Early-Middle Permian tectonic evolution of the central-northern margin of the North China Craton: Constraints from zircon U-Pb ages and geochemistry of the granitoids
-
摘要:
内蒙古温都尔庙南-铁沙盖黑云角闪石英闪长岩和角闪黑云花岗闪长岩位于华北板块北缘中段晚古生代构造岩浆活动带中；锆石LA-ICP-MS U-Pb定年结果显示，其形成时代分别为271.8±2.4Ma，271.4±1.3Ma、268.7±1.3Ma。主量元素SiO2含量61.42%~71.73%，K2O含量3.10%~5.11%，K2O/Na2O值介于0.93~1.96之间，Mg#值介于42.54~49.93之间，A/CNK为0.90~1.03；副矿物为锆石、磷灰石和磁铁矿，属亚碱性高钾钙碱性系列、Ⅰ型花岗岩类；富集轻稀土(LREEs)、大离子亲石元素(LILEs，Cs、Rb、K、Ba、Th和U)，亏损重稀土元素(HREEs)及高场强元素(HFSEs，Nb、Ta和Ti)，弱Eu负异常(δEu=0.55~0.95)，形成于活动大陆边缘弧环境，是上地壳部分熔融的产物。黑云角闪石英闪长岩和角闪黑云花岗闪长岩中发育大量暗色微粒包体(黑云闪长岩)，包体可能是岩石圈地幔部分熔融的产物，相对于寄主岩石贫Si、K富Fe、Mg、Ca、Ti、大离子亲石元素(LILEs，Rb、Cs、Sr和U)和高场强元素(HFSEs，Nb、Ta、Zr、Hf)。本文花岗岩类的侵位反映了早中二叠世古亚洲洋俯冲于华北板块北缘之下及岩浆混合作用的岩浆事件。
Abstract:This paper presents petrological, geochronological and geochemical study on Late Paleozoic intermediate-felsic intrusions from the Ondor Sum-Tieshagai area in Inner Mongolia, which is tectonically located in the central-northern margin of the North China Craton. These intrusions comprise mainly biotite-hornblende quartz diorite and hornblende-biotite granodiorite with abundant mafic enclaves in field. U-Pb dating of zircons from three samples by LA-ICP-MS yield weighed mean 206Pb/238U ages of 271.8±2.4Ma, 271.4±1.3Ma and 268.7±1.3Ma, respectively. These rocks have SiO2=61.42%~71.73%, K2O=3.10%~5.11%, K2O/Na2O=0.93~1.96, Mg#=42.54~49.93, A/CNK=0.90~1.03, features of high-K calc-alkaline I-type granitoids. They also show strong enrichments in light rare earth (LREEs) and large ion lithophile elements (LILEs, e.g., Cs, Rb, Ba, K, Th and U) and depletions in high field-strength elements (HFSEs, e.g., Nb, Ta and Ti) and heavy rare earth (HREEs), with weakly negative Eu anomalies (δEu=0.55~0.95). The primary magma for granitoids could be mainly derived from partial melting of the upper crust. The mafic microgranular enclaves (MMEs) are biotite diorites, characterized by low Si and K, enrichment in Fe, Mg, Ca, Ti, LILEs (Rb, Cs, Sr, U) and HFSEs (Nb, Ta, Zr, Hf) when compared with the host rocks, its primary magma could be mainly derived from partial melting of lithospheric mantle, implying an important role of magma mixing during the magmatic differentiation. The combined geochemical features of these intermediate-felsic intrusions and the MMEs likely indicate their formation in an active continental margin as a result of Middle Permian subduction of the Paleo-Asian Ocean beneath the northern margin of the North China Craton.
-
-
图 1
研究区大地构造位置(据Xiao et al., 2003修改)
Figure 1.
Geological regional location of research area (modified after Xiao et al., 2003)
图 3
石英闪长岩、花岗闪长岩及黑云闪长岩(包体)的宏观特征
Figure 3.
Macro-characteristics for quartz diorite and granodiorite and biotite diorite (enclave)
图 4
石英闪长岩、花岗闪长岩及黑云闪长岩的显微特征
Figure 4.
Microscopic characteristics of quartz diorite and granodiorite and biotite diorite
图 5
石英闪长岩和花岗闪长岩部分锆石CL图像
Figure 5.
CL images of selected zircons for quartz diorite and granodiorite
图 6
石英闪长岩和花岗闪长岩锆石U-Pb谐和图
Figure 6.
U-Pb concordia diagrams of zircon for quartz diorite and granodiorite
图 7
石英闪长岩、花岗闪长岩及黑云闪长岩(包体)的TAS图解(a)和SiO2-K2O图解(b)
Figure 7.
TAS (a) and SiO2-K2O (b) diagrams for quartz diorite and granodiorite and biotite diorite (enclave)
图 8
石英闪长岩、花岗闪长岩及黑云闪长岩(包体)的稀土元素球粒陨石标准化配分图(a)和微量元素原始地幔标准化蛛网图(b)
Figure 8.
Chondrite-normalized REE distribution patterns (a) and primitive mantle-normalized trace element patterns (b) for quartz diorite and granodiorite and biotite diorite (enclave)
图 9
石英闪长岩、花岗闪长岩及黑云闪长岩(包体)的共分母和不共分母协变图
Figure 9.
Covariant diagrams for compositions of quartz diorite and granodiorite and biotite diorite (enclave)
图 10
石英闪长岩、花岗闪长岩及黑云闪长岩(包体)的Y+Nb-Rb、Y-Nb和R1-R2图解
Figure 10.
Y+Nb-Rb, Y-Nb and R1-R2 diagrams for quartz diorite and granodiorite and biotite diorite (enclave)
图 11
早中二叠世温都尔庙南-铁沙盖地区构造环境示意图(据Xiao et al., 2003；Jian et al., 2010修改)
Figure 11.
Schematic diagram of tectonic setting for the area between the south of Ondor Sum and Tieshagai area during Early-Middle Permian (modified after Xiao et al., 2003；Jian et al., 2010)
-
Barth MG, McDonough WF and Rndnick RL. 2000. Tracking the budget of Nb and Ta in the continental crust. Chemical Geology, 165(3-4): 197-213
Bureau Geology and Mineral Resources of Inner Mongolia Autonomous Region. 1991. Regional Geology of Inner Mongolia Autonomous Region. Beijing: Geological Publish House, 351-458 (in Chinese)
Chen B, Zhao GC and Simon W. 2001. Subduction- and collision-related granitoids from southern Sonidzuoqi, Inner Mongolia: Isotopic ages and tectonic implications. Geological Review, 47(4): 361-367 (in Chinese with English abstract)
Chen B. 2011. Sedimentary characteristics and tectonic setting of Permian in the Xing'an region of Inner Mongolian autonomous region. Master Degree Thesis. Beijing: China University of Geosciences, 30-53 (in Chinese with English summary)
Chen Q, Chou GL, Xue LF, Zou XM, Zhou HP and Du YS. 1993. Palaeoplate evolution in the southern part of the Inner Monglian Orogenic Belt. Geological Review, 39(6): 477-483 (in Chinese with English abstract)
Didier J and Barbarin B. 1991. Enclaves and Granite Petrology. Amsterdam: Elsevier, 625
Frey FA and Prinz M. 1978. Ultramafic inclusions from San Carlos, Arizona: Petrologic and geochemical data bearing on their petrogenesis. Earth and Planetary Science Letters, 38(1): 129-176
Guo F, Nakamuru E, Fan WM, Kobayashi K and Li CW. 2007. Generation of Palaeocene adakitic andesites by magma mixing, Yanji area, NE China. Journal of Petrology, 48(4): 661-692
Guo SZ. 1986. On determination of convergence time between Siberian Plate and Sino-Korean Plate and its biostratigraphic evidence. Bulletin of Shenyang Institute of Geology and Mineral Resources Chinese Academy of Geological Sciences, 14: 127-136 (in Chinese with English abstract)
Hao BW and Jiang J. 2010. Chronology, geochemistry of the Hadamiao complex related to gold deposits in Xianghuang Banner, Inner Mongolia. Acta Petrologica et Mineralogica, 29(6): 750-762 (in Chinese with English abstract)
Hong DW. 1994. Recent developments in granite research. Earth Science Frontiers, 1(1-2): 79-86 (in Chinese with English abstract)
Hong DW, Huang HZ, Xiao YJ, Xu HM and Jin MY. 1994. The Permian alkaline granites in central Inner Mongolia and their geodynamic significance. Acta Geologica Sinica, 68(3): 219-230 (in Chinese with English abstract)
Hibbard MJ. 1991. Textural anatomy of twelve magma-mixed granitoid systems. In: Didier J and Barbarin B (eds.). Enclaves and Granite Petrology. Amsterdam: Elsevier, 431-444
Ionov DA, Grégoire M and Prikhodko VS. 1999. Feldspar-Ti-oxide metasomatism in off-cratonic continental and oceanic upper mantle. Earth Planet. Sci. Lett., 165(1): 37-44
Jian P, Liu DY, Kröner A, Windley BF, Shi YR, Zhang W, Zhang FQ, Miao LC, Zhang LQ and Tomurhuu D. 2010. Evolution of a Permian intraoceanic arc-trench system in the Solonker suture zone, Central Asian Orogenic Belt, China and Mongolia. Lithos, 118(1-2): 169-190
Jiang XJ, Liu YQ, Peng N, Shi YR, Xu H, Wei WT, Liu ZX, Zhao HP and Yao BG. 2011. Geochemistry and SHRIMP U-Pb dating of the Guangxingyuan composite pluton in Hexigten Qi, Inner Mongolia and its geological implication. Acta Geologica Sinica, 85(1): 114-128 (in Chinese with English abstract)
Koschek G. 1993. Origin and significance of the SEM cathodoluminescence from zircon. Journal of Microscopy, 171(3): 223-232
Li HK, Geng JZ, Hao S, Zhang YQ and Li HM. 2009. Research on the dating zircon U-Pb age by LA-MC-ICPMS. Acta Mineralogica Sinica, 29(Suppl.1): 600-601 (in Chinese)
Li JY. 2006. Permian geodynamic setting of Northeast China and adjacent regions: Closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific plate. Journal of Asian Earth Sciences, 26(3-4): 207-224
Li JY, Gao LM, Sun GH, Li YP and Wang YB. 2007. Shuangjingzi Middle Triassic syn-collisional crust-derived granite in the east Inner Mongolia and its constraint on the timing of collision between Siberian and Sino-Korean paleo-plates. Acta Petrologica Sinica, 23(3): 565-582 (in Chinese with English abstract)
Li SL and Ouyang ZY. 1998. Tectonic framework and evolution of Xing'anling-Mongolian Orogenic Belt (XMOB) and its adjacent region. Marine Geology and Quaternary Geology, 18(3): 45-54 (in Chinese with English abstract)
Liang MH, Zhou XA, Gong QS and Li HL. 2002. Magma hybrid process: Field evidences from Gansu Beishan Mountains. Acta Geologica Gansu, 11(1): 44-49 (in Chinese with English abstract)
Liu CF. 2010. Paleozoic-Early Mesozoic magmatic belts and tectonic significance in Siziwangqi area, Inner Mongolia. Ph. D. Dissertation. Beijing: China University of Geosciences, 111-117 (in Chinese with English summary)
Liu CF, Zhang HR, Yu YS, Zhou ZG, Liu WC and Zhang HF. 2010a. Dating and petrochemistry of the Beijige pluton in Siziwangqi, Inner Mongolia. Geoscience, 24(1): 112-150 (in Chinese with English abstract)
Liu CF, Yang SS, Wu JW and Zhang HF. 2010b. Dating and petrogenesis of Late Permian-Early Triassic peraluminous granites in the Siziwangqi area, Inner Mongolia. Acta Geologica Sinica, 84(7): 1002-1016 (in Chinese with English abstract)
Liu CF, Zhou ZG, Zhang HF, Liu WC and Zhang L. 2011. Petrochemical characteristics and timing of Wuertagaolemiao granitoids, Siziwangqi, Inner Mongolia. Journal of Mineralogy and Petrology, 31(4): 34-43 (in Chinese with English abstract)
Lu LZ and Xu WL. 2011. Petrology. Beijing: Geological Publish House, 80-83 (in Chinese)
Ludwig KR. 1991. Isoplot: A plotting and regression program for radiogenic-isotope date. US Geological Survey Open-File Report, 39: 91-445
Miao LC, Fan WM, Liu DY, Zhang FQ, Shi YR and Guo F. 2008. Geochronology and geochemistry of the Hegenshan ophiolitic complex: Implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China. Journal of Asian Earth Sciences, 32(5-6): 348-370
Pan SY, Chi XG, Sun W, Quan JY, Hu ZC and Da JW. 2012. Geochemical characteristics and tectonic significance of Late Carboniferous volcanic rocks in Benbatu Formation of Sonid Youqi, Inner Mongolia. Global Geology, 31(1): 40-50 (in Chinese with English abstract)
Qi CD, Ji CH, Han J, Guo AC, Di X and Sun YX. 2005. The genetic mechanism of the Late Permian-Early Triassic granite from Jilin to Hunchun. Jilin Geology, 24(2): 10-15 (in Chinese with English abstract)
Rudnick RL and Gao S. 2003. Composition of the continental crust. In: Rudnick RL (ed.). The Crust: Treatise on Geochemistry. Oxford: Elsevier Pergamon, 1-64
Shao JA. 1991. Crustal Evolution in the Middle Part of the Northern Margin of the Sino-Korean Plate. Beijing: Peking University Press, 136 (in Chinese)
Shi RD. 2005. Comment on the progress in and problems on ophiolite study. Geological Review, 51(6): 681-693 (in Chinese with English abstract)
Sun DY, Wu FY, Zhang YB and Gao S. 2004. The final closing time of the west Lamulun River-Changchun-Yanji plate suture zone: Evidence from the Dayushan granitic pluton, Jilin Province. Journal of Jilin University (Earth Science Edition), 34(2): 174-181 (in Chinese with English abstract)
Tang KD. 1989. On tectonic development of the fold belts in the north margin of Sino-Korean Platform. Geoscience, 3(2): 195-204 (in Chinese with English abstract)
Tang KD and Zhang YP. 1991. Tectonic evolution of the Inner Mongolia suture. In: Xiao XC and Tang YQ (eds.). Tectonic Evolution of the Southern Margin of the Paleo-Asian Composite Megsuture. Beijing: Scientific and Technical Publishing House, 30-54 (in Chinese)
Tian CL, Cao CZ and Yang FL. 1986. Geochemical features of ophiolite in the fold belt on the north side of the Sino-Korean Platform. Bulletin of the Chinese Academy of Geological Sciences, 19: 107-129 (in Chinese with English abstract)
Tong Y, Hong DW, Wang T, Shi XJ, Zhang JJ and Zeng T. 2010. Spatial and temporal distribution of granitoids in the middle segment of the Sino-Mongolian border and its tectonic and metallogenic implications. Acta Geoscientia Sinica, 31(3): 395-412 (in Chinese with English abstract)
Wang DZ and Xie L. 2008. Magma mingling: Evidence from enclaves. Geological Journal of China Universities, 14(1): 16-21 (in Chinese with English abstract)
Wang L, Guo XD, Jia LQ, Wang ZH and Zhang YY. 2012. Petrography and genesis of the dark microgranular enclaves in the Machangqing intrusive body, western Yunnan Province. Geology and Resources, 21(3): 332-337 (in Chinese with English abstract)
Wang Q. 1986. Recognition of the suture between the Sino-korean and Siberian paleoplates in the middle part of Inner Mongolia. Acta Geologica Sinica, (1): 31-43 (in Chinese with English abstract)
Xiao QH, Deng JF, Ma DQ and Hong DW. 2002. The Ways of Investigation on Granitoids. Beijing: Geological Publishing House, 53-63 (in Chinese)
Xiao WJ, Windly BF, Hao J and Zhai MG. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt. Tectonics, 22(6): 1069-1089
Xiao WJ, Shu LS, Gao J, Xiong XL, Wang JB, Guo ZJ, Li JY and Sun M. 2008. Continental dynamics of the Central Asian Orogenic Belt and its metallogeny. Xinjiang Geology, 26(1): 5-8 (in Chinese with English abstract)
Xing JL. 2010. The geochemic characteristics and geodynamic significance of the granite in Wenduermiao uplift zone in Inner Mogolia. Master Degree Thesis. Changchun: Jilin University, 23-26 (in Chinese with English summary)
Xu B and Chen B. 1997. The structure and evolution of a Middle Paleozoic orogenic belt between the North China and Siberian blocks, northern Inner Mongolia, China. Science in China (Series D), 27(3): 227-232 (in Chinese)
Xu LQ. 2005. The characteristics of magmatic rocks and discussion of geotectonics evolution from Caledonian through Hercynian to Indosinian stage in the Baiyun'ebo-Mandula region, Inner Mongolia. Ph. D. Dissertation. Beijing: China University of Geosciences, 8-86 (in Chinese with English summary)
Yang XM, Yang XY and Chen SX. 2000. Petrological Geochemistry. Hefei: Press of University of Science and Technology of China, 83-97 (in Chinese)
Yuan GB and Wang HC. 2006. Magmatic activity and it's tectonic implications during the Early Permian in the northwestward of Wuchuan, Inner Mongolia. Geological Survey and Research, 29(4): 303-310 (in Chinese with English abstract)
Zhang JJ, Wang T, Zhang ZC, Tong Y, Zhang L, Shi XJ, Guo L, Li S and Zeng T. 2012. Magma mixing origin of Yamatu granite in Nuoergong-Langshan area, western part of the northern margin of North China Craton: Petrological and geochemical evidences. Geological Review, 58(1): 53-66 (in Chinese with English abstract)
Zhang Q, Pan GQ, Li CD, Jin WJ and Jia XQ. 2007. Granitic magma mixing versus basaltic magma mixing: New viewpoints on granitic magma mixing process: Some crucial questions on granite study (1). Acta Petrologica Sinica, 23(5): 1141-1152 (in Chinese with English abstract)
Zhang SH, Zhao Y, Liu JM, Hu JM, Song B, Liu J and Wu H. 2010. Geochronology, geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block: A preliminary review. Acta Petrologica et Mineralogica, 29(6): 824-842 (in Chinese with English abstract)
Zhang YM, Zhang HF, Liu WC and Zhou ZG. 2009. Timing and petrogenesis of the Damiao granodiorite, Siziwangqi, Inner Mongolia. Acta Petrologica Sinica, 25(12): 3165-3181 (in Chinese with English abstract)
Zhao Y, Chen B, Zhang SH, Liu JM, Hu JM, Liu J and Pei JL. 2010. Pre-Yanshanian geological events in the northern margin of North China Craton and its adjacent areas. Geology China, 37(4): 900-915 (in Chinese with English abstract)
陈斌, 赵国春, Simon W. 2001. 内蒙古苏尼特左旗南两类花岗岩同位素年代学及其构造意义. 地质评论, 47(4): 361-367
陈斌. 2011. 内蒙古兴安地区二叠系沉积特征及构造背景. 硕士学位论文. 北京: 中国地质大学, 30-53
陈琦, 仇甘霖, 薛林福, 邹新民, 周和平, 杜玉申. 1993. 内蒙造山带南部古板块构造演化. 地质评论, 39(6): 477-483
郭胜哲. 1986. 中朝板块与西伯利亚板块拼合时限的确定及其生物地层学依据. 中国地质科学院沈阳地质矿产研究所所刊, 14: 127-136
郝百武, 蒋杰. 2010. 内蒙古镶黄旗哈达庙金矿杂岩体年代学、地球化学及其形成机制. 岩石矿物学杂志, 29(6): 750-762
洪大卫. 1994. 花岗岩研究的最新进展及发展趋势. 地学前缘, 1(1-2): 79-86
洪大卫, 黄怀曾, 肖宜君, 徐海明, 靳满元. 1994. 内蒙古中部二叠纪碱性花岗岩及其地球动力学意义. 地质学报, 68(3): 219-230
江小均, 柳永清, 彭楠, 石玉若, 许欢, 魏文通, 刘增校, 赵华平, 姚宝钢. 2011. 内蒙古克什克腾旗广兴源复式岩体SHRIMP U-Pb定年及地质意义讨论. 地质学报, 85(1): 114-128
李怀坤, 耿建珍, 郝爽, 张永清, 李惠民. 2009. 用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究. 矿物学报, 29(增刊): 600-601
李锦轶, 高立明, 孙桂华, 李亚萍, 王彦斌. 2007. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束. 岩石学报, 23(3): 565-582
李双林, 欧阳自远. 1998. 兴蒙造山带及邻区的构造格局与构造演化. 海洋地质与第四纪地质, 18(3): 45-54
梁明宏, 周兴安, 龚全胜, 李海林. 2002. 岩浆混合作用——来自甘肃北山的野外证据. 甘肃地质学报, 11(1): 44-49
柳长峰. 2010. 内蒙古四子王旗地区古生代-早中生代岩浆岩带及其构造意义. 博士学位论文. 北京: 中国地质大学, 111-117
柳长峰, 张浩然, 於炀森, 周志广, 刘文灿, 张华锋. 2010a. 内蒙古中部四子王旗地区北极各岩体锆石定年及其岩石化学特征. 现代地质, 24(1): 112-150
柳长峰, 杨帅师, 武将伟, 张华锋. 2010b. 内蒙古中部四子王旗地区晚二叠-早三叠世过铝花岗岩定年及成因.地质学报, 84(7): 1002-1016
柳长峰, 周志广, 张华锋, 刘文灿, 张磊. 2011. 内蒙古四子王旗乌尔塔高勒庙岩体的侵位时代及岩石地球化学特征. 矿物岩石, 31(4): 34-43
卢良兆, 许文良. 2011. 岩石学. 北京: 地质出版社, 80-83
内蒙古自治区地质矿产局. 1991. 内蒙古自治区区域地质志. 北京: 地质出版社, 351-458
潘世语, 迟效国, 孙巍, 权京玉, 胡兆初, 达佳伟. 2012. 内蒙古苏尼特右旗晚石炭世本巴图组火山岩地球化学特征及构造意义. 世界地质, 31(1): 40-50
齐成栋, 纪春华, 韩江, 郭安臣, 邸新, 孙元喜. 2005. 吉林至珲春地区晚二叠世-早三叠世花岗岩成因机制. 吉林地质, 24(2): 10-15
邵济安. 1991. 中朝板块北缘中段地壳演化. 北京: 北京大学出版社, 136
史仁灯. 2005. 蛇绿岩研究进展、存在问题及思考. 地质评论, 51(6): 681-693
孙德有, 吴福元, 张艳斌, 高山. 2004. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据. 吉林大学学报(地球科学版), 34(2): 174-181
唐克东. 1989. 中朝陆台北侧褶皱带构造发展的几个问题. 现代地质, 3(2): 195-204
唐克东, 张允平. 1991. 内蒙古缝合带的构造演化. 见: 肖序常, 汤耀庆编. 古中亚复合巨型缝合带南缘构造演化. 北京: 北京科学技术出版社, 30-54
田昌烈, 曹从周, 杨芳林. 1986. 中朝陆台北侧褶皱带(中段)蛇绿岩的地球化学特征. 中国地质科学院院报, 19: 107-129
童英, 洪大卫, 王涛, 史兴俊, 张建军, 曾涛. 2010. 中蒙边境中段花岗岩时空分布特征及构造和找矿意义. 地球学报, 31(3): 395-412
王德滋, 谢磊. 2008. 岩浆混合作用: 来自岩石包体的证据. 高校地质学报, 14(1): 16-21
王梁, 郭晓东, 贾丽琼, 王治华, 张延彦. 2012. 滇西马厂箐岩体暗色微粒包体岩相学特征及成因机制探讨. 地质与资源, 21(3): 332-337
王荃. 1986. 内蒙古中部中朝与西伯利亚古板块间缝合线的确定. 地质学报, (1): 31-43
刑济麟. 2010. 内蒙古温都尔庙隆起带花岗岩的地球化学特征及地球动力学意义. 硕士学位论文. 长春: 吉林大学, 23-26
肖庆辉, 邓晋福, 马大铨, 洪大卫. 2002. 花岗岩研究思维与方法. 北京: 地质出版社, 53-63
肖文交, 舒良树, 高俊, 熊小林, 王京彬, 郭召杰, 李锦轶, 孙敏. 2008. 中亚造山带大陆动力学过程与成矿作用. 新疆地质, 26(1): 5-8
徐备, 陈斌. 1997. 内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构及演化. 中国科学(D辑), 27(3): 227-232
许立权. 2005. 内蒙古白云鄂博-满都拉地区加里东期-华力西期-印支期岩浆岩特征与大地构造演化探讨. 博士学位论文. 北京: 中国地质大学, 8-86
杨学明,杨晓勇,陈双喜. 2000. 岩石地球化学. 合肥:中国科学技术大学出版社,83-97
袁桂邦, 王惠初. 2006. 内蒙古武川西北部早二叠世岩浆活动及其构造意义. 地质调查与研究, 29(4): 303-310
张建军, 王涛, 张招崇, 童英, 张磊, 史兴俊, 郭磊, 李舢, 曾涛. 2012. 华北地块北缘西段巴音诺尔公-狼山地区牙马图岩体的岩浆混合成因——岩相学和元素地球化学证据. 地质评论, 58(1): 53-66
张旗, 潘国强, 李承东, 金惟俊, 贾秀勤. 2007. 花岗岩混合问题: 与玄武岩对比的启示——关于花岗岩研究的思考之一. 岩石学报, 23(5): 1141-1152
张拴宏, 赵越, 刘建民, 胡健民, 宋彪, 刘健, 吴海. 2010. 华北地块北缘晚古生代-早中生代岩浆活动期次、特征及构造背景. 岩石矿物学杂志, 29(6): 824-842
章永梅, 张华峰, 刘文灿, 周志广. 2009. 内蒙古中部四子王旗大庙岩体时代及成因. 岩石学报, 25(12): 3165-3181
赵越, 陈斌, 张拴宏, 刘建民, 胡健民, 刘健, 裴军令. 2010. 华北克拉通北缘及邻区前燕山期主要地质事件. 中国地质, 37(4): 900-915
-
下载:
图(11)
计量
- 文章访问数: 8198
- PDF下载数: 9239
- 施引文献: 0