继贤.科洛—五大连池—二克山火山群[J].华东地质学院学报,1987,10(2):1-262.
[4]邱家骧,廖群安,杜向荣.黑龙江二克山、五大连池、科洛富钾火山岩带的岩石特征及成因分析[J].岩石矿物杂志,1988,7(2):92-108.
[5]邱家骧,廖群安,刘蒙华,等.五大连池—科洛—二克山富钾火山岩[M].武汉:中国地质大学出版社,1991:204-207.
[6]刘蒙华.白榴霓霞岩包体的岩石学及成因研究[J].华东地质学院院报,1990,13(2):41-50.
[7]穆治国,刘驰,黄宝玲,等.黑龙江科洛晚新生代火山岩K-Ar定年和地球化学[J].北京大学学报:自然科学版,1992,28(6):733-744.
[8]夏林圻.论五大连池火山岩浆演化[J].岩石学报,1990(1):13-29.
[9]王俊文,解广轰,等.五大连池钾质火山岩的Sr、Nd、Pb同位素地球化学及岩浆的化学演化[J].地球化学,1988(4):310-318.
[10]张剑波.东北高钾玄武质岩类源区特征及区域地幔地球化学研究[D].北京:中国科学院地质研究所,1992:3-29.
[11]樊祺诚,刘若新,隋建立.五大连池裂谷型富钾火山岩带的岩石学与地球化学[J].地质论评,1999,45(增刊):358-368.
[12]李齐,陈文寄,李大明,等.五大连池地区火山岩年代学研究[J].地震地质,1999,45(增刊):393-399.
[13]曲成柱,崔建伟.新生代科洛火山群富钾玄武岩特征及形成的构造环境与富钾原因的初探[J].黑龙江地质,1991,2(3):50-57.
[14]巩杰生.小古里河—科洛—五大连池火山带[J].黑龙江地质,1997,8(4):29-39.
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