甘肃阿克塞余石山铌钽矿区二长花岗岩成因和形成环境:来自年代学及地球化学的证据

廖风云; 陈威; 曹晓峰; 陈广琛; 何昆洋; 杨文; 吴义布; 李通国

doi:10.3799/dqkx.2019.260

甘肃阿克塞余石山铌钽矿区二长花岗岩成因和形成环境:来自年代学及地球化学的证据

doi: 10.3799/dqkx.2019.260

廖风云^1,,
陈威¹,
曹晓峰^{1, 2, ,},
陈广琛¹,
何昆洋¹,
杨文¹,
吴义布³,
李通国³

1.
中国地质大学资源学院, 湖北武汉 430074
2.
中国地质大学固体矿产勘查国家级实验教学示范中心, 湖北武汉 430074
3.
甘肃省地质调查院, 甘肃兰州 730000

基金项目:

中祁连西段稀有金属矿产综合勘查示范项目 2017YFC0602404

详细信息

作者简介:
廖风云(1995-), 男, 硕士研究生, 矿产普查与勘探专业.E-mail:2268437453@qq.com

通讯作者:
曹晓峰, E-mail:250204560@qq.com

中图分类号: P581
计量
- 文章访问数: 753
- HTML全文浏览量: 182
- PDF下载量: 41
- 被引次数: 0
出版历程
- 收稿日期: 2019-07-24
- 刊出日期: 2020-12-15

Petrogenesis and Forming Environment of Monzonitic Granite in Yushishan Nb-Ta Mining Area, Akesai, Gansu Province:Evidences from Chronology and Geochemistry

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
National Demonstration Center for Experimental Mineral Exploration Education, China University of Geosciences, Wuhan 430074, China
3.
Gansu Geological Survey, Lanzhou 730000, China

摘要

摘要: 余石山铌钽矿区位于北阿尔金-柴北缘-祁连的交汇部位，该区域构造演化复杂.为了揭示矿区内二长花岗岩的成因和形成环境，运用岩石学、岩石地球化学、锆石U-Pb年代学、锆石Lu-Hf同位素等理论及技术方法对该二长花岗岩进行了系统的研究.该二长花岗岩的详细定名为中细粒似斑状黑云二长花岗岩，暗色矿物以黑云母、角闪石为主.地球化学特征表明，余石山的二长花岗岩属于钾玄质准铝质-弱过铝质系列，富集Rb、Th、K等大离子亲石元素，相对亏损Nb、Sr、P、Ti等高场强元素，稀土元素配分曲线具有明显的负Eu异常，δEu的平均值为0.57，（La/Yb）_N的平均值为11.09，说明该二长花岗岩体岩浆部分熔融程度较高.根据岩石学及地球化学特征可判断该岩体为I型花岗岩.锆石LA-ICP-MS U-Pb定年显示，该二长花岗岩的结晶年龄为481.3±1.7 Ma，形成于早奥陶世.锆石Lu-Hf同位素分析表明，锆石ε_Hf（t）的值为+0.4~+11.8，均为正值，二阶段模式年龄的范围为675~1 308 Ma，指示其源岩主要为元古代新生地壳物质.该二长花岗岩的形成与早奥陶世时期北阿尔金洋壳俯冲中南祁连陆壳密切相关，在中南祁连陆壳边缘的余石山地区（弧后），由于洋壳俯冲导致了陆壳的伸展从而产生了裂隙，俯冲产生的熔融岩浆通过裂隙上侵而形成了该二长花岗岩岩体.
- 余石山 /
- 二长花岗岩 /
- U-Pb定年 /
- 地球化学 /
- Lu-Hf同位素 /
- 岩石学
Abstract: The Yushishan Nb-Ta mining area is located at the junction of North Altun, Qaidam and Qilian, and the tectonic evolution of this area is complex. The research of petrology, rock geochemistry, zircon U-Pb chronology and zircon Lu-Hf isotope was carried out on the monzonitic granite to reveal petrogenesis and forming environment of it. The detailed name of the monzonitic granite is medium-fine-grained porphyritic biotite monzonitic granite and its dark minerals are mainly biotite and hornblende. The geochemical characteristics show that the monzonitic granite belongs to the typical high-K series with quasi-aluminous to weakly peraluminous. Large ion lithophile elements (Rb, Th and K) are relatively enriched and high field strength elements (Nb, Sr, P and Ti) are in distinct negative anomaly. The REE distribution patterns show negative Eu anomaly, with the mean δEu value of 0.57 and the mean (La/Yb)_N value of 11.09, they show that the monzonitic granite magma has a high degree of partial melting. The features of petrological and geochemical indicate that the monzonitic granite belongs to I-type granite. Zircon LA-ICP-MS U-Pb dating of the monzonitic granite yielded a crystallization age of 481.3±1.7 Ma and it was formed in the Early Ordovician. The zircons Lu-Hf isotope analysis shows that the ε_Hf(t) ranges from +0.4 to +11.8 and the two-stage Hf model ages range from 675 to 1 308 Ma, suggesting that the source rocks are partial melting of Neoproterozoic juvenile crustal materials. The formation of the monzonitic granite was closely related to that North Altun oceanic crust subducted Middle-South Qilian continental crust, in the Yushishan area on the edge of Middle-South Qilian continental crust (back arc), the upward intrusion of molten magma from the fractures formed the monzonitic granite because of the subduction of the oceanic crust.
- Yushishan /
- monzonitic granite /
- U-Pb dating /
- geochemistry /
- Lu-Hf isotope /
- petrology

HTML全文

图 1 余石山铌钽矿区大地构造位置图

1.第四系；2.石炭.二叠系杨虎沟组；3.寒武.奥陶系拉配泉群；4.奥陶纪辉长岩体；5.蓟县.青白口系冰沟南组；6.长城系熬油沟组二段；7.长城系熬油沟组五段；8.长城系熬油沟组六段；9.二长花岗岩；10.石英闪长岩；11.断层及产状；12.余石山铌钽矿床位置；13.采样位置；图据杨再朝等(2014)修改

Fig. 1. Yushishan Nb-Ta mining area geotectonic location map

下载: 全尺寸图片幻灯片

图 2 矿区中细粒似斑状黑云二长花岗岩标本(a、b)和镜下显微特征(c、d)

Pl.斜长石；Kfs.钾长石；Bt.黑云母；Hb.角闪石；QZ.石英

Fig. 2. Medium-fine-grained porphyritic biotite monzonitic granite specimens (a, b) and microscopic characteristics (c, d) in the mining area

下载: 全尺寸图片幻灯片

图 3 余石山二长花岗岩K₂O-Na₂O(a)、A/NK-A/CNK图解(b)

据Maniar and Piccoli(1989)

Fig. 3. K₂O-Na₂O (a), A/NK-A/CNK (b) diagrams of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

图 4 余石山二长花岗岩原始地幔标准化微量元素蛛网图(a)稀土元素球粒陨石标准化曲线图(b)

a据Sun and Macdonough(1989); b据Taylor and Mclennan(1985)

Fig. 4. Primitive mantle-normalized trace element spider map of the original mantle (a) and rare earth element chondrite standardization curve (b) of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

图 5 余石山二长花岗岩锆石LA-ICP-MS激光点位及年龄

Fig. 5. Zircon LA-ICP-MS laser point and age of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

图 6 余石山二长花岗岩锆石U-Pb年龄谐和曲线(a)和平均年龄计算图(b)

Fig. 6. Zircon U-Pb age harmonic curve (a) and average age calculation (b) of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

图 7 余石山二长花岗岩锆石Hf同位素t-ε_Hf(t)(a)、t-¹⁷⁶Hf/¹⁷⁷Hf图解(b)

据吴福元等(2007)

Fig. 7. Zircon Hf isotope t-ε_Hf(t) (a), t-¹⁷⁶Hf/¹⁷⁷Hf (b) diagrams of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

图 8 余石山二长花岗岩K₂O-Na₂O(a)、Zr-TiO₂图解(b)

据Collins et al.(1982)

Fig. 8. K₂O-Na₂O (a) and Zr-TiO₂ (b) diagrams of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

图 9 余石山二长花岗岩Y-Nb(a)、Yb-Ta构造环境判别图(b)

WPG.板内花岗岩；VAG.火山弧花岗岩；ORG.洋脊花岗岩；syn-COLG.同造山期碰撞花岗岩；据Pearce et al.(1984)

Fig. 9. Judging diagram of Y-Nb(a) and Yb-Ta tectonic environment (b) of Yushishan monzonitic granite

下载: 全尺寸图片幻灯片

表 1 余石山二长花岗岩主量元素含量(%)

Table 1. Contents of main elements in Yushishan monzonitic granite(%)

样品号	YT3-01	YT3-02	YT3-03	YT3-04	YT3-05	YT3-06	YT3-07
Al₂O₃	16.78	16.66	17.28	17.20	17.29	17.44	17.43
As₂O₃	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
BaO	0.15	0.12	0.18	0.17	0.17	0.20	0.13
CaO	3.38	3.15	3.10	3.31	3.26	3.25	3.85
Cl	＜0.01	＜0.01	0.01	＜0.01	0.01	＜0.01	0.01
CoO	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
Cr₂O₃	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
CuO	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
TFe₂O₃	5.12	5.33	6.16	6.74	6.31	6.06	7.65
K₂O	4.02	3.42	3.92	3.65	3.56	4.00	2.89
MgO	1.86	2.04	2.26	2.49	2.31	2.27	3.07
MnO	0.07	0.07	0.08	0.08	0.08	0.08	0.10
Na₂O	4.83	5.14	4.30	4.34	4.74	4.42	4.67
NiO	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
P₂O₅	0.20	0.21	0.27	0.30	0.27	0.25	0.39
PbO	0.01	0.01	0.01	0.01	0.01	0.01	0.01
SiO₂	60.26	60.48	59.22	58.74	59.09	59.17	56.05
SnO₂	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
SO₃	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01	＜0.01
SrO	0.03	0.02	0.04	0.04	0.04	0.05	0.04
TiO₂	0.74	0.74	0.92	1.02	0.95	0.90	1.04
V₂O₅	0.01	0.01	0.01	0.02	0.01	0.01	0.02
ZnO	0.01	0.01	0.01	0.01	0.01	0.01	0.01
ZrO₂	0.05	0.04	0.05	0.06	0.06	0.05	0.05
LOI	2.06	2.08	1.55	1.58	1.56	1.49	2.10

下载: 导出CSV

表 2 余石山二长花岗岩微量元素含量(10^-6)

Table 2. Trace element contents (10^-6) of Yushishan monzonitic granite

样品号	YT3-01	YT3-02	YT3-03	YT3-04	YT3-05	YT3-06	YT3-07
Ba	1 445	1 200	1 785	1 645	1 685	1 835	1 230
Ce	183	210	223	228	219	194	185
Cr	20	20	20	20	20	10	10
Cs	0.72	0.61	2.95	3.58	2.58	2.83	2.40
Dy	10.10	9.94	11.70	12.95	11.80	10.05	9.73
Er	5.71	5.54	6.78	7.16	6.98	5.86	5.59
Eu	2.46	2.47	2.85	3.07	2.92	2.59	2.53
Ga	19.8	19.8	21.6	22.9	21.8	20.9	23.6
Gd	11.35	11.35	13.50	14.65	13.85	12.20	11.85
Hf	10.3	8.9	11.8	13.9	11.9	11.5	9.4
Ho	2.02	1.95	2.34	2.56	2.44	2.11	2.06
La	79.1	104.0	100.5	90.7	92.6	83.7	76.7
Lu	0.76	0.73	0.91	0.96	0.89	0.84	0.79
Nb	47.7	47.7	54.9	60.0	55.8	49.7	48.3
Nd	74.0	77.8	86.9	93.1	88.0	77.0	73.5
Pr	20.7	22.2	24.6	26.2	24.8	22.1	20.6
Rb	116.0	97.6	139.5	132.5	125.0	125.5	106.0
Sm	14.20	14.00	16.60	17.90	16.70	14.80	14.05
Sn	4	4	5	5	5	4	4
Sr	220	195	418	418	360	380	352
Ta	3.7	3.6	4.0	4.5	4.1	3.7	3.5
Tb	1.72	1.78	2.06	2.21	2.11	1.80	1.77
Th	12.40	16.30	21.00	19.80	15.95	16.25	13.35
Tm	0.85	0.84	1.02	1.13	1.03	0.90	0.82
U	2.63	2.47	4.18	4.66	3.80	3.52	3.57
V	86	90	98	108	99	90	115
W	＜1	35	＜1	1	1	1	1
Y	59.6	59.9	69.7	77.4	71.1	62.0	59.2
Yb	5.45	5.30	6.31	6.92	6.59	5.77	5.61
Zr	423	376	511	583	500	483	396

下载: 导出CSV

参考文献(125)

[1]	Amelin, Y., Lee, D.C., Halliday, A.N., et al., 1999.Nature of the Earth's Earliest Crust from Hafnium Isotopes in Single Detrital Zircons.Nature, 399:252-255. https://www.researchgate.net/publication/30863322_Nature_of_the_Earth's_earliest_crust_from_hafnium_isotopes_in_single_detrital_zircons
[2]	Andersen, T., 2002.Correction of Common Lead in U-Pb Analyses That do not Report ²⁰⁴Pb.Chemical Geology, 192(1-2):59-79. https://www.sciencedirect.com/science/article/pii/S000925410200195X
[3]	Andersson, J., Miller, C., Johansson, L., 2002.Zircon Geochronology of Migmatite Gneisses along the Mylonite Zone (Sweden):A Major Sveconorwegian Terrane Boundary in the Baltic Shield.Precambrian Research, 114(1-2):121-147.
[4]	Bonin, B., 2007.A-Type Granites and Related Rocks:Evolution of a Concept, Prospects.Lithos, 97(1-2):1-29. https://www.sciencedirect.com/science/article/abs/pii/S0024493706003252
[5]	Bouvier, A., Vervoort, J.D., Patchett, P.J., 2008.The Lu-Hf and Sm-Nd Isotopic Composition of CHUR:Constraints from Unepuilibrated Chondrites and Implications for the Bulk Composition of Terrestrial Planets.Earth and Planetary Science Letters, 273(1-2):48-57. https://www.sciencedirect.com/science/article/pii/S0012821X08003828
[6]	Chen, B.L., Li, S.B., Jiang, R.B., et al., 2016.Zircon SHRIMP U-Pb Dating of Intermediate-Felsic Volcanic Rocks from the Kaladawan Area, Altun Mountains and Its Tectonic Environment.Acta Geologica Sinica, 90 (4):708-727(in Chinese with English abstract).
[7]	Chen, D.L., Liu, L., Sun, Y., et al., 2009.Geochemistry and Zircon U-Pb Dating and Its Implications of the Yukahe HP/UHP Terrane, the North Qaidam, NW China.Journal of Asian Earth Sciences, 35(1-4):259-272. https://www.sciencedirect.com/science/article/pii/S1367912008001946
[8]	Chen, H.J., Wu, C.L., Lei, M., et al., 2018.Genesis and Geological Significance of the Neoproterozoic Granite in the Kekesayi, Nanerjin Block.Earth Science, 43(4):1278-1295(in Chinese with English abstract).
[9]	Chen, J.L., Li, H.B., Wang, H.L., et al., 2007.LA-ICPMS Zircon U-Pb Dating of a Quartz Diorite Pluton from Wangjiacha, the Junction Area between the Qinling and Qilian Orogenic Belts and Its Tectonic Significance.Journal of Jilin University (Earth Science Edition), 37(3):423-431(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200703001.htm
[10]	Chen, J.L., Xu, X.Y., Zeng, Z.X., et al., 2008.Geochemical Characters and LA-ICPMS Zircon U-Pb Dating Constraints on the Petrogenesis and Tectonic Setting of the Shichuan Intrusion, East Segment of the Cental Qilian, NW China.Acta Petrologica Sinica, 24(4):841-854(in Chinese with English abstract). https://www.researchgate.net/profile/Jl-Chen
[11]	Chen, X.H., Gehrels, G., Wang, X.F., et al., 2003.Discussion on the Formation Age of Granite in the Northern Margin of the Altun Mountains and Its Tectonic Setting.Bulletin of Mineralogy, Petrology and Geochemistry, 22(4):294-298(in Chinese with English abstract).
[12]	Claesson, S., Vetrin, V., Bayanova, T., et al., 2008.U-Pb Zircon Ages from a Devonian Carbonatite Dyke, Kols Peninsula, Russia:A Record of Geological Evolution from the Archaean to the Palaeozoic Lithos.Journal of Metamorphic Geology, 32(1-2):95-108. https://www.sciencedirect.com/science/article/abs/pii/S0024493799000766
[13]	Collins, W.J., Beams, S.D., White, A.J.R., et al., 1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology, 80(2):189-200. doi: 10.1007/BF00374895
[14]	Defant, M.J., Xu, J.F., Kepezhinskas, P., et al., 2002.Adakites:Some Variations on a Theme.Acta Petrologica Sinica, 18 (2):129-142. https://www.researchgate.net/publication/298585840_Adakites_Some_variations_on_a_theme
[15]	Diwu, C.R., Sun, Y., Lin, C.L., et al., 2007.Zircon U-Pb Ages and Hf Isotopes and Their Geological Significance of Yiyang TTG Gneisses from Henan Province, China.Acta Petrologica Sinica, 23(2):253-262(in Chinese with English abstract). https://www.researchgate.net/publication/280015308_Zircon_U-Pb_ages_and_Hf_isotopes_and_their_geological_significance_of_Yiyang_TTG_gneisses_from_Henan_province_China
[16]	Gao, D., Wu, C.L., Gao, Y.H., et al., 2019.Zircon U-Pb Geochronology, Geochemical Characteristics and Geological Significance of the Yusupuleke Granite Pluton in South Altyn and Its Geological Implications.Earth Science, 44(11):3812-3828(in Chinese with English abstract).
[17]	Ge, X.H., Liu, J.L., 1999.Formation and Tectonic Background of the Northern Qilian Orogenic Belt.Earth Science Frontiers, , 6(4):223-230(in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S1342937X12000445
[18]	Hoskin, P.W.O., Black, L.P., 2000.Metamorphic Zircon Formation by Solid-State Recrystallization of Protolith Igneous Zircon.Journal of Metamorphic Geology, 18(4):423-439. doi: 10.1046/j.1525-1314.2000.00266.x
[19]	Hoskin, P.W.O., Schaltegger, U., 2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Zircon, 53(1):27-62. https://pubs.geoscienceworld.org/msa/rimg/article-abstract/53/1/27/87468/The-Composition-of-Zircon-and-Igneous-and
[20]	Hou, K.J., Li, Y.H., Zou, T.R., et al., 2007.Laser Ablation-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon and Its Geological Applications.Acta Petrologica Sinica, 23(10):2595-2604(in Chinese with English abstract).
[21]	Hou, R.N., Wang, S.H., Zhang, X., et al., 2015.Geochemical Characteristics and Tectonic Significance of the Granotoids in the Western Section of the Mid-Qilian.Advances in Earth Science, 30(9):1034-1049(in Chinese with English abstract).
[22]	Huang, Z.B., Zhen, J.P., Li, B.H., et al., 2015.Geochronology and Geochemistry of Yemashan Batholiths in Western Central Qilian and Its Tectonic Implications.Geology in China, 45(2):406-420(in Chinese with English abstract).
[23]	Jia, Q.Z., Yang, Z.T., Xiao, C.Y., et al., 2007.The Metallogenic Regularity and Metallogenic Prognosis of the Copper, Gold, Tungsten, Lead, Zinc Deposits in Qilian Mountains.Geological Publishing House, Beijing(in Chinese).
[24]	Jia, Z.L., 2016.Geological and Metallogenic Characteristics of Nb-Ta-Rb Deposits South Qilian-Beishan, Gansu Province (Dissertation).Lanzhou University, Lanzhou (in Chinese with English abstract).
[25]	Jia, Z.L., Dou, X.Y., Wang, J.R., et al., 2016.Protolith Reconstruction of Leptynite in Yushishan Area, South Qilian, Gansu.Gansu Geology, 25(2):9-14(in Chinese with English abstract).
[26]	Li, H.K., Zhu, S.X., Xiang, Z.Q., et al., 2010.Zircon U-Pb Dating on Tuff Bed from Gaoyuzhuang Formation in Yanqing, Beijing:Further Constraints on the New Subdivision of the Mesoproterozoic Stratigraphy in the Northern North China.Acta Petrologica Sinica, 26(8):2131-2140(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201007016.htm
[27]	Li, J.F., Zhang, Z.C., Han, B.F., 2010.Geochronolgy and Geochemistry of Early Paleozoic Plutons from Subei and Shibaocheng Areas, the Western Segment of Central Qilian and Their Geological Implications.Acta Petrologica Sinica, 26(8):2431-2444(in Chinese with English abstract).
[28]	Li, Q., Zeng, Z.C., Chen, N., et al., 2015.Zircon U-Pb Ages, Geochemical Characteristics and Tectonic Implications of Neoproterozoic Gailike Gneiss in the South Altyn Tagh.Geoscience, 29(6):1271-1283(in Chinese with English abstract).
[29]	Liu, J.H., Liu, L., Gai, Y.S., et al., 2017.Zircon U-Pb Dating and Hf Isotopic Compositions of the Baijianshan Granodiorite in North Altyn Tagh and Its Geological Significance.Acta Geologica Sinica, 91(5):1022-1038(in Chinese with English abstract).
[30]	Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43. https://www.researchgate.net/publication/222034389_In_situ_analysis_of_major_and_trace_elements_of_anhydrous_minerals_by_LA-ICP-MSLA-ICP-MS_without_applying_an_internal_standard
[31]	Liu, Z.W., Wang, C.L., 2007.Granitoid Geochemistry and Gold-Copper Mineralization in the Danghenanshan Area, Southern Qilian Mountains.Geology and Prospecting, 43(1):64-73(in Chinese with English abstract).
[32]	Liu, Z.W., Wang, C.L., Shi, X.H., 2006.Granitoids Characteristics and Tectonic Setting of Danghenanshan Area in South Qilian Mountains.Geoscience, 20(4):545-554(in Chinese with English abstract).
[33]	Ludwig, K.R., 2003.User's Manual for Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley.
[34]	Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643. https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/101/5/635/182281/Tectonic-discrimination-of-granitoids
[35]	Mcdonough, W.F., 2003.Compositional Model for the Earth's Core.Treatise on Geochemistry, 2:547-568. https://www.researchgate.net/publication/234489093_Compositional_Model_for_the_Earth's_Core
[36]	Miller, C.F., 1985.Are Strongly Petaluminous Magmas Derived from Politic Sedimentary Sources?The Journal of Geology, 93(6):673-689. doi: 10.1086/628995
[37]	Pan, X.F., Jiao, J.G., Wu, C.L., et al., 2019.Zircon U-Pb Dating and Hf Isotope Characteristics of the Aketishan Granite in the Southern Margin of Altun and Their Tectonics Implications.Acta Geologica Sinica, 93(3):633-646(in Chinese with English abstract).
[38]	Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology, 25(4):956-983. https://www.researchgate.net/profile/Julian_Pearce2/publication/31497296_Trace_Element_Discrimination_Diagrams_for_the_Tectonic_Interpretation_of_Granitic_Rocks/links/00b495369517451efc000000/Trace-Element-Discrimination-Diagrams-for-the-Tectonic-Interpretation-of-Granitic-Rocks.pdf
[39]	Peng, Y.B., Yu, S.Y., Zhang, J.X., et al., 2018.Timing of Early Paleozoic Oceanic Crust Subduction in North Altun:Evidence from Plagiogranite and Granodiorite.Geology in China, 45(2):334-350(in Chinese with English abstract). https://www.researchgate.net/publication/328852228_Timing_of_Early_Paleozoic_oceanic_crust_subduction_in_North_Altun_Evidence_from_plagiogranite_and_granodiorite
[40]	Qi, R.R., 2012.LA-ICP-MS Zircon U-Pb Ages and Geological Implications for the Bagadeerji Granitic Plutons in the Central Qilian Mountains, Gansu.Sedimentary Geology and Tethyan Geology, 32(4):86-93(in Chinese with English abstract).
[41]	Qin, X.F., Xia, B., Li, C.Q., et al., 2008.Geochemical Characteristics and Tectonic Setting of Precambrian Granitic Gneiss in the Western Segment of Altyn Tagh Tectonic Belt. Geoscience, 22(1):34-44(in Chinese with English abstract).
[42]	Sang, L.K., Ma, C.Q., Wang, G.Q., et al., 2001.Petrology (Second Edition).Geological Publishing House, Beijing, 188(in Chinese).
[43]	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.
[44]	Su, J.P., Hu, N.G., Zhang, H.F., et al., 2004.U-Pb Zircon Dating and Genesis of Heigouliangzi Granitic Intrusion in the West Segment of the Middle Qilian Mountains.Geoscience, 18(1):70-75(in Chinese with English abstract).
[45]	Su, J.P., Zhang, X.H., Hu, N.G., et al., 2004.Geochemical Characteristics and Genesis of Adakite-Like Granites at Yema Nanshan in the Western Segment of the Central Qilian Mountains.Geology in China, 31(4):365-371(in Chinese with English abstract).
[46]	Sun, 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://www.researchgate.net/publication/231575101_Chemical_and_isotopic_systematics_of_oceanic_basalts_Implications_for_mantle_composition_and_processes
[47]	Taylor, S.R., McLennan, S.M., 1985.The Continental Crust:Its Composition and Evolution.Geological Magazine, 122(6):673-674. doi: 10.1002/gj.3350210116
[48]	Taylor, S.R., McLennan, S.M., 1995.The Geochemical Evolution of the Continental Crust.Reviews of Geophysics, 33(2):241-265. doi: 10.1029/95RG00262
[49]	Vervoort, J.D., Patchett, P.J., Gehrels, G.E., et al., 1996.Constraints on Early Earth Differentiation from Hafnium and Neodymium Isotopes.Nature, 379:624-627. https://ui.adsabs.harvard.edu/abs/1996Natur.379..624V
[50]	Wang, L.S., Zhang, W., Duan, X.X., et al., 2015.Isotopic Age and Genesis of the Monzogranitic Gneiss at the Huanxingshan in Middle Altyn Tagh.Acta Petrologica Sinica, 31(1):119-132(in Chinese with English abstract). https://core.ac.uk/display/71731772
[51]	Wang, M.J., Song, S.G., Niu, Y.L., et al., 2014.Post-Collisional Magmatism:Consequences of UHPM Terrane Exhumation and Orogen Collapse, N.Qaidam UHPM Belt, NW China.Lithos, (210-211):181-198. https://www.sciencedirect.com/science/article/pii/S0024493714003727
[52]	Wang, X.F., Chen, X.H., Chen, Z.L., et al., 2002.Long-Term Prediction of Geological Conditions in the Altun Mineralization.Geological Publishing House, Beijing, 135-159(in Chinese with English abstract).
[53]	Wu, C.L., Gao, Y.H., Wu, S.P., et al., 2008.Zircon SHRIMP U-Pb Dating of the Western Segment of the Northern Margin of the Qaibei Margin and Its Petrochemical Characteristics.Science in China (Ser.D), 38(8):930-949(in Chinese).
[54]	Wu, C.L., Yang, J.S., Irland, T., et al., 2001.Zircon SHRIMP Ages of Aolaoshan Granite from the South Margin of Qilianshan and Its Geological Significance.Acta Petrologica Sinica, 17(2):215-221(in Chinese with English abstract).
[55]	Wu, C.L., Yang, J.S., Xu, Z.Q., et al., 2004.Granitic Magmatism on the Early Paleozoic UHP Belt of Northern Qaidam, NW China. Acta Geologica Sinica, 78(5):658-674(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200405009.htm
[56]	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). https://www.researchgate.net/publication/279910636_Lu-Hf_isotopic_systematics_and_their_application_in_petrology
[57]	Wu, Y., Chen, Z.L., Chen, B.L., et al., 2019.Early Paleozoic Tectonic Deformation in Qiashenkansayigou Area, North Altun, and Implication for Tectonic Evolution.Journal of Geomechanics, 25(3):301-312(in Chinese with English abstract).
[58]	Wu, Y.B., Zheng, Y.F., 2004.Zircon Genesis Mineralogical Study and Its Constraints on U-Pb Age Interpretation.Chinese Science Bulletin, 49(16):1589-1604(in Chinese). doi: 10.1007/BF03184122
[59]	Xin, H.T., Wang, H.C., Zhou, S.J., 2006.Geological Events and Tectonic Evolution of the North Margin of the Qaidam Basin.Geological Survey and Research, 29(4):311-320(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ200604010.htm
[60]	Xiong, Q., Zheng, J.P., Griffin, W.L., et al., 2011.Zircons in the Shenglikou Ultrahigh-Pressure Garnet Peridotite Massif and Its Country Rocks from the North Qaidam Terrane (Western China):Meso-Neoproterozoic Crust-Mantle Coupling and Early Paleozoic Convergent Plate-Margin Processes.Precambrian Research, 187 (1-2):33-57. https://www.sciencedirect.com/science/article/pii/S0301926811000416
[61]	Xiong, Q., Zheng, J.P., Griffin, W.L., et al., 2012.Decoupling of U-Pb and Lu-Hf Isotopes and Trace Elements in Zircon from the UHP North Qaidam Orogeny, NE Tibet (China):Tracing the Deep Subduction of Continental Blocks.Lithos, 155:125-145.
[62]	Xu, Z.Q., Yang, J.S., Zhang, J.X., et al., 1999.Comparison between the Tectonic Units on the Two Sides of the Altun Sinistral Strike-Slip Fault and the Mechanism of Lithospheric Shearing.Acta Geologica Sinica, 73(3):193-205(in Chinese with English abstract).
[63]	Yang, Y., Chen, X.H., Gehrels, G., et al., 2004.Early Paleozoic Magmatism and Gold Metallogenesis in Altun Mountains, Northwest China.Mineral Deposits, 23(4):464-472(in Chinese with English abstract).
[64]	Yang, Z.C., Xiao, P.X., Gao, X.F., et al., 2014.LA-ICP-MS Dating of the Aegirine-Augite Syenite of Yushishan Nb-Ta Deposit in Eastern Altun and Its Constraints on the Metallogenetic Age.Northwestern Geology, 47(4):187-197(in Chinese with English abstract).
[65]	Yin, H.F., Zhang, K.X., 1998.Evolution and Characteristics of the Central Orogenic Belt.Earth Science, 23(5):438-442(in Chinese with English abstract).
[66]	Yong, Y., Xiao, W.J., Yuan, C., et al., 2008.Geochronology and Geochemistry of Paleozoic Granitic Plutons from the Eastern Central Qilian and Their Tectonic Implications.Acta Petrologica Sinica, 24(4):855-866(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200804025.htm
[67]	Yu, J.P., Wu, Y.B., Liang, M.H., et al., 2015.New Progress of the Southern Altyn Tagh Geological Mapping and Guide the Prospecting Support:According to 1:50 000 Mobeier and other Five Regional Geological Maps in Gansu Province. Geological Survey of China, 2(2):40-47(in Chinese with English abstract).
[68]	Yu, S.Y., Zhang, J.X., Mattinson, C.G., et al., 2014.Paleozoic HP Granulite-Facies Metamorphism and Anatexis in the Dulan Area of the North Qaidam UHP Terrane, Western China:Constraints from Petrology, Zircon U-Pb and Amphibole Ar-Ar Geochronology.Lithos, 198-199:58-76. https://www.sciencedirect.com/science/article/pii/S0024493714000991
[69]	Zhang, C., Roermund, H., Zhang, L.F., et al., 2012.A Polyphase Metamorphic Evolution for the Xitieshan Paragneiss of the North Qaidam UHP Metamorphic Belt, Western China:In Situ EMP Monazite and U-Pb Zircon SHRIMP Dating.Lithos, 136-139:27-45. https://www.sciencedirect.com/science/article/pii/S0024493711002192
[70]	Zhang, G.B., Zhang, L.F., Christy, A.G., 2013.From Oceanic Subduction to Continental Collision:An Overview of HP-UHP Metamorphic Rocks in the North Qaidam UHP Belt, NW China.Journal of Asian Earth Sciences, 63:98-111. https://www.sciencedirect.com/science/article/pii/S1367912012003185
[71]	Zhang, J.X., Mattinson, C.G., Yu, S.Y., 2010.U-Pb Geochronology of Coesite-Bearing Eclogites from the Southern Dulan Area of the North Qaidam UHP Terrane, Northwestern China:Spatially and Temporally Extensive UHP Metamorphism during Continental Subduction.Journal of Metamorphic Geology, 28(9):955-978. https://www.researchgate.net/publication/258370920_U-Pb_zircon_geochronology_of_coesite-bearing_eclogites_from_the_southern_Dulan_area_of_the_North_Qaidam_UHP_terrane_northwestern_China_Spatially_and_temporally_extensive_UHP_metamorphism_during_contin
[72]	Zhang, J.X., Meng, F.C., Yu, S.Y., et al., 2007.³⁹Ar-⁴⁰Ar Geochronology of High-Pressure/Low-Temperature Blueschist and Eclogite in the North Altyn Tagh and Their Tectonic Implications.Geology in China, 34(4):558-564(in Chinese with English abstract).
[73]	Zhang, J.X., Yu, S.Y., Li, Y.S., et al., 2015.Subduction, Accretion and Closure of Proto-Tethyan Ocean:Early Paleozoic Accretion/Collision Orogeny in the Altun-Qilian-North Qaidam Orogenic System.Acta Petrologica Sinica, 31(12):3531-3554(in Chinese with English abstract). https://www.researchgate.net/publication/292476172_Subduction_accretion_and_closure_of_Proto-Tethyan_Ocean_Early_Paleozoic_accretioncollision_orogeny_in_the_Altun-Qilian-North_Qaidam_orogenic_system
[74]	Zhang, Q., Wang, Y., Li, C.D., et al., 2006.Granite Classification on the Basis of Sr and Yb Contents and Its Implications.Acta Petrologica Sinica, 22(9):2249-2269(in Chinese with English abstract). https://www.researchgate.net/publication/279655758_Granite_classification_on_the_basis_of_Sr_and_Yb_contents_and_its_implications
[75]	Zhang, Z.W., Li, W.Y., Gao, Y.B., et al., 2012.ID-TIMS Zircon U-Pb Age of Yulonggou Intrusive Rocks in Southern Qilian Mountain and Its Geological Significance.Geological Bulletin of China, 31(2):455-462(in Chinese with English abstract).
[76]	Zhao, G.X., Mao, D.B., Zhang, Y., et al., 2007.Main Metallogenic Systems of the Alytn Metallogenic Belt in Caledonian.Geological Survey and Research, 30(2):90-97(in Chinese with English abstract).
[77]	Zhao, Z.X., 2011.Geochronology and Tectonic Significance of Paleozoie Granites in the Eastern Altun-North Qaidam Western China (Dissertation).Lanzhou University, Lanzhou (in Chinese with English abstract).
[78]	陈柏林, 李松彬, 蒋荣宝, 等, 2016.阿尔金喀腊大湾地区中酸性火山岩SHRIMP年龄及其构造环境.地质学报, 90(4):708-727. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201604008.htm
[79]	陈红杰, 吴才来, 雷敏, 等, 2018.南阿尔金陆块科克萨依新元古代花岗岩成因及地质意义.地球科学, 43(4):1278-1295. doi: 10.3799/dqkx.2018.720
[80]	陈隽璐, 李好斌, 王洪亮, 等, 2007.秦祁结合部位王家岔石英闪长岩体锆石LA-ICPMS定年及地质意义.吉林大学学报(地球科学版), 37(3):423-431. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200703001.htm
[81]	陈隽璐, 徐学义, 曾佐勋, 等, 2008.中祁连东段什川杂岩基的岩石化学特征及年代学研究.岩石学报, 24 (4):841-854. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200804024.htm
[82]	陈宣华, Gehrels, G., 王小凤, 等, 2003.阿尔金山北缘花岗岩的形成时代及其构造环境探讨.矿物岩石地球化学通报, 22(4):294-298. https://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200304002.htm
[83]	第五春荣, 孙勇, 林慈銮, 等, 2007.豫西宜阳地区TTG质片麻岩锆石U-Pb定年和Hf同位素地质学.岩石学报, 23(2):253-262. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702007.htm
[84]	高栋, 吴才来, 郜源红, 等, 2019.南阿尔金玉苏普阿勒克塔格花岗岩体锆石U-Pb年代学、地球化学特征及地质意义.地球科学, 44(11):3812-3828. doi: 10.3799/dqkx.2018.279
[85]	葛肖虹, 刘俊来, 1999.北祁连造山带的形成与背景.地学前缘, 6(4):223-230. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199904005.htm
[86]	侯可军, 李延河, 邹天人, 等, 2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报, 23(10):2595-2604. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200710026.htm
[87]	侯荣娜, 王淑华, 张翔, 等, 2015.中祁连西段花岗岩类的地球化学特征及构造意义.地球科学进展, 30(9):1034-1049. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201509010.htm
[88]	黄增保, 郑建平, 李葆华, 等, 2015.中祁连西段野马山岩基年代学、地球化学特征及地质意义.中国地质, 45(2):406-420. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201502004.htm
[89]	贾群子, 杨忠堂, 肖朝阳, 等.2007.祁连山铜金钨铅锌矿床成矿规律和成矿预测.北京:地质出版社.
[90]	贾志磊, 2016.甘肃南祁连-北山铌钽铷等稀有金属成矿地质特征与成矿规律的研究(博士学位论文).兰州: 兰州大学.
[91]	贾志磊, 窦小雨, 王金荣, 等, 2016.甘肃南祁连余石山地区变粒岩原岩恢复.甘肃地质, 25(2):9-14. https://www.cnki.com.cn/Article/CJFDTOTAL-GSDZ201602002.htm
[92]	李怀坤, 朱士兴, 相振群, 等, 2010.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束.岩石学报, 26(7):2131-2140. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201007016.htm
[93]	李建锋, 张志诚, 韩宝福, 2010.中祁连西段肃北、石包城地区早古生代花岗岩年代学、地球化学特征及其地质意义.岩石学报, 26(8):2431-2444. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201008017.htm
[94]	李琦, 曾忠诚, 陈宁, 等, 2015.阿尔金南缘新元古代盖里克片麻岩年代学、地球化学特征及其构造意义.现代地质, 29(6):1271-1283. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201506002.htm
[95]	刘锦宏, 刘良, 盖永升, 等, 2017.北阿尔金白尖山地区花岗闪长岩锆石U-Pb定年、Hf同位素组成及其地质意义.地质学报, 91(5):1022-1038. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201705005.htm
[96]	刘志武, 王崇礼, 2007.南祁连党河南山花岗岩类地球化学及其金铜矿化.地质与勘探, 43(1):64-73. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200701013.htm
[97]	刘志武, 王崇礼, 石小虎, 2006.南祁连党河南山花岗岩类特征及其构造环境.现代地质, 20(4):545-554. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200604003.htm
[98]	潘雪峰, 焦建刚, 吴才来, 等, 2019.阿尔金南缘阿克提山岩体锆石U-Pb定年、Hf同位素特征及构造意义.地质学报, 93(3):633-646. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201903009.htm
[99]	彭银彪, 于胜尧, 张建新, 等, 2018.北阿尔金地区早古生代洋壳俯冲时限:来自斜长花岗岩和花岗闪长岩的证据.中国地质, 45(2):334-350. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201802010.htm
[100]	齐瑞荣, 2012.中祁连西段巴嘎德尔基岩体LA-ICP-MS锆石U-Pb年龄及地质意义.沉积与特提斯地质, 32 (4):86-93. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD201204013.htm
[101]	覃小锋, 夏斌, 黎春泉, 等, 2008.阿尔金构造带西段前寒武纪花岗质片麻岩的地球化学特征及其构造背景.现代地质, 22(1):34-44. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200801006.htm
[102]	桑隆康, 马昌前, 王国庆, 等, 2001.岩石学(第二版), 北京:地质出版社, 188.
[103]	苏建平, 胡能高, 张海峰, 等, 2004a.中祁连西段黑沟梁子花岗岩的锆石U-Pb同位素年龄及成因.现代地质, 18(1):70-74. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200401010.htm
[104]	苏建平, 张新虎, 胡能高, 等.2004b.中祁连西段野马南山埃达克质花岗岩的地球化学特征及成因.中国地质, 31(4):365-371. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200404003.htm
[105]	王立社, 张巍, 段星星, 等, 2015.阿尔金环形山花岗片麻岩同位素年龄及成因研究.岩石学报, 31(1):119-132. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501009.htm
[106]	王小凤, 陈宣华, 陈正乐, 等, 2002.阿尔金成矿地质条件远景预测.北京:地质出版社, 135-159.
[107]	辛后田, 王惠初, 周世军, 2006.柴北缘的大地构造演化及其地质事件群.地质调查与研究, 29(4):311-323. https://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200604010.htm
[108]	吴才来, 郜源红, 吴锁平, 等, 2008.柴北缘西段花岗岩锆石SHRIMP U-Pb定年及其岩石地球化学特征.中国科学(D辑), 38(8):930-949. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200808002.htm
[109]	吴才来, 杨经绥, Irland, T., 等, 2001.祁连南缘嗷唠山花岗岩SHRIMP锆石年龄及其地质意义.岩石学报, 17(2):215-221. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200102004.htm
[110]	吴才来, 杨经绥, 许志琴, 等, 2004.柴达木盆地北缘古生代超高压带中花岗质岩浆作用.地质学报, 78(5):658-674. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200405009.htm
[111]	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. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702002.htm
[112]	吴玉, 陈正乐, 陈柏林, 等, 2019.北阿尔金恰什坎萨依沟地区早古生代构造变形特征及构造演化启示.地质力学学报, 25(3):301-312. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201903016.htm
[113]	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. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200416001.htm
[114]	许志琴, 杨经绥, 张建新, 等, 1999.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制.地质学报, 73(3):193-205. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199903000.htm
[115]	杨屹, 陈宣华, Griffin, W.L., 等, 2004.阿尔金山早古生代岩浆活动与金成矿作用.矿床地质, 23(4):464-472. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200404005.htm
[116]	杨再朝, 校培喜, 高晓峰, 等, 2014.阿尔金山东端余石山铌钽矿区霓辉正长岩的LA-ICP-MS定年及对成矿时代的制约.西北地质, 47(4):187-197. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDI201404022.htm
[117]	殷鸿福, 张克信, 1998.中央造山带的演化及其特点.地球科学, 23(5):438-442. http://www.earth-science.net/article/id/696
[118]	雍拥, 肖文交, 袁超, 等, 2008.中祁连东段古生代花岗岩的年代学、地球化学特征及其大地构造意义.岩石学报, 24(4):855-866. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200804025.htm
[119]	余君鹏, 吴义布, 梁明宏, 等, 2015.阿尔金南缘地质填图新进展及对找矿的启示:据甘肃1:5万莫坝尔等六幅区调.中国地质调查, 2(2):40-47. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDC201502007.htm
[120]	张建新, 孟繁聪, 于胜尧, 等, 2007.北阿尔金HP/LT蓝片岩和榴辉岩的Ar-Ar年代学及其区域构造意义.中国地质, 34(4):558-564. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200704003.htm
[121]	张建新, 于胜尧, 李云帅, 等, 2015.原特提斯洋的俯冲、增生及闭合:阿尔金-祁连-柴北缘造山系早古生代增生/碰撞造山作用.岩石学报, 31(12):3531-3554. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201512003.htm
[122]	张旗, 王焰, 李承东, 等, 2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报, 22(9):2249-2269. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200609000.htm
[123]	张照伟, 李文渊, 高永宝, 等, 2012.南祁连裕龙沟岩体ID-TIMS锆石U-Pb年龄及其地质意义.地质通报, 31(2):455-462. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2012Z1030.htm
[124]	赵更新, 毛德宝, 张燕, 等, 2007.阿尔金成矿带加里东期主要成矿系统.地质调查与研究, 30(2):90-97. https://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200702003.htm
[125]	赵志雄, 2011.阿尔金东段-柴北缘古生代花岗岩年代学及其构造意义的研究(博士学位论文).兰州: 兰州大学.