南岭地区与东南沿海地区中生代花岗岩放射性地球化学特征及岩石圈热结构对比研究
|
摘要
华南地区广泛发育中生代花岗岩,主要出露于南岭地区和东南沿海地区。受大地构造作用影响,自西向东,莫霍面深度逐渐变薄,深部温度逐渐升高,软流圈顶部上升,花岗岩形成时代也随之逐渐年轻化。南岭和东南沿海地区的地表和钻孔花岗岩放射性生热元素含量测试结果表明,南岭地区放射性生热率平均值为5.18μW/m~3,东南沿海地区为3.01μW/m~3,最高生热率为南岭佛冈岩体7.56μW/m~3;热贡献率主要来自Th和U的放射性衰变热,K的热贡献率一般不超过10%。通过本文研究结果,结合前人地质学、地球物理学和地热学研究成果,发现南岭地区和东南沿海地区地壳热流对地表热流值的贡献率分别为60%~65%和40%~45%,指示两者分别为"热壳冷幔"和"冷壳热幔"型岩石圈热结构。
Mesozoic granite is widely distributed in southeast China,which can be divided into Nanling and southeast coastal granitic belts.Due to the effect of tectonism,the depth of Moho and the thickness of lithosphere together with the emplacement age of granite bodies decrease eastward,but the temperature at the depth increases eastward.Radioactive heat-producing element content determinations of granites from surface and drill holes within Nanling region and Southeast coastal region show that the average radioactive heat generation ratios are 5.18 and 3.01 μW/m~3,respectively,and that the Fogang granitic body exhibits the highest value of 7.56 μW/m~3.In addition,the thermal contribution rate mainly comes from the radioactive decay heat of Th and U with ~(40)K thermal contribution being less than 10%.The new data obtained by the authors,in combination with previous geological,geophysical and geothermal data,indicate that the contribution rate from the crust to the surface heat flow in Nanling region and Southeast coastal region is about 60%~ 65% and 40%~ 45%,respectively.The result suggests that Nanling region is of "hot crust-cold mantle" type and the Southeast coastal region is of "cold crust-hot mantle" type lithospheric thermal structure.
Mesozoic granite is widely distributed in southeast China,which can be divided into Nanling and southeast coastal granitic belts.Due to the effect of tectonism,the depth of Moho and the thickness of lithosphere together with the emplacement age of granite bodies decrease eastward,but the temperature at the depth increases eastward.Radioactive heat-producing element content determinations of granites from surface and drill holes within Nanling region and Southeast coastal region show that the average radioactive heat generation ratios are 5.18 and 3.01 μW/m~3,respectively,and that the Fogang granitic body exhibits the highest value of 7.56 μW/m~3.In addition,the thermal contribution rate mainly comes from the radioactive decay heat of Th and U with ~(40)K thermal contribution being less than 10%.The new data obtained by the authors,in combination with previous geological,geophysical and geothermal data,indicate that the contribution rate from the crust to the surface heat flow in Nanling region and Southeast coastal region is about 60%~ 65% and 40%~ 45%,respectively.The result suggests that Nanling region is of "hot crust-cold mantle" type and the Southeast coastal region is of "cold crust-hot mantle" type lithospheric thermal structure.
引文
Bai Daoyuam Jia Baohua,Ma Tieqiu,et al.2007.Relationship of petro-geochemical characteristics to met allogenic capacity differences between Indosinian and Early Yanshanian granites in southeastern Hunan[J].Acta Petrologica et Mineralogica.26(5):387~398(in Chinese with English abstract).
Bao Zhiwei and Zhao Zhenhua.2003.Geochemistry and tectonic setting of the Fogang aluminous A-type granite,Guangdong province,China—A preliminary study[J].Geology-Geochemistry.31(1):52~61(in Chinese with English abstract).
Cermak V and Rybach L.1987.International conference report:Terrestrial heat flow and the lithosphere structure[J].Geothermics.16(5):583~585.
Chen Peirong,Hua Renmin.Zhang Bangtong.et al.2002.Post-orogenic of the early Yanshanian(Jurassic)granitoids:Petrological constraints and dynamic background of the earth[J].Science in China(Series D),32(4):279~289(in Chinese).
Chopra P and Wyborn D.2003.Australia's first hot dry rock geothermal energy extraction project is up and running in granite beneath the cooper basin.NE South Australia[A].The Ishihara Symposium:Granite and Associated Met allogenesis[C].
Deng Ping.Shu Liangshu and Tan Zhengzhong.2003.The geological setting for the formation of rich uranium ores in Zhuguang-Guidong large-scale uranium met allogenetic area[J].Geological Review.49(5):486~494(in Chinese with English abstract).
Geology Department of Nanjing University.1981.Granitoids of Different Ages in Southern China and Their Relationship with Mineralization[M].Beijing:Science Press(in Chinese).
Hao Yi.2010.Caledonian Structural Characteristics and Dynamics in South China(Doctoral dissertation)[D].Ocean University of China(in Chinese with English abstract).
He L J.2015.Thermal regime of the North China Cra ton:Implications forcarton destruction[J].Earth-Science Reviews.140:14~26.
Hu S,He L and Wang J.2000.Heat flow in the continental area of China:A new data set[J].Earth and Planetary Science Letters.179(2):407~419.
Hu Shengbiao,He Lijuan and Wang Jiyang.2001.Complation of heat flow data in the China continental area(3rd edition)[J].Chinese Journal of Geophysics.44(5):611~626(in Chinese with English abstract).
Hu Shengbiao and Wang Jiyang.1994.Heat production rate of the crust with mantle heat flow in the southeast China[J].Science in China(Series B).2:185~196(in Chinese).
Hua Renmin.Chen Peirong.Zhang Wenlan.et al.2005.Met allogeneses and their geodynamic settings related to Mesozoic granitoids in the Nanling range[J].Geological Journal of China Universities.11(3):601~601(in Chinese with English abstract).
Huang H Q,Li X H,Li Z X,et al.2015.Formation of the Jurassic South China large granitic orovince:Insights from the genesis of the Jiufeng pluton[J].Chemical Geology,401:43~58.
Li Guohua.2008.Discussion on genesis of the Zhangzhou Basin-A diffrencially erosioned basin rather than a fault-depressed basin[J].Geological Review,54(2):199~206(in Chinese with English abstract).
Li Xianhua,Hu Ruizhong and Lin Jinrong.1997.Geochronology and geochemistry of Cretaceous mafic dikes from Northern Guangdong,SE China[J].Geochimica,26(2):14~31(in Chinese with English abstract).
Li Xianhua,Li Wuxian and Li Zhengxiang.2007.Genetic types and tectonic significance of early Yanshan Nanling granite[J].Chinese science Bulletin,52(9):981~991(in Chinese with English abstract).
Li Z,Qiu J S and Yang X.2014.A review of the geochronology and geochemistryof Late Yanshanian(Cretaceous)plutons along the Fujian costal area of southeastern China:Implications for magma evolution related to slabbreak-off and rollback in the Cretaceous[J].Earth-Science Reviews,128(1):232~248.
Lin Wenjing,Liu Zhiming,Ma Feng,et al.2012.An estimation of HDR resources in China's mainland[J].Acta Geoscientica Sinica,(5):807~811(in Chinese with English abstract).
Liu Changshi,Chen Xiaoming,Wang Rucheng,et al.2003.Origin of Nankunshan aluminous A-type granite,Longkou County,Guangdong Province[J].Acta Petrologica et Mineralogica,22(1):1~10(in Chinese with English abstract).
Ma Feng,Sun Hongli,Lin Wenjing,et al.2015.Target site selection and index matrix evaluation of EGS trial project in China[J].Science and Technology Review,(8):41~47(in Chinese with English abstract).
Ma Xingyuan,Liu Hefu,Wang Weixiang,et al.1983.Meso-Cenozoic taphrogeny and extensional tectonics in eastern China[J].Acta Geologica Sinica,(1):24~34(in Chinese with English abstract).
McLaren S,Sandiford M,Hand M,et al.2003.The hot southern continent:Heat flow and heat production in Australian Proterozoic terranes[J].Geological Society of America Special Papers,372(22):151~161.
Morgan P.1984.The thermal structure and thermal evolution of'the continental lithosphere[J].Physics and Chemistry of the Earth,15:107~193.
Nyblade A A and Pollack H N.1993.A global analysis of heat flow from Precambrian terrains:implications for the thermal structure of Archeanand Proterozoic lithosphere[J].Journal of Geophysical Research:Solid Earth(1978-2012),98(B7):12207~12 218.
Pang Z H.2005.Origin of sulphur compounds and application of isotope geothermometry in selected geothermal systems of China[A].IAEA.Use of Isotopes to Trace the Origin of Acidic Fluid in Geothermal Systems[C].
Pang Zhonghe.1987.Zhangzhou Basin Geothermal System-Genesis Model,Energy Pottential and the Occurrence of Thermal Water(Doctoral dissertation)[D].Beijing:Institute of Geology(in Chinese with English abstract).
Rudnick R L and Fountain D M.1995.Nat ure and composition of the continental crust:A lower crustal perspective[J].Rev.Geophys,33:267~309.
Rybach L.1988.Determination of heat production rate[A].H(a|¨)nel R,Rybach L and Stegena L.Handbook of Terrestrial Heat Flow Density Determination[C].Kluwer,Dordrecht,125~142.
Rybach L.Bodmer P.Pavoni N,et al.1978.Siting Criteria for heat extraction from hot dry rock:Application to Switzerland[J].Pageoph,116(6):1211~1224.
Shen W,Ling H,Li H,et al.2000.The thermal history of the miaroliticgranite at Xincun,Fujian Province,China[J].Chinese Science Bulletin.45(21):1991~1995.
ShenWeizhou,Ling Hongfei,Li Wuxian.et al.1999.Study on the Nd-Sr isotopic compositions of granitoids in SE China[J].Geological Journal of China Universities.(1):22~32(in Chinese with English abstract).
Shu Liangshu and Zhou Xinmin.2002.Late Mesozoic tectonism of southeast China[J].Geological Review,48(3):249-260(in Chinese with English abstract).
Shu Liangshu,Zhou Xinmin,Deng Ping,et al.2004.Geological features and tectonic evolution of Meso-Cenozoic basins in southeastern China[J]Geological Bulletin of China,23(9):876~884(in Chinese with English abstract).
Shu Liangshu,Zhou Xinmin,Deng Ping,et al.2006.Principal geological features of Nanling tectonic belt South China[J].Geological Review,52(2):251~265(in Chinese with English abstract).
Sun Tao.2006.A new map showing the distribution of granites in South China and its explanatory notes[J].Geological Bulletin of China,25(3):332~335(in Chinese without English abstract).
Sun Z,Wang A,Liu J,et al.2015.Radiogenic heat production of granitesand potential for hot dry rock geothermal resource in Guangdong Province.Southern China[A].Proceedings World Geothermal Congress[C].
Wan Jianjun.Sun Zhanxue.Hu Baoqun.et al.2015.Radiogenic geochemistry investigationon granitic rocks from Fogang complex.Northern Guangdong Province and its Implications for Hot Dry rock resource[J].Journal of East China Institute of Technology.38(4):398~406(in Chinese with English abstract).
Wang A.Sun Z and Liu J.2016.Thermal conductivity and radioactive heat-producing element content determinations for rocks from Zhangzhou region.SE China,and their constraints on lithospheric thermal regime[J].Environmental Earth Sciences.75(17):1213.
Wang Andong.Sun Zhanxue.Liu Jinhui et al.2015.Radiogenic heat production of rocks from Zhangzhou.Southeast China and its implications for thermal regime of lithosphere[J].Science and Technology Review.33(24):41~45(in Chinese with English abstract).
Wang Dezi and Zhou Jincheng.1999.Look back and look forward to granite research[J].Acta Petrologica Sinica.15(2):161~169C in Chinese with English abstract).
Wang Dezi and Zhou Xinmin.2002.Petrogenesis and Crustal Evolution of Late Mesozoic Granitic Volcanic Intrusive Complexes in Southeastern China[M].Beijing:Science Press(in Chinese without English abstract).
Wang Guiling.Liu Zhiming and Lin Wenjing.2001.Tectonic control of geothermal resources in the peripheral of Ordos basin[J].Acta Geologica Sinica.78(1):44~51(in Chinese with English abstract).
Wang Guiling.Zhang Fawang and Liu Zhiming.2000.An analysis of present situation and prospects of geothermal energy development and utilization in the world[J].Acta Geoscientia Sinica.21(2):134~139(in Chinese with English abstract).
Wang Jiyang.1996.Low-Medium temperature geothermal system of convective type[J].Earth Science Frontiers(China University of Geosciences.Beijing).(3):96~100(in Chinese with English abstract).
Wang Jiyang and Huang Shaopeng.1988.Complation of heat flow data in the China Continental Area(2rd edition)[J].Seismology and Geology.44(4):351~366(in Chinese with English abstract).
Wang Jiyang.Hu Shengbiao.Pang Zhonghe.et al.2012.Estimate of geothermal resources potential for hot dry rock in the continental area of China[J].Science and Technology Review.30(32):3~10(in Chinese with English abstract).
Wang Lili.2015.Geochemistry and Petrogenesis of Early PaleozoicMesozoic Granites in Ganzhou.Jiangxi Province.South China Block(Doctoral dissertation)[D].China University of Geosciences(Beijing)(in Chinese with English abstract).
Wang Peizong.Chen Yaoan.Cao Baoting,et al.1993.Crust-uppermantle structure and deep structural setting of Fujian Province[J].Geology of Fujian.(2):79~158(in Chinese with English abstract).
Wu Jiansheng.Wang Jialin.Chen Bin.et al.2014.Integrated regional geophysical study on lithospheric structure in eastern China seas and adjacent regions[J].Chinese Journal of Geophysics.57(12):3 884~3 895(in Chinese with English abstract).
Xiong Shaobai and Jin Dongming.1991.Some characteristics of deep structure of the Zhangzhou geothermal field and it's neighbourhood in the Fujian Province[J].Acta Geoscientica Sinica.34(1):55~63(in Chinese with English abstract).
Xu Yan.Hu Yanhua.Gu Mingguang.et al.2013.The tectonic extensional event during the Late Indosinian Period in the southeastern Zhejiang Province:Evidence from the Dashuang pluton in Zhuji Cbunty[J].Acta Petrologica Sinica.29(9):3 131~3 141(in Chinese with English abstract).
Yang Lizhong.2016.The Radioactive Heat-producing Characteristics and the Hot Dry Rock Resources Potential of Prototypes Granite Rocks in Zhangzhou Region(Doctoral dissertation)[D].East China Institute of Technology)(in Chinese with English abstract).
Yang S Y.Jiang S Y.Jiang Y H.et al.2011.Geochemical.zircon UPb dating and Sr-Nd-Hf isotopic constraints on the age and petrogenesis of an Early Cretaceous volcanic-intrusive complex at Xiangshan.Southeast China[J].Mineralogy and Petrology.101(1):21~48.
Yao Jin.Li Jingrong and Ling Zao.2011.Using remote sensing technique to investigate geothermal water in north of Guangdong province.China[J].Journal of Geoinformation Science.13(1):144~150(in Chinese with English abstract).
Yuan Bingqiang and Zhang Guowei.2005.The correlation between the effective elastic thickness of the continental lithosphere and some related geophysical parameters:A case study of the Quanzhou-Heishui geoscience transect[J].Acta Geoscientica Sinica.26(3):203~208(in Chinese with English abstract).
Zhang Bangtong.Ling Hongfei and Chen Peirong.2005.On the relationship between basalt underplating and felsic igneous rock-formation:A case study of the volcano-intrusive complex in Eastrn China[J].Geological Review,51(4):393~400(in Chinese with English abstract).
Zhang Bangtong.Xie Bingrong and Dai Yongshan.1990.The analysis and calculation of metallogenic heat source for granite-type uranium deposits in South China[J].Mineral Deposits.(3):270~278(in Chinese with English abstract).
Zhang Shugen.Yuan Ying and Yao Cuixia.2014.Petrology and orecontrol of Zhuguangshan composite granitic pluton in middle section of Nanling region[J].The Chinese Journal of Nonferrous Metals.(6):1 585~1 598(in Chinese with English abstract).
Zhao Ping.1995.Research of Heat Production in SE China(Doctoral dissertation)[D].Institute of Geology.Chinese Academy of Sciences)(in Chinese).
Zhao Ping.He Lijuan.Liu Shaowen,et al.2015.Terrestrial heat flow of China[A].Wang Jiyang.Geothermics and Its Applications[C](in Chinese).
Zhou Xinmin.2007.Late Mesozoic Granite Genesis and Evolution of Lithospheric Dynamics in Nanling Region[M].Science Press(in Chinese).
Zhou X M and Li W X.2000.Origin of Late Mesozoic igneous rocks in Southeastern China:Implications for lithosphere subduction and underplating of mafic magmas[J].Tectonophysics.326(3~4):269~287.
Zhou X,Shen W,Shu L,et al.2006.Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:A response to tectonic evolution[J].Episodes.29(1):26~33.
柏道远,贾宝华,马铁球,等.2007.湘东南印支期与燕山早期花岗岩成矿能力差异与岩石地球化学特征关系探讨[J].岩石矿物学杂志,26(5):387~398.
包志伟,赵振华.2003.佛冈铝质A型花岗岩的地球化学及其形成环境初探[J].地球与环境,31(1):52~61.
陈培荣,华仁民,章邦桐,等.2002.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学:地球科学,32(4):279~289.
邓平,舒良树,谭正中.2003,诸广-贵东大型铀矿聚集区富铀矿成矿地质条件[J].地质论评,49(5):486~494.
郝义.2010.华南加里东期构造变形特征和动力学机制(博士论文)[D].中国海洋大学.
胡圣标,何丽娟,汪集旸.2001.中国大陆地区大地热流数据汇编(第三版)[J].地球物理学报,44(5):611~626.
胡圣标,黄少鹏.2015.中国陆地大地热流[A].汪集旸,等.地热学及其应用[C].北京:科学出版社,64~122.
胡圣标,汪集旸.1994.中国东南地区地壳生热率与地幔热流[J].中国科学,化学(2):185~196.
华仁民,陈培荣,张文兰,等.2005.南岭与中生代花岗岩类有关的成矿作用及其大地构造背景[J].高校地质学报,11(3):601~601.
李国华.2008.论漳州盆地的成因——是差异侵蚀盆地而非断陷盆地[J].地质论评,54(2):199~206.
李献华,胡瑞忠.1997.粤北白垩纪基性岩脉的年代学和地球化学[J].地球化学,26(2):14~31.
李献华,李武显,李正祥.2007.再论南岭燕山早期花岗岩的成因类型与构造意义[J].科学通报,52(9):981~991.
蔺文静,刘志明,马峰,等.2012.我国陆区干热岩资源潜力估算[J].地球学报,(5):807~811.
刘昌实,陈小明,王汝成,等.2003.广东龙口南昆山铝质A型花岗岩的成因[J].岩石矿物学杂志,22(1):1~10.
马杏垣,刘和甫,王维襄,等.1983.中国东部中、新生代裂陷作用和伸展构造[J].地质学报,(1):24~34.
马峰,孙红丽,蔺文静,等.2015.中国EGS示范工程靶区选址与指标矩阵评价[J].科技导报,(8):41~47.
南京大学地质系.1981.华南不同时代花岗岩类及其与成矿关系[M].北京:科学出版社.
庞忠和.1987.漳州盆地地热系统——成因模式、热能潜力与热水分布规律的研究(博士论文)[D].中国科学院地质研究所.
沈渭洲,凌洪飞,李武显,等.1999.中国东南部花岗岩类Nd-Sr同位素研究[J].高校地质学报,(1):22~32.
舒良树,周新民.2002.中国东南部晚中生代构造作用[J].地质论评,48(3):249~260.
舒良树,周新民,邓平,等.2004.中国东南部中、新生代盆地特征与构造演化[J].地质通报,23(9):876~884.
舒良树,周新民,邓平,等.2006.南岭构造带的基本地质特征[J].地质论评,52(2):251~265.
孙涛.2006.新编华南花岗岩分布图及其说明[J].地质通报,25(3):332~335.
万建军,孙占学,胡宝群,等.2015.广东佛冈岩体放射性地球化学特征及其干热岩资源潜力研究[J].东华理工大学学报(自然科学版),38(4):398~406.
汪集旸.1996.中低温对流型地热系统[J].地学前缘,(3):96~100.
汪集旸,胡圣标,庞忠和,等.2012.中国大陆干热岩地热资源潜力评估[J].科技导报,30(32):3~10.
汪集旸,黄少鹏.1990.中国大陆地区大地热流数据汇编(第二版)[J].地震地质,44(4):351~366.
王丽丽.2015.华南赣州地区早古生代晚期-中生代花岗岩类地球化学与岩石成因(博士论文)[D].中国地质大学(北京).
王安东,孙占学,刘金辉,等.2015.漳州地区岩石放射性地球化学特征及岩石圈热结构[J].科技导报,33(24):41~45.
王德滋,周金城.1999.我国花岗岩研究的回顾与展望[J].岩石学报,15(2):161~169.
王德滋,周新民.2002.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化[M].北京:科学出版社.
王贵玲,刘志明,蔺文静.2004.鄂尔多斯周缘地质构造对地热资源形成的控制作用[J].地质学报,78(1):44~51.
王贵玲,张发旺,刘志明.2000.国内外地热能开发利用现状及前景分析[J].地球学报,21(2):134~139.
王培宗,陈耀安,曹宝庭,等.1993.福建省地壳-上地幔结构及深部构造背景的研究[J]福建地质,(2):79~158.
吴健生,王家林,陈冰,等.2014.中国东部海区岩石层结构的区域综合地球物理研究[J].地球物理学报,57(12):3 884~3 895.
熊绍柏,金东敏.1991.福建漳州地热田及其邻近地区的地壳深部构造特征[J].地球物理学报,34(1):55~63.
徐岩,胡艳华,顾明光,等.2013.浙江东南印支晚期的构造伸展事件:来自诸暨大爽岩体的证据[J].岩石学报,29(9):175~185.
杨立中.2016.漳州地区典型花岗岩体放射性生热特征及干热岩资源潜力研究(博士论文)[D].东华理工大学.
姚金,李静荣,凌造.2011.粤北地热资源遥感调查探测模式与应用[J].地球信息科学学报,13(1):144~150.
袁炳强,张国伟.2005.大陆岩石圈有效弹性厚度与有关地球物理参数的关系——以泉州黑水地学断面为例[J].地球学报,26(3):203~208.
袁学诚.1996.中国地球物理图集[M].地质出版社.
章邦桐,凌洪飞,陈培荣.2005.论玄武岩底侵作用与长英质火成岩形成的关系——以华东南花岗质火山-侵入杂岩为例[J].地质论评,51(4):393~400.
章邦桐,谢炳荣,戴永善.1990.华南花岗岩型铀矿床成矿热源的分析和计算[J].矿床地质,(3):270~278.
张术根,袁莹,姚翠霞.2014.南岭中段诸广山复式花岗岩岩石学及其控矿作用[J].中国有色金属学报,(6):1 585~1 598.
赵平.1995.中国东南地区岩石生热率研究(博士论文)[D].中国科学院地质与地球物理研究所
赵平,何丽娟,刘绍文,等.2015.中国陆地大地热流[A].汪集旸.地热学及其应用[C].北京:科学出版社,186~253.
周新民.2007.南岭地区晚中生代花岗岩成因与岩石圈动力学演化[M].北京:科学出版社.
Bao Zhiwei and Zhao Zhenhua.2003.Geochemistry and tectonic setting of the Fogang aluminous A-type granite,Guangdong province,China—A preliminary study[J].Geology-Geochemistry.31(1):52~61(in Chinese with English abstract).
Cermak V and Rybach L.1987.International conference report:Terrestrial heat flow and the lithosphere structure[J].Geothermics.16(5):583~585.
Chen Peirong,Hua Renmin.Zhang Bangtong.et al.2002.Post-orogenic of the early Yanshanian(Jurassic)granitoids:Petrological constraints and dynamic background of the earth[J].Science in China(Series D),32(4):279~289(in Chinese).
Chopra P and Wyborn D.2003.Australia's first hot dry rock geothermal energy extraction project is up and running in granite beneath the cooper basin.NE South Australia[A].The Ishihara Symposium:Granite and Associated Met allogenesis[C].
Deng Ping.Shu Liangshu and Tan Zhengzhong.2003.The geological setting for the formation of rich uranium ores in Zhuguang-Guidong large-scale uranium met allogenetic area[J].Geological Review.49(5):486~494(in Chinese with English abstract).
Geology Department of Nanjing University.1981.Granitoids of Different Ages in Southern China and Their Relationship with Mineralization[M].Beijing:Science Press(in Chinese).
Hao Yi.2010.Caledonian Structural Characteristics and Dynamics in South China(Doctoral dissertation)[D].Ocean University of China(in Chinese with English abstract).
He L J.2015.Thermal regime of the North China Cra ton:Implications forcarton destruction[J].Earth-Science Reviews.140:14~26.
Hu S,He L and Wang J.2000.Heat flow in the continental area of China:A new data set[J].Earth and Planetary Science Letters.179(2):407~419.
Hu Shengbiao,He Lijuan and Wang Jiyang.2001.Complation of heat flow data in the China continental area(3rd edition)[J].Chinese Journal of Geophysics.44(5):611~626(in Chinese with English abstract).
Hu Shengbiao and Wang Jiyang.1994.Heat production rate of the crust with mantle heat flow in the southeast China[J].Science in China(Series B).2:185~196(in Chinese).
Hua Renmin.Chen Peirong.Zhang Wenlan.et al.2005.Met allogeneses and their geodynamic settings related to Mesozoic granitoids in the Nanling range[J].Geological Journal of China Universities.11(3):601~601(in Chinese with English abstract).
Huang H Q,Li X H,Li Z X,et al.2015.Formation of the Jurassic South China large granitic orovince:Insights from the genesis of the Jiufeng pluton[J].Chemical Geology,401:43~58.
Li Guohua.2008.Discussion on genesis of the Zhangzhou Basin-A diffrencially erosioned basin rather than a fault-depressed basin[J].Geological Review,54(2):199~206(in Chinese with English abstract).
Li Xianhua,Hu Ruizhong and Lin Jinrong.1997.Geochronology and geochemistry of Cretaceous mafic dikes from Northern Guangdong,SE China[J].Geochimica,26(2):14~31(in Chinese with English abstract).
Li Xianhua,Li Wuxian and Li Zhengxiang.2007.Genetic types and tectonic significance of early Yanshan Nanling granite[J].Chinese science Bulletin,52(9):981~991(in Chinese with English abstract).
Li Z,Qiu J S and Yang X.2014.A review of the geochronology and geochemistryof Late Yanshanian(Cretaceous)plutons along the Fujian costal area of southeastern China:Implications for magma evolution related to slabbreak-off and rollback in the Cretaceous[J].Earth-Science Reviews,128(1):232~248.
Lin Wenjing,Liu Zhiming,Ma Feng,et al.2012.An estimation of HDR resources in China's mainland[J].Acta Geoscientica Sinica,(5):807~811(in Chinese with English abstract).
Liu Changshi,Chen Xiaoming,Wang Rucheng,et al.2003.Origin of Nankunshan aluminous A-type granite,Longkou County,Guangdong Province[J].Acta Petrologica et Mineralogica,22(1):1~10(in Chinese with English abstract).
Ma Feng,Sun Hongli,Lin Wenjing,et al.2015.Target site selection and index matrix evaluation of EGS trial project in China[J].Science and Technology Review,(8):41~47(in Chinese with English abstract).
Ma Xingyuan,Liu Hefu,Wang Weixiang,et al.1983.Meso-Cenozoic taphrogeny and extensional tectonics in eastern China[J].Acta Geologica Sinica,(1):24~34(in Chinese with English abstract).
McLaren S,Sandiford M,Hand M,et al.2003.The hot southern continent:Heat flow and heat production in Australian Proterozoic terranes[J].Geological Society of America Special Papers,372(22):151~161.
Morgan P.1984.The thermal structure and thermal evolution of'the continental lithosphere[J].Physics and Chemistry of the Earth,15:107~193.
Nyblade A A and Pollack H N.1993.A global analysis of heat flow from Precambrian terrains:implications for the thermal structure of Archeanand Proterozoic lithosphere[J].Journal of Geophysical Research:Solid Earth(1978-2012),98(B7):12207~12 218.
Pang Z H.2005.Origin of sulphur compounds and application of isotope geothermometry in selected geothermal systems of China[A].IAEA.Use of Isotopes to Trace the Origin of Acidic Fluid in Geothermal Systems[C].
Pang Zhonghe.1987.Zhangzhou Basin Geothermal System-Genesis Model,Energy Pottential and the Occurrence of Thermal Water(Doctoral dissertation)[D].Beijing:Institute of Geology(in Chinese with English abstract).
Rudnick R L and Fountain D M.1995.Nat ure and composition of the continental crust:A lower crustal perspective[J].Rev.Geophys,33:267~309.
Rybach L.1988.Determination of heat production rate[A].H(a|¨)nel R,Rybach L and Stegena L.Handbook of Terrestrial Heat Flow Density Determination[C].Kluwer,Dordrecht,125~142.
Rybach L.Bodmer P.Pavoni N,et al.1978.Siting Criteria for heat extraction from hot dry rock:Application to Switzerland[J].Pageoph,116(6):1211~1224.
Shen W,Ling H,Li H,et al.2000.The thermal history of the miaroliticgranite at Xincun,Fujian Province,China[J].Chinese Science Bulletin.45(21):1991~1995.
ShenWeizhou,Ling Hongfei,Li Wuxian.et al.1999.Study on the Nd-Sr isotopic compositions of granitoids in SE China[J].Geological Journal of China Universities.(1):22~32(in Chinese with English abstract).
Shu Liangshu and Zhou Xinmin.2002.Late Mesozoic tectonism of southeast China[J].Geological Review,48(3):249-260(in Chinese with English abstract).
Shu Liangshu,Zhou Xinmin,Deng Ping,et al.2004.Geological features and tectonic evolution of Meso-Cenozoic basins in southeastern China[J]Geological Bulletin of China,23(9):876~884(in Chinese with English abstract).
Shu Liangshu,Zhou Xinmin,Deng Ping,et al.2006.Principal geological features of Nanling tectonic belt South China[J].Geological Review,52(2):251~265(in Chinese with English abstract).
Sun Tao.2006.A new map showing the distribution of granites in South China and its explanatory notes[J].Geological Bulletin of China,25(3):332~335(in Chinese without English abstract).
Sun Z,Wang A,Liu J,et al.2015.Radiogenic heat production of granitesand potential for hot dry rock geothermal resource in Guangdong Province.Southern China[A].Proceedings World Geothermal Congress[C].
Wan Jianjun.Sun Zhanxue.Hu Baoqun.et al.2015.Radiogenic geochemistry investigationon granitic rocks from Fogang complex.Northern Guangdong Province and its Implications for Hot Dry rock resource[J].Journal of East China Institute of Technology.38(4):398~406(in Chinese with English abstract).
Wang A.Sun Z and Liu J.2016.Thermal conductivity and radioactive heat-producing element content determinations for rocks from Zhangzhou region.SE China,and their constraints on lithospheric thermal regime[J].Environmental Earth Sciences.75(17):1213.
Wang Andong.Sun Zhanxue.Liu Jinhui et al.2015.Radiogenic heat production of rocks from Zhangzhou.Southeast China and its implications for thermal regime of lithosphere[J].Science and Technology Review.33(24):41~45(in Chinese with English abstract).
Wang Dezi and Zhou Jincheng.1999.Look back and look forward to granite research[J].Acta Petrologica Sinica.15(2):161~169C in Chinese with English abstract).
Wang Dezi and Zhou Xinmin.2002.Petrogenesis and Crustal Evolution of Late Mesozoic Granitic Volcanic Intrusive Complexes in Southeastern China[M].Beijing:Science Press(in Chinese without English abstract).
Wang Guiling.Liu Zhiming and Lin Wenjing.2001.Tectonic control of geothermal resources in the peripheral of Ordos basin[J].Acta Geologica Sinica.78(1):44~51(in Chinese with English abstract).
Wang Guiling.Zhang Fawang and Liu Zhiming.2000.An analysis of present situation and prospects of geothermal energy development and utilization in the world[J].Acta Geoscientia Sinica.21(2):134~139(in Chinese with English abstract).
Wang Jiyang.1996.Low-Medium temperature geothermal system of convective type[J].Earth Science Frontiers(China University of Geosciences.Beijing).(3):96~100(in Chinese with English abstract).
Wang Jiyang and Huang Shaopeng.1988.Complation of heat flow data in the China Continental Area(2rd edition)[J].Seismology and Geology.44(4):351~366(in Chinese with English abstract).
Wang Jiyang.Hu Shengbiao.Pang Zhonghe.et al.2012.Estimate of geothermal resources potential for hot dry rock in the continental area of China[J].Science and Technology Review.30(32):3~10(in Chinese with English abstract).
Wang Lili.2015.Geochemistry and Petrogenesis of Early PaleozoicMesozoic Granites in Ganzhou.Jiangxi Province.South China Block(Doctoral dissertation)[D].China University of Geosciences(Beijing)(in Chinese with English abstract).
Wang Peizong.Chen Yaoan.Cao Baoting,et al.1993.Crust-uppermantle structure and deep structural setting of Fujian Province[J].Geology of Fujian.(2):79~158(in Chinese with English abstract).
Wu Jiansheng.Wang Jialin.Chen Bin.et al.2014.Integrated regional geophysical study on lithospheric structure in eastern China seas and adjacent regions[J].Chinese Journal of Geophysics.57(12):3 884~3 895(in Chinese with English abstract).
Xiong Shaobai and Jin Dongming.1991.Some characteristics of deep structure of the Zhangzhou geothermal field and it's neighbourhood in the Fujian Province[J].Acta Geoscientica Sinica.34(1):55~63(in Chinese with English abstract).
Xu Yan.Hu Yanhua.Gu Mingguang.et al.2013.The tectonic extensional event during the Late Indosinian Period in the southeastern Zhejiang Province:Evidence from the Dashuang pluton in Zhuji Cbunty[J].Acta Petrologica Sinica.29(9):3 131~3 141(in Chinese with English abstract).
Yang Lizhong.2016.The Radioactive Heat-producing Characteristics and the Hot Dry Rock Resources Potential of Prototypes Granite Rocks in Zhangzhou Region(Doctoral dissertation)[D].East China Institute of Technology)(in Chinese with English abstract).
Yang S Y.Jiang S Y.Jiang Y H.et al.2011.Geochemical.zircon UPb dating and Sr-Nd-Hf isotopic constraints on the age and petrogenesis of an Early Cretaceous volcanic-intrusive complex at Xiangshan.Southeast China[J].Mineralogy and Petrology.101(1):21~48.
Yao Jin.Li Jingrong and Ling Zao.2011.Using remote sensing technique to investigate geothermal water in north of Guangdong province.China[J].Journal of Geoinformation Science.13(1):144~150(in Chinese with English abstract).
Yuan Bingqiang and Zhang Guowei.2005.The correlation between the effective elastic thickness of the continental lithosphere and some related geophysical parameters:A case study of the Quanzhou-Heishui geoscience transect[J].Acta Geoscientica Sinica.26(3):203~208(in Chinese with English abstract).
Zhang Bangtong.Ling Hongfei and Chen Peirong.2005.On the relationship between basalt underplating and felsic igneous rock-formation:A case study of the volcano-intrusive complex in Eastrn China[J].Geological Review,51(4):393~400(in Chinese with English abstract).
Zhang Bangtong.Xie Bingrong and Dai Yongshan.1990.The analysis and calculation of metallogenic heat source for granite-type uranium deposits in South China[J].Mineral Deposits.(3):270~278(in Chinese with English abstract).
Zhang Shugen.Yuan Ying and Yao Cuixia.2014.Petrology and orecontrol of Zhuguangshan composite granitic pluton in middle section of Nanling region[J].The Chinese Journal of Nonferrous Metals.(6):1 585~1 598(in Chinese with English abstract).
Zhao Ping.1995.Research of Heat Production in SE China(Doctoral dissertation)[D].Institute of Geology.Chinese Academy of Sciences)(in Chinese).
Zhao Ping.He Lijuan.Liu Shaowen,et al.2015.Terrestrial heat flow of China[A].Wang Jiyang.Geothermics and Its Applications[C](in Chinese).
Zhou Xinmin.2007.Late Mesozoic Granite Genesis and Evolution of Lithospheric Dynamics in Nanling Region[M].Science Press(in Chinese).
Zhou X M and Li W X.2000.Origin of Late Mesozoic igneous rocks in Southeastern China:Implications for lithosphere subduction and underplating of mafic magmas[J].Tectonophysics.326(3~4):269~287.
Zhou X,Shen W,Shu L,et al.2006.Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:A response to tectonic evolution[J].Episodes.29(1):26~33.
柏道远,贾宝华,马铁球,等.2007.湘东南印支期与燕山早期花岗岩成矿能力差异与岩石地球化学特征关系探讨[J].岩石矿物学杂志,26(5):387~398.
包志伟,赵振华.2003.佛冈铝质A型花岗岩的地球化学及其形成环境初探[J].地球与环境,31(1):52~61.
陈培荣,华仁民,章邦桐,等.2002.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学:地球科学,32(4):279~289.
邓平,舒良树,谭正中.2003,诸广-贵东大型铀矿聚集区富铀矿成矿地质条件[J].地质论评,49(5):486~494.
郝义.2010.华南加里东期构造变形特征和动力学机制(博士论文)[D].中国海洋大学.
胡圣标,何丽娟,汪集旸.2001.中国大陆地区大地热流数据汇编(第三版)[J].地球物理学报,44(5):611~626.
胡圣标,黄少鹏.2015.中国陆地大地热流[A].汪集旸,等.地热学及其应用[C].北京:科学出版社,64~122.
胡圣标,汪集旸.1994.中国东南地区地壳生热率与地幔热流[J].中国科学,化学(2):185~196.
华仁民,陈培荣,张文兰,等.2005.南岭与中生代花岗岩类有关的成矿作用及其大地构造背景[J].高校地质学报,11(3):601~601.
李国华.2008.论漳州盆地的成因——是差异侵蚀盆地而非断陷盆地[J].地质论评,54(2):199~206.
李献华,胡瑞忠.1997.粤北白垩纪基性岩脉的年代学和地球化学[J].地球化学,26(2):14~31.
李献华,李武显,李正祥.2007.再论南岭燕山早期花岗岩的成因类型与构造意义[J].科学通报,52(9):981~991.
蔺文静,刘志明,马峰,等.2012.我国陆区干热岩资源潜力估算[J].地球学报,(5):807~811.
刘昌实,陈小明,王汝成,等.2003.广东龙口南昆山铝质A型花岗岩的成因[J].岩石矿物学杂志,22(1):1~10.
马杏垣,刘和甫,王维襄,等.1983.中国东部中、新生代裂陷作用和伸展构造[J].地质学报,(1):24~34.
马峰,孙红丽,蔺文静,等.2015.中国EGS示范工程靶区选址与指标矩阵评价[J].科技导报,(8):41~47.
南京大学地质系.1981.华南不同时代花岗岩类及其与成矿关系[M].北京:科学出版社.
庞忠和.1987.漳州盆地地热系统——成因模式、热能潜力与热水分布规律的研究(博士论文)[D].中国科学院地质研究所.
沈渭洲,凌洪飞,李武显,等.1999.中国东南部花岗岩类Nd-Sr同位素研究[J].高校地质学报,(1):22~32.
舒良树,周新民.2002.中国东南部晚中生代构造作用[J].地质论评,48(3):249~260.
舒良树,周新民,邓平,等.2004.中国东南部中、新生代盆地特征与构造演化[J].地质通报,23(9):876~884.
舒良树,周新民,邓平,等.2006.南岭构造带的基本地质特征[J].地质论评,52(2):251~265.
孙涛.2006.新编华南花岗岩分布图及其说明[J].地质通报,25(3):332~335.
万建军,孙占学,胡宝群,等.2015.广东佛冈岩体放射性地球化学特征及其干热岩资源潜力研究[J].东华理工大学学报(自然科学版),38(4):398~406.
汪集旸.1996.中低温对流型地热系统[J].地学前缘,(3):96~100.
汪集旸,胡圣标,庞忠和,等.2012.中国大陆干热岩地热资源潜力评估[J].科技导报,30(32):3~10.
汪集旸,黄少鹏.1990.中国大陆地区大地热流数据汇编(第二版)[J].地震地质,44(4):351~366.
王丽丽.2015.华南赣州地区早古生代晚期-中生代花岗岩类地球化学与岩石成因(博士论文)[D].中国地质大学(北京).
王安东,孙占学,刘金辉,等.2015.漳州地区岩石放射性地球化学特征及岩石圈热结构[J].科技导报,33(24):41~45.
王德滋,周金城.1999.我国花岗岩研究的回顾与展望[J].岩石学报,15(2):161~169.
王德滋,周新民.2002.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化[M].北京:科学出版社.
王贵玲,刘志明,蔺文静.2004.鄂尔多斯周缘地质构造对地热资源形成的控制作用[J].地质学报,78(1):44~51.
王贵玲,张发旺,刘志明.2000.国内外地热能开发利用现状及前景分析[J].地球学报,21(2):134~139.
王培宗,陈耀安,曹宝庭,等.1993.福建省地壳-上地幔结构及深部构造背景的研究[J]福建地质,(2):79~158.
吴健生,王家林,陈冰,等.2014.中国东部海区岩石层结构的区域综合地球物理研究[J].地球物理学报,57(12):3 884~3 895.
熊绍柏,金东敏.1991.福建漳州地热田及其邻近地区的地壳深部构造特征[J].地球物理学报,34(1):55~63.
徐岩,胡艳华,顾明光,等.2013.浙江东南印支晚期的构造伸展事件:来自诸暨大爽岩体的证据[J].岩石学报,29(9):175~185.
杨立中.2016.漳州地区典型花岗岩体放射性生热特征及干热岩资源潜力研究(博士论文)[D].东华理工大学.
姚金,李静荣,凌造.2011.粤北地热资源遥感调查探测模式与应用[J].地球信息科学学报,13(1):144~150.
袁炳强,张国伟.2005.大陆岩石圈有效弹性厚度与有关地球物理参数的关系——以泉州黑水地学断面为例[J].地球学报,26(3):203~208.
袁学诚.1996.中国地球物理图集[M].地质出版社.
章邦桐,凌洪飞,陈培荣.2005.论玄武岩底侵作用与长英质火成岩形成的关系——以华东南花岗质火山-侵入杂岩为例[J].地质论评,51(4):393~400.
章邦桐,谢炳荣,戴永善.1990.华南花岗岩型铀矿床成矿热源的分析和计算[J].矿床地质,(3):270~278.
张术根,袁莹,姚翠霞.2014.南岭中段诸广山复式花岗岩岩石学及其控矿作用[J].中国有色金属学报,(6):1 585~1 598.
赵平.1995.中国东南地区岩石生热率研究(博士论文)[D].中国科学院地质与地球物理研究所
赵平,何丽娟,刘绍文,等.2015.中国陆地大地热流[A].汪集旸.地热学及其应用[C].北京:科学出版社,186~253.
周新民.2007.南岭地区晚中生代花岗岩成因与岩石圈动力学演化[M].北京:科学出版社.