福建大田广平推覆构造特征及地质意义
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摘要
福建省内各类推覆构造是广泛存在的,并具有一定的规模。广平推覆构造位于福建省大田县北部广平—建爱,太华—上京一带,是福建省境内发育最完整,且面积较大的一个推覆构造。推覆构造南北长大于20km,东西宽大于12km,面积大于100 km~2。
本文综合运用构造地质学、岩石学、同位素地质年代学、数学建模、统计分析、平衡面积法等多种方法,研究总结了广平推覆构造几何学、运动学、年代学特征并得出初步的动力学模式。得出结论如下:
1.广平推覆构造的外来岩系、原地岩系从宏观到微观变形特征不同,外来岩系表现为堆垛式、叠瓦式断层,原地岩系表现为褶皱发育。该区作为闽西南推覆构造的前缘带,受到推覆构造强烈挤压,推覆面波状起伏。
2.经过比对汤泉花岗闪长岩岩体和花岗斑岩脉,发现花岗斑岩脉比汤泉岩体对于说明推覆构造的年代学特征更有意义,对花岗斑岩脉进行锆石U-Pb测年研究,本文认为广平推覆构造发生于142±1Ma。
3.应用面积平衡方法对原地岩系能干性较差的童子岩组含煤地层做了地层缩短率的估算,并给出计算结果的不确定度。认为缩短率为(10.94±0.32)%。
4.研究区内的白云母二长花岗岩在岩石学、岩石地球化学、岩相学、同位素年代学方面与顺昌地区的张坊岩体有着较高的相似性,本文认为张坊岩体很可能是广平推覆构造外来岩系的源头。因此,对外来岩系起源的问题建立数学模型,综合考虑到郑和—大埔断裂的左旋走滑影响,认为广平推覆构造推覆距离介于55~105km之间,方向是北西60°到南北方向之间。
5.广平推覆构造是由于燕山期伊佐奈崎板块向欧亚板块俯冲、挤压,中国大陆逆时针旋转,从而使闽西南地区出现大规模的推覆构造。
Nappe structure of a certain scale exists extensively in Fujian province. Guangping nappe structure is located in the area of Guangping-Jian’ai and Taihua-Shangjing, in the north of Datian county, Fujian province. It is the most complete nappe structure with large area in Fujian province. It is 20 kilometers from north to south and 12 kilometers from east to west, covering an area of over 100 square kilometers.
This paper carries out the theories and methods in structural geology, petrology, isotopic geochronology, mathematical modeling, statistic analysis, area balancing to study the characteristics of geometry, kinematics and chronology of Guangping nappe structure and to work out a preliminary dynamic model. We draw conclusions as follows:
1. The allochthone marked by imbricate faults and the autochthone marked by folds of Guangping nappe structure are much different in characteristics of deformation from macroscopic to microcosmic. Located in Southwest Fujian nappe frontal belt, the study area is compressed intensively by the nappe structure, with undulating plane.
2. A comparison between the Tangquan granodiorite and the granite porphyry proves it can be more significant to use the age of the granite porphyry to describe the characteristics of chronology of Guangping nappe structure than that of the Tangquan granodiorite. U-Pb dating of zircons from the granite porphyry gives an age of 142±1Ma, indicating the age for the formation of Guangping nappe structure.
3. We used the area balancing method to calculate shortening estimates and analyze the errors of the incompetent coal-bearing stratum in the Tongziyan Formation belonging to autochthone. The result is 10.94±0.32% shortening.
4. There is good similarity in petrology, lithogeochemistry, facieology and isotopic geochronology between the muscovite monzonitic granite in the study area and the Zhangfang granitoid in Shunchang area. The Zhangfang granitoid is likely to be the source of the autochthone of Guangping nappe structure. In this case, we found mathematical model on the problem of the source of the autochthone. In consideration of the affect of the left-lateral slip of the Zhenghe-Dabu fault, we draw a conclusion that the thrusting distance is between 55 to 105 kilometers, with a direction of N60W to N-S.
5. Guangping nappe structure is the result of the subduction and the compression of the Izanagi plate underneath the Eurasian plate, with counter-clockwise rotation of the continent during Yanshanian.
本文综合运用构造地质学、岩石学、同位素地质年代学、数学建模、统计分析、平衡面积法等多种方法,研究总结了广平推覆构造几何学、运动学、年代学特征并得出初步的动力学模式。得出结论如下:
1.广平推覆构造的外来岩系、原地岩系从宏观到微观变形特征不同,外来岩系表现为堆垛式、叠瓦式断层,原地岩系表现为褶皱发育。该区作为闽西南推覆构造的前缘带,受到推覆构造强烈挤压,推覆面波状起伏。
2.经过比对汤泉花岗闪长岩岩体和花岗斑岩脉,发现花岗斑岩脉比汤泉岩体对于说明推覆构造的年代学特征更有意义,对花岗斑岩脉进行锆石U-Pb测年研究,本文认为广平推覆构造发生于142±1Ma。
3.应用面积平衡方法对原地岩系能干性较差的童子岩组含煤地层做了地层缩短率的估算,并给出计算结果的不确定度。认为缩短率为(10.94±0.32)%。
4.研究区内的白云母二长花岗岩在岩石学、岩石地球化学、岩相学、同位素年代学方面与顺昌地区的张坊岩体有着较高的相似性,本文认为张坊岩体很可能是广平推覆构造外来岩系的源头。因此,对外来岩系起源的问题建立数学模型,综合考虑到郑和—大埔断裂的左旋走滑影响,认为广平推覆构造推覆距离介于55~105km之间,方向是北西60°到南北方向之间。
5.广平推覆构造是由于燕山期伊佐奈崎板块向欧亚板块俯冲、挤压,中国大陆逆时针旋转,从而使闽西南地区出现大规模的推覆构造。
Nappe structure of a certain scale exists extensively in Fujian province. Guangping nappe structure is located in the area of Guangping-Jian’ai and Taihua-Shangjing, in the north of Datian county, Fujian province. It is the most complete nappe structure with large area in Fujian province. It is 20 kilometers from north to south and 12 kilometers from east to west, covering an area of over 100 square kilometers.
This paper carries out the theories and methods in structural geology, petrology, isotopic geochronology, mathematical modeling, statistic analysis, area balancing to study the characteristics of geometry, kinematics and chronology of Guangping nappe structure and to work out a preliminary dynamic model. We draw conclusions as follows:
1. The allochthone marked by imbricate faults and the autochthone marked by folds of Guangping nappe structure are much different in characteristics of deformation from macroscopic to microcosmic. Located in Southwest Fujian nappe frontal belt, the study area is compressed intensively by the nappe structure, with undulating plane.
2. A comparison between the Tangquan granodiorite and the granite porphyry proves it can be more significant to use the age of the granite porphyry to describe the characteristics of chronology of Guangping nappe structure than that of the Tangquan granodiorite. U-Pb dating of zircons from the granite porphyry gives an age of 142±1Ma, indicating the age for the formation of Guangping nappe structure.
3. We used the area balancing method to calculate shortening estimates and analyze the errors of the incompetent coal-bearing stratum in the Tongziyan Formation belonging to autochthone. The result is 10.94±0.32% shortening.
4. There is good similarity in petrology, lithogeochemistry, facieology and isotopic geochronology between the muscovite monzonitic granite in the study area and the Zhangfang granitoid in Shunchang area. The Zhangfang granitoid is likely to be the source of the autochthone of Guangping nappe structure. In this case, we found mathematical model on the problem of the source of the autochthone. In consideration of the affect of the left-lateral slip of the Zhenghe-Dabu fault, we draw a conclusion that the thrusting distance is between 55 to 105 kilometers, with a direction of N60W to N-S.
5. Guangping nappe structure is the result of the subduction and the compression of the Izanagi plate underneath the Eurasian plate, with counter-clockwise rotation of the continent during Yanshanian.
引文
[1] A.Chen, Mirror-image thrusting in the South China Orogenic Belt: tectonic evidence from western Fujian, southeastern China, Tectonophysics, 1999
[2] Bevington, P.R., and Robinson, D.K., , Data 246 reduction and error analysis:, New York, McGraw-Hill Higher Education:320 p., 2003
[3] Harris, J.W., and St?cker, H., , Handbook of mathematics and computational science:, New York, Springer, 1028 p., 1998
[4] Mc Quarrie, N., Ehlers, T.A., Barnes, J.B., and Meade, B., , Temporal variation in climate and tectonic coupling in the central Andes:, Geology, v. 36, no. 12, pp. 999-1002, doi:10.1130/G25124A.1., 2008
[5] Phoebe A.Judge and Richard W.Allmendinger, Error propagation in balanced cross sections and the significance of shortening variations in the central Andes, Geological Society of America, 2009
[6] Wenjiao Xiao, Haiqing He, Early Mesozoic thrust tectonics of the northwest Zhejiang region, Geological Society of America, 2005
[7]鲍继坤,福建高陂矿区构造演化分析,煤田地质与勘探, 2007, 35(5):6-10 , 2007
[8]陈爱根,吴正文,福建宁化湖村盆地构造解析及其地质意义,地质评论, 1996, 42(3):193-199 , 1996
[9]陈爱根,吴正文,闽西地区逆冲推覆构造格局及其演化,中国区域地质, 1996, 12(4):335-343 , 1996
[10]陈柏林,黄仁生,谢艳霞,叶允均,吴淦国,福建蒲洋变质核杂岩构造及其控矿作用初探,福建地质, 1998, 17(3):139-146, 1998
[11]陈火炮,李敬珠,福建顺昌山后铅锌矿床地质特征及成因探讨,福建地质, 2008, 27(2):204-210, 2008
[12]陈锦麟,论闽西北推覆体构造,西部探矿工程2008, 20(11):153-155, 2008
[13]陈开彪,福建省大田县广平含煤区推覆构造特征及找煤预测,中国煤田地质, 2006, 18(2):16-17, 70, 2006
[14]陈泉霖,福建龙岩白沙南煤矿区煤层的形变特征及变化规律分析,中国煤田地质, 2007,19(3):17-18 , 2007
[15]陈润生,林东燕,江剑丽,福建早侏罗世火山作用的动力学机制及大地构造学意义探讨,福建地质, 2008, 27(2):156-165, 2007
[16]戴定贤,福建省天湖山煤矿区F31推覆断层及找煤方向探讨,中国煤矿地质, 2009, 21(3):6-10, 2009
[17]方如健,福建政和星溪金矿床构造控矿特征及找矿前景,福建地质, 2007, 26(1):20-26 , 2006
[18]傅树超,福建省将乐顺昌一带中—上石炭统碎屑岩的发现及其地质意义,福建地质, 1988, (3), 1988
[19]关玉祥,杨添水,福建省推覆构造研究及其意义,福建地质, 1994, 13(4):248-277, 1994
[20]韩胜康,福建永定新村钼铅锌多金属矿床地质特征及成因探讨,福建地质, 2008, 27(4):352-360, 2008
[21]黄昌旗,曹明志,闽西南回龙地区逆冲推覆构造,福建地质, 2002, 21(2):85-90, 2001
[22]黄春鹏,刘庆生,张克尧,福建紫金山铜金矿田地球物理地球化学特征及找矿模型,福建地质, 1999, 18(4):189-206, 1999
[23]黄道锐,福建南平巨口白石岩钼矿床地质特征及成因探讨,福建地质, 2008, 27(3):275-280, 2007
[24]黄和,福建省广平煤矿区推覆体下煤系地层构造特征,中国煤炭地质, 2009, 21(8):12-14, 2009
[25]黄家龙,福建将乐盖竹洋绿片岩地质特征及构造环境探讨,福建地质, 2001, 20(4):177-184, 2001
[26]黄仁生,福建尤溪梅仙矿田铅锌银矿床特征及找矿方向,福建地质, 2007, 26(4):211-221 , 2006
[27]黄仁生,福建大田广平推覆构造与隐伏煤、多金属矿,福建地质, 2007, 26(3):142-150 , 2007
[28]黄尚泉,龙永煤田四集矿区逆冲推覆构造特征与找煤分析,煤炭技术, 2009, 28(1):134-137, 2009
[29]黄廷淦,揭育金,福建明溪盆地成因探讨,福建地质, 1999, 18(1):1-5 , 1998
[30]黄长煌,福建大田建爱地区多金属矿的构造特征及其成矿意义,福建地质, 1999, 18(1):6-11, 1999
[31]揭育金,庄建民,黄泉祯,郑声俭,福建长汀童坊地区推覆构造,福建地质, 2001, 20(4):157-162, 2001
[32]李观富,福建晚古生代地层中推覆构造成因机制,福建地质, 1989, 8(1):35-45, 1978
[33]李兼海,福建省构造运动_构造层划分及其主要特征,福建地质, 1998, 17(3):115-130 , 1998
[34]李其康,福建永定高陂煤矿区构造控煤作用分析,能源与环境, 2008(3):89-90, 2008
[35]李学燮,张开毕,揭育金,张引娥,闽西北将乐地区大源片麻岩的地质特征,中国区域地质, 2001, 20(1):39-45, 2001
[36]练光春,福建永定龙川矿区构造特征及其演化过程,中国煤田地质2004, 16(Z1):26-27, 2004
[37]梁乐辉,福建莆田泗洋铅锌矿地质特征及成因探讨,福建地质, 2008, 27(3):259-266, 2008
[38]林传勇,史兰斌,陈孝德,韩秀玲,福建明溪上地幔热结构及流变学特征,地质评论, 1999, 45(4):352-360, 1999
[39]林全胜,福建三明吉口矿区推覆构造特征与控煤作用,福建地质, 2009, 28(4):275-280, 2009
[40]林增品,福建大田地区下二叠统童子岩组底部砾岩层,福建地质, 1991, 10(3):205-210, 1991
[41]刘玉萍,张洁,尹宏伟,徐士进,面积平衡法与川东大池干推覆带区域滑脱面预测,大地构造与成矿学, 2008, 32(4):410-417, 2008
[42]卢聪生,福建龙岩吕凤矿区构造特征及其演化,煤, 2008, 17(7):39-42, 2008
[43]卢聪生,福建永定东中矿区控煤构造特征及其对含煤地层的影响,中国西部科技, 2008, 7(16):4-6, 2008
[44]卢清地,福建中生代火山活动的基本特征及构造环境,岩石矿物学杂志, 2001, 20(1):57-68, 2001
[45]马金清,福建若干基础地质问题及研究方向探讨,福建地质, 2002, 21(4):200-205, 2002
[46]毛建仁,陈荣,李寄嵎,叶海敏,赵希林,闽西南地区晚中生代花岗质岩石的同位素年代学、地球化学及其构造演化,岩石学报, 2006, 22(6):1723-1734, 2006
[47]毛建仁,陶奎元,李寄嵎,谢芳贵,闽西南地区中生代花岗闪长质岩石的特征及其构造演化,岩石矿物学杂志, 2002, 21(2):135-142, 2002
[48]毛建仁,陶奎元,谢芳贵,许乃政,陈三元,闽西南地区成岩成矿作用与构造环境,岩石矿物学杂志, 2001, 20(3):329-336, 2001
[49]毛建仁,许乃政,胡青,李寄嵎,谢芳,闽西南地区中生代花岗闪长质岩石的同位素年代学、地球化学及其构造演化,吉林大学学报(地球科学版), 2004, 34(1):12-20, 2004
[50]莫一迪,福建大田县高峰岬铅锌多金属矿区构造特征及其成矿作用,矿业天地, 2008(23):653-654, 2008
[51]沈荣泉,福建省将乐县肖公洞钨矿成矿规律研究,中国西部科技, 2008, 7(23):1-3, 2007
[52]孙淑静,李星,宋立军,周珍琦,冯常茂,闽西南苏桥-小溪洋井田推(滑)覆构造形成演化,煤田地质与勘探, 2008, 36(3):6-11, 2008
[53]唐来发,龙永煤田推覆构造特征及找煤预测,能源与环境, 2009(3):61-63, 2009
[54]陶建华,闽西南地区东部逆冲推覆构造及其形成机制,福建地质, 1987, (4) , 1987
[55]陶建华,福建推覆构造研究与找矿突破,福建地质, 2008.27(2):105-124, 2008
[56]陶建华,陈福龙,福建推覆构造研究,石油实验地质, 2006, 28(3):259-263, 285, 2006
[57]陶于祥,福建前寒武纪基底构造格局及演化浅析,中国区域地质, 1997, 16(1):60-65, 110, 1997
[58]万天丰,中国大地构造学纲要,地质出版社:135-151, 2004
[59]王尔康,欧阳钟辉,刘聪,福建大田推覆构造群的发现及其地质意义,科学通报, 1985, 30(3):203-203 , 1985
[60]王国平,福建印支运动基本特征探讨,福建地质, 1983, (2) , 1983
[61]王绍雄,福建境内壳幔成分和岩石圈构造的演化与成矿作用的关系,福建地质, 2003, 22(2):89-100, 2003
[62]韦德光,揭育金,黄廷淦,福建省区域地质构造特征,中国区域地质, 1997, 16(2):162-170, 1997
[63]游天寿,黄新鹏,福建将乐一带白云母化花岗岩成因的初步探讨,福建地质, 1989, 8(3):225-234, T001 , 1989
[64]余学东,邵跃,李应桂,福建紫金山铜金矿床地质地球化学找矿模型及应用,物探与化探, 1995, 19(5):321-331 , 1995
[65]张贵山,温汉捷,胡瑞忠,裘愉卓,福建新生代碱性超基性火山岩地球化学特征及构造意义,地质学报, 2009, 83(2):284-294, 2009
[66]张家菁,陈郑辉,王登红,陈振宇,刘善宝,王成辉,福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义,大地构造与成矿学, 2008, 32(1):92-97, 2007
[67]张小亮,福建省大田县姜坑铅锌成矿带成矿地质特征及成矿模式,矿业天地, 2008(24):635-637, 2008
[68]赵荣文,陈柏林,吴淦国,黄仁生,吴建设,福建尤溪肖板地区构造与金矿化的关系,有色金属矿产与勘查, 1999, 8(3):147-152, 1999
[69]赵希林,毛建仁,陈荣,许乃政,曾庆涛,叶海敏,闽西南地区才溪岩体锆石SHRIMP定年及其地球化学特征,岩石矿物学杂志, 2007, 26(3):223-231, 2007
[70]郑志强,苏江湖,马金清,闽北仁寿地区逆冲推覆构造,福建地质, 2001, 20(2):78-86, 2000
[71]周汉民,王文斌,福建德化杨梅地区金矿成矿地质条件和矿床成因,火山地质与矿产, 1996, (Z1) , 1996
[72]周珍琦,闽西南地区推覆构造特征,石油实验地质, 2006, 28(1):38-41 , 2006
[73]周珍琦,闽西南地区推覆构造形成的动力学机制——以广平推覆构造为例,石油实验地质, 2007, 29(2):128-132 , 2007
[74]朱根灵,福建前寒武纪地体中的锆石U-Pb同位素年龄的地质意义,地质调查与研究, 2007, 30(1):13-21 , 2007
[2] Bevington, P.R., and Robinson, D.K., , Data 246 reduction and error analysis:, New York, McGraw-Hill Higher Education:320 p., 2003
[3] Harris, J.W., and St?cker, H., , Handbook of mathematics and computational science:, New York, Springer, 1028 p., 1998
[4] Mc Quarrie, N., Ehlers, T.A., Barnes, J.B., and Meade, B., , Temporal variation in climate and tectonic coupling in the central Andes:, Geology, v. 36, no. 12, pp. 999-1002, doi:10.1130/G25124A.1., 2008
[5] Phoebe A.Judge and Richard W.Allmendinger, Error propagation in balanced cross sections and the significance of shortening variations in the central Andes, Geological Society of America, 2009
[6] Wenjiao Xiao, Haiqing He, Early Mesozoic thrust tectonics of the northwest Zhejiang region, Geological Society of America, 2005
[7]鲍继坤,福建高陂矿区构造演化分析,煤田地质与勘探, 2007, 35(5):6-10 , 2007
[8]陈爱根,吴正文,福建宁化湖村盆地构造解析及其地质意义,地质评论, 1996, 42(3):193-199 , 1996
[9]陈爱根,吴正文,闽西地区逆冲推覆构造格局及其演化,中国区域地质, 1996, 12(4):335-343 , 1996
[10]陈柏林,黄仁生,谢艳霞,叶允均,吴淦国,福建蒲洋变质核杂岩构造及其控矿作用初探,福建地质, 1998, 17(3):139-146, 1998
[11]陈火炮,李敬珠,福建顺昌山后铅锌矿床地质特征及成因探讨,福建地质, 2008, 27(2):204-210, 2008
[12]陈锦麟,论闽西北推覆体构造,西部探矿工程2008, 20(11):153-155, 2008
[13]陈开彪,福建省大田县广平含煤区推覆构造特征及找煤预测,中国煤田地质, 2006, 18(2):16-17, 70, 2006
[14]陈泉霖,福建龙岩白沙南煤矿区煤层的形变特征及变化规律分析,中国煤田地质, 2007,19(3):17-18 , 2007
[15]陈润生,林东燕,江剑丽,福建早侏罗世火山作用的动力学机制及大地构造学意义探讨,福建地质, 2008, 27(2):156-165, 2007
[16]戴定贤,福建省天湖山煤矿区F31推覆断层及找煤方向探讨,中国煤矿地质, 2009, 21(3):6-10, 2009
[17]方如健,福建政和星溪金矿床构造控矿特征及找矿前景,福建地质, 2007, 26(1):20-26 , 2006
[18]傅树超,福建省将乐顺昌一带中—上石炭统碎屑岩的发现及其地质意义,福建地质, 1988, (3), 1988
[19]关玉祥,杨添水,福建省推覆构造研究及其意义,福建地质, 1994, 13(4):248-277, 1994
[20]韩胜康,福建永定新村钼铅锌多金属矿床地质特征及成因探讨,福建地质, 2008, 27(4):352-360, 2008
[21]黄昌旗,曹明志,闽西南回龙地区逆冲推覆构造,福建地质, 2002, 21(2):85-90, 2001
[22]黄春鹏,刘庆生,张克尧,福建紫金山铜金矿田地球物理地球化学特征及找矿模型,福建地质, 1999, 18(4):189-206, 1999
[23]黄道锐,福建南平巨口白石岩钼矿床地质特征及成因探讨,福建地质, 2008, 27(3):275-280, 2007
[24]黄和,福建省广平煤矿区推覆体下煤系地层构造特征,中国煤炭地质, 2009, 21(8):12-14, 2009
[25]黄家龙,福建将乐盖竹洋绿片岩地质特征及构造环境探讨,福建地质, 2001, 20(4):177-184, 2001
[26]黄仁生,福建尤溪梅仙矿田铅锌银矿床特征及找矿方向,福建地质, 2007, 26(4):211-221 , 2006
[27]黄仁生,福建大田广平推覆构造与隐伏煤、多金属矿,福建地质, 2007, 26(3):142-150 , 2007
[28]黄尚泉,龙永煤田四集矿区逆冲推覆构造特征与找煤分析,煤炭技术, 2009, 28(1):134-137, 2009
[29]黄廷淦,揭育金,福建明溪盆地成因探讨,福建地质, 1999, 18(1):1-5 , 1998
[30]黄长煌,福建大田建爱地区多金属矿的构造特征及其成矿意义,福建地质, 1999, 18(1):6-11, 1999
[31]揭育金,庄建民,黄泉祯,郑声俭,福建长汀童坊地区推覆构造,福建地质, 2001, 20(4):157-162, 2001
[32]李观富,福建晚古生代地层中推覆构造成因机制,福建地质, 1989, 8(1):35-45, 1978
[33]李兼海,福建省构造运动_构造层划分及其主要特征,福建地质, 1998, 17(3):115-130 , 1998
[34]李其康,福建永定高陂煤矿区构造控煤作用分析,能源与环境, 2008(3):89-90, 2008
[35]李学燮,张开毕,揭育金,张引娥,闽西北将乐地区大源片麻岩的地质特征,中国区域地质, 2001, 20(1):39-45, 2001
[36]练光春,福建永定龙川矿区构造特征及其演化过程,中国煤田地质2004, 16(Z1):26-27, 2004
[37]梁乐辉,福建莆田泗洋铅锌矿地质特征及成因探讨,福建地质, 2008, 27(3):259-266, 2008
[38]林传勇,史兰斌,陈孝德,韩秀玲,福建明溪上地幔热结构及流变学特征,地质评论, 1999, 45(4):352-360, 1999
[39]林全胜,福建三明吉口矿区推覆构造特征与控煤作用,福建地质, 2009, 28(4):275-280, 2009
[40]林增品,福建大田地区下二叠统童子岩组底部砾岩层,福建地质, 1991, 10(3):205-210, 1991
[41]刘玉萍,张洁,尹宏伟,徐士进,面积平衡法与川东大池干推覆带区域滑脱面预测,大地构造与成矿学, 2008, 32(4):410-417, 2008
[42]卢聪生,福建龙岩吕凤矿区构造特征及其演化,煤, 2008, 17(7):39-42, 2008
[43]卢聪生,福建永定东中矿区控煤构造特征及其对含煤地层的影响,中国西部科技, 2008, 7(16):4-6, 2008
[44]卢清地,福建中生代火山活动的基本特征及构造环境,岩石矿物学杂志, 2001, 20(1):57-68, 2001
[45]马金清,福建若干基础地质问题及研究方向探讨,福建地质, 2002, 21(4):200-205, 2002
[46]毛建仁,陈荣,李寄嵎,叶海敏,赵希林,闽西南地区晚中生代花岗质岩石的同位素年代学、地球化学及其构造演化,岩石学报, 2006, 22(6):1723-1734, 2006
[47]毛建仁,陶奎元,李寄嵎,谢芳贵,闽西南地区中生代花岗闪长质岩石的特征及其构造演化,岩石矿物学杂志, 2002, 21(2):135-142, 2002
[48]毛建仁,陶奎元,谢芳贵,许乃政,陈三元,闽西南地区成岩成矿作用与构造环境,岩石矿物学杂志, 2001, 20(3):329-336, 2001
[49]毛建仁,许乃政,胡青,李寄嵎,谢芳,闽西南地区中生代花岗闪长质岩石的同位素年代学、地球化学及其构造演化,吉林大学学报(地球科学版), 2004, 34(1):12-20, 2004
[50]莫一迪,福建大田县高峰岬铅锌多金属矿区构造特征及其成矿作用,矿业天地, 2008(23):653-654, 2008
[51]沈荣泉,福建省将乐县肖公洞钨矿成矿规律研究,中国西部科技, 2008, 7(23):1-3, 2007
[52]孙淑静,李星,宋立军,周珍琦,冯常茂,闽西南苏桥-小溪洋井田推(滑)覆构造形成演化,煤田地质与勘探, 2008, 36(3):6-11, 2008
[53]唐来发,龙永煤田推覆构造特征及找煤预测,能源与环境, 2009(3):61-63, 2009
[54]陶建华,闽西南地区东部逆冲推覆构造及其形成机制,福建地质, 1987, (4) , 1987
[55]陶建华,福建推覆构造研究与找矿突破,福建地质, 2008.27(2):105-124, 2008
[56]陶建华,陈福龙,福建推覆构造研究,石油实验地质, 2006, 28(3):259-263, 285, 2006
[57]陶于祥,福建前寒武纪基底构造格局及演化浅析,中国区域地质, 1997, 16(1):60-65, 110, 1997
[58]万天丰,中国大地构造学纲要,地质出版社:135-151, 2004
[59]王尔康,欧阳钟辉,刘聪,福建大田推覆构造群的发现及其地质意义,科学通报, 1985, 30(3):203-203 , 1985
[60]王国平,福建印支运动基本特征探讨,福建地质, 1983, (2) , 1983
[61]王绍雄,福建境内壳幔成分和岩石圈构造的演化与成矿作用的关系,福建地质, 2003, 22(2):89-100, 2003
[62]韦德光,揭育金,黄廷淦,福建省区域地质构造特征,中国区域地质, 1997, 16(2):162-170, 1997
[63]游天寿,黄新鹏,福建将乐一带白云母化花岗岩成因的初步探讨,福建地质, 1989, 8(3):225-234, T001 , 1989
[64]余学东,邵跃,李应桂,福建紫金山铜金矿床地质地球化学找矿模型及应用,物探与化探, 1995, 19(5):321-331 , 1995
[65]张贵山,温汉捷,胡瑞忠,裘愉卓,福建新生代碱性超基性火山岩地球化学特征及构造意义,地质学报, 2009, 83(2):284-294, 2009
[66]张家菁,陈郑辉,王登红,陈振宇,刘善宝,王成辉,福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义,大地构造与成矿学, 2008, 32(1):92-97, 2007
[67]张小亮,福建省大田县姜坑铅锌成矿带成矿地质特征及成矿模式,矿业天地, 2008(24):635-637, 2008
[68]赵荣文,陈柏林,吴淦国,黄仁生,吴建设,福建尤溪肖板地区构造与金矿化的关系,有色金属矿产与勘查, 1999, 8(3):147-152, 1999
[69]赵希林,毛建仁,陈荣,许乃政,曾庆涛,叶海敏,闽西南地区才溪岩体锆石SHRIMP定年及其地球化学特征,岩石矿物学杂志, 2007, 26(3):223-231, 2007
[70]郑志强,苏江湖,马金清,闽北仁寿地区逆冲推覆构造,福建地质, 2001, 20(2):78-86, 2000
[71]周汉民,王文斌,福建德化杨梅地区金矿成矿地质条件和矿床成因,火山地质与矿产, 1996, (Z1) , 1996
[72]周珍琦,闽西南地区推覆构造特征,石油实验地质, 2006, 28(1):38-41 , 2006
[73]周珍琦,闽西南地区推覆构造形成的动力学机制——以广平推覆构造为例,石油实验地质, 2007, 29(2):128-132 , 2007
[74]朱根灵,福建前寒武纪地体中的锆石U-Pb同位素年龄的地质意义,地质调查与研究, 2007, 30(1):13-21 , 2007
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