内蒙古哈珠地区晚古生代花岗岩类成因及其构造意义

李敏; 辛后田; 任邦方; 任云伟; 张阔; 段霄龙; 牛文超; 段连峰

doi:10.3799/dqkx.2018.238

内蒙古哈珠地区晚古生代花岗岩类成因及其构造意义

doi: 10.3799/dqkx.2018.238

中国地质调查局天津地质调查中心, 天津 300170

基金项目:

中国地质调查项目 121201006000172601

中国地质调查项目 12120114064601

详细信息

作者简介:
李敏(1986-), 男, 硕士, 工程师, 从事岩石地球化学及岩石大地构造研究

通讯作者:
辛后田

中图分类号: P597.1;P597.3;P581
计量
- 文章访问数: 4326
- HTML全文浏览量: 1936
- PDF下载量: 56
- 被引次数: 0
出版历程
- 收稿日期: 2018-05-23
- 刊出日期: 2019-01-15

Petrogenesis and Tectonic Significance of the Late Palaeozoic Granitoids in Hazhu Area, Inner Mongolia

Tianjin Center of China Geological Survey, Tianjin 300170, China

摘要

摘要: 系统研究了北山造山带北部哈珠地区花岗岩类的年代学、地球化学和锆石Hf同位素特征，并据此探讨了岩体的成因及其对晚古生代构造岩浆演化的制约.锆石LA-MC-ICP-MS U-Pb测年结果显示花岗闪长岩（298.6±1.7 Ma）和二长花岗岩（306.0±1.3 Ma）、碱长花岗岩（289.3±1.3 Ma）分别为晚石炭世晚期、早二叠世岩浆活动的产物.花岗闪长岩、二长花岗岩化学组成上表现为中钾钙碱性、Mg^#值较低，分异程度中等（D.I.=79.2~86.9），属准铝质、镁质岩石；碱长花岗岩则表现高硅、富碱、准铝，贫钙、镁、铁，分异程度高（D.I.=94.4~96.5）.三者均富集Rb、Ba、Th、U、La、Ce等，不同程度亏损高场强元素Nb、Ta、P、Ti、Sr、Eu.花岗闪长岩、碱长花岗岩样品的ε_Hf（t）均为正值，T_DM^C主要集中于450~800 Ma.本文和最近获得的数据表明，俯冲板块脱水交代新生下地壳，并诱发新生地壳的部分熔融，形成晚石炭世花岗岩类；早二叠世由于后碰撞伸展作用导致岩石圈拉伸减薄，促使新生地壳部分熔融，再经高程度的分异演化形成本文碱长花岗岩.
- 北山拼贴造山带 /
- 晚古生代 /
- 俯冲 /
- 伸展 /
- 岩石成因 /
- 锆石Hf同位素 /
- 地球化学
Abstract: The chronology, geochemistry and zircon Hf isotopes of granitoids in Hazhu area of the northern Beishan belt are systematically studied, and the genesis of the plutons and their restrictions on the tectonic magma evolution in Late Paleozoic are discussed. The zircon LA-MC-ICP-MS U-Pb dating results show that the granodiorites and monzogranites formed during the late Late Carboniferous in 298.6±1.7 Ma and 306.0±1.3 Ma, and the alkali-feldspar granites formed in Early Permian 289.3±1.3 Ma. Chemically, the granodiorites and monzogranites are characterized by middle potassium calc alkaline, low Mg^# value and middle degree of differentiation (D.I.=79.2-86.9), metaluminum and enriched-magnesium. And alkali-feldspar granites show high contents of silica and alkalis, metaluminum, low abundances of calcium, magnesium and iron, and high degree of differentiation (D.I.=94.4-96.5). All of them are enriched in Rb, Ba, Th, U, La, Ce, and so on, and depleted in high field strength elements, Nb, Ta, P, Ti, Sr, and so on. The ε_Hf(t) values in this paper are all positive. The Hf isotopic crustal model age T_DM^C is mainly concentrated from 800 Ma to 450 Ma. According to the data obtained in this paper and other regional geological data acquired recently, the subduction plate dehydrated, after then, the subduction fluid entered into the juvenile crust, and induced partial melting of the juvenile crust, forming the granitoids in Late Carboniferous. The extension resulted in the thinning and stretching of the lithosphere due to the post collisional extension in Early Permian, which caused the partial melting of the new crust, and then the alkali-spar granites were formed by a high degree of differentiation and evolution.
- Beishan orogenic collage /
- Late Palaeozoic /
- subduction /
- extension /
- petrogenesis /
- zircon Hf-isotope /
- geochemistry

HTML全文

图 1 额济纳旗哈珠地区地质简图

Fig. 1. Geological sketch of Hazhu area in Ejina banner

下载: 全尺寸图片幻灯片

图 2 哈珠地区花岗岩类野外与显微照片

a.花岗闪长岩；b.花岗闪长岩偏光显微照片；c.二长花岗岩；d.二长花岗岩偏光显微照片；e.碱长花岗岩；f.碱长花岗岩偏光显微照片；Q.石英；Pl.斜长石；Af.碱性长石；Bi.黑云母

Fig. 2. Field photos and photomicrographs of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 3 哈珠地区花岗岩类部分锆石阴极发光图像及年龄(Ma)

Fig. 3. CL image and dating (Ma) of zircons for the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 4 哈珠地区花岗岩类的LA-MC-ICP-MS锆石U-Pb年龄谐和图

Fig. 4. Zircon LA-MC-ICP-MS U-Pb concordia diagrams of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 5 哈珠地区花岗岩类的主量元素图解

a.ANOR-Q'图解，Q'=Q×100/(Q+Or+Ab+An), ANOR=An×100/(Or+An)；b.SiO₂-FeO^T/MgO图；c.A/CNK-A/NK图解；d.SiO₂-K₂O图解；e.SiO₂-FeO^T/(FeO^T+MgO)图解，底图据Frost et al.(2001)；f.SiO₂-(Na₂O+ K₂O-CaO)图解，底图据Frost et al.(2001).IAG.岛弧花岗岩类；CAG.大陆弧花岗岩类；CCG.大陆碰撞花岗岩类；POG.后造山花岗岩类；RRG.与裂谷有关的花岗岩类

Fig. 5. Major element diagrams of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 6 哈珠地区花岗岩类稀土元素球粒陨石标准化配分模式图(a)和原始地幔标准化微量元素蛛网图(b)

球粒陨石标准化值、原始地幔标准化值据Sun and McDonough(1989)

Fig. 6. Chondrite-normalized rare earth element patterns (a) and primitive mantle-normoalized trace elemets spider diagram (b) of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 7 哈珠地区花岗岩类Hf同位素与U-Pb年龄图解

Fig. 7. ¹⁷⁶Hf/¹⁷⁷Hf vs. ²⁰⁶Pb/²³⁸U age diagram (a)、ε_Hf(t) vs. ²⁰⁶Pb/²³⁸U age diagram (b) and ε_Hf(t) vs. age diagram (c) of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 8 哈珠地区花岗岩类ε_Hf(t)值和地壳模式年龄(T_DM^C)柱状图

Fig. 8. ε_Hf(t) value and crustal model age (T_DM^C) histogram of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 9 哈珠地区花岗岩类成因类型判别图解

Ⅰ、S和A分别代表Ⅰ型、S型和A型花岗岩，OGT代表未分异的Ⅰ、S型花岗岩区，FG代表分异的Ⅰ型花岗岩区

Fig. 9. Various chemical discrimination diagrams for the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 10 哈珠地区花岗岩类(La/Yb)_N-La (a), Sr-δEu (b), Rb-Sr (c), Ba-Sr(d)关系图及分离结晶趋势

图a中副矿物结晶分离趋势线据Wu(2003)，底图据邱检生等(2008)；图d底图据Li et al.(2007).Zr.锆石；Ap.磷灰石；Mon.独居石；Allan.褐帘石；PlAn15.斜长石(An=15)；PlAn50.斜长石(An=50)；Pl.斜长石；Kf.钾长石；Bi.黑云母；Ms.白云母；Amp.角闪石；Hb.角闪石；Grt.石榴石

Fig. 10. (La/Yb)_N-La (a), Sr-δEu (b), Rb-Sr (c), Ba-Sr (d) diagrams showing the fractional crystallization trends for the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 11 哈珠地区花岗岩类微量元素构造环境判别图

Fig. 11. Trace element diagrams for the tectonic discrimination of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 12 哈珠地区花岗岩类R₁-R₂判别图(a)和主量元素构造环境判别图(b, c)

R₁=4Si-11(Na+K)-2(Fe+Ti)，R₂=6Ca+2Mg+Al；IAG.岛弧花岗岩类；CAG.大陆弧花岗岩类；CCG.大陆碰撞花岗岩类；POG.后碰撞花岗岩类；RRG.与裂谷有关的花岗岩类；CEUG.与大陆造陆抬升有关花岗岩类

Fig. 12. R₁-R₂ (a) and major element diagrams (b, c) for the tectonic discrimination of the granitoids in Hazhu area

下载: 全尺寸图片幻灯片

图 13 北山造山带北部石炭纪-二叠纪三阶段构造岩浆演化示意

Fig. 13. Schematic diagram of tectonic evolution for 3 stages from Carboniferous to Permian in northern part of Beishan orogenic collage

下载: 全尺寸图片幻灯片

参考文献(78)

Ao, S.J., Xiao, W.J., Han, C.M., et al., 2010.Geochronology and Geochemistry of Early Permian Mafic-Ultramafic Complexes in the Beishan Area, Xinjiang, NW China:Implications for Late Paleozoic Tectonic Evolution of the Southern Altaids.Gondwana Research, 18(2-3):466-478. https://doi.org/10.1016/j.gr.2010.01.004
Ao, S.J., Xiao, W.J., Windley, B.F., et al., 2016.Paleozoic Accretionary Orogenesis in the Eastern Beishan Orogen:Constraints from Zircon U-Pb and ⁴⁰Ar/³⁹Ar Geochronology.Gondwana Research, 30:224-235. https://doi.org/10.1016/j.gr.2015.03.004
Bouvier, A., Vervoort, J.D., Patchett, P.J., 2008.The Lu-Hf and Sm-Nd Isotopic Composition of CHUR:Constraints from Unequilibrated Chondrites and Implications for the Bulk Composition of Terrestrial Planets.Earth and Planetary Science Letters, 273(1-2):48-57. https://doi.org/10.1016/j.epsl.2008.06.010
Cai, K.D., Sun, M., Yuan, C., et al., 2012.Carboniferous Mantle-Derived Felsic Intrusion in the Chinese Altai, NW China:Implications for Geodynamic Change of the Accretionary Orogenic Belt.Gondwana Research, 22(2):681-698. https://doi.org/10.1016/j.gr.2011.11.008
Chappell, B.W., White, A.J.R., 2001.Two Contrasting Granite Types:25 Years Later.Australian Journal of Earth Sciences, 48(4):489-499. https://doi.org/10.1046/j.1440-0952.2001.00882.x
Cleven, N.R., Lin, S.F., Xiao, W.J., 2015.The Hongliuhe Fold-and-Thrust Belt:Evidence of Terminal Collision and Suture-Reactivation after the Early Permian in the Beishan Orogenic Collage, Northwest China.Gondwana Research, 27(2):796-810. https://doi.org/10.1016/j.gr.2013.12.004
Frost, B.R., Barnes, C.G., Collins, W.J., et al., 2001.A Geochemical Classification for Granitic Rocks.Journal of Petrology, 42(11):2033-2048. https://doi.org/10.1093/petrology/42.11.2033
Geng, J.Z., Li, H.K., Zhang, J., et al., 2011.Zircon Hf Isotope Analysis by Means of LA-MC-ICP-MS.Geological Bulletin of China, 30(10):1508-1513 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201110005.htm
Griffin, W.L., Pearson, N.J., Belousova, E., et al., 2000.The Hf Isotope Composition of Cratonic Mantle:LAM-MC-ICPMS Analysis of Zircon Megacrysts in Kimberlites.Geochimica et Cosmochimica Acta, 64(1):133-147. https://doi.org/10.1016/s0016-7037(99)00343-9
Griffin, W.L., Wang, X., Jackson, S.E., et al., 2002.Zircon Chemistry and Magma Mixing, SE China:In-Situ Analysis of Hf Isotopes, Tonglu and Pingtan Igneous Complexes.Lithos, 61(3-4):237-269. https://doi.org/10.1016/s0024-4937(02)00082-8
He, F., Xu, L.Q., Su, H.W., et al., 2004.Characteristics and Tectonic Setting of Middle-Permian A-Type Granites in Tianshuijing Area, West of Inner Mongolia.Northwestern Geology, 37(3):7-14 (in Chinese with English abstract).
He, S.P., Zhou, H.W., Ren, B.C., et al., 2005.Crustal Evolution of Palaeozoic in Beishan Area, Gansu and Inner Mongolia, China.Northwestern Geology, 38(3):6-15 (in Chinese with English abstract).
He, Z.Y., Sun, L.X., Mao, L.J., et al., 2015.Zircon U-Pb and Hf Isotopic Study of Gneiss and Granodiorite from the Southern Beishan Orogenic Collage:Mesoproterozoic Magmatism and Crustal Growth.Chinese Science Bulletin, 60(4):389-399 (in Chinese). doi: 10.1360/N972014-00898
Hong, D.W., Guo, W.Q., Li, G.J., et al., 1987.Petrology of the Miarolitic Granite Belt in the Southeast Coast of Fujian Province and Their Petrogenesis.Science and Technology Press of Beijing, Beijing (in Chinese).
Jahn, B.M., Windley, B., Natal'in, B., et al., 2004.Phanerozoic Continental Growth in Central Asia.Journal of Asian Earth Sciences, 23(5):599-603. https://doi.org/10.1016/s1367-9120(03)00124-x
Jiang, S.H., Nie, F.J., 2006.Nd-Isotope Constrains on Origin of Granitoids in Beishan Mountain Area.Acta Geologica Sinica, 80(6):826-842 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200606005.htm
Ju, Y.J., Zhang, X.L., Lai, S.C., et al., 2017.Permian-Triassic Highly-Fractionated Ⅰ-Type Granites from the Southwestern Qaidam Basin (NW China):Implications for the Evolution of the Paleo-Tethys in the Eastern Kunlun Orogenic Belt.Journal of Earth Science, 28(1):51-62. https://doi.org/10.1007/s12583-017-0745-5
Kröner, A., Kovach, V., Belousova, E., et al., 2014.Reassessment of Continental Growth during the Accretionary History of the Central Asian Orogenic Belt.Gondwana Research, 25(1):103-125. https://doi.org/10.1016/j.gr.2012.12.023
Li, X.H., Li, Z.X., Li, W.X., et al., 2007.U-Pb Zircon, Geochemical and Sr-Nd-Hf Isotopic Constraints on Age and Origin of Jurassic Ⅰ-and A-Type Granites from Central Guangdong, SE China:A Major Igneous Event in Response to Foundering of a Subducted Flat-Slab?Lithos, 96(1-2):186-204. https://doi.org/10.1016/j.lithos.2006.09.018
Liu, M., Zhao, H.T., Zhang, D., et al., 2017.Chronology, Geochemistry and Tectonic Implications of Late Paleozoic Instrusions from South of Xiwuqi, Inner Mongolia.Earth Science, 42(4):527-548 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.042
Liu, M.Q., 2007.Geochemical Characteristics and Geological Significance of Adakitic Granitoids in Hongshishan Area of the Beishan Orogenic Belt, Gansu Province.Acta Petrologica et Mineralogica, 26(3):232-238 (in Chinese with English abstract).
Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010.Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths.Journal of Petrology, 51(1/2):537-571. https://doi.org/10.1093/petrology/egp082
Ludwig, K.R., 2003.ISOPLOT/EX 3.0: A Geochronological Toolkit for Microsoft Excel, 4.Berkeley Geochronology Centre, Berkeley.
Mao, Q.G., Xiao, W.J., Fang, T.H., et al., 2012.Late Ordovician to Early Devonian Adakites and Nb-Enriched Basalts in the Liuyuan Area, Beishan, NW China:Implications for Early Paleozoic Slab-Melting and Crustal Growth in the Southern Altaids.Gondwana Research, 22(2):534-553. https://doi.org/10.1016/j.gr.2011.06.006
Pirajno, F., 2010.Intracontinental Strike-Slip Faults, Associated Magmatism, Mineral Systems and Mantle Dynamics:Examples from NW China and Altay-Sayan (Siberia).Journal of Geodynamics, 50(3-4):325-346. https://doi.org/10.1016/j.jog.2010.01.018
Qi, R.R., Huang, Z.B., Jin, X., 2006.Geochemical Characteristics and Tectonic Implications of the Dashishan A-Type Granitic Intrusion in Beishan Area, Gansu Province.Acta Petrologica et Mineralogica, 25(2):90-96 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSKW200602002.htm
Qian, X.Y., Zhang, Z.C., Chen, Y., et al., 2017.Geochronology and Geochemistry of the Early Paleozoic Igneous Rocks in Zhurihe Area, Inner Mongolia and Its Tectonic Significance.Earth Science, 42(9):1472-1494 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.545
Qiu, J.S., Xiao, E., Hu, J., 2008.Petrogenesis of Highly Fractionated Ⅰ-Type Granites in the Coastal Area of Northeastern Fujian Province:Constraints from Zircon U-Pb Geochronology, Geochemistry and Nd-Hf Isotopes.Acta Petrologica Sinca, 24(11):2468-2484 (in Chinese with English abstract).
Söderlund, U., Patchett, P.J., Vervoort, J.D., et al., 2004.The ¹⁷⁶Lu Decay Constant Determined by Lu-Hf and U-Pb Isotope Systematics of Precambrian Mafic Intrusions.Earth and Planetary Science Letters, 219(3-4):311-324. https://doi.org/10.1016/s0012-821x(04)00012-3
Song, D.F., Xiao, W.J., Han, C.M., et al., 2013.Progressive Accretionary Tectonics of the Beishan Orogenic Collage, Southern Altaids:Insights from Zircon U-Pb and Hf Isotopic Data of High-Grade Complexes.Precambrian Research, 227:368-388. https://doi.org/10.1016/j.precamres.2012.06.011
Song, X.Y., Xie, W., Deng, Y.F., et al., 2011.Slab Break-Off and the Formation of Permian Mafic-Ultramafic Intrusions in Southern Margin of Central Asian Orogenic Belt, Xinjiang, NW China.Lithos, 127(1-2):128-143. https://doi.org/10.1016/j.lithos.2011.08.011
Sun, M., Yuan, C., Xiao, W.J., et al., 2008.Zircon U-Pb and Hf Isotopic Study of Gneissic Rocks from the Chinese Altai:Progressive Accretionary History in the Early to Middle Palaeozoic.Chemical Geology, 247(3-4):352-383. https://doi.org/10.1016/j.chemgeo.2007.10.026
Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
Tian, Z.H., Xiao, W.J., Windley, B.F., et al., 2014.Structure, Age, and Tectonic Development of the Huoshishan-Niujuanzi Ophiolitic Mélange, Beishan, Southernmost Altaids.Gondwana Research, 25(2):820-841. https://doi.org/10.1016/j.gr.2013.05.006
Tong, Y., Wang, T., Hong, D.W., et al., 2010.Spatial and Temporal Distribution of the Carboniferous-Permian Granitoids in Northern Xinjiang and Its Adjacent Areas, and Its Tectonic Significance.Acta Petrologica et Mineralogica, 29(6):619-641 (in Chinese with English abstract).
Whalen, J.B., Currie, K.L., Chappell, B.W., 1987.A-Type Granites:Geochemical Characteristics, Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology, 95(4):407-419. https://doi.org/10.1007/bf00402202
Wang, G.Q., Li, X.M., Xu, X.Y., et al., 2014.Zircon U-Pb Chronological Study of the Hongshishan Ophiolite in the Beishan Area and Their Tectonic Significance.Acta Petrologica Sinica, 30(6):1685-1694 (in Chinese with English abstract).
Wang, S.D., Zhang, K.X., Song, B.W., et al., 2018.Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China:Provenance and Tectonic Implications.Journal of Earth Science, 29(1):103-113. https://doi.org/10.1007/s12583-018-0824-2
Wang, X.H., Yang, J.G., Xie, X., et al., 2013.The Genetic Type and Tectonic Significance of Hongshishan Basic-Ultrabasic Rocks in Beishan, Gansu Province.Northwest Geology, 46(1):40-55 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XBDI201301009.htm
Wilhem, C., Windley, B.F., Stampfli, G.M., 2012.The Altaids of Central Asia:A Tectonic and Evolutionary Innovative Review.Earth-Science Reviews, 113(3-4):303-341. https://doi.org/10.1016/j.earscirev.2012.04.001
Windley, B.F., Alexeiev, D., Xiao, W., et al., 2007.Tectonic Models for Accretion of the Central Asian Orogenic Belt.Journal of the Geological Society, 164(1):31-47. https://doi.org/10.1144/0016-76492006-022
Wu, F.Y., 2003.Highly Fractionated Ⅰ-Type Granites in NE China (Ⅰ):Geochronology and Petrogenesis.Lithos, 66(3-4):241-273. https://doi.org/10.1016/s0024-4937(02)00222-0
Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007.Lu-Hf Isotopic Systematics and Their Applications in Petrology.Acta Petrologica Sinica, 23(2):185-220 (in Chinese with English abstract).
Wu, F.Y., Liu, X.C., Ji, W.Q., et al., 2017.Highly Fractionated Granites:Recognition and Research.Science in China (Series D), 47(7):745-765 (in Chinese). http://d.old.wanfangdata.com.cn/Periodical/dizhixb201708010
Wu, Y.B., Zheng, Y.F., 2004.Genetic Mineralogy of Zircons and Its Constraints to the Age of U-Pb Geochronology.Chinese Science Bulletin, 49(16):1589-1604 (in Chinese).
Xiao, W.J., Mao, Q.G., Windley, B.F., et al., 2010.Paleozoic Multiple Accretionary and Collisional Processes of the Beishan Orogenic Collage.American Journal of Science, 310(10):1553-1594. https://doi.org/10.2475/10.2010.12
Xiao, W.J., Windley, B.F., Badarch, G., et al., 2004.Palaeozoic Accretionary and Convergent Tectonics of the Southern Altaids:Implications for the Growth of Central Asia.Journal of the Geological Society, 161(3):339-342. https://doi.org/10.1144/0016-764903-165
Xiao, W.J., Windley, B.F., Huang, B.C., et al., 2009.End-Permian to Mid-Triassic Termination of the Accretionary Processes of the Southern Altaids:Implications for the Geodynamic Evolution, Phanerozoic Continental Growth, and Metallogeny of Central Asia.International Journal of Earth Sciences, 98(6):1219-1220. https://doi.org/10.1007/s00531-009-0419-3
Xie, C.L., Yang, J.G., Wang, L.S., et al., 2009.Disscussion on the Location of Paleozoic Island Arc Zone on the South Margin of Paleo-Asian Ocean in the Beishan Area of Gansu Province.Acta Geologica Sinica, 83(11):1584-1600 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE200911006.htm
Xu, X.Y., He, S.P., Wang, H.L., et al., 2008.An Outline of Geology in Northwest China:Qinling Mountains, Qilian and Tianshan Area.Science Press, Beijing (in Chinese).
Yang, H.Q., Zhao, G.B., Li, Y., et al., 2012.The Relationship between Paleozoic Tectonic Setting and Mineralization in Xinjiang-Gansu-Inner Mongolia Juncture Area.Geological Bulletin of China, 31(2):413-421 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD2012Z1026.htm
Yuan, H.L., Gao, S., Liu, X.M., et al., 2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 28(3):353-370. https://doi.org/10.1111/j.1751-908x.2004.tb00755.x
Yuan, Y., Zong, K.Q., He, Z.Y., et al., 2015.Geochemical and Geochronological Evidence for a Former Early Neoproterozoic Microcontinent in the South Beishan Orogenic Belt, Southernmost Central Asian Orogenic Belt.Precambrian Research, 266:409-424. https://doi.org/10.1016/j.precamres.2015.05.034
Zheng, R.G., Wu, T.R., Zhang, W., et al., 2014.Geochronology and Geochemistry of Late Paleozoic Magmatic Rocks in the Yinwaxia Area, Beishan:Implications for Rift Magmatism in the Southern Central Asian Orogenic Belt.Journal of Asian Earth Sciences, 91:39-55. https://doi.org/10.1016/j.jseaes.2014.04.022
Zhu, D.C., Mo, X.X., Wang, L.Q., et al., 2009.Petrogenesis of Highly Fractionated Ⅰ-Type Granites in the Zayu Area of Eastern Gangdese, Tibet:Constraints from Zircon U-Pb Geochronology, Geochemistry and Sr-Nd-Hf Isotopes.Science in China (Series D), 39(7):833-848 (in Chinese). doi: 10.1007/s11430-009-0132-x
Zong, K.Q., Klemd, R., Yuan, Y., et al., 2017.The Assembly of Rodinia:The Correlation of Early Neoproterozoic (ca.900 Ma) High-Grade Metamorphism and Continental Arc Formation in the Southern Beishan Orogen, Southern Central Asian Orogenic Belt (CAOB).Precambrian Research, 290:32-48. https://doi.org/10.1016/j.precamres.2016.12.010
Zuo, G.C., Zhang, S.L., He, G.Q., et al., 1991.Plate Tectonic Characteristics during the Early Paleozoic in Beishan near the Sino-Mongolian Border Region, China.Tectonophysics, 188(3-4):385-392. https://doi.org/10.1016/0040-1951(91)90466-6
耿建珍, 李怀坤, 张健, 等, 2011.锆石Hf同位素组成的LA-MC-ICP-MS测定.地质通报, 30(10):1508-1513. doi: 10.3969/j.issn.1671-2552.2011.10.004
贺锋, 许立权, 苏宏伟, 等, 2004.内蒙古西部甜水井地区中二叠世A型花岗岩.西北地质, 37(3):7-14. doi: 10.3969/j.issn.1009-6248.2004.03.002
何世平, 周会武, 任秉琛, 等, 2005.甘肃内蒙古北山地区古生代地壳演化.西北地质, 38(3):6-15. doi: 10.3969/j.issn.1009-6248.2005.03.002
贺振宇, 孙立新, 毛玲娟, 等, 2015.北山造山带南部片麻岩和花岗闪长岩的锆石U-Pb定年和Hf同位素:中元古代的岩浆作用于地壳生长.科学通报, 60(4):389-399. http://www.cnki.com.cn/Article/CJFDTotal-KXTB201504008.htm
洪大卫, 郭文歧, 李戈晶, 等, 1987.福建沿海晶洞花岗岩带的岩石学和成因演化.北京:北京科学技术出版社.
江思宏, 聂凤军, 2006.北山地区花岗岩类成因的Nd同位素制约.地质学报, 80(6):826-842. doi: 10.3321/j.issn:0001-5717.2006.06.005
刘敏, 赵洪涛, 张达, 等, 2017.内蒙古西乌旗南部晚古生代侵入岩年代学、地球化学特征及地质意义.地球科学, 42(4):527-548. http://earth-science.net/WebPage/Article.aspx?id=3560
刘明强, 2007.甘肃北山造山带红石山地区埃达克质花岗岩类的发现及其地质意义.岩石矿物学杂志, 26(3):232-238. doi: 10.3969/j.issn.1000-6524.2007.03.004
齐瑞荣, 黄增保, 金霞, 2006.甘肃北山大石山A型花岗岩体的地球化学特征及构造意义.岩石矿物学杂志, 25(2):90-96. doi: 10.3969/j.issn.1000-6524.2006.02.002
钱筱嫣, 张志诚, 陈彦, 等, 2017.内蒙古朱日和地区早古生代岩浆岩年代学、地球化学特征及其构造意义.地球科学, 42(9):1472-1494.doi: 10.3799/dqkx.2017.545
邱检生, 肖娥, 胡建, 2008.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报, 24(11):2468-2484. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200811002
童英, 王涛, 洪大卫, 等, 2010.北疆及邻区石炭-二叠纪花岗岩时空分布特征及其构造意义.岩石矿物学杂志, 29(6):619-641. doi: 10.3969/j.issn.1000-6524.2010.06.003
王国强, 李向民, 徐学义, 等, 2014.甘肃北山红石山蛇绿岩锆石U-Pb年代学研究及构造意义.岩石学报, 30(6):1685-1694. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201406011
王小红, 杨建国, 谢燮, 等, 2013.甘肃北山红石山基性-超基性岩体的成因类型及构造意义.西北地质, 46(1):40-55. doi: 10.3969/j.issn.1009-6248.2013.01.005
吴福元, 李献华, 郑永飞, 等, 2007.Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2):185-220. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200702001
吴福元, 刘小驰, 纪伟强, 等, 2017.高分异花岗岩的识别与研究.中国科学(D辑), 47(7):745-765. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201707001.htm
吴元保, 郑永飞, 2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报, 49(16):1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002
谢春林, 杨建国, 王立社, 等, 2009.甘肃北山地区古亚洲南缘古生代岛弧带位置的讨论.地质学报, 83(11):1584-1600. doi: 10.3321/j.issn:0001-5717.2009.11.004
徐学义, 何世平, 王洪亮, 等, 2008.中国西北部地质概论——秦岭、祁连、天山地区.北京:科学出版社.
杨合群, 赵国斌, 李英, 等, 2012.新疆-甘肃-内蒙古衔接区古生代构造背景与成矿的关系.地质通报, 31(2):413-421. doi: 10.3969/j.issn.1671-2552.2012.02.027
朱弟成, 莫宣学, 王立全, 等, 2009.西藏冈底斯东部察隅高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Sr-Nd-Hf同位素约束.中国科学(D辑), 39(7):833-848. http://www.cnki.com.cn/Article/CJFDTotal-JDXK200907001.htm