沂沭断裂带研究进展综述
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摘要
为了更好地了解沂沭断裂带的研究进展,整理分析了大量前人研究资料,对其深部结构特征、构造形成演化、成盆成矿作用等方面做了阐述。认为进一步研究应综合利用多地球物理场深部探测技术,获取高精度深部结构信息,研究沂沭断裂带岩石圈流变结构、构造断裂体系分布,实现沂沭断裂带地质结构"透明化"。加强沂沭断裂带及周边韧性剪切带的时代、断裂带的同位素地质,以及沿断裂带中生代变动与古老基底变动的关系研究。开展对沂沭断裂带地区晚中生代岩浆时空演化、成岩构造动力学背景以及与金及多金属矿成矿作用之间的耦合关系的研究,并对比沂沭断裂带内及两侧金及多金属矿成矿作用异同。断裂带各段盆地及控油机理的差异、断裂带与两侧金刚石矿带的关系也值得进一步研究。
In order to better understand the research progress of the Yishu fault zone,a large number of research data have been collated and analyzed. Structural characteristics,the formation and evolution of the fractures,and the basin-forming and mineralization in the deep part have been elaborated. Multi-geophysical field deep detection techniques should be used comprehensively to obtain high-precision deep structural information,study the distribution of lithosphere rheological structures and tectonic fault systems in the Yishu fault zone,realize the " transparency" of geological structures of the Yishu fault zone,strengthen the study of the relationship between the age of the ductile shear zone,the isotopic geology of the fault zone,and the relation between the Mesozoic changes and the changes of ancient basement along the fault zone. The spatiotemporal evolution of magma in the late Mesozoic,dynamic background of diagenetic structures,and the coupling relationship with the gold and polymetallic ore mineralization in the Yishu fault zone have been studied. The similarities and differences between gold and polymetallic ore mineralization in and on both sides of the belt have been compared. The differences in basins and oil control mechanisms in each segment of the fault zone,and the relationship between the fault zone and diamond belts on both sides are also worth further study.
In order to better understand the research progress of the Yishu fault zone,a large number of research data have been collated and analyzed. Structural characteristics,the formation and evolution of the fractures,and the basin-forming and mineralization in the deep part have been elaborated. Multi-geophysical field deep detection techniques should be used comprehensively to obtain high-precision deep structural information,study the distribution of lithosphere rheological structures and tectonic fault systems in the Yishu fault zone,realize the " transparency" of geological structures of the Yishu fault zone,strengthen the study of the relationship between the age of the ductile shear zone,the isotopic geology of the fault zone,and the relation between the Mesozoic changes and the changes of ancient basement along the fault zone. The spatiotemporal evolution of magma in the late Mesozoic,dynamic background of diagenetic structures,and the coupling relationship with the gold and polymetallic ore mineralization in the Yishu fault zone have been studied. The similarities and differences between gold and polymetallic ore mineralization in and on both sides of the belt have been compared. The differences in basins and oil control mechanisms in each segment of the fault zone,and the relationship between the fault zone and diamond belts on both sides are also worth further study.
引文
[1]Yin An,Nie S.Y.An indentation model for the North and South China collision and the development of the Tan-Lu and Honam Fault systems,Eastern Asia[J].Tectonics,1993,12(4):810-813.
[2]王小凤,李中坚,陈柏林,等.郯庐断裂带[M],北京:地质出版社,2000:1-30.
[3]方仲景,丁梦林,向宏发,等.郯庐断裂带的基本特征[J].科学通报,1986(1):52-55.
[4]李家灵,晁洪太,崔昭文,等.郯庐活断层的分段及其大震危险性分析[J].地震地质,1994(2):121-126.
[5]李洪奎,杨永波,杨锋杰.山东沂沭断裂带构造演化与成矿作用[M].北京:地质出版社,2009:1-30.
[6]徐嘉炜,马国烽.郯庐断裂带研究的十年回顾[J].地质论评,1992,38(4):316-324.
[7]Xu J W,Zhu G.Tectonic models of the Tan-Lu Fault Zone,Eastern China[J].International Geological Review,1994(36):771-784.
[8]万天丰,朱鸿,赵磊,等.郯庐断裂带的形成与演化综述[J].现代地质,1996(2):159-168.
[9]Lin A,Miyata T,Wan T.Tectonic characteristics of the central segment of the Tancheng-Lujiang fault zone in the central segment,Shandong Peninsula,eastern China[J].Tectonophysics,1998(293):85-104.
[10]张鹏,王良书,石火生,等.郯庐断裂带山东段的中新生代构造演化特征[J].地质学报,2010,84(9):1316-1323.
[11]Zhu R X,Chen L,Wu F Y,etc.Scale and mechanism of the destruction of the North China Craton[J].Sci China Earth Sci,2011(54):789-797.
[12]林爱明,饶刚,闫兵.从水系的分布形态探讨沂沭断裂带的运动特征[J].地学前缘,2013,20(4):125-136.
[13]Li Chunlin,WANG Zongxiu,WU Qingzi,etc.Late Cretaceous Transpressional Fault System:A Case Study of the Yishu Fault Belt,Shandong Province,Eastern China[J].Acta Geologica Sinica(English Edition),2015,89(5):1531-1545.
[14]李洪奎,陈国栋,梁太涛,等.沂沭断裂带构造活动与胶东金矿形成关系之探讨[J].山东国土资源,2017,33(11):6-14.
[15]李洪奎,禚传源,耿科,等.郯-庐断裂带陆内伸展构造:以沂沭断裂带的表现特征为例[J].地学前缘,2017,24(2):73-84.
[16]徐贵忠,周瑞,王艺芬,等.胶东和鲁西地区中生代成矿作用重大差异性的内在因素[J].现代地质,2002(1):9-18.
[17]罗志立,李景明,李小军,等.试论郯城-庐江断裂带形成、演化及问题[J].吉林大学学报(地球科学版),2005(6):21-28.
[18]高维明,李家灵,孙竹友.沂沭大陆裂谷的生成与演化[J].地震地质,1980(3):11-18.
[19]杜晓娟,孟令顺,张凤旭,等.利用重磁场研究郯庐断裂及周边构造[J].吉林大学学报(地球科学版),2005(S1):51-56.
[20]唐新功,陈永顺,唐哲.应用布格重力异常研究郯庐断裂构造[J].地震学报,2006(6):603-610,679.
[21]李春峰,陈冰,周祖翼.中国东部及邻近海域磁异常数据所揭示的深部构造[J].中国科学(D辑:地球科学),2009,39(12):1770-1779.
[22]王鑫,张景发,付萍杰,等.沂沭断裂带重力场及地壳结构特征[J].地震地质,2015,37(3):731-747.
[23]Guang Zhu,Wei Hu,Lihong Song,etc.Quaternary activity along the Tan-Lu fault zone in the Bohai Bay,East China:Evidence from seismic profiles[J].Journal of Asian Earth Sciences,2015,114(1):5-17.
[24]张碧秀,汤永安.沂沭断裂带地壳结构特征[J].中国地震,1988(3):22-28.
[25]马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面[J].地质学报,1991(3):199-215.
[26]江钊,孙洁,徐常芳,等.江苏响水—内蒙满都拉地壳上地幔电性结构初探—地学断面研究报道之三[J].地震地质,1990(3):193-199,206.
[27]刘昌铨,嘉世旭,杜官恒.江苏响水—内蒙古满都拉地学断面地震折射测深结果[J].地震地质,1991(3):193-204.
[28]T.Y.Zheng,L.Zhao,W.W.Xu,etc.Insight into modification of North China Craton from seismological study in the Shandong Province[J].GEOPHYSICAL RESEARCH LETTERS,2008(35):L22305,doi:10.1029/2008GL035661.
[29]孙洁,徐常芳,江钊.鲁南地区大地电磁测深结果[J].中国地震,1988(3):36-43.
[30]宋国奇.郯庐断裂带鲁苏皖段大地电磁测深剖面与地壳结构[J].油气地质与采收率,2006(6):1-4,105.
[31]Chen,L,Zheng,T,Xu,W.A thinned lithospheric image of the Tanlu Fault Zone,eastern China:constructed from wave equation based receiver function migration[J].JOURNAL OF GEOPHYSICAL RESEARCH,2006(111),B09312,doi:10.1029/2005JB003974.
[32]宋国奇.郯庐断裂带渤海段的深部构造与动力学意义[J].合肥工业大学学报(自然科学版),2007(6):663-667.
[33]叶高峰,魏文博,金胜,等.郯庐断裂带中段电性结构及其地学意义研究[J].地球物理学报,2009,52(11):2818-2825.
[34]张继红,赵国泽,肖骑彬,等.郯庐断裂带中段(沂沭断裂带)电性结构研究与孕震环境[J].地球物理学报,2010,53(3):605-611.
[35]王志才,邓起东,杜宪宋,等.莱州湾海域郯庐断裂带活断层探测[J].地震学报,2006(5):493-503,560.
[36]李西双,刘保华,赵月霞,等.渤海海域晚更新世—全新世的活动构造[J].海洋学报(中文版),2010,32(5):2-59.
[37]Li,Z.X.Collision between the North and South China blocks:a crustal-detachment model for suturing in the region east of the Tanlu fault[J].Geology,1994(22):739-742.
[38]Chang,E.Z.Collisional orogene between north and south China and its eastern extension in the Korean Peninsula[J].Journal of Southeast Asian Earth Sciences,1996,13(3-5):267-277.
[39]Gilder,S.A.,Leloup,P.H,Courtillot,V,etc.Tectonic evolution of the Tancheng-Lujiang(Tan-Lu)fault via middle Triassic to Early Cenozoic paleomagnetic data[J].Journal of Geophysical Research:Solid Earth,1999(104):15365-15390.
[40]Zhu,G,Liu,G.S,Niu,M.L,etc.Syn-collisional transform faulting of the Tan-Lu fault zone,East China[J].International Journal of Earth Sciences,2009(98):135-155.
[41]朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003(3):200-207.
[42]Zhu Guang,Wang Yongsheng,Liu Guosheng,etc.40Ar/39Ar dating of st rikeslip motion on the Tan-Lu fault zone,East China[J].Journal of Structural Geology,2005(27):1379-1398.
[43]朱光,张力,谢成龙,等.郯庐断裂带构造演化的同位素年代学制约[J].地质科学,2009,44(4):1327-1342.
[44]朱光,王薇,顾承串,等.郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示[J].岩石学报,2016,32(4):935-949.
[45]薛金声,李师汤.山东沂沭断裂带成生时代探讨[J].山东海洋学院学报,1982(4):51-59.
[46]张家声.沂沭断裂带中段基底韧性剪切带[J].地震地质,1983(2):11-23,93.
[47]张用夏,李卢玲.郯庐断裂带的平移及其对邻区构造的影响[A]//构造地质论丛(3)[C].北京:地质出版社,1984:1-8.
[48]周建波,胡克,孙加鹏.郯庐断裂中段鲁中基底韧性变形带的形成时代[J].中国区域地质,1998(2):52-56.
[49]乔秀夫,高林志,彭阳,等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学(D辑:地球科学),2001(11):911-918.
[50]乔秀夫.中朝板块元古宙板内地震带与盆地格局[J].地学前缘,2002(3):141-149.
[51]万天丰,朱鸿.郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报,1996(1):14-27.
[52]Zhang Kai jun.North and south China collision along the eastern and southern North China margins[J].Tectonophysics,1997,270(1-2):145-156.
[53]徐嘉炜,崔可锐,刘庆,等.东亚大陆边缘中生代的左行平移断裂作用[J].海洋地质与第四纪地质,1985,5(2):51-64.
[54]徐嘉炜,朱光,吕培基,等.郯庐断裂带平移年代学研究的进展[J].安徽地质,1995(1):1-12.
[55]张岳桥,董树文.郯庐断裂带中生代构造演化史:进展与新认识[J].地质通报,2008(9):1371-1390.
[56]Zhang Yueqiao,Dong Shuwen,Shi Wei.Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province,eastern China[J].Tectonophysics,2003(363):243-258.
[57]陈宣华,王小凤,张青,等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000(3):215-220.
[58]朱光,牛漫兰,宋传中,等.郯庐断裂带新生代的上地幔剪切作用与火山活动[J].安徽地质,2001(2):106-112.
[59]汤加富,许卫.郯庐断裂带南段并无巨大平移—来自安徽境内的证据[J].地质论评,2002(5):449-456.
[60]汤加富,李怀坤,娄清.郯庐断裂南段研究进展与断裂性质讨论[J].地质通报,2003(6):426-436.
[61]李洪奎,杨永波,李英平,等.沂沭断裂带中段地质特征与金矿成矿作用[J].地质调查与研究,2004(4):255-260.
[62]石文杰,魏俊浩,谭俊,等.郯庐断裂带晚白垩世金成矿作用:来自龙泉站金矿床黄铁矿Rb-Sr年代学证据[J].地球科学(中国地质大学学报),2014,39(3):325-340.
[63]吴齐,牛漫兰,朱光,等.郯庐断裂带莒县地区早白垩世中酸性火山岩成因及其地质意义[J].地质学报,2013,87(7):979-993.
[64]刘昊,石义远,徐静.沂沭断裂带中段金矿构造控矿规律研究[J].河北工程大学学报(自然科学版),2011,28(3):47-51.
[65]郭瑞朋,王来明,田京祥,等.沂沭断裂带中段金矿特征及找矿方向研究[J].山东国土资源,2014,30(1):1-7.
[66]邓运华.郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J].中国海上油气地质,2001(5):2-6.
[67]胡望水,吕炳全,官大勇,等.郯庐断裂带及其周缘中新生代盆地发育特征[J].海洋地质与第四纪地质,2003(4):51-58.
[68]万桂梅,周东红,汤良杰.渤海海域郯庐断裂带对油气成藏的控制作用[J].石油与天然气地质,2009,30(4):450-454,461.
[69]吴根耀,马力,梁兴,等.从郯庐断裂带两侧的“盆”“山”耦合演化看前白垩纪“郯庐断裂带”的性质[J].地质通报,2008(3):308-325.
[2]王小凤,李中坚,陈柏林,等.郯庐断裂带[M],北京:地质出版社,2000:1-30.
[3]方仲景,丁梦林,向宏发,等.郯庐断裂带的基本特征[J].科学通报,1986(1):52-55.
[4]李家灵,晁洪太,崔昭文,等.郯庐活断层的分段及其大震危险性分析[J].地震地质,1994(2):121-126.
[5]李洪奎,杨永波,杨锋杰.山东沂沭断裂带构造演化与成矿作用[M].北京:地质出版社,2009:1-30.
[6]徐嘉炜,马国烽.郯庐断裂带研究的十年回顾[J].地质论评,1992,38(4):316-324.
[7]Xu J W,Zhu G.Tectonic models of the Tan-Lu Fault Zone,Eastern China[J].International Geological Review,1994(36):771-784.
[8]万天丰,朱鸿,赵磊,等.郯庐断裂带的形成与演化综述[J].现代地质,1996(2):159-168.
[9]Lin A,Miyata T,Wan T.Tectonic characteristics of the central segment of the Tancheng-Lujiang fault zone in the central segment,Shandong Peninsula,eastern China[J].Tectonophysics,1998(293):85-104.
[10]张鹏,王良书,石火生,等.郯庐断裂带山东段的中新生代构造演化特征[J].地质学报,2010,84(9):1316-1323.
[11]Zhu R X,Chen L,Wu F Y,etc.Scale and mechanism of the destruction of the North China Craton[J].Sci China Earth Sci,2011(54):789-797.
[12]林爱明,饶刚,闫兵.从水系的分布形态探讨沂沭断裂带的运动特征[J].地学前缘,2013,20(4):125-136.
[13]Li Chunlin,WANG Zongxiu,WU Qingzi,etc.Late Cretaceous Transpressional Fault System:A Case Study of the Yishu Fault Belt,Shandong Province,Eastern China[J].Acta Geologica Sinica(English Edition),2015,89(5):1531-1545.
[14]李洪奎,陈国栋,梁太涛,等.沂沭断裂带构造活动与胶东金矿形成关系之探讨[J].山东国土资源,2017,33(11):6-14.
[15]李洪奎,禚传源,耿科,等.郯-庐断裂带陆内伸展构造:以沂沭断裂带的表现特征为例[J].地学前缘,2017,24(2):73-84.
[16]徐贵忠,周瑞,王艺芬,等.胶东和鲁西地区中生代成矿作用重大差异性的内在因素[J].现代地质,2002(1):9-18.
[17]罗志立,李景明,李小军,等.试论郯城-庐江断裂带形成、演化及问题[J].吉林大学学报(地球科学版),2005(6):21-28.
[18]高维明,李家灵,孙竹友.沂沭大陆裂谷的生成与演化[J].地震地质,1980(3):11-18.
[19]杜晓娟,孟令顺,张凤旭,等.利用重磁场研究郯庐断裂及周边构造[J].吉林大学学报(地球科学版),2005(S1):51-56.
[20]唐新功,陈永顺,唐哲.应用布格重力异常研究郯庐断裂构造[J].地震学报,2006(6):603-610,679.
[21]李春峰,陈冰,周祖翼.中国东部及邻近海域磁异常数据所揭示的深部构造[J].中国科学(D辑:地球科学),2009,39(12):1770-1779.
[22]王鑫,张景发,付萍杰,等.沂沭断裂带重力场及地壳结构特征[J].地震地质,2015,37(3):731-747.
[23]Guang Zhu,Wei Hu,Lihong Song,etc.Quaternary activity along the Tan-Lu fault zone in the Bohai Bay,East China:Evidence from seismic profiles[J].Journal of Asian Earth Sciences,2015,114(1):5-17.
[24]张碧秀,汤永安.沂沭断裂带地壳结构特征[J].中国地震,1988(3):22-28.
[25]马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面[J].地质学报,1991(3):199-215.
[26]江钊,孙洁,徐常芳,等.江苏响水—内蒙满都拉地壳上地幔电性结构初探—地学断面研究报道之三[J].地震地质,1990(3):193-199,206.
[27]刘昌铨,嘉世旭,杜官恒.江苏响水—内蒙古满都拉地学断面地震折射测深结果[J].地震地质,1991(3):193-204.
[28]T.Y.Zheng,L.Zhao,W.W.Xu,etc.Insight into modification of North China Craton from seismological study in the Shandong Province[J].GEOPHYSICAL RESEARCH LETTERS,2008(35):L22305,doi:10.1029/2008GL035661.
[29]孙洁,徐常芳,江钊.鲁南地区大地电磁测深结果[J].中国地震,1988(3):36-43.
[30]宋国奇.郯庐断裂带鲁苏皖段大地电磁测深剖面与地壳结构[J].油气地质与采收率,2006(6):1-4,105.
[31]Chen,L,Zheng,T,Xu,W.A thinned lithospheric image of the Tanlu Fault Zone,eastern China:constructed from wave equation based receiver function migration[J].JOURNAL OF GEOPHYSICAL RESEARCH,2006(111),B09312,doi:10.1029/2005JB003974.
[32]宋国奇.郯庐断裂带渤海段的深部构造与动力学意义[J].合肥工业大学学报(自然科学版),2007(6):663-667.
[33]叶高峰,魏文博,金胜,等.郯庐断裂带中段电性结构及其地学意义研究[J].地球物理学报,2009,52(11):2818-2825.
[34]张继红,赵国泽,肖骑彬,等.郯庐断裂带中段(沂沭断裂带)电性结构研究与孕震环境[J].地球物理学报,2010,53(3):605-611.
[35]王志才,邓起东,杜宪宋,等.莱州湾海域郯庐断裂带活断层探测[J].地震学报,2006(5):493-503,560.
[36]李西双,刘保华,赵月霞,等.渤海海域晚更新世—全新世的活动构造[J].海洋学报(中文版),2010,32(5):2-59.
[37]Li,Z.X.Collision between the North and South China blocks:a crustal-detachment model for suturing in the region east of the Tanlu fault[J].Geology,1994(22):739-742.
[38]Chang,E.Z.Collisional orogene between north and south China and its eastern extension in the Korean Peninsula[J].Journal of Southeast Asian Earth Sciences,1996,13(3-5):267-277.
[39]Gilder,S.A.,Leloup,P.H,Courtillot,V,etc.Tectonic evolution of the Tancheng-Lujiang(Tan-Lu)fault via middle Triassic to Early Cenozoic paleomagnetic data[J].Journal of Geophysical Research:Solid Earth,1999(104):15365-15390.
[40]Zhu,G,Liu,G.S,Niu,M.L,etc.Syn-collisional transform faulting of the Tan-Lu fault zone,East China[J].International Journal of Earth Sciences,2009(98):135-155.
[41]朱光,刘国生,牛漫兰,等.郯庐断裂带的平移运动与成因[J].地质通报,2003(3):200-207.
[42]Zhu Guang,Wang Yongsheng,Liu Guosheng,etc.40Ar/39Ar dating of st rikeslip motion on the Tan-Lu fault zone,East China[J].Journal of Structural Geology,2005(27):1379-1398.
[43]朱光,张力,谢成龙,等.郯庐断裂带构造演化的同位素年代学制约[J].地质科学,2009,44(4):1327-1342.
[44]朱光,王薇,顾承串,等.郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示[J].岩石学报,2016,32(4):935-949.
[45]薛金声,李师汤.山东沂沭断裂带成生时代探讨[J].山东海洋学院学报,1982(4):51-59.
[46]张家声.沂沭断裂带中段基底韧性剪切带[J].地震地质,1983(2):11-23,93.
[47]张用夏,李卢玲.郯庐断裂带的平移及其对邻区构造的影响[A]//构造地质论丛(3)[C].北京:地质出版社,1984:1-8.
[48]周建波,胡克,孙加鹏.郯庐断裂中段鲁中基底韧性变形带的形成时代[J].中国区域地质,1998(2):52-56.
[49]乔秀夫,高林志,彭阳,等.古郯庐带沧浪铺阶地震事件、层序及构造意义[J].中国科学(D辑:地球科学),2001(11):911-918.
[50]乔秀夫.中朝板块元古宙板内地震带与盆地格局[J].地学前缘,2002(3):141-149.
[51]万天丰,朱鸿.郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报,1996(1):14-27.
[52]Zhang Kai jun.North and south China collision along the eastern and southern North China margins[J].Tectonophysics,1997,270(1-2):145-156.
[53]徐嘉炜,崔可锐,刘庆,等.东亚大陆边缘中生代的左行平移断裂作用[J].海洋地质与第四纪地质,1985,5(2):51-64.
[54]徐嘉炜,朱光,吕培基,等.郯庐断裂带平移年代学研究的进展[J].安徽地质,1995(1):1-12.
[55]张岳桥,董树文.郯庐断裂带中生代构造演化史:进展与新认识[J].地质通报,2008(9):1371-1390.
[56]Zhang Yueqiao,Dong Shuwen,Shi Wei.Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province,eastern China[J].Tectonophysics,2003(363):243-258.
[57]陈宣华,王小凤,张青,等.郯庐断裂带形成演化的年代学研究[J].长春科技大学学报,2000(3):215-220.
[58]朱光,牛漫兰,宋传中,等.郯庐断裂带新生代的上地幔剪切作用与火山活动[J].安徽地质,2001(2):106-112.
[59]汤加富,许卫.郯庐断裂带南段并无巨大平移—来自安徽境内的证据[J].地质论评,2002(5):449-456.
[60]汤加富,李怀坤,娄清.郯庐断裂南段研究进展与断裂性质讨论[J].地质通报,2003(6):426-436.
[61]李洪奎,杨永波,李英平,等.沂沭断裂带中段地质特征与金矿成矿作用[J].地质调查与研究,2004(4):255-260.
[62]石文杰,魏俊浩,谭俊,等.郯庐断裂带晚白垩世金成矿作用:来自龙泉站金矿床黄铁矿Rb-Sr年代学证据[J].地球科学(中国地质大学学报),2014,39(3):325-340.
[63]吴齐,牛漫兰,朱光,等.郯庐断裂带莒县地区早白垩世中酸性火山岩成因及其地质意义[J].地质学报,2013,87(7):979-993.
[64]刘昊,石义远,徐静.沂沭断裂带中段金矿构造控矿规律研究[J].河北工程大学学报(自然科学版),2011,28(3):47-51.
[65]郭瑞朋,王来明,田京祥,等.沂沭断裂带中段金矿特征及找矿方向研究[J].山东国土资源,2014,30(1):1-7.
[66]邓运华.郯庐断裂带新构造运动对渤海东部油气聚集的控制作用[J].中国海上油气地质,2001(5):2-6.
[67]胡望水,吕炳全,官大勇,等.郯庐断裂带及其周缘中新生代盆地发育特征[J].海洋地质与第四纪地质,2003(4):51-58.
[68]万桂梅,周东红,汤良杰.渤海海域郯庐断裂带对油气成藏的控制作用[J].石油与天然气地质,2009,30(4):450-454,461.
[69]吴根耀,马力,梁兴,等.从郯庐断裂带两侧的“盆”“山”耦合演化看前白垩纪“郯庐断裂带”的性质[J].地质通报,2008(3):308-325.