摘要
鲁西新太古代花岗-绿岩带位于华北克拉通东部,主要由泰山岩群和花岗质岩石组成。早期研究认为,泰山岩群雁翎关组、山草峪组和柳杭组形成时代相同(-2.7 Ga),自下而上整合接触,构成单斜地层。表壳岩系以较小规模分布于不同时代花岗质岩石“海”中。七星台是鲁西花岗-绿岩带典型代表,泰山岩群表壳岩和各类太古宙花岗质岩石都有出露,是研究鲁西花岗-绿岩带形成演化的最理想地区之一。
本论文以七星台地区为研究对象,在详细野外地质工作基础上,以SHRIMP锆石U-Pb年代学和岩石地球化学为主要研究手段,对泰山岩群和周边各类花岗质岩石的组成和形成时代进行了研究,重新拟定了柳杭岩组与山草峪岩组的含义和界线,确定了深熔作用的空间分布和时代,探讨了鲁西花岗-绿岩带的形成构造环境以及构造演化。取得主要成果和认识如下。
(1)在原1:50000地质图基础上,对重点研究区进行了详细野外工作,获得许多新的重要发现,对原地质图作了重大修改。
(2)“柳杭岩组”主要由变质块状和枕状玄武岩组成,存在火山凝灰质与沉积岩夹层。变质玄武岩具MORB组成特征。形成时代为2.71—2.75 Ga。
(3)“山草峪岩组”主要由黑云变粒岩和细粒片麻岩(黑云变粒岩受变质深熔作用改造产物)组成,与“柳杭岩组”为构造接触。变质原岩主体为碎屑沉积岩,但具岛弧中酸性岩浆岩组成特征。碎屑锆石最小年龄(2.52—2.53 Ga)限制了最大沉积时代。
(4)划分出三套TTG片麻岩,形成时代分别为2.71 Ga、2.62 Ga和2.52 Ga。前两者以较大规模分布于表壳岩系西侧,后者以脉状侵入“山草峪岩组”,限定了“山草峪岩组”最大沉积时代。
(5)确定深熔岩石带,并把其进一步划分为四个亚带。发生深熔的主要地质体为“山草峪岩组”表壳岩。深熔作用时代为~2.51 Ga。大面积二长花岗岩的形成与之有关。
(6)将鲁西花岗-绿岩代的形成演化划分为两个阶段。第一阶段(2.60—2.75 Ga),在洋底高原环境形成“柳杭岩组”,洋内俯冲导致~2.7 Ga的TTG花岗质岩石形成。第二阶段(2.50—2.60 Ga),在岛弧环境形成“山草峪岩组”,大范围~2.5 Ga壳源花岗岩形成标志着鲁西地块克拉通化的结束。
The Archean granite-greenstone belt of Western Shandong Province (WSP) is located in the eastern North China Craton and is mainly composed of the Taishan Group and surrounding granitoid association. In early studies, the Taishan group, formed at~2.7 Ga, was subdivided into the Yanglingguan, Shancaoyu and Liuhang formations, which are considered to be comfortable to each other and constitute a monoclinal strata. Qixingtai is one of the typical areas of the WSP granite-greenstone belt, where the Taishan Group and different kinds of granitoids of Archean are well exposed. Based on geological mapping, this paper carried out a series of research, including SHRIMP zircon U-Pb chronology and geochemistry, in the Qixingtai Area And arrived some important conclusions as follows.
(1) "The Liuhang Formation" was mainly composed of massive meta-basalt and pillow meta-basalt intercalated with some thin tuff and sedimentary layers. The meta-basalts are same in geochemistry as MORB, derived form depleted mantle source at 2.75-2.71Ga.
(2) "The Shancaoyu Formation" was composed of leptite and fine-grained gneiss, with the latter being formed by anatectic reconstruction of the former. It shows a tectonic contact with "the Liuhang Formation". All the meta-sedimentary rocks of "the Shancaoyu Formation" show the geochemical charactaristics of magmatic rocks formed in island arc environmnet. Nd isotope compositions suggest a short crustal residence time in their source region. The meta-sediments contain detrital zircons of 2.56-2.53 Ga,-2.7 Ga and 2.53-2.52, limiting the deposition age of "the Shancaoyu Formation".
(3) Three suites of TTG rocks, formed at 2.71Ga,2.62Ga and 2.52Ga respectively, have been identified in the area.
(4) An anatectic belt has been identified. It can be further divided from west to east into four sub belts, namely the belts of lepite, leptite+felsic or granitic veins, fine-grained gneiss+felsic or granitic veins and migmatite. It is probably the anatexis at~2.51 Ga that resulted in the formation of crustally-derived granites which are widely distributed in the east of the anatectic belt.
(5) The WSP granite-greenstone belt is considered to undergo two evolution periods. First period (2.75-2.6 Ga), "the Liuhang Formation" was formed in oceanic plateau environment, and the TTG of~2.7 Ga was formed as a result of intra-ocean subduction. Second period (2.6-2.5Ga), "the Shancaoyu Formation" was formed in island arc environment. The large-scale crustally-derived granites were produced at~2.5 Ga, remarking the cratonization of the WSP Block.
引文
Alexander, F.M.K., Richard, W.B., Marc, P. et al.,2010. Continental growth and convergence-related arc plutonism in the Mesoarchaean:Evidence from the Barberton granitoid-greenstone terrain, South Africa Precambrian Research,178(1-4):15-26.
Arndt, N.T., Nisbet, E.G,1982. Geochemistry of Munro township basalts. Komatiite. Allen and Unwin, London.
Arndt, N.T.,1994. Archean komatiites. Archean Crustal Evolution. Elsevier, Amsterdam.
Ayer, J., Amelin, Y., Corfu, F. et al.,2002. Evolution of the southern Abitibi greenstone belt based on U-Pb geochronology:autochthonous volcanic construction followed by plutonism, regional deformation and sedimentation. Precambrian Research,115:63-95.
Barley, M.E., Sylvester, G.C., Groves, GD.B. et al.,1984. Archaean calc-alkaline volcanism in the Pilbara Block, Western Australia. Precambrian Research,24(3-4):285-319.
Barnes, S.J.,1985. The petrography and geochemistry of komatiite flows from the Abitibi Greenstone Belt. Lithos,18:241-270.
Bateman, R.,1995. The interplay between crystallization, replenishment and hybridization in large felsic magma chambers. Earth Science Res.,39(91-106).
Bateman, R., Costa, S., Swe, T. et al.,2001. Archaean mafic magmatism in the Kalgoorlie area of the Yilgarn Craton, Western Australia:a geochemical and Nd isotopic study of the petrogenetic and tectonic evolution of a greenstone belt. Precambrian Research,108:75-112.
Bergantz, GW.,1989. Underplating and partial melting:Implications for melt generation and extractioin. Science,254:1093-1095.
Black, L.P., Kamo, S.L., Allen, C.M. et al.,2003. TEMORA 1:a new zircon standard for Phanerozoic U-Pb geochronology. Chemical Geology,200:155-170.
Brown, M.,1994. The generation, segregation, ascent and emplacement of granite magma:the migmatite to crustally-derived granite connection in thichened orogens. Earth Science Res.,36:83-130.
Brown, M., Averkin, Y.A., Mclellan, E.,1995. Melt segregation in migmatites. J, Geophys. Res,100: 655-679.
Condie, K.C.,1972. A plate-tectonic evolutionary model of the South Pass Archean greenstone belt, southwestern Wyoming.24th Int. Geol. Congr., Sect.,1(104-112).
Condie, K.C.,1981. Archean Greenstone Belts. Elsevier Scientific Publishing Company, Amsterdam,1-381 pp.
Cumming, G.L., Richards, J.R.,1975. Ore lead isotope ratios in a continuously changing Earth. Earth Planet. Sci. Lett,28:155-171.
Dostal, J., Mueller, W.U.,1997. Komatiite flooding of a riftedArchean rhyolite arc complex:geochemical signature and tectonic significance of Stoughton-Roquemaure Group, Abitibi greenstone belt. Canada J. Geol.,105:545-563.
Dostal, J., Mueller, W.U., Murphy, J.B.,2004. Archean molasse basin evolution and magmatism,Wabigoon Subprovince. Canada J. Geol.,112:435-454.
Drummond, M.S., Defant, M.J.,1990. A model for trondhjemite-tonalite-dacite genesis and crustal growth via slab melting:Archean to modern comparisons. J, Geophys. Res,95:503-521.
Geng, Y.S., Liu, F.L., Yang, C.H.,2006. Magmatic event at the end of the Archean in eastern Hebei Province and its geological implication. Acta Geologica Sinica,80(6):819-833.
Glikson, A.Y.,1993. A steroids and early Precambran crustal evolution. Earth Science Res.,35:285-319.
Guo, J.H., Sun, M., Chen, F.K. et al.,2005. Sm-Nd and SHRIMP U-Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China Craton:timing of Paleoproterozoic continental collision. J. Asian Earth Sci.,24:629-642.
Harris, N., Inger, S., Massey, J.,1993. The role of fluids in the formation of High Himalayan leucogranites. In Himalayan Tectonics. Special Publication 74. Geological Society, London.
Harris, N., Massey, J.,1994. Decomposition and anatexis of Himalayan metapelites. Tectonics,13(6): 537-546.
Herzberg, C.,2004. Geodynamic information in peridotite petrology. J. Petrol.,45:2507-2530.
Hill, R.E.T., Barnes, S.J., Gole, M.J. et al.,1995. The volcanology of komatiites as deduced from field relationships in the Norseman-Wiluna greenstone belt, Western Australia Lithos,34(1-3):159-188.
Hodges, K.V., Fort, P.L., Pecher, A.,1988. Possible themal buffering by crustal anatexis in collisional orogens:thembarometric evidence from the Nepalese Himalaya. Geology,16(8):707-710.
Hollings, P., Wyman, D., Kerrich, R.,1999. Komatiite-basalt-rhyolite volcanic associations in Northern Superior Province greenstone belts:significance of plume-arc interaction in the generation of the proto continental Superior Province Lithos,46(1):137-161.
Jachson, S.L., Fyon, J.A., Corfu, F.,1994. Review of Archean supracrustal assemblages of the southern Abitibi greenstone belt in Ontario, Canada:products of microplate interaction within a large-scale plate-tectonic setting Precambrian Research,65(1-4):183-205.
Jahn, B.M., Auvray, B., Shen, Q.H. et al.,1988. Archean crustal evolution in China:the Taishan Complex, and evidence for juvenile crustal addition from long-term depleted mantle. Precambrian Research, 38:381-403.
Jean, H.B., Francois, L., Lyal, B.H. et al.,2009. Intra-sill magmatic evolution in the Cummings Complex, Abitibi greenstone belt:Tholeiitic to calc-alkaline magmatism recorded in an Archaean subvolcanic conduit system. Lithos,111(1-2):47-71.
Kerr, A.C., Marriner, G.F., Arndt, N.T. et al.,1996. The petrogenesis of Gorgona komatiites, picrites, and basalts:new field, petrographic and geochemical constraints. Lithos,37(245-260).
Kroner, A., Wilde, S.A., Li, J.H. et al.,2005. Age and evolution of a late Archean to Paleoproterozoic upper to lower crustal section in the Wutaishan/Hengshan/Fuping terrain of northern China. J. Asian Earth Sci.,24(5):577-595.
Kusky, T.M., Polat, A.,1999. Growth of granite-greenstone terranes at convergent margins, and stabilization of Archean cratons Tectonophysics.
Kusky, T.M., Li, J.H.,2003. Paleoproterozoic tectonic evolution of the North China Craton. Journal of Asian Earth Sciences,22:383-397.
Li, S.Z., Zhao, G.C., Sun, M. et al.,2005. Deformation history of the Paleoproterozoic Liaohe Group in the Eastern Block of the North China Craton. J. Asian Earth Sci.,24:659-674.
Li, S.Z., Zhao, G.C., Sun, M. et al.,2006. Are the South and North Liaohe Group of North China Craton different exotic terranes? Nd isotope constraints. Gondwana Research,9:198-208.
Li, S.Z., Zhao, G.C.,2007. SHRIMP U-Pb zircon geochronology of the Liaoji granitoids:Constraints on the evolution of the Paleoproterozoic Jiao-Liao-Ji belt in the Eastern Block of the North China Craton. Precambrian Research,158:1-16.
Ludwig, K.R.,2001. Squid 1.02:a user's manual. Berkeley Geochronology Centre, Special Publication 2, 1-19 pp.
Manikyamba, C., Kerrich, R., Naqvi, S.M. et al.,2004. Ceochemical systematics of tholeiitic basalts fromthe 2.7 Ga Ramagiri-Hungundcomposite greenstone belt, Dharwar craton. Precambrian Research,134:21-39.
McDonough, W.F., Ireland, T.R.,1993. Intraplate origin of komatiites inferred from trace elements in glass inclusions. Nature,365:432-434.
Morris, P.A., Witt, W.K.,1997. Geochemistry and tectonic setting of two contrasting Archean felsic volcanic associations in the eastern goldfields,Western Australia. Precambrian Research,83: 83-107.
Nasdala, L., Hofmeister, W., Norberg, N. et al.,2008. Zircon M257—a homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon. Geostandards and Geoanalytical Reseach, 32:247-265.
Nelson, D.R.,1997. Evolution of the Archaean granite-greenstone terranes of the Eastern Goldfields, Western Australia:SHRIMP U---Pb zircon constraints Precambrian Research,83(1-3):57-81.
Nesbitt, H.W., Young, G.M., Bosman, S.A.,2009. Major and trace element geochemistry and genesis of supracrustal rocks of the North Spirit Lake Greenstone belt, NW Ontario, Canada Precambrian Research,174(1-2):16-34.
Nesbitt, R.W., Sun, S.-S., Purvis, A.C.,1979. Komatiites:geochemistry and genesis. Can. Mimeral,17: 165-186.
Nutman, A.P., Chadwich, B., Krishna, R.B. et al.,1996. SHRIMP U/Pb zircon ages of acid volcanic rocks in the Chitradurga and Sandur Groups and granites adjacent to the Sandur schist belt, Karnataka. Journal Geological Society of India,47(153-164).
Parman, S.W., Dann, J.C., Grove, T.L. et al.,1997. Emplacement conditions of komatiite magmas from the 3.49Ga Komati Formation, Barberton Greenstone Belt, South Africa. Earth and Planetary Science Letters,150:303-323.
Parman, S.W., Shimizu, N., Grove, T.L. et al.,2003. Constraints on the pre-metamorphic trace element composition of Barberton komatiites from ion probe analyses of preserved clinopyroxene. Contrib. Mineral. Petrol.,144:383-396.
Peschler, A.P., Benn, K., Roest, W.R.,2006. Gold-bearing fault zones related to Late Archean orogenic folding of upper and middle crust in the Abitibi granite-greenstone belt, Ontario Precambrian Research,151(3-4):143-159.
Pidgeon, R.T., Wilde, S.A.,1990. The distribution of 3.0 Ga and 2.7 Ga volcanic episodes in the Yilgarn Craton of Western Australia. Precambrian Research,47:157-167.
Polat, A., Kerrich, R.,2001. Geodynamic processes, continental growth, and mantle evolution recorded in late Archean greenstone belts of the southern Superior Province, Canada Precambrian Research, 112(1-2):5-25.
Polat, A., Hofmann, A.,2003. Alteration and geochemical patterns in the 3.7-3.8 Ga Isua greenstone belt,West Greenland. Precambrian Research,126:197-218.
Polat, A., Li, J., Fryer, B. et al.,2006. Geochemical characteristics of the Neoarchean (2800-2700 Ma) Taishan greenstone belt, North China Craton:Evidence for plume-craton interaction. Chemical Geology,230:60-87.
Puchtel, I.S., Hofmann, A.W., Mezger, K. et al.,1998. Oceanic plateau model for continental crustal growth in the Archean:a case study from the Kostomuksha greenstone belt, NWBaltic Shield. Earth and Planetary Science Letters,155(57-74).
Puchtel, I.S., Hofmann, A.W., Amelin, Y.W. et al.,1999. Sumozero-Kenozero greenstone belt, SE Baltic Shield:Isotope and trace element constraints. Geochimica et Cosmochemica Acta,63:3579-3595.
Rapp, R.P., Shimizu, N., Norman, M.D. et al.,1999. Reaction between slab derived melts and peridotite in the mantle wedge:experimental constraints at 3.8Ga. Chemical Geology,160:335-356.
Rudnick, R.L., Fountain, D.M.,1995. Nature and composition of the continental crust:a lower crust perspective. Res. Geophys.,33(3):267-309.
Rushmer, T,1995. An experimental deformation study of partially-melten amphibolite:application to low-melt fraction segregation. J, Geophys. Res,100:681-695.
Samsonov, A.V., Bogina, M.M., Bibikova, E.V. et al.,2005. The relationship between adakitic, calc-alkaline volcanic rocks and TTGs:implications for the tectonic setting of the Karelian greenstone belts, Baltic Shield. Lithos,79:83-106.
Sandeman, H.A., Hanmer, S., Davis, WJ. et al.,2004. Neoarchean volcanic rocks, Central Hearne supracrustal belt, Western Churchill Province,Canada:geochemical and isotopic evidence supporting intra-oceanic, suprasubduction zone extension. Precambrian Research,134:113-141.
Scott, C.R., Mueller, W.U., Pilote, P.,2002. Physical volcanology, stratigraphy, and lithogeochemistry of an Archean volcanic arc:evolution from plume-related volcanism to arc rifting of SE Abitibi Greenstone Belt, Val d'Or, Canada. Precambrian Research,115(1-4):223-260.
Smithies, R.H., Champion, D.C., van Kranendonk, M.J. et al.,2005. Modern-style subduction processes in the Mesoarchean:geochemical evidence from the 3.12 Ga Whundo intra-oceanic arc. Earth and Planetary Science Letters,231:221-237.
Stone, W.E., Crocket, J.H., Fleet, M.E. et al.,1996. PGE mineralization in Archean volcanic systems: geochemical evidence from thick, differentiated mafic-ultramafic flows, Abitibi greenstone belt, Ontario, and implications for exploration. Journal of Geochemical Exploration,56(3):237-263.
Swager, C.P.,1997. Tectono-stratigraphy of late Archaean greenstone terranes in the southern Eastern Goldfields, Western Australia Precambrian Research,83(1-3):11-42.
Swager, C.P., Nelson, D.R.,1997. Extensional emplacement of a high-grade granite gneiss complex into low-grade greenstones, Eastern Goldfields, Yilgarn Craton, Western Australia Precambrian Research,83(1-3):203-219.
Taylor, S.R., McLennan, S.M.,1985. The Continental Crust:Its Composition and Evolution. Blackwell, Oxford,1-312 pp.
Thompson, A.B., James, A., Connolly, D.,1995. Melting of the continental crust:some themal and petrological sonstraints on anatexis in continental collision zones and other tectonic settings. J, Geophys. Res,100:565-579.
Trofimovs, J., Cas, R.A.F., Davis, B.K.,2004. An Archaean submarine volcanic debris avalanche deposit, Yilgarn Craton, western Australia, with komatiite, basalt and dacite megablocks:The product of dome collapse Journal of Volcanology and Geothermal Research,138(1-2):111-126.
Wan, Y.S., Song, B., Liu, D.Y. et al.,2006. SHRIMP U-Pb zircon geochronology of palaeoproterozoic metasedimentary rocks in the North China Craton:evidence for a major Late Palaeoproterozoic tectonothermal event. Precambrian Research,149:249-271.
Wang, Y.J., Zhang, Y.Z., Zhao, GC. et al.,2009. Zircon U-Pb geochronological and geochemical constraints on the petrogenesis of the Taishan sanukitoids(Shandong):Implications for Neoarchean subduction in the Eastern Block, North China Craton. Precambrian Research,174:273-286.
Wang, Z.H., Wilde, S.A., Wang, K.Y. et al.,2004. A MORB-arc basalt-adakite association in the 2.5Ga Wutai greenstone belt:late Archean magmatism and crustal growth in the North China Craton. Precambrian Research,131:323-343.
White, A.J.R., Jakes, P., Christie, D.M.,1971. Composition of greenstones and the hypothesis of sea-floor spreading in the Archean. Geol. Soc. Aust., Spec. Publ.,3(47-56).
Wilde, S.A., Cawood, P.A., Wang, K.Y. et al.,2005. Granitoid evolution in the Late Archean Wutai Complex. North China Craton. J. Asian Earth Sci.,24:597-613.
Williams, I.S.,1998. U-Th-Pb geochronology by ion microprobe. In:McKibben M A, Shanks W C, Ridley W I, eds. Applications of Microanalytical Techniques to Understanding Mineralizing Processes. Review of Economic Geology,7:1-35.
Wyman, D.A.,1999. A 2.7 Ga depleted tholeiite suite:evidence of plume-arc interaction in the Abitibi Greenstone Belt, Canada Precambrian Research,97(1-2):27-42.
Xie, Q., Kerrich, R., Fan, J.,1993. HFSE/REE fractionations recorded in three komatiite-basalt sequence, Archean Abitibi greenstone belt:implications for multiple plume sources and depths. Geochimica et Cosmochemica Acta,57:4111-4118.
Zhao, G.C., Wilde, S.A., Cawood, P.A. et al.,1998. Thermal evolution of the Archaean basement rocks from the eastern part of the North China Craton and tis bearing on tectonic setting. International Geology Review,40:706-721.
Zhao, G.C., Wilde, S.A., Cawood, P.A. et al.,2000. Petrology and P-T path of the Fuping mafic granulites: implications for tectonic evolution of the central zone of the North China craton. J. metamorphic Geol.,,18:375-391.
Zhao, G.C., Wilde, S.A., Cawood, P.A. et al.,2001. Archean blocks and their boundaries in the North China Craton lithological, geochemical, structural and P-T path constraints and tectonic evolution. Precambrian Research,107(1-2):45-73.
Zhao, G.C., Wilde, S.A., Cawood, P.A. et al.,2002. SHRIMP U-Pb zircon ages of the Fuping complex: implications for Late Archean to Paleoproterozoic accretion and assembly of the North China Craton. Am. J. Sci,302:191-226.
Zhao, G.C., Sun, M., Wilde, S.A. et al.,2005. Late Archean to paleoproterozoic evolution of the North China Craton:key issues revisited. Precambrian Research,136:177-202.
Zhao, G.C., Wilde, S.A., Sun, M. et al.,2008. SHRIMP U-Pb zircon geochronology of the Huai'an complex:Constraints on late Archean to Paleoproterozoic magmatic and metamorphic events in the Trans-North China Orogen. Am. J. Sci,308(3):270-303.
山东地调院,1995.1:5万大王庄、仲宫、雪野、博山四幅地质图区调报告,济南.
万渝生,1986.山东雁翎关地区雌山混合花岗岩地球化学特征及其成因.岩石矿物学杂志,5(3):203-211.
万渝生,1993.辽宁弓长岭含铁岩系的形成与演化.北京科学技术出版社,北京,1-108 pp.
万渝生,张巧大,宋天锐,2003.北京十三陵长城系常州沟组碎屑锆石SHRIMP年龄:华北克拉通盖层物源区及最大沉积年龄的限定.科学通报,48(18):1970-1975.
万渝生,宋彪,耿元生等,2005a.辽北抚顺—清原地区太古宙基底地球化学组成特征及其地质意义.地质论评,51(2):128-137.
万渝生,宋彪,杨淳等,2005b.辽宁抚顺—清原地区太古宙岩石SHRIMP U-Pb年代学及其地质意义.地质学报,79(1):78-87.
王世进,1993.鲁西地区早前寒武纪地质构造.中国区域地质,3:216-222.
王世进,万喻生,张成基等,2008.鲁西地区早前寒武纪地质研究新进展.山东国土资源,24(1):10-20.
王伟,杨恩秀,王世进等,2009.鲁西泰山岩群变质枕状玄武岩岩相学和侵入的奥长花岗岩SHRIMP锆石U-Pb年代学.地质论评,55(5):737-745.
王伟,王世进,刘敦一等,2010.鲁西新太古代济宁群含铁岩系形成时代SHRIMP U-Pb锆石定年.岩石学报,26(4):1175-1181.
伍家善,耿元生,沈其韩,1998.中朝古大陆太古宙地质特征及构造演化.地质出版社,北京,1-212pp.
庄育勋,王新社,徐洪林等,1997.泰山地区早前寒武纪主要地质事件与陆壳演化.岩石学报,13(3):313-330.
李俊建,沈保丰,李双保等,1999.辽北—吉南地区太古宙绿岩带.华北地质矿产杂志,14(1):27-34.
杜利林,庄育勋,杨崇辉等,2003.山东新泰孟家屯岩组锆石特征及其年代学意义.地质学报,77(3):359-366.
杜利林,庄育勋,杨崇辉等,2005.鲁西孟家屯一种细粒斜长角闪岩的锆石SHRIMP年代学.地球学报,26(5):429-434.
沈其韩,宋彪,徐惠芬等,2004.山东沂水太古宙蔡峪和大山岩体SHRIMP锆石年代学.地质论评,50(3):275-284.
沈其韩,耿元生,宋彪等,2005.华北和扬子陆块及秦岭—大别造山带地表和深部太古宙基底的新信息.地质学报,79(5):617-627.
沈其韩,赵子然,宋彪等,2007.山东沂水新太古代马山和雪山岩体的地质、岩石化学特征和SHRIMP锆石年代研究.地质论评,53(2):181-186.
沈保丰,李俊建,毛德宝,1997.华北地台绿岩带地质特征类型和演化.前寒武纪研究进展,20(1):2-11.
周喜文,耿元生,2009.贺兰山孔兹岩系的变质时代及其对华北克拉通西部陆块演化的制约.岩石学报,25:1843-1852.
邱家骧,1985.岩浆岩岩石学.地质出版社,北京,99-120 pp.
胡凤翔,黄占起,李四娃et al.,2002.内蒙古中部地区绿岩及绿岩型金矿成矿地质特征.前寒武纪研究进展,25(3):190-198.
徐惠芬,1992.鲁西花岗绿岩带.地质出版社,北京,1-67 pp.
曹国权,1996.鲁西早前寒武纪地质.地质出版社,北京,1-210 pp.
程裕淇,沈其韩,王泽九等,1964.山东新泰雁翎关一带泰山群变质岩类和岩浆岩类的地质年代学研究.地质论评,22(3):198-209.
程裕淇,沈其韩,王泽九,1977.山东新泰雁翎关一带泰山群变质岩系的初步.地质矿产研究,3(1-158).
程裕淇,沈其韩,王泽九,1982.山东太古代雁翎关变质火山—沉积岩.地质出版社,北京,1-72 pp.
董春艳,刘敦一,李俊建等,,2007.华北克拉通西部孔兹岩带形成时代新证据:巴彦乌拉—贺兰山地区锆石SHRIMP定年和Hf同位素组成.科学通报,53(16):1923-1934.
翟明国,卞爱国,赵太平,2000.华北克拉通新太古代末超大陆拼合及古元古代末—中元古代裂解.中国科学(D),30:129-137.
赵子然,宋会侠,沈其韩等,2008.山东沂水英灵山花岗岩及其捕虏体的地质、岩石地球化学特征和锆石SHRIMP U-Pb定年.地质通报,27(9):1551-1558.
赵子然,宋会侠,沈其韩等,2009.山东沂水杂岩中变基性岩岩石地球化学特征及锆石SHRIMP U-Pb定年.地质论评,55(286-299).
韩玉珍,王世进,李培远,2008.济宁颜店铁矿地质特征及济宁岩群含矿性研究.山东国土资源,24(2):3-8.
黄吉友,宋立品,2000.胶北太古宙并花岗岩—绿岩带概述.山东地质,16(3):15-21.
陆松年,陈志宏,相振群.泰山世界地质公园古老侵入岩系年代格架.北京:地质出版社,2008:45-80.
①山东省地质矿产局第一地质队,1989,1:5万东王庄幅区调报告
②山东地质调查研究院,1990,1:20万新泰幅区调报告