华北东部早白垩世A型花岗岩与克拉通破坏

孙金凤; 杨进辉

华北东部早白垩世A型花岗岩与克拉通破坏

孙金凤,
杨进辉^,

中国科学院地质与地球物理研究所岩石圈演化国家重点实验室, 北京 100029

基金项目:

国家自然科学基金 40873010

国家自然科学基金 40672055

详细信息

作者简介:
孙金凤(_1983—), 女, 在读博士研究生.专业方向: 同位素地球化学和岩石学

通讯作者:
杨进辉, E-mail: jinhui@mail.igcas.ac.cn

中图分类号: P588
计量
- 文章访问数: 3874
- HTML全文浏览量: 537
- PDF下载量: 97
- 被引次数: 0
出版历程
- 收稿日期: 2008-10-15
- 刊出日期: 2009-01-25

Early Cretaceous A-Type Granites in the Eastern North China Block with Relation to Destruction of the Craton

SUN Jin-feng,
YANG Jin-hui^,

State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

摘要

摘要: A型花岗岩是非造山的、无水的碱性花岗岩, 具有独特的矿物学、岩石学和地球化学特征, 形成于造山后、板内非造山或者地幔热柱等伸展动力学背景, 蕴涵着大陆地壳生长、岩石圈演化及区域构造发展等大陆动力学的重要信息.在华北东部广泛分布着一期中生代A型花岗岩及伴生的碱性岩, 结合前人的研究成果以及笔者近年来的研究发现: 它们主要侵位于早白垩世(130~110Ma), 来源于上地壳、下地壳和地幔等多元源区, 是不同成分的岩浆经过分离结晶、岩浆混合作用形成; 综合区域地球动力学研究和A型花岗岩本身的地球化学特征, 认为华北东部早白垩世A型花岗岩形成于地壳伸展背景之下, 是岩石圈减薄和克拉通破坏的浅部地质响应, 标志着华北东部岩石圈减薄和克拉通破坏作用的峰期.
- A型花岗岩 /
- 早白垩世 /
- 华北克拉通 /
- 去克拉通化作用
Abstract: A-type granite is anorogenic, anhydrous and alkaline granite and has unique mineralogical, petrological and geochemical characteristics, which is considered to be emplaced in post-orogenic, within-plate or plume-related extensional setting.A-type granites and related alkaline rocks imply important information of geodynamics and are the key to understand the growth of continental crust, the lithospheric evolution and the development of regional tectonics.Late Mesozoic A-type granites and related alkaline rocks are widespread in the eastern North China craton.Previous studies and our recently published data show that they formed via a complex process involving mixing of magmas derived from mantle and upper and lower crust sources, crystal fractionation and infracrustal melting during Early Cretaceous (130-110Ma).On the basis of the study of regional geology, it is suggested that the A-type granites and related alkaline rocks were formed in an extensional setting and were the shallow responses to the lithospheric thinning and decratonization, which indicate the peak time of lithospheric thinning and destruction of the North China craton.
- A-type granite /
- Early Cretaceous /
- North China craton /
- decratonization

HTML全文

图 1 华北克拉通东部早白垩世A型花岗岩分布

Fig. 1. Sketch map showing the distribution of Early Cretaceous A-type granites in the eastern North China craton

下载: 全尺寸图片幻灯片

图 2 辽东半岛千山A型花岗岩岩体地质图(a, b), 镁铁质包体与花岗岩野外照片(c) 及其Sr-Nd同位素组成(d) (据Yang et al., 2006)

Fig. 2. Geological map (a, b), field picture of A-type granite and mafic enclave (c) and Sr-Nd isotopic compositions (d)

下载: 全尺寸图片幻灯片

图 3 华北东部早白垩世A型花岗岩的Sr、Nd同位素组成

Fig. 3. Sr and Nd isotopic compositions of Early Cretaceous A-type granites in the eastern North China craton

下载: 全尺寸图片幻灯片

表 1 华北东部早白垩世A型花岗岩的锆石U-Pb年龄

Table 1. Zircon U-Pb ages data of the Early Cretaceous A-type granites in the eastern North China craton

参考文献(93)

Barbarin, B., 1990. Granitoids main petrogenetic classifica-tionin relation to origin and tectonic setting. Geochemi-cal Journal, 25: 227-238.
Barbarin, B., 1999. A review of the relationships betweengranitoid types, their origins and their geodynamic envi-ronments. Lithos, 46: 605-626. doi: 10.1016/S0024-4937(98)00085-1
Bedard, J., 1990. Enclaves from the A-type granite of theMegantic complex, White Mountain magma series: Cluesto granite magmagenesis. J. Geophy. Res., 95: 17797-17819. doi: 10.1029/JB095iB11p17797
Bonin, B., 2007. A-type granites and related rocks: Evolutionof a concept, problems and prospects. Lithos, 97: 1-29. doi: 10.1016/j.lithos.2006.12.007
Bonin, B., Azzouni, S. A., Bussy, F., et al., 1998. Alkali-cal-cic and alkaline post-orogenic (PO) granite magmatism: Petrologic constraints and geodynamic settings. Lithos, 45 (1-4): 45-70. doi: 10.1016/S0024-4937(98)00025-5
Carlson, R. W., Pearson, D. G., James, D. E., 2005. Physi-cal, chemical, and chronological characteristics of conti-nental mantle. Rev. Geophys., 43, doi: 10.1029/2004RG000156.
Chappell, B. W., White, A. J. R., 1992. I and S-type granitesin the Lachlan fold belt. Trans. Royal Soc. Edinburgh: Earth Sci., 83: 1-26. doi: 10.1017/S0263593300007720
Clemens, J. D., Holloway, J. R., White, A. J. R., 1986. Ori-gin of an A-type granite: Experimental constraints. American Mineralogist, 71 (3-4): 317-324.
Coleman, D. S., Frost, T. P., Glazner, A. F., 1992. Evidencefrom the Lamarck granodiorite for rapid Late Creta-ceous crust formationin California. Science, 258 (5090): 1924-1926. doi: 10.1126/science.258.5090.1924
Collins, W. J., Beams, S. D., White, A. J. R., et al., 1982. Nature and origin of A-type granites with particular ref-erence to southeastern Australia. Contributions to Min-eralogy and Petrology, 80 (2): 189-200. doi: 10.1007/BF00374895
Creaser, R. A., Price, R. C., Wormald, R. J., 1991. A-typegranites revisited: Assessment of a residual-source mod-el. Geology, 19: 163-166.
Davis, G. A., Zheng, Y. D., Wang, C., et al., 2001. Mesozoictectonic evolution of the Yanshan fold and thrust belt, with emphasis on Hebei and Liaoning provinces, north-ern China. In: Hendrix, M. S., Davis, G. A., eds., Pale-ozoic and Mesozoic tectonic evolution of Central Asia: Fromcontinental assembly to intracontinental deforma-tion. Geological Society of America, Memoirs, 194: 171-198.
Eby, G. N., 1990. The A-type granitoids: A review of theiroccurrence and chemical characteristics and speculationson their petrogenesis. Lithos, 26: 115-134. doi: 10.1016/0024-4937(90)90043-Z
Eby, G. N., 1992. Chemical subdivision of the A-type granit-oids: Petrogenetic and tectonic implications. Geology, 20 (7): 641-644. doi: 10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2
Fan, W. M., Menzies, M. A., 1992. Destruction of aged lower lithosphere and accretion of asthenosphere mantle be-neath eastern China. Geotectonic et Metallogenia, 16: 171-180.
Förster, H. J., Tischendorf, G., Trumbull, R. B., 1997. Anevaluation of the Rb vs. (Y+Nb) discrimination dia-gram to infer tectonic setting of silicic igneous rocks. Lithos, 40: 261-293. doi: 10.1016/S0024-4937(97)00032-7
Gao, S., Rudnick, R. L., Yuan, H. L., et al., 2004. Recyclinglower continental crust in the North China craton. Nature, 432: 892-897. doi: 10.1038/nature03162
Griffin, W. L., Zhang, A. D., O'Reilly, S. Y., et al., 1998. Phanerozoic evolution of the lithosphere beneath the Si-no-Korean craton. In: Flower, M. F. J., Chung, S. L., Lo, C. H., et al., eds., Mantle dynamics and plateinter-actions in East Asia. Am. Geophy. Union, WashingtonD. C., Geodyn., 27: 107-126.
Guo, C. L., Wu, F. Y., Yang, J. H., et al., 2004. The exten-sional setting of the Early Cretaceous magmatism ineastern China: Example fromthe Yinmawanshan plutonin southern Liaodong Peninsula. Acta Petrologica Sini-ca, 20 (5): 1193-1204 (in Chinese with English ab-stract).
Hawkesworth, C. J., Kemp, A. I. S., 2006. Using hafniumand oxygenisotopes in zircons to unravel the record ofcrustal evolution. Chemical Geology, 226 (3-4): 144-162. doi: 10.1016/j.chemgeo.2005.09.018
Jahn, B. M., Griffin, W. L., Windley, B. F., 2000. Continentalgrowthin the Phanerozoic: Evidence from Central Asi-an. Tectonophysics, 328: 1-227. doi: 10.1016/S0040-1951(00)00175-X
Jordan, T. H., 1975. The continental tectosphere. Reviews ofGeophysics and Space Physics, 13: 1-12.
Kerr, A., Fryer, B. J., 1993. Nd isotopic evidence for crustmantle interactionin the generation of A-type granitoidsuites in Labrador, Canada. Chem. Geol. , 104: 39-60. doi: 10.1016/0009-2541(93)90141-5
King, P. L., White, A. J. R., Chappell, B. W., et al., 1997. Characterization and origin of aluminous A-type gran-ites fromthe Lachlan fold belt, southeastern Australia. J. Petrol., 38 (3): 371-391. doi: 10.1093/petroj/38.3.371
Loisselle, M. C., Wones, D. R., 1979. Characteristics and ori-gin of anorogenic granites. Geological Society of Amer-ica, 11: 468.
Maniar, P. D., Piccoli, P. M., 1989. Tectonic discriminationof granitoids. GSA Bull., 101 (5): 635-643. doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2
Meng, Q. R., 2003. What drove Late Mesozoic extension ofthe northern China-Mongolia tract? Tectonophysics, 369: 155-174. doi: 10.1016/S0040-1951(03)00195-1
Menzies, M. A., Fan, W. M., Zhang, M., 1993. Palaeozoicand Cenozoic lithoprobe and theloss of & amp; gt;120kmof Ar-chean lithosphere, Sino-Korean craton, China. In: Pri-chard, H. M., Alabaster, T., Harris, N. B. W., et al., eds., Magmatic processes and plate tectonics. Geol. Soc. Spec. Pub., 76: 71-81.
Mingram, B., Trumbull, R. B., Litt man, S., et al., 2000. Apetrogenetic study of anorogenic felsic magmatism inthe Cretaceous Paresis Ring complex, Namibia: Evi-dence for mixing of crust and mantle-derived compo-nents. Lithos, 54: 1-22. doi: 10.1016/S0024-4937(00)00033-5
Mushkin, A., Navon, O., Halicz, L., et al., 2003. The petro-genesis of A-type magmas from the Amram massif, southern Israel. Journal of Petrology, 44 (5): 815-832. doi: 10.1093/petrology/44.5.815
Patino Douce, A. E., 1997. Generation of metaluminousA-type granites by low-pressure melting of calc-alkalinegranitoids. Geology, 25 (8): 743-746. doi: 10.1130/0091-7613(1997)025<0743:GOMATG>2.3.CO;2
Pearce, J. A., 1996. Sources and settings of granitic rocks. Episodes, 19 (4): 120-125. doi: 10.18814/epiiugs/1996/v19i4/005
Pearce, J. A., Harris, N. B. W., Tindle, A. G., 1984. Traceelement discrimination diagrams for the tectonic inter-pretation of granitic rocks. Journal of Petrology, 25: 956-983. doi: 10.1093/petrology/25.4.956
Pitcher, W. S., 1997. The nature and origin of granite. Chap-man and Hall, London, 1-386.
Skjerlie, K. P., Johnston, A. D., 1992. Vapor-absent meltingat10kbar of a biotite-and amphibole-bearing tonaliticgneiss: Implications for the generation of A-type gran-ites. Geology, 20 (3): 263-266. doi: 10.1130/0091-7613(1992)020<0263:VAMAKO>2.3.CO;2
Thompson, A. B., 1999. Some time-space relationships forcrustal melting and granitic intrusion at various depths. In: Castro, A., Femandez, C., Vigneresse, J. L., eds., Understanding granites: Intergrating new and classicaltechniques. Geol. Soc. Spec. Pub., 168: 7-25.
Turner, S. P., Arnaud, N., Liu, J., et al., 1996. Post colli-sion, shoshonitic volcanism on the Tibetan Plateau: Im-plications for convective thinning of the lithosphere andthe source of ocean island basalts. Journal of Petrolo-gy, 37: 45-71. doi: 10.1093/petrology/37.1.45
Turner, S. P., Foden, J. D., Morrison, R. S., 1992. Derivationof some A-type magmas by fractionation of basalticmagma: An example fromthe Padthaway Ridge, SouthAustralia. Lithos, 28: 151-179. doi: 10.1016/0024-4937(92)90029-X
Wang, Q., Zhao, Z. H., Xiong, X. L., 2000. The Ascertain-ment of Late Yanshanian A-type Granite in Tongbai-Dabie orogenic belt. Acta Petrologica et Mineralogica, 19: 297-315 (in Chinese with English abstract).
Wei, C. S., Zheng, Y. F., Zhao, Z. F., 2001. Nd-Sr-Oisotopic geochemistry constraints onthe age and origin of the A-type granites in eastern China. Acta Petrologica Sini-ca, 17 (1): 95-111 (in Chinese with English abstract).
Wei, C. S., Zheng, Y. F., Zhao, Z. F., et al., 2002. Oxygenand neodymiumisotope evidence for recycling of Juven-ile crust in Northeast China. Geology, 30: 375-378.
Whalen, J. B., Currie, K. L., Chappell, B. W., 1987. A-typegranites: Geochemical characteristics, discrimination andpetrogenesis. Contributions to Mineralogy and Petrolo-gy, 95 (4): 407-419. doi: 10.1007/BF00402202
Wu, F. Y., Han, R. H., Yang, J. H., et al., 2007a. Initialconstraints on the timing of granitic magmatism inNorth Korea using U-Pb zircon geochronology. Chem. Geol., 238 (3-4): 232-248. doi: 10.1016/j.chemgeo.2006.11.012
Wu, F. Y., Jahn, B. M., Wilde, S. A., et al., 2003a. Highlyfractionated I-type granites in NE China (Ⅰ): Geochro-nology and petrogenesis. Lithos, 66 (3-4): 241-273. doi: 10.1016/S0024-4937(02)00222-0
Wu, F. Y., Jahn, B. M., Wilde, S. A., et al., 2003b. Highlyfractionated I-type granites in NE China (Ⅱ): Isotopic geochemistry and implications for crustal growth in thePhanerozoic. Lithos, 67: 191-204. doi: 10.1016/S0024-4937(03)00015-X
Wu, F. Y., Li, X. H., Yang, J. H., et al., 2007b. Discussionson the petrogenesis of granites. Acta Petrotogica Sini-ca, 23 (6): 1217-1238 (in Chinese with English ab-stract).
Wu, F. Y., Lin, J. Q., Wilde, S. A., et al., 2005a. Nature andsignificance of the Early Cretaceous giant igneous eventin eastern China. Earth Planet. Sci. Lett., 233: 103-119. doi: 10.1016/j.epsl.2005.02.019
Wu, F. Y., Sun, D. Y., 1999. The Mesozoic magmatism andlithospheric thinning in eastern China. Changchun Uni. Sci. Tech., 29 (4): 313-318 (in Chinese with Englishabstract).
Wu, F. Y., Sun, D. Y., Li, H. M., et al., 2002. A-type gran-ites in northeastern China: Age and geochemical con-straints on their petrogenesis. Chemical Geology, 187: 143-173. doi: 10.1016/S0009-2541(02)00018-9
Wu, F. Y., Walker, R. J., Ren, X. W., et al., 2003c. Osmiumisotopic constraints on the age of lithospheric mantlebeneath northeastern China. Chem. Geol., 196 (1-4): 107-129. doi: 10.1016/S0009-2541(02)00409-6
Wu, F. Y., Walker, R. J., Yang, Y. H., et al., 2006b. Thechemical-temporal evolution of lithospheric mantle un-derlying the North China craton. Geochim. Cosmochim. Acta, 70: 5013-5034. doi: 10.1016/j.gca.2006.07.014
Wu, F. Y., Yang, J. H., Liu, X. M., 2005b. Geochronological framework of the Mesozoic granitic magmatismin theLiaodong Peninsula, northeast China. Geological Jour-nal of China Universities, 11 (3): 305-317 (in Chinesewith English abstract).
Wu, F. Y., Yang, J. H., Zhang, Y. B., et al., 2006a. Emplace-ment ages of the Mesozoic granites in southeastern part ofthe western Liaoning Province. Acta Petrologica Sinica, 22 (2): 315-325 (in Chinese with English abstract).
Xie, Z., Zheng, Y. F., Yan, J., et al., 2004. Source evolution relationship between A-type granites and mafic rocksfrom Shacun in Dabieshan. Acta Petrologica Sinica, 20 (5): 1175-1184 (in Chinese with English abstract).
Xu, B. L., Wang, S. G., Han, B. F., et al., 1998. A-typegranites with the character of enrichment and loss withparticular reference to both suites of the Yanshan, North China and Wulunguhe, Northwest China. ActaScientiarum Naturalium Universitatis Pekinensis, 34 (2-3): 352-362 (in Chinese with English abstract).
Xu, B. L., Yan, G. H., Huang, F. S., et al., 1994. Rock-forming minerals and magmatic history of evolution andcrystallization of Wulingshan A-type granitic complex. Acta Scientiarum Naturalium Universitatis Pekinen-sis, 30 (6): 703-716 (in Chinese with English ab-stract).
Xu, Y. G., 2001. Thermo-tectonic destruction of the Archae-an lithospheric keel beneath the Sino-Korean craton inChina: Evidence, timing and mechanism. Phys. Chem. Earth. (A), 26: 747-757.
Yan, G. H., Xu, B. L., Mu, B. L., et al., 2001. Characteris-tics and implications of Nd, Sr, Pb in Mesozoic Alka-line-richintrusionin North China. Bulletinof Mineral-ogy, Petrology and Geochemistry, 20 (4): 234-237 (inChinese with English abstract).
Yang, J. H., Wu, F. Y., Chung, S. L., et al., 2004. Multiplesources for the origin of granites: Geochemical and Nd/Sr isotopic evidence fromthe Gudaoling granite and itsmafic enclaves, Northeast China. Geochim. Cosmochim. Acta, 68: 4469-4483. doi: 10.1016/j.gca.2004.04.015
Yang, J. H., Wu, F. Y., Chung, S. L., et al., 2005. Petrogen-esis and tectonic significance of Early Cretaceous granit-ic magmastismin the Sulu ultrahigh-pressure orogenicbelt, East China. Chem. Geol., 222: 200-231. doi: 10.1016/j.chemgeo.2005.07.006
Yang, J. H., Wu, F. Y., Chung, S. L., et al., 2006. A hybridorigin for the Qianshan A-type granites, Northeast Chi-na: Geochemical and Sr-Nd-Hf isotopic evidence. Lithos, 89 (1-2): 89-106. doi: 10.1016/j.lithos.2005.10.002
Yang, J. H., Wu, F. Y., Wilde, S. A., 2003. A review of thegeodynamic setting of large-scale Late Mesozoic gold mineralization in the North China craton: An associationwith lithospheric thinning. Ore. Geol. Rev., 23: 125-152. doi: 10.1016/S0169-1368(03)00033-7
Yang, J. H., Wu, F. Y., Wilde, S. A., et al., 2007a. Tracingmagma mixing in granite genesis: In situ U-Pb datingand Hf-isotope analysis of zircons. Contrib. Mineral. Petrol., 153: 177-190.
Yang, J. H., Wu, F. Y., Chung, S. L., et al., 2007b. Rapidexhumation and cooling of the Liaonan metamorphiccore compex: Inferences from ⁴⁰Ar/³⁹Ar thermochronol-ogy and implications for Late Mesozoic extensionin theeastern North China craton. GSA Bulletin, 119 (11): 1405-1414.
Yang, J. H., Sun, J. F., Chen, F. K., et al., 2007c. Sourcesand petrogenesis of Late Triassic dolerite dikes in theLiaodong Peninsula: Implications for post-collisional lithosphere thinning of eastern North China craton. J. Petrol., 48 (10): 1973-1997. doi: 10.1093/petrology/egm046
Yang, J. H., Wu, F. Y., Wilde, S. A., et al., 2007d. Petro-genesis of Late Triassic granitoids and their enclaveswith implications for post-collisional lithospheric thinning of the Liaodong Peninsula, North China cra-ton. Chem. Geol., 242 (1-2): 155-175. doi: 10.1016/j.chemgeo.2007.03.007
Yang, J. H., Wu, F. Y., Chung, S. L., et al., 2008c. The ex-tensional geodynamic setting of Early Cretaceous gra-nitic intrusions in the eastern North China craton: Evi-dence fromlaser ablation ⁴⁰Ar/³⁹Ar dating of K-bearingminerals. Acta Petrologica Sinica, 24: 1175-1184 (inChinese with English abstract).
Yang, J. H., Wu, F. Y., Wilde, S. A., et al., 2008a. Mesozoic decratonization of the North China block. Geology, 36 (6): 467-470.
Yang, J. H., Wu, F. Y., Wilde, S. A., et al., 2008b. Petro-genesis of an Alkali syenite-granite-rhyolite suite in theYanshan fold and thrust belt, eastern North China cra-ton: Geochronological, geochemical and Nd-Sr-Hf iso-topic evidence for lithospheric thinning. Journal of Pe-trology, 49 (2): 315-351.
Ying, J. F., Zhang, H. F., Sun, M., et al., 2007. Petrologyand geochemistry of Zijinshan alkaline intrusive com-plex in Shanxi Province, western North China craton: Implication for magma mixing of different sources in anextensional regime. Lithos, 98 (1-4): 45-66. doi: 10.1016/j.lithos.2007.02.001
Zhang, H. F., 2005. Transformation of lithospheric mantlethrough peridotite-melt reaction: Acase of Sino-Koreancraton. Earth Planet. Sci. Lett., 237: 768-780. doi: 10.1016/j.epsl.2005.06.041
Zhao, G. T., Wang, D. Z., Cao, Q. C., 1997. The geochemis-try and genesis of the Laoshan granitoids, ShandongProvince. Geological Journal of China Universities, 3 (1): 1-15 (in Chinese with English abstract).
Zheng, J. P., Griffin, W. L., O'Reilly, S. Y., et al., 2007. Mechanismand timing of lithospheric modification andreplacement beneath the eastern North China craton: Peridotitic xenoliths fromthe100Ma Fuxin basalts anda regional synthesis. Geochim. Cosmochim. Acta, 71 (2): 5203-5225.
Zheng , J.P., 1999.Mesozoic-Cenozoic mantle replacement and lithospheric thinning beneath the eastern China.China University of Geosciences Press, Wuhan (in Chinese)
Zhou, L., Chen, B., 2006. Petrogenesis and significance of theHongshan syenitic pluton, South Taihang: Zircon SHRI MPU-Pb age, chemical compositions and Sr-Nd isotopes. Pro-gress in Natural Science, 16 (2): 192-200. doi: 10.1080/10020070612331343213
Zhou, L. D., Zhao, Z. H., 1994. Petrographic and petrochemical characteristics of alkali-rich intrusions in China. Science inChina (Ser. B), 24 (10): 1093-1101 (in Chinese).
Zhou, T. X., Chen, J. F., Zhang, X., et al., 1995. Geochemis-try of the North Huaiyang granite-syenite zone and itstectonic implication. Geological Review, 41 (2): 144-151 (in Chinese with English abstract).
郭春丽, 吴福元, 杨进辉, 等, 2004. 中国东部早白垩世岩浆作用的伸展构造性质——以辽东半岛南部饮马湾山岩体为例. 岩石学报, 20 (5): 1193-1204. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200405014.htm
王强, 赵振华, 熊小林, 2000. 桐柏-大别造山带燕山晚期A型花岗岩的厘定. 岩石矿物学杂志, 19: 297-315. doi: 10.3969/j.issn.1000-6524.2000.04.002
魏春生, 郑永飞, 赵子福, 2001. 中国东部A型花岗岩形成时代及物质来源的Nd-Sr-O同位素地球化学制约. 岩石学报, 17 (1): 95-111. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200101009.htm
吴福元, 李献华, 杨进辉, 等, 2007b. 花岗岩成因研究的若干问题. 岩石学报, 23 (6): 1217-1238. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200706000.htm
吴福元, 孙德有, 1999. 中国东部中生代岩浆作用与岩石圈减薄. 长春科技大学学报, 29 (4): 313-318. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ199904000.htm
吴福元, 杨进辉, 柳小明, 2005b. 辽东半岛中生代花岗质岩浆作用的年代学格架. 高校地质学报, 11 (3): 305-317. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200503003.htm
吴福元, 杨进辉, 张艳斌, 等, 2006a. 辽西东南部中生代花岗岩的时代. 岩石学报, 22 (2): 315-325. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200602006.htm
谢智, 郑永飞, 闫峻, 等, 2004. 大别山沙村中生代A型花岗岩和基性岩的源区演化关系. 岩石学报, 20 (5): 1175-1184. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200405012.htm
许保良, 王式洸, 韩宝福, 等, 1998. 富集性和亏损性A型花岗岩——以华北燕山和新疆乌伦古河地区岩石为例. 北京大学学报(自然科学版), 34 (2-3): 352-362. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ8Z1.028.htm
许保良, 阎国瀚, 黄福生, 等, 1994. 雾灵山A型花岗岩系的矿物学特征及成因意义. 北京大学学报(自然科学版), 30 (6): 703-716. doi: 10.3321/j.issn:0479-8023.1994.06.001
阎国瀚, 许保良, 牟保磊, 等, 2001. 中国北方中生代富碱侵入岩钕、锶、铅同位素特征及其意义. 矿物岩石地球化学通报, 20: 234-237. doi: 10.3969/j.issn.1007-2802.2001.04.008
杨进辉, 吴福元, 钟孙霖, 等, 2008. 华北东部早白垩世花岗岩侵位的伸展地球动力学背景: 激光⁴⁰Ar/³⁹Ar年代学证据. 岩石学报, 24: 1175-1184. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200806002.htm
赵广涛, 王德滋, 曹钦臣, 1997. 崂山花岗岩岩石地球化学与成因. 高校地质学报, 3 (1): 1-15. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX701.000.htm
郑建平, 1999. 中国东部地幔置换作用与中新生代岩石圈减薄. 武汉: 中国地质大学出版社.
周玲棣, 赵振华, 1994. 我国富碱侵入岩的岩石学和岩石化学特征. 中国科学(B辑), 24 (10): 1093-1101. https://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199410012.htm
周泰禧, 陈江峰, 张巽, 等, 1995. 北淮阳花岗岩—正长岩带地球化学特征及其大地构造意义. 地质论评, 41 (2): 144-151. doi: 10.3321/j.issn:0371-5736.1995.02.006