东天山铜鱼梁铜矿区闪长玢岩SHRIMP锆石U-Pb年代学、岩石地球化学及其地质意义

孙志远; 龙灵利; 王玉往; 罗照华; 赵路通; 武承贺

doi:10.3799/dqkx.2018.997

东天山铜鱼梁铜矿区闪长玢岩SHRIMP锆石U-Pb年代学、岩石地球化学及其地质意义

doi: 10.3799/dqkx.2018.997

1.
中国地质大学地球科学与资源学院, 北京 100083
2.
北京矿产地质研究院, 北京 100012
3.
昆明理工大学国土资源工程学院, 云南昆明 650093
4.
吐鲁番工企矿业有限责任公司, 新疆吐鲁番 838000

基金项目:

国家重点基础发展研究计划（973计划）项目 2014CB440803

国家自然科学基金项目 41202046

中国地质调查局项目 12120113086300

详细信息

作者简介:
孙志远(1989-), 男, 博士, 主要从事矿产普查与勘探方面的研究.E-mail:sunzhiyuan010@163.com

中图分类号: P611;P629;P632
计量
- 文章访问数: 4051
- HTML全文浏览量: 1905
- PDF下载量: 50
- 被引次数: 0
出版历程
- 收稿日期: 2018-03-20
- 刊出日期: 2018-09-15

SHRIMP Zircon U-Pb Geochronology and Geochemistry of Diorite Porphyrite in Tongyuliang Copper Deposit, Eastern Tianshan and Its Geological Significance

1.
School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China
3.
Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China
4.
Turpan Mining and Matallurgy Co., Ltd., Turpan 838000, China

摘要

摘要: 位于新疆东天山阿齐山-雅满苏成矿带东段的铜鱼梁矿床是近年来新发现的铜矿点，但带内热液型铜矿的研究和找矿勘查程度不高，通过SHRIMP锆石U-Pb定年获得矿区与成矿密切相关的闪长玢岩年龄为317.7±2.4 Ma，表明矿区在晚石炭世可能存在重要的岩浆-成矿事件.通过岩石地球化学特征研究可得铜鱼梁闪长玢岩SiO₂含量为56.71%~66.03%，Mg^#=49.75~55.29，Na₂O+K₂O=5.15%~6.40%，Na₂O/K₂O=4.49~53.62，铝指数A/CNK=0.9~1.1，为富钠、准铝质-过铝质、低钾（拉斑）系列岩石.稀土总量较低（39.56×10^-6~60.60×10^-6），具有轻稀土富集、重稀土亏损的右倾配分模式，富集Ba、U、K、Sr等大离子亲石元素（LILE），亏损Nb、Ta、Ti高场强元素（HFSE），显示弧岩浆的特征.闪长玢岩（⁸⁷Sr/⁸⁶Sr）_i变化于0.704 030~0.704 413之间，ε_Nd（t）=1.02~6.42，具有低的锶同位素初始值和正的ε_Nd（t）值，表明其岩浆源区主要来源于亏损地幔源区.综合已有资料，认为研究区闪长玢岩形成于岛弧的构造背景，为石炭世古康古尔洋壳向南俯冲的流体交代地幔后的产物.至晚石炭世早期，古康古尔洋俯冲交代，在上升中富含铜金属元素的岩浆流体当运移到浅部时，次火山岩通过交代岩体本身或火山地层形成了铜鱼梁铜矿床.
- 铜鱼梁铜矿床 /
- 闪长玢岩 /
- SHRIMP锆石U-Pb定年 /
- 地球化学 /
- 东天山
Abstract: The Tongyuliang is a newly discovered copper deposit in recent years, which is located in the Aqishan-Yamansu Carboniferous volcanic belt of eastern Tianshan, Xinjiang, NW China. However, the research for this hydrothermal copper deposit is limited. The SHRIMP zircon U-Pb dating of diorite porphyrite which is genetically related with the copper deposit is 317.7±2.4 Ma. It can be inferred that the ore-forming epoch of this deposit may be Late Carboniferous. The major elements data show that the diorite porphyrites contain 56.71%-66.03% of SiO₂, 49.75-55.29 of Mg^#, 5.15%-6.40% of Na₂O+K₂O and 4.49-53.62 of Na₂O/K₂O, and the aluminium index (A/CNK)=0.9-1.1. The diorite porphyrites are relatively enriched in sodium and alumina and belong to the low K (IAT) series. They have low ∑REE (39.56×10^-6-60.60×10^-6) and are enriched in LREE relative to HREE. The primitive mantle normalized trace elements spider diagram is characterized by Ba, U, K, Sr (large ion lithophile elements) enrichment and Nb, Ta, Ti (high field strength elements) depletion, which shows the island-arc volcanic characteristics. The (⁸⁷Sr/⁸⁶Sr)_i ratios range from 0.704 030 to 0.704 413, and ε_Nd(t) values vary from 1.02 to 6.42, which indicates that the magma source of diorite porphyrites may be derived from depleted mantle source. The geochronology, geochemistry, and isotope characteristics of diorite porphyrites suggest that the Tongyuliang copper deposit was formed in the arc setting. Combining existing geological data, the ore-bearing materials probably came from the mantle wedge, which had undergone metasomatism induced by southward subduction of Paleo-Kangguer oceanic plate. In early Late Carboniferous, the fluids which contained copper element intruded, and the Tongyuliang copper deposit formed after sub-volcanics replaced their own bodies or volcanic rocks when they reached the upper area.
- Tongyuliang copper deposit /
- diorite porphyrite /
- SHRIMP zircon U-Pb geochronology /
- geochemistry /
- eastern Tianshan

HTML全文

图 1 中亚造山带构造简图(a)和东天山地区地质矿产简图(b)

图a据Jahn et al.(2000)；图b据王京彬等(2006)

Fig. 1. Tectonic sketch of the Central Asian orogenic belt (a) and geological sketch and deposits distribution in the eastern Tianshan (b)

下载: 全尺寸图片幻灯片

图 2 铜鱼梁矿区地质简图

Fig. 2. Geological sketch of Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 3 铜鱼梁矿区52勘探线剖面

Fig. 3. The profile of No.52 exploration line in Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 4 铜鱼梁铜矿地表探槽及钻孔矿化特征

Mal.孔雀石；Bn.斑铜矿；Ccp.黄铜矿

Fig. 4. The mineralized characteristics of the exploratory trench and drillhole in Tongyuliang copper deposit

下载: 全尺寸图片幻灯片

图 5 铜鱼梁闪长玢岩手标本及镜下显微照片

Hbl.普通角闪石；Pl.斜长石；Chl.绿泥石；Mt.磁铁矿

Fig. 5. The hand specimens and photomicrographs of diorite porphyrite in Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 6 闪长玢岩锆石U-Pb谐和年龄和CL图像

Fig. 6. SHRIMP zircon U-Pb concordia diagram and zircon CL images of diorite porphyrite

下载: 全尺寸图片幻灯片

图 7 铜鱼梁矿区闪长玢岩Nb/Y-Zr/TiO₂图解(a)、SiO₂-K₂O图解(b)、Na₂O-K₂O图解(c)和A/CNK-A/NK图解(d)

图a据Winchester and Floyd(1977)；图b据Ringwood(1975)；图c据Middlemost(1972)；图d据Maniar and Piccoli(1989)

Fig. 7. Nb/Y-Zr/TiO₂ diagram (a), SiO₂-K₂O diagram (b), Na₂O-K₂O diagram (c) and A/CNK-A/NK diagram (d) of the diorite porphyrite in Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 8 闪长玢岩稀土元素球粒陨石标准化曲线(a)和微量元素原始地幔标准化曲线(b)图解

标准数值据Sun and McDonough(1989)

Fig. 8. Chondrite normalized REE diagram (a) and primitive mantle normalized trace elements spider diagram (b) of the diorite porphyrite in Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 9 铜鱼梁闪长玢岩ε_Nd(t)-(⁸⁷Sr/⁸⁶Sr)_i图解

据Zindler and Hart(1986)

Fig. 9. ε_Nd(t)-(⁸⁷Sr/⁸⁶Sr)_i diagram for the diorite porphyrite

下载: 全尺寸图片幻灯片

图 10 铜鱼梁闪长玢岩Y-Sr/Y(a)、Rb/30-Hf-3Ta(b)、Y-Nb(c)和(Y+Nb)-Rb(d)构造环境判别图

图a据Defant and Drummond(1990)；图b据Harris et al.(1986)；图c据Pearce et al.(1984)；图d据Pearce et al.(1984)

Fig. 10. The tectonic setting discrimination diagrams of Y-Sr/Y (a), Rb/30-Hf-3Ta (b), Y-Nb (c) and (Y+Nb)-Rb (d) for the diorite porphyrite in Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 11 铜鱼梁闪长玢岩Rb/Y-Nb/Y和Nb/Zr-Th/Zr图解

据Kepezhinskas et al.(1997)

Fig. 11. Rb/Y-Nb/Y and Nb/Zr-Th/Zr diagrams of the diorite porphyrite in Tongyuliang ore district

下载: 全尺寸图片幻灯片

图 12 石炭世雅满苏岛弧带构造演化-成矿模式

Fig. 12. The model for the setting evolution and mineralization of Aqishan-Yamansu island arc belt during Carboniferous

下载: 全尺寸图片幻灯片

表 1 铜鱼梁闪长玢岩SHRIMP锆石U-Pb同位素分析结果

Table 1. SHRIMP zircons U-Pb isotopic data of diorite porphyrite from Tongyuliang copper deposit

测试点	含量(10^-6)			Th/U	同位素比值						年龄(Ma)
测试点	²⁰⁶Pb_c	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb	±%	²⁰⁷Pb/²³⁵U	±%	²⁰⁶Pb/²³⁸U	±%	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁸Pb/²³²Th	1σ
J4723-10-1.1	2.42	115	263	0.4377	0.0517	4.7	0.355	4.8	0.04973	1.1	317.3	3.5	725	73	329	10
J4723-10-2.1	4.67	67	140	0.4815	0.0270	57	0.180	57	0.04890	2.3	316.0	5.6	185	452	283	53
J4723-10-3.1	4.35	87	192	0.4521	0.0460	24	0.314	24	0.04920	1.8	315.5	4.8	680	254	344	39
J4723-10-4.1	3.14	148	281	0.5266	0.0506	17	0.351	17	0.05039	1.5	321.0	4.0	653	194	355	31
J4723-10-5.1	5.62	65	126	0.5207	0.0420	40	0.280	40	0.04850	2.4	314.6	5.6	834	317	353	46
J4723-10-6.1	5.08	67	159	0.4208	0.0240	58	0.158	58	0.04870	2.6	314.0	7.2	-74	534	246	60
J4723-10-7.1	3.21	222	258	0.8602	0.0551	13	0.380	13	0.05000	1.4	319.0	3.8	831	132	336	13
J4723-10-8.1	6.81	65	100	0.6479	-	-	-	-	0.04800	4.2	313.9	9.0	-	-	282	77
J4723-10-9.1	3.14	242	241	1.0071	0.0443	19	0.307	19	0.05028	1.5	320.9	4.1	481	240	301	15
J4723-10-10.1	5.66	89	116	0.7698	0.0330	49	0.230	49	0.04980	2.4	323.6	5.9	654	328	313	33
J4723-10-11.1	7.82	95	121	0.7827	0.0320	67	0.220	67	0.04990	2.8	322.9	7.0	497	624	327	49
J4723-10-12.1	3.49	112	155	0.7197	0.0340	36	0.234	37	0.05021	1.9	323.3	4.9	362	332	302	29
J4723-10-13.1	1.50	111	373	0.2978	0.0367	19	0.252	19	0.04984	1.3	316.6	3.7	-57	278	263	44
J4723-10-14.1	0.47	69	1119	0.0614	0.0519	3.2	0.362	3.4	0.05067	1.1	319.6	3.5	394	38	346	30
J4723-10-14.1	0.89	521	475	1.0959	0.0508	7	0.349	7.1	0.04979	1.1	315.6	3.0	495	71	310	5
J4723-10-16.1	4.84	77	129	0.5953	0.0310	53	0.200	53	0.04650	2.4	301.4	5.4	430	403	300	41
注：Pb_c代表普通铅；“-”表示未检出.

下载: 导出CSV

表 2 铜鱼梁铜矿区闪长玢岩主量(%)、稀土和微量元素(10^-6)地球化学数据

Table 2. Major elements (%), trace elements and rare earth elements (10^-6) compositions of the diorite porphyrite in Tongyuliang copper deposit

样品	ZK5201-18	ZK5201-23	J4723-5	J4723-6	J4723-10	J4723-16	J4723-17
SiO₂	57.14	64.48	56.71	66.03	61.63	61.66	61.20
TiO₂	0.92	0.44	0.68	0.37	0.55	0.45	0.45
Al₂O₃	17.88	16.05	18.58	16.32	16.55	16.59	16.76
Fe₂O₃	7.09	4.22	6.47	3.72	5.14	4.81	4.95
FeO	4.30	2.33	2.97	1.57	2.48	2.69	2.61
MnO	0.11	0.07	0.13	0.07	0.08	0.08	0.08
MgO	4.12	2.33	4.04	1.87	3.16	2.73	2.82
CaO	4.15	4.67	4.07	3.40	5.22	4.98	3.97
Na₂O	4.57	4.39	5.75	5.97	4.53	5.63	5.61
K₂O	0.63	0.76	0.46	0.33	1.01	0.11	0.79
P₂O₅	0.20	0.13	0.17	0.11	0.14	0.13	0.14
LOI	3.16	2.41	2.91	1.78	1.96	2.70	3.18
TOTAL	104.27	102.29	102.93	101.55	102.44	102.55	102.55
Na₂O/K₂O	7.22	5.81	12.64	18.37	4.49	53.62	7.07
MgO^#	49.75	49.79	55.29	50.92	54.27	50.30	51.20
La	8.60	7.88	7.40	6.04	8.68	7.71	7.75
Ce	20.20	18.80	16.90	13.60	19.80	17.60	17.60
Pr	2.89	2.59	2.42	1.88	2.87	2.51	2.47
Nd	13.60	11.70	11.30	8.43	13.10	11.20	11.40
Sm	3.26	2.67	2.69	2.01	2.93	2.66	2.64
Eu	1.19	0.93	1.08	0.67	1.04	0.90	0.92
Gd	2.88	2.36	2.27	2.12	2.43	2.19	2.12
Tb	0.56	0.44	0.46	0.32	0.45	0.40	0.42
Dy	3.10	2.22	2.71	1.68	2.39	1.97	2.02
Ho	0.57	0.43	0.57	0.36	0.44	0.44	0.46
Er	1.52	1.25	1.34	0.96	1.40	1.13	1.34
Tm	0.27	0.19	0.25	0.15	0.21	0.20	0.21
Yb	1.74	1.46	1.58	1.16	1.32	1.27	1.43
Lu	0.21	0.16	0.25	0.17	0.20	0.22	0.20
Y	16.70	13.40	14.80	10.50	12.90	12.70	13.80
∑REE	60.60	53.07	51.21	39.56	57.26	50.39	50.98
La_N/Yb_N	3.55	3.87	3.36	3.73	4.72	4.35	3.89
δEu	1.16	1.10	1.30	0.99	1.16	1.10	1.15
Rb	11.00	16.10	6.88	5.24	12.30	2.27	17.20
Ba	143.00	83.80	60.30	173.00	269.00	53.40	159.00
Th	0.95	1.21	0.91	0.73	1.17	1.04	1.05
U	0.80	0.98	0.39	0.58	0.61	0.49	0.55
Nb	3.14	1.65	1.76	1.34	1.28	1.34	1.15
Ta	0.23	0.13	0.15	0.09	0.11	0.07	0.11
Pb	3.50	4.28	7.22	10.90	6.47	10.60	4.98
Sr	201.00	327.00	461.00	496.00	591.00	517.00	849.00
Zr	121.00	151.00	94.70	135.00	132.00	149.00	163.00
Hf	3.49	4.14	2.48	3.66	3.71	4.19	4.58
Sc	14.60	8.74	13.80	7.32	13.60	10.20	10.60
Sb	0.26	0.12	0.14	0.19	0.05	0.63	0.26
Cs	0.86	1.44	1.80	0.88	0.72	0.46	0.83
注：La_N/Yb_N为球粒陨石标准化值，标准化值据Sun and McDonough(1989).

下载: 导出CSV

表 3 铜鱼梁铜矿区闪长玢岩Rb、Sr、Sm、Nd同位素分析数据

Table 3. Sr and Nd isotope data of the diorite porphyrite in Tongyuliang copper deposit

样品号	Rb(10^-6)	Sr(10^-6)	⁸⁷Rb/⁸⁶Sr	⁸⁷Sr/⁸⁶Sr	2σ	Sm(10^-6)	Nd(10^-6)	¹⁴⁷Sm/¹⁴⁴Nd	¹⁴³Nd/¹⁴⁴Nd	2σ	(⁸⁷Sr/⁸⁶Sr)_i	ε_Nd(t)
ZK5201-18	13.003 6	224	0.168 3	0.704 789	0.000 010	3.168	13.569 4	0.141 1	0.512 575	0.000 007	0.704 03	1.02
J4723-5	8.373 0	525	0.046 2	0.704 499	0.000 013	2.803	11.817 0	0.143 4	0.512 592	0.000 011	0.704 29	1.26
J4723-10	12.825 2	578	0.064 2	0.704 703	0.000 013	2.764	12.187 1	0.137 1	0.512 843	0.000 008	0.704 41	6.42
注：年龄按照t=318Ma计算.

下载: 导出CSV

参考文献(117)

Belousova, E.A., Griffin, W.L., O'Reilly, S.Y., et al., 2002.Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type.Contributions to Mineralogy and Petrology, 143(5):602-622. https://doi.org/10.1007/s00410-002-0364-7
Chen, F.W., He, G.Q., Li, H.Q., 2003.Tectonic Attribute of the Qoltag Orogenic Belt in the East Tianshan Mountains, Northwestern China.Geology in China, 30(4):361-366 (in Chinese with English abstract).
Compston, W., Williams, I.S., Kirschvink, J.L., et al., 1992.Zircon U-Pb Ages for the Early Cambrian Time-Scale.Journal of the Geological Society, 149(2):171-184. https://doi.org/10.1144/gsjgs.149.2.0171
Condie, K.C., 1982.Plate Tectonics and Crustal Evolution (Second Edition).Elsevier, New York. https://doi.org/10.1016/B978-075063386-4/50008-2
Debari, S.M., 1994.Petrogenesis of the Fiambala Gabbroic Intrusion, Northwestern Argentina, a Deep Crustal Syntectonic Pluton in a Continental Magmatic Arc.Journal of Petrology, 35(3):679-713. https://doi.org/10.1093/petrology/35.3.679
Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665. https://doi.org/10.1038/347662a0
Dickinson, W.R., 1975.Potash-Depth (K-H) Relations in Continental Margin and Intra-Oceanic Magmatic Arcs.Geology, 3(2):53-56.https://doi.org/10.1130/0091-7613(1975)3<53:pkricm>2.0.co; 2 doi: 10.1130/0091-7613(1975)3<53:pkricm>2.0.co;2
Fang, W.X., Gao, Z.Q., Jia, R.X., et al., 2006.Geological Exploration Potentials and Geochemical Study on Rocks and Ores in Shaquanzi Copper and Copper-Iron Deposits, East Xinjiang.Acta Petrologica Sinica, 22(5):1413-1424 (in Chinese with English abstract).
Feng, Y.M., Zhu, B.Q., Yang, J.L., et al., 2002.Tectonics and Evolution of the Eastern Tianshan Mountains-A Brief Introduction to Tectonic Map (1:500 000) of the Eastern Tianshan Mountains of Xinjiang.Xinjiang Geology, 20(4):309-314 (in Chinese with English abstract).
Gao, Z.Q., 2002.Copper-Gold Polymetal Metallogeny and Prospecting Systematic Engineering of East Tianshan, Xinjiang, China.Central South Universitty, Changsha (in Chinese with English abstract).
Gill, J.B., 1981.Orogenic Andesites and Plate Tectonics.Springer-Verlag.New York. https://doi.org/10.1180/minmag.1982.046.339.22
Green, T.H., 1995.Significance of Nb/Ta as an Indicator of Geochemical Processes in the Crust-Mantle System.Chemical Geology, 120(3-4):347-359. https://doi.org/10.1016/0009-2541(94)00145-x
Gu, L.X., Hu, S.X., Yu, C.S., et al., 2001.Intrusive Activities during Compression-Extension Tectonic Conversion in the Bogda Intrascontinental Orogen.Acta Petrologica Sinica, 17(2):187-198 (in Chinese with English abstract).
Harris, N.B.W., Pearce, J.A., Tindle, A.G., 1986.Geochemical Characteristics of Collision-Zone Magmatism.Geological Society, London, Special Publications, 19(1):67-81. https://doi.org/10.1144/GSL.SP.1986.019.01.04
He, G.Q., Li, M.S., Liu, D.Q., et al., 1994.Paleozoic Crustal Evolution and Mineralization in Xinjiang of China.Xinjiang People's Publication House, Urumqi (in Chinese with English abstract).
He, G.Q., Liu, D.Q., Li, M.S., et al., 1995.The Five-Stage Model of Crust Evolution and Metallogenic Series of Chief Orogenic Belts in Xinjiang.Xinjiang Geology, 13(2):99-176, 178-196 (in Chinese with English abstract).
Huang, X.W., Qi, L., Wang, Y.C., et al., 2014.Re-Os Dating of Magnetite from the Shaquanzi Fe-Cu Deposit, Eastern Tianshan, NW China.Science in China (Series D), 44(4):605-616 (in Chinese with English abstract).
Hou, T., Zhang, Z.C., Santosh, M., et al., 2014.Geochronology and Geochemistry of Submarine Volcanic Rocks in the Yamansu Iron Deposit, Eastern Tianshan Mountains, NW China:Constraints on the Metallogenesis.Ore Geology Reviews, 56:487-502. https://doi.org/10.1016/j.oregeorev.2013.03.008
Jahn, B.M., Wu, F.Y., Chen, B., 2000.Granitoids of the Central Asian Orogenic Belt and Continental Growth in the Phanerozoic.In: Barbarin, B., Stephens, W.E., Bonin, B., eds., The Fourth Hutton Symposium on the Origin of Granites and Related Rocks.Geological Society of America, New York.
Ji, J.S., Tao, H.X., Zeng, Z.R., et al., 1994a.Geology and Mineralization of the Kangguertage Gold Metallogenic Belt in Eastern Tianshan.Geological Publishing House, Beijing (in Chinese).
Ji, J.S., Yang, X.K., Su, S.R., 1994b.Analysis of the Metallogenetic Conditions and Division of the Mineralizing Subbelt in the Region of Kanguertage of Easten Tianshan.Contributions to Geology and Mineral Resources Research, 9(4):49-56 (in Chinese with English abstract).
Jiang, F.Z., Qin, K.Z., Fang, T.H., et al., 2002.Types, Geological Characteristics, Metallogenic Regularity and Exploration Target of Iron Deposits in Eastern Tianshan Mountains.Xinjiang Geology, 20(4):379-383 (in Chinese with English abstract).
Johnson, K.T.M., 1998.Experimental Determination of Partition Coefficients for Rare Earth and High-Field-Strength Elements between Clinopyroxene, Garnet, and Basaltic Melt at High Pressures.Contributions to Mineralogy and Petrology, 133(1-2):60-68. https://doi.org/10.1007/s004100050437
Kepezhinskas, P., McDermott, F., Defant, M.J., et al., 1997.Trace Element and Sr-Nd-Pb Isotopic Constraints on a Three-Component Model of Kamchatka Arc Petrogenesis.Geochimica et Cosmochimica Acta, 61(3):577-600. https://doi.org/10.1016/s0016-7037(96)00349-3
Lei, R.X., Wu, C.Z., Zhang, Z.Z., et al., 2013.Geochronology, Geochemistry and Tectonic Significances of the Yamansubei Pluton in Eastern Tianshan, Northwest China.Acta Petrologica Sinica, 29(8):2653 -2664 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201308003
Li, H.M., Ding, J.H., Li, L.X., et al., 2014.The Genesis of the Skarn and the Genetic Type of the Yamansu Iron Deposit, Eastern Tianshan, Xinjiang.Acta Geologica Sinica, 88(12):2477-2489 (in Chinese with English abstract).
Li, J.Y., Wang, K.Z., Li, W.Q., et al., 2002.Tectonic Evolution since the Late Paleozoic and Mineral Prospecting in Eastern Tianshan Mountains, NW China.Xinjiang Geology, 20(4):295-301 (in Chinese with English abstract).
Li, J.Y., Wang, K.Z., Sun, G.H., et al., 2006.Paleozoic Active Margin Slices in the Southern Turfan-Hami Basin:Geological Records of Subduction of the Paleo-Asian Ocean Plate in Central Asian Regions.Acta Petrologica Sinica, 22(5):1087-1102 (in Chinese with English abstract).
Li, Y., Yang, J.S., Zhang, J., et al., 2011.Tectonical Significance of the Carboniferous Volcanic Rocks in Eastern Tianshan.Acta Petrologica Sinica, 27(1):193-209 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201101012
Ludwig, K.R., 2003.Using ISOPLOT/Ex:A Geochronological Toolkit for Microsoft Excel Version 3.0.Berkeley Geochronology Center, Berkeley, 1-40.
Luo, G.C., Yang, X.K., Cheng, H.B., 1999.Establish of Lower Carboniferous Aqishan Formation in Jueluoyage Zone of Xinjiang.Journal of Xi'an Engineering University, 21(S1):39-44 (in Chinese with English abstract).
Luo, T., Liao, Q.A., Chen, J.P., et al., 2012.LA-ICP-MS Zircon U-Pb Dating of the Volcanic Rocks from Yamansu Formation in the Eastern Tianshan, and Its Geological Significance.Earth Science, 37(6):1338-1352 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2012.141
Ma, R.S., Wang, C, Y., Ye, S.F., et al., 1993.Tectonic Framework and Crust Evolution of Eastern Tianshan Mountains.Nanjing University Press, Nanjing (in Chinese).
Macdonald, R., Hawkesworth, C.J., Heath, E., 2000.The Lesser Antilles Volcanic Chain:A Study in Arc Magmatism.Earth Science Reviews, 49(1-4):1-76. https://doi.org/10.1016/s0012-8252(99)00069-0
Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co; 2 doi: 10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
McCulloch, M.T., Gamble, J.A., 1991.Geochemical and Geodynamical Constraints on Subduction Zone Magmatism.Earth and Planetary Science Letters, 102(3-4):358-374. https://doi.org/10.1016/0012-821x(91)90029-h
Middlemost, E.A.K., 1972.A Simple Classification of Volcanic Rocks.Bulletin Volcanologique, 36(2):382-397. https://doi.org/10.1007/bf02596878
Miyashiro, A., 1974.Volcanic Rock Series in Island Arcs and Active Continental Margins.American Journal of Science, 274(4):321-355. https://doi.org/10.2475/ajs.274.4.321
Muhetaer, Z., Nijat, A., Wu, Z.N., 2015.Geochemical Characteristics of the Volcanics from the Southern Jueluotage Area and Their Constraints on the Tectonic Evolution of Paleo-Asian Ocean.Earth Science Frontiers, 22(1):238-250 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201501020
Niu, X.L., Liu, F., Feng, G.Y., et al., 2018.Discovery and Significance of Early Silurian Andesites in Wuwamen Area, Southern Margin of Central Tianshan Block.Earth Science, 43(4):1350-1366 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2018.725
Pearce, J.A., 1982.Trace Element Characteristics of Lavas from Destructive Plate Boundaries.In: Thorpe, R.S., ed., Orogenic Andesites and Related Rocks.John Wiely and Sons, Chichester.
Pearce, J.A., 1983.The Role of Subcontinental Lithosphere in Magma Genesis at Destructive Plate Margins.In: Hawkesworh, C.J., Norry, M.J., eds., Continental Basalts and Mantal Xenolith.Shiva Publishing Ltd., Nantwich.
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://doi.org/10.1093/petrology/25.4.956
Pearce, J.A., Peate, D.W., 1995.Tectonic Implications of the Composition of Volcanic Arc Magmas.Annual Review of Earth and Planetary Sciences, 23(1):251-285. https://doi.org/10.1146/annurev.ea.23.050195.001343
Qin, K.Z., Fang, T.H., Wang, S.L., et al., 2002.Plate Tectonics Division, Evolution and Metallogenic Settings in Eastern Tianshan Mountains, NW China.Xinjiang Geology, 20(4):302-308 (in Chinese with English abstract).
Ringwood, A.E., 1975.Composition and Petrology of the Earth's Mantle.McGraw-Hill, New York.https://doi.org/10.1016/0012-8252(77)90112-X
Ringwood, A.E., 1990.Slab-Mantle Interactions:3.Petrogenisis of Interplate Magmas and Structure of the Upper Mantle.Chemical Geology, 82(3-4):187-207. https://doi.org/10.1016/0009-2541(90)90081-H
Rui, Z.Y., Wang, L.S., Wang, Y.T., et al., 2002.Discussion on Metallogenic Epoch of Tuwu and Yandong Porphyry Copper Deposits in Eastern Tianshan Mountains, Xinjiang.Mineral Deposits, 21(1):16-22 (in Chinese with English abstract).
Song, A.J., Zhu, Z.X., Shi, Y., et al., 2006.SHRIMP U-Pb Dating of Zircons from the Tugutu Bulak Formation in the Western Segment of the Aqqikkuduk Fault in the East Tianshan, Xinjiang, China.Geological Bulletin of China, 25(8):953-956 (in Chinese with English abstract).
Su, C.Q., Jiang, C.Y., Xia, M.Z., et al., 2009.Geochemistry and Zircons SHRIMP U-Pb Age of Volcanic Rocks of Aqishan Formation in the Eastern Area of North Tianshan, China.Acta Petrologica Sinica, 25(4):901-915 (in Chinese with English abstract).
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
Sun.Z.Y., Long, L.L., Wang, Y.W., et al., 2016.Geochemical Characteristics and Tectonic Setting of the Volcanic Rocks in Jingxia Copper Deposit, Xinjiang.Mineral Exploration, 7(1):53-64 (in Chinese with English abstract).
Wang, D.H., Li, C.J., Chen, Z.H., et al., 2006.Metallogenic Characteristics and Direction in Mineral Search in the East Tianshan, Xinjiang, China.Geologcal Bulletin of China, 25(8):910-915 (in Chinese with English abstract).
Wang, J.B., Wang, Y.W., He, Z.J., 2006.Ore Deposits as a Guide to the Tectonic Evolution in the East Tianshan Mountains, NW China.Geology in China, 33(3):461-469 (in Chinese with English abstract).
Wang, L.S., Li, H.Q., Chen, Y.C., et al., 2005a.Geological Feature and Mineralization Epoch of Bailingshan Iron Deposit, Hami, Xinjiang, China.Mineral Deposits, 24(3):264-269 (in Chinese with English abstract).
Wang, L.S., Li, H.Q., Liu, D.Q., et al., 2005b.Geological Characteristics and Mineralization Epoch of Weiquan Silver(Copper) Deposit, Hami, Xinjiang, China.Mineral Deposits, 24(3):280-284 (in Chinese with English abstract).
Williams, I.S., 1998.U-Th-Pb Geochronology by Ion Microprobe.In: McKibben, M.A., Shanks, W.C., Ridley, W.I., eds., Applications of Microanalytical Techniques to Understanding Mineralizing Processes.Reviews in Economic Geology, 7: 1-35.
Winchester, J.A., Floyd, P.A., 1977.Geochemical Discrimination of Different Magma Series and Their Differentiation Products Using Immobile Elements.Chemical Geology, 20:325-343. https://doi.org/10.1016/0009-2541(77)90057-2
Windley, B.F., Alexeiev, D., Xiao, W.J., 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
Wood, D.A., Joron, J.L., Treuil, M., et al., 1979.Elemental and Sr Isotope Variations in Basic Lavas from Iceland and the Surrounding Ocean Floor.Contributions to Mineralogy and Petrology, 70(3):319-339. https://doi.org/10.1007/bf00375360
Wu, C.Z., Zhang, Z.Z., Zaw, K., et al., 2006.Geochronology, Geochemistry and Tectonic Significances of the Hongyuntan Granitoids in the Qoltag Area, Eastern Tianshan.Acta Petrologica Sinica, 22(5):1121-1134 (in Chinese with English abstract).
Xiao, W.J., Windley, B.F., Allen, M.B., et al., 2013.Paleozoic Multiple Accretionary and Collisional Tectonics of the Chinese Tianshan Orogenic Collage.Gondwana Research, 23(4):1316-1341. https://doi.org/10.1016/j.gr.2012.01.012
Xiao, Y., 2003.The Geological Character and Prospecting Orientation in Shaquanzi Copper Deposit of Hami, Xinjiang.Mineral Resources and Geology, 97(17):345-347 (in Chinese with English abstract).
Xu, L.L., Chai, F.M., Li, Q., et al., 2014.Geochemistry and Zircon U-Pb Age of Volcanic Rocks from the Shaquanzi Fe-Cu Deposit in East Tianshan Mountains and Their Geological Significance.Geology in China, 41(6):1771-1790 (in Chinese with English abstract).
Xu, S.Q., Zhao, T.Y., Feng, J., et al., 2011.Study on Regional Metallogenic Regularity of Marine Volcanic Type Iron Ore in the East Tianshan of Xinjiang.Xinjiang Geology, 29(2):173-177 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz201102011
Yang, X.K., Ji, J.S., Luo, G.C., et al., 1997.Plate Tectonics and Forming Law of the Metallic Ore Deposits in Eastern Tianshan.Journal of Xi'an Engineering University, 19(3):34-42 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700576227
Yang, X.K., Ji, J.S., Zhang, L.C., et al., 1998.Basic Features and Gold Prognosis of the Regional Ductile Shear Zone in Eastern Tianshan.Geotectonica et Metallogenia, 22(3):209-218 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800040863
Yuan, F., Zhou, T.F., Zhang, D.Y., et al., 2010.Source, Evolution and Tectonic Setting of the Basalts from the Native Copper Mineralization Area in Eastern Tianshan, Xinjiang.Acta Petrologica Sinica, 26(2):533-546 (in Chinese with English abstract).
Zhang, D.Y., 2012.Petrogenesis, Mineralization and Geodynamic Evolution in Jueluotage Area, Eastern Tianshan, Northwest China (Dissertation).Hefei University of Technology, Hefei (in Chinese with English abstract).
Zhang, Z.C., Chai, F.M., Xie, Q.H., 2016.High-Angle Subduction in a Thermal Structure with Warm Mantle-Cool Crust:Formation of Submarine Volcanics-Hosted Iron Deposits.Geology in China, 43(2):367-379 (in Chinese with English abstract).
Zindler, A., Hart, S., 1986.Chemical Geodynamics.Annual Review of Earth and Planetary Sciences, 14(1):493-571. https://doi.org/10.1146/annurev.ea.14.050186.002425
Zhou, J.Y., Cui, B.F., Xiao, H.L., et al., 2001.Kangguertag-Huangshan Collision Zone of Bilateral Subduction and Its Metallogenic Model and Prognosis in Xingjiang, China.Volcanology and Mineral Resources, 22(4):252-263 (in Chinese with English abstract).
Zhou, T.F., Yuan, F., Zhang, D.Y., et al., 2010.Geochronology, Tectonic Setting and Mineralization of Granitoids in Jueluotage Area, Eastern Tianshan, Xinjiang.Acta Petrologica Sinica, 26(2):478-502 (in Chinese with English abstract).
Zhu, Y.F., An, F., Feng, W.Y., et al., 2016.Geological Evolution and Huge Ore-Forming Belts in the Core Part of the Central Asian Metallogenic Region.Journal of Earth Science, 27(3):491-506. https://doi.org/10.1007/s12583-016-0673-7
Zuo, G.C., Liang, G.L., Chen, J., et al., 2006.Late Paleozoic Tectonic Framework and Evolution in the Jiabaishan Area, Qoltag, Eastern Tianshan Mountains, Northwest China.Geological Bulletin of China, 25(1-2):48-57 (in Chinese with English abstract).
陈富文, 何国琦, 李华芹, 2003.论东天山觉罗塔格造山带的大地构造属性.中国地质, 30(4):361-366. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200304007
方维萱, 高珍权, 贾润幸, 等, 2006.东疆沙泉子铜和铜铁矿床岩(矿)石地球化学研究与地质找矿前景.岩石学报, 22(5):1413-1424. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605030
冯益民, 朱宝清, 杨军录, 等, 2002.东天山大地构造及演化——1:50万东天山大地构造图简要说明.新疆地质, 20(4):309-314. doi: 10.3969/j.issn.1000-8845.2002.04.003
高珍权, 2002.东天山铜金多金属成矿学及找矿系统工程学(博士学位论文).长沙: 中南大学.
顾连兴, 胡受奚, 于春水, 等, 2001.博格达陆内碰撞造山带挤压-拉张构造转折期的侵入活动.岩石学报, 17(2):187-198. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200102002
何国琦, 李茂松, 刘德权, 等, 1994.中国新疆古生代地壳演化及成矿.乌鲁木齐:新疆人民出版社.
何国琦, 刘德权, 李茂松, 等, 1995.新疆主要造山带地壳发展的五阶段模式及成矿系列.新疆地质, 13(2):99-176, 178-196. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199500544065
黄小文, 漆亮, 王怡昌, 等, 2014.东天山沙泉子铜铁矿床磁铁矿Re-Os定年初探.中国科学(D辑), 44(4):605-616.
姬金生, 陶洪祥, 曾章仁, 等, 1994a.东天山康古尔塔格金矿地质与成矿.北京:地质出版社.
姬金生, 杨兴科, 苏生瑞, 1994b.东天山康古尔塔格金矿带成矿条件分析.地质找矿论丛, 9(4):49-56. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400058312
姜福芝, 秦克章, 方同辉, 等, 2002.东天山铁矿类型、地质特征成矿规律与找矿方向.新疆地质, 20(4):379-383. doi: 10.3969/j.issn.1000-8845.2002.04.019
雷如雄, 吴昌志, 张遵忠, 等, 2013.东天山雅满苏北岩体的年代学、地球化学及其构造意义.岩石学报, 29(8):2653-2664. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201308003
李厚民, 丁建华, 李立兴, 等, 2014.东天山雅满苏铁矿床矽卡岩成因及矿床成因类型.地质学报, 88(12):2477-2489. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201412024
李锦轶, 王克卓, 李文铅, 等, 2002.东天山晚古生代以来大地构造与矿产勘查.新疆地质, 20(4):295-301. doi: 10.3969/j.issn.1000-8845.2002.04.001
李锦轶, 王克卓, 孙桂华, 等, 2006.东天山吐哈盆地南缘古生代活动陆缘残片:中亚地区古亚洲洋板块俯冲的地质记录.岩石学报, 22(5):1087-1102. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605004
李源, 杨经绥, 张健, 等, 2011.新疆东天山石炭纪火山岩及其构造意义.岩石学报, 27(1):193-209. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201101012
罗桂昌, 杨兴科, 程宏宾, 1999.新疆觉罗塔格地区下石炭统阿奇山组的确立.西安工程学院学报, 21(S1):39-44. http://d.old.wanfangdata.com.cn/Periodical/xagcxyxb1999Z1011
罗婷, 廖群安, 陈继平, 等, 2012.东天山雅满苏组火山岩LA-ICP-MS锆石U-Pb定年及其地质意义.地球科学, 37(6):1338-1352. http://www.earth-science.net/WebPage/Article.aspx?id=2338
马瑞士, 王赐银, 叶尚夫, 等, 1993.东天山构造格架及地壳演化.南京:南京大学出版社.
木合塔尔·扎日, 尼加提·阿布都逊, 吴兆宁, 2015.觉罗塔格南缘石炭系火山岩地球化学特征及其对古亚洲洋南缘构造演化的指示意义.地学前缘, 22(1):238-250. http://d.old.wanfangdata.com.cn/Periodical/dxqy201501020
牛晓露, 刘飞, 冯光英, 等, 2018.中天山南缘乌瓦门早志留世安第斯型安山岩的发现及意义.地球科学, 43(4):1350-1366. http://www.earth-science.net/WebPage/Article.aspx?id=3773
秦克章, 方同辉, 王书来, 等, 2002.东天山古生代板块构造分区、演化与成矿地质背景研究.新疆地质, 20(4):302-308. doi: 10.3969/j.issn.1000-8845.2002.04.002
芮宗瑶, 王龙生, 王义天, 等, 2002.东天山土屋和延东斑岩铜矿床时代讨论.矿床地质, 21(1):16-22. doi: 10.3969/j.issn.0258-7106.2002.01.003
宋安江, 朱志新, 石莹, 等, 2006.东天山阿其克库都克断裂带西段土古土布拉克组锆石SHRIMP U-Pb测年.地质通报, 25(8):953-956. doi: 10.3969/j.issn.1671-2552.2006.08.010
苏春乾, 姜常义, 夏明哲, 等, 2009.北天山东段阿奇山组火山岩的地球化学特征及锆石U-Pb年龄.岩石学报, 25(4):901-915. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200904014
孙志远, 龙灵利, 王玉往, 等, 2016.新疆景峡铜矿区火山岩地球化学特征与构造环境探讨.矿产勘查, 7(1):53-64. doi: 10.3969/j.issn.1674-7801.2016.01.007
王登红, 李纯杰, 陈郑辉, 等, 2006.东天山成矿规律与找矿方向的初步研究.地质通报, 25(8):910-915. doi: 10.3969/j.issn.1671-2552.2006.08.002
王京彬, 王玉往, 何志军, 2006.东天山大地构造演化的成矿示踪.中国地质, 33(3):461-469. doi: 10.3969/j.issn.1000-3657.2006.03.002
王龙生, 李华芹, 陈毓川, 等, 2005a.新疆哈密百灵山铁矿地质特征及成矿时代.矿床地质, 24(3):264-269. http://d.old.wanfangdata.com.cn/Periodical/kcdz200503005
王龙生, 李华芹, 刘德权, 等, 2005b.新疆哈密维权银(铜)矿床地质特征和成矿时代.矿床地质, 24(3):280-284. http://d.old.wanfangdata.com.cn/Periodical/kcdz200503007
吴昌志, 张遵忠, Zaw, K., 等, 2006.东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义.岩石学报, 22(5):1121-1134. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605006
肖昱, 2003.新疆哈密市沙泉子铜矿地质特征及找矿方向.矿产与地质, 97(17):345-347. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcydz2003z1023
徐璐璐, 柴凤梅, 李强, 等, 2014.东天山沙泉子铁铜矿区火山岩地球化学特征、锆石U-Pb年龄及地质意义.中国地质, 41(6):1771-1790. doi: 10.3969/j.issn.1000-3657.2014.06.002
徐仕琪, 赵同阳, 冯京, 等, 2011.东天山海相火山岩型铁矿区域成矿规律研究.新疆地质, 29(2):173-177. doi: 10.3969/j.issn.1000-8845.2011.02.011
杨兴科, 姬金生, 罗桂昌, 等, 1997.东天山板块构造与金属矿产成矿规律.西安地质学院学报, 19(3):34-42. http://d.old.wanfangdata.com.cn/Periodical/kjysh201603026
杨兴科, 姬金生, 张连昌, 等, 1998.东天山大型韧性剪切带基本特征与金矿预测.大地构造与成矿学, 22(3):209-218. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800040863
袁峰, 周涛发, 张达玉, 等, 2010.东天山自然铜矿化带玄武岩的起源、演化及成岩构造背景.岩石学报, 26(2):533-546. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201002015
张达玉, 2012.新疆东天山觉罗塔格地区成岩成矿作用及地球动力学过程(博士学位论文).合肥: 合肥工业大学.
张招崇, 柴凤梅, 谢秋红, 2016.热幔-冷壳背景下的高角度俯冲:海相火山岩型铁矿的形成.中国地质, 43(2):367-379. doi: 10.3969/j.issn.1000-3657.2016.02.001
周济元, 崔炳芳, 肖惠良, 等, 2001.新疆康古尔-黄山对接碰撞带的存在、成矿模式及成矿预测.火山地质与矿产, 22(4):252-263. doi: 10.3969/j.issn.1671-4814.2001.04.004
周涛发, 袁峰, 张达玉, 等, 2010.新疆东天山觉罗塔格地区花岗岩类年代学、构造背景及其成矿作用研究.岩石学报, 26(2):478-502. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201002012
左国朝, 梁广林, 陈俊, 等, 2006.东天山觉罗塔格地区夹白山一带晚古生代构造格局及演化.地质通报, 25(1-2):48-57. http://d.old.wanfangdata.com.cn/Periodical/zgqydz200601009