新疆东准噶尔库拉比也铜镍矿床含矿岩体的成因及构造意义: 年代学、岩石地球化学和Sr⁃Nd⁃Hf同位素证据

汤贺军; 孟贵祥; 王召林; 邓震; 李成文; 祁光; 薛融晖

doi:10.3799/dqkx.2022.128

新疆东准噶尔库拉比也铜镍矿床含矿岩体的成因及构造意义: 年代学、岩石地球化学和Sr⁃Nd⁃Hf同位素证据

doi: 10.3799/dqkx.2022.128

汤贺军^{1, 2, ,},
孟贵祥^{1, 2, , ,},
王召林^{1, 2},
邓震^{1, 2},
李成文³,
祁光^{1, 2},
薛融晖^{1, 2}

1.
中国地质科学院, 北京 100037
2.
中国地质调查局中国地质科学院地球深部探测中心, 北京 100037
3.
新疆地质矿产开发局第二区域地质调查大队, 新疆昌吉 831100

基金项目:

国家重点研发计划专项 2018YFC0604002

中国地质调查局项目 DD20221643⁃6

中国地质科学院基本科研业务费项目 JKY21021

中国地质科学院基本科研业务费项目 JKY202122

详细信息

作者简介:
汤贺军（1987—），男，博士，高级工程师，主要从事矿产资源勘查及矿床学研究.ORCID：0000⁃0002⁃0720⁃3682.E⁃mail：tanghejungeo@163.com

通讯作者:
孟贵祥，ORCID：0000⁃0002⁃4473⁃057X. E⁃mail: mgxlw@126.com

中图分类号: P618
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出版历程
- 收稿日期: 2022-04-08
- 刊出日期: 2022-09-25

Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes

Tang Hejun^{1, 2
,
,},
Meng Guixiang^{1, 2
, ,
,},
Wang Zhaolin^{1, 2},
Deng Zhen^{1, 2},
Li Chengwen³,
Qi Guang^{1, 2},
Xue Ronghui^{1, 2}

1.
Chinese Academy of Geological Sciences, Beijing 100037, China
2.
China Deep Exploration Center⁃SinoProbe Center, China Geological Survey & Chinese Academy of Geological Sciences, Beijing 100037, China
3.
No. 2 Regional Geological Survey Team of the Xinjiang Bureau of Geology and Mineral Exploration and Development, Changji 831100, China

摘要

摘要: 新疆北部是中亚造山带的重要组成部分，具有众多含铜‒镍硫化物的镁铁质‒超镁铁质侵入体，是中国第二大铜镍成矿区.库拉比也铜镍矿床位于新疆阿勒泰富蕴县，是继新疆北部最大的铜镍矿（喀拉通克）发现以来，在东准噶尔北缘铜镍矿找矿的新突破.尽管前人对该矿床的地质、地球物理特征进行了总结，提出了矿床成因及找矿标志，但含矿岩体的成因及构造意义等一些关键问题尚未解决.本文对库拉比也含矿岩体进行了岩石学、年代学、岩石地球化学和Sr-Nd-Hf同位素研究.结果表明，库拉比也铜镍矿床含矿岩体主要为辉长岩，表现出轻稀土富集、重稀土亏损的右倾模式，富集大离子亲石元素Ba、U、K，亏损高场强元素Nb、Ta、Ti、Lu.辉长岩的（⁸⁷Sr/⁸⁶Sr）_i为0.703 948~0.704 109，ε_Nd（t）在5.28~5.74之间，其锆石的¹⁷⁶Hf/¹⁷⁷Hf和ε_Hf（t）变化较大，分别为0.282 851~0.283 034和+8.6~+15.1，ε_Hf（t）平均值为12.9.主微量元素及Sr-Nd-Hf同位素特征显示源区有壳源物质的加入.库拉比也含矿岩体的形成年龄（约278 Ma）与区域性铜镍矿床的矿化年龄一致（约300~270 Ma），很可能形成于后碰撞伸展环境，其初始岩浆可能与软流圈岩浆上涌并导致被交代的地幔楔的部分熔融与岩浆混合有关.库拉比也成岩成矿时代揭示了早二叠世与铜镍成矿相关的岩浆活动在东准噶尔地区广泛发生，东准噶尔北缘具有很好的铜镍找矿潜力.
- 铜镍硫化物 /
- Sr⁃Nd⁃Hf同位素 /
- 锆石U⁃Pb年代学 /
- 后碰撞伸展 /
- 东准噶尔 /
- 地球化学
Abstract: Northern Xinjiang is the second largest Cu-Ni metallogenic area in China as an important part of the Central Asian Orogenic Belt with many mafic-ultramafic intrusions containing Cu-Ni sulfide. Kulabiye Cu-Ni deposit located in Fuyun County, Xinjiang is a new breakthrough in Cu-Ni prospecting in the northern margin of East Junggar after the largest Cu-Ni deposit (Kalatongke) in northern Xinjiang. Although the geological and geophysical characteristics of the deposit have been summarized and the genesis and prospecting criteria of deposit have been put forward in the previous studies, some key problems such as the genesis and tectonic significance of the ore bearing rock mass have not been solved. In this paper, the petrology, geochronology, chemistry and Sr-Nd-Hf isotope of Kulabiye ore bearing rock mass are studied. The ore bearing rock mass of Kulabiye Cu-Ni deposit are mainly gabbro. They show the right dipping pattern of LREE enrichment and HREE loss, enriched in LILE Ba, U and K, and depleted in HFSE Nb, Ta, Ti and Lu. The (⁸⁷Sr/⁸⁶Sr)_i of gabbro is 0.703 948-0.704 109, ε_Nd(t) is between 5.28 and 5.74, ¹⁷⁶Hf/¹⁷⁷Hf and ε_Hf(t) varies greatly, ranging from 0.282 851 to 0.283 034 and +8.6-+15.1. The average value of ε_Hf(t) is 12.9. Trace elements and Sr-Nd-Hf isotopes also show the addition of shell source materials in the source area. The formation age of the Kulabiye complex (about 278 Ma) is consistent with the mineralization age of the regional Cu-Ni deposit (about 300-270 Ma). The Kulabiye complex has probably been formed in a post collisional extensional environment, which is related to the upwelling of asthenosphere magma and the partial melting and magma mixing of the metasomatic mantle wedge. The diagenetic and metallogenic age of Kulabiye also reveals that magmatic activities related to Cu-Ni mineralization in the Early Permian occurred widely in the eastern Junggar area, and the northern margin of the eastern Junggar has superior Cu-Ni prospecting potential.
- Cu⁃Ni sulfide /
- Sr⁃Nd⁃Hf isotope /
- zircon U⁃Pb geochronology /
- post collisional extension /
- East Junggar /
- geochemistry

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图 1 东准噶尔大地构造位置图（a）及库拉比也地区地质简图（b）

图a据冯京和张招崇（2009）；图b据新疆维吾尔自治区地质局，1971，1：20万恰库尔特图幅区域地质矿产报告

Fig. 1. Tectonic map of East Junggar (a) and regional geological map of Kulabiye area (b)

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图 2 库拉比也矿区1^#杂岩体地质简图（a）及矿区实测地质剖面（b）

图a据新疆地质矿产开发局第二区域地质调查大队，2016，新疆富蕴县库拉比也西铜镍矿调查评价报告；位置见图 1

Fig. 2. Geological map of Kulabiye area (a), geological profile (b) of the mining area

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图 3 库拉比也含矿岩石及矿石镜下照片

a.辉长岩；b.块状矿石；c.辉长岩镜下正交偏光照片；d.辉长岩镜下单偏光照片；e.辉长闪长岩镜下正交偏光照片；f.矿石镜下反光照片. Px.辉石；Hbl.角闪石；Pl.斜长石；Ccp.黄铜矿；Pn.镍黄铁矿；Py.黄铁矿

Fig. 3. Ore bearing rock mass of Kulabiye deposit and microscopic photos

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图 4 库拉比也含矿辉长岩锆石CL照片

Fig. 4. Zircon CL photos of Kulabiye gabbro

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图 5 库拉比也含矿辉长岩锆石U-Pb年龄

Fig. 5. Zircon U-Pb dating of Kulabiye gabbro

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图 6 库拉比也含矿辉长岩SiO₂-Na₂O+K₂O图解（a）及SiO₂-K₂O图解（b）

图a据Middlemost（1994）；图b据Rollinson（1993）

Fig. 6. SiO₂-Na₂O+K₂O (a) and SiO₂-K₂O (b) diagrams of Kulabiye gabbro

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图 7 库拉比也含矿辉长岩稀土元素配分曲线及微量元素蛛网图

图据Sun and McDonough（1989）

Fig. 7. Chondrite-normalized REE distribution patterns and continental primitive mantle-normalized multi-element distribution patterns of Kulabiye gabbro

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图 8 库拉比也辉长岩ε_Nd(t)‒(⁸⁷Sr/⁸⁶Sr)_i图解（a）及ε_Nd(t)‒t图解（b）

东准噶尔数据引自Liu and Liu（2014）；喀拉通克岩体数据引自冯延清（2018）；EM I、EM II.富集地幔；MORB.洋中脊玄武岩；HIMU.高U/Pb比值的地幔；东准噶尔数据引自Zhang et al.（2009）；阿尔泰数据引自Wang et al.（2009）；中元古代地壳、北疆地区古生代洋壳数据引自韩宝福等（2006）和Hu et al.（2000）

Fig. 8. ε_Nd(t)‒(⁸⁷Sr/⁸⁶Sr)_i (a) and ε_Nd(t)‒t (b) diagrams of Kulabiye gabbro

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图 9 库拉比也辉长岩年龄‒ε_Hf(t)图解

东准噶尔北缘320~330Ma花岗岩类引自Liu and Liu（2014）；喀拉通克岩体数据引自冯延清（2018）

Fig. 9. Age‒ε_Hf(t) diagram of Kulabiye gabbro

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表 1 库拉比也含矿辉长岩LA⁃ICP⁃MS锆石U⁃Pb分析结果

Table 1. LA⁃ICP⁃MS zircon U⁃Pb isotopic data of Kulabiye gabbro

Spot	Pb（10^‒6）	Th（10^‒6）	U（10^‒6）	Th/U	比值						年龄（Ma）
Spot	Pb（10^‒6）	Th（10^‒6）	U（10^‒6）	Th/U	²⁰⁷Pb/²⁰⁶Pb	±1σ	²⁰⁷Pb/²³⁵U	±1σ	²⁰⁶Pb/²³⁸U	±1σ	²⁰⁷Pb/²³⁵U	±1σ	²⁰⁶Pb/²³⁸U	±1σ
KL1-01	14	176	253	0.69	0.052 0	0.001 2	0.314 4	0.006 9	0.044 1	0.000 5	277.6	5.4	277.9	3.2
KL1-02	10	77	203	0.38	0.052 9	0.001 1	0.312 0	0.006 7	0.042 8	0.000 4	275.7	5.2	270.0	2.5
KL1-03	14	145	266	0.54	0.053 1	0.001 1	0.320 1	0.006 8	0.043 7	0.000 4	282.0	5.3	275.9	2.6
KL1-04	23	262	410	0.64	0.052 7	0.000 9	0.324 8	0.005 8	0.044 7	0.000 5	285.6	4.4	282.0	2.9
KL1-06	23	241	413	0.58	0.053 1	0.000 7	0.329 7	0.005 3	0.045 0	0.000 4	289.3	4.0	283.6	2.6
KL1-07	2	13	37	0.35	0.055 3	0.003 5	0.334 9	0.019 0	0.045 0	0.000 8	293.3	14.5	283.9	4.8
KL1-08	7	64	126	0.51	0.051 0	0.001 5	0.307 6	0.008 8	0.044 0	0.000 4	272.3	6.8	277.5	2.7
KL1-09	19	208	349	0.60	0.051 7	0.000 9	0.315 1	0.006 0	0.044 2	0.000 5	278.1	4.6	279.0	2.8
KL1-10	12	114	229	0.50	0.052 7	0.001 3	0.320 0	0.007 6	0.044 1	0.000 4	281.9	5.8	278.3	2.5
KL1-11	4	30	72	0.41	0.055 0	0.002 5	0.336 6	0.015 8	0.044 5	0.000 7	294.6	12.0	280.7	4.0
KL1-12	11	88	214	0.41	0.052 3	0.001 1	0.326 4	0.007 8	0.045 2	0.000 4	286.8	6.0	285.0	2.8
KL1-15	5	42	99	0.43	0.049 5	0.001 9	0.305 2	0.011 2	0.045 0	0.000 5	270.5	8.7	284.0	3.1
KL1-16	12	187	211	0.88	0.058 1	0.001 3	0.347 8	0.007 8	0.043 5	0.000 4	303.0	5.9	274.2	2.4
KL1-17	14	167	251	0.67	0.053 6	0.001 3	0.329 4	0.008 1	0.044 6	0.000 5	289.1	6.2	281.5	2.8
KL1-18	12	136	233	0.58	0.049 0	0.001 0	0.293 5	0.006 1	0.043 5	0.000 4	261.3	4.8	274.7	2.7
KL1-19	8	100	154	0.65	0.050 6	0.001 5	0.300 7	0.008 7	0.043 1	0.000 5	267.0	6.8	272.2	2.9
KL1-22	12	103	232	0.44	0.051 6	0.001 2	0.313 7	0.007 5	0.044 1	0.000 5	277.0	5.8	278.2	2.8
KL1-23	9	92	171	0.54	0.055 4	0.001 6	0.329 0	0.010 0	0.043 1	0.000 4	288.8	7.6	272.0	2.7
KL1-24	10	115	170	0.68	0.065 1	0.001 7	0.386 9	0.010 2	0.043 1	0.0005	332.1	7.5	272.1	2.9
KL1-25	16	211	274	0.77	0.054 3	0.001 1	0.334 4	0.006 7	0.044 8	0.000 5	292.9	5.1	282.3	3.0

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表 2 库拉比也含矿辉长岩主量及微量元素组成

Table 2. Chemical composition of major and trace elements of Kulabiye gabbro

样品编号	K1-2	KL-7	K1-8	ZK4002-14-3	ZK4003-14-1	ZK4003-14-7	ZK4003-15-2
岩性	辉长岩
SiO₂	49.71	50.96	48.11	47.59	46.21	47.61	46.93
Al₂O₃	15.22	15.13	14.87	14.36	15.28	14.51	14.24
CaO	4.89	4.69	2.69	6.96	7.04	7.23	6.91
TFe₂O₃	10.82	10.59	15.19	17.99	19.45	16.05	19.72
K₂O	1.92	1.55	1.96	0.76	0.76	0.74	0.72
MgO	4.48	4.38	3.88	3.76	3.28	3.77	3.75
MnO	0.19	0.18	0.18	0.17	0.16	0.17	0.17
Na₂O	4.51	4.77	4.68	3.05	3.53	3.36	3.00
P₂O₅	0.77	0.76	0.87	0.66	0.57	0.63	0.65
TiO₂	2.24	2.22	2.46	1.90	1.79	1.93	1.92
LOI	5.22	4.08	4.27	1.39	0.53	2.56	0.56
Total	99.97	99.31	99.16	98.59	98.59	98.57	98.57
A/NK	1.60	1.59	1.51	2.46	2.31	2.29	2.49
A/CNK	0.83	0.84	1.01	0.78	0.79	0.74	0.78
Mg^#	42	42	31	27	23	30	25
Sc	21.5	21.5	23.4	21.1	17.9	20.9	21.2
V	195	192	221	229	206	240	239
Co	29.4	30.0	103	114	117	86.6	132
Ni	53.4	42.8	1 740	1 974	2 125	1 403	2 438
Cu	281	174	2 380	4 253	4 968	3 193	5 046
Zn	136	135	162	136	132	155	144
Ga	22.1	21.7	21.4	18.1	18.7	19.5	18.6
Rb	27.2	22.1	25.9	12.4	10.7	10.6	11.3
Sr	786	759	621	617	640	695	607
Y	44.1	44.6	48.9	35.1	33.1	35.9	35.1
Zr	482	470	443	219	248	258	216
Nb	17.1	17.4	16.8	15.8	14.7	17.8	15.1
Cs	0.71	0.41	0.49	0.93	0.95	1.10	0.93
Ba	1 172	768	727	363	389	456	365
La	40.3	39.6	34.3	29.5	28.2	30.2	29.9
Ce	90.1	89.5	84.5	62.5	60.5	63.4	63.3
Pr	12.30	12.10	11.40	8.47	7.82	8.58	8.66
Nd	56.7	59.5	55.2	34.4	31.8	34.9	35.0
Sm	10.70	10.40	11.10	7.86	7.00	7.78	7.81
Eu	2.87	2.75	3.01	2.22	2.04	2.30	2.31
Gd	11.10	10.70	11.70	7.94	7.19	7.99	7.97
Tb	1.74	1.71	1.86	1.14	1.03	1.12	1.12
Dy	10.2	9.96	10.8	6.25	5.76	6.63	6.53
Ho	2.04	2.03	2.14	1.23	1.13	1.23	1.20
Er	5.36	5.29	5.68	3.18	3.06	3.35	3.24
Tm	0.81	0.80	0.83	0.45	0.45	0.48	0.46
Yb	4.84	4.81	4.91	2.81	2.76	3.05	2.89
Lu	0.78	0.76	0.77	0.43	0.43	0.48	0.44
Hf	9.91	9.53	8.93	4.76	5.56	5.60	4.89
Ta	1.10	1.08	1.05	0.63	0.60	0.73	0.62
Pb	4.53	6.57	3.08	46.20	40.50	34.70	53.50
Th	2.60	2.61	2.06	1.44	1.39	1.35	1.49
U	1.85	2.92	3.16	0.52	0.50	0.48	0.54
∑REE	250	250	238	168	159	171	171
（La/Yb）N	5.97	5.91	5.01	7.52	7.32	7.10	7.42
δEu	0.80	0.79	0.80	0.85	0.87	0.88	0.89

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表 3 库拉比也含矿岩辉长岩Sr⁃Nd同位素组成

Table 3. Sr⁃Nd isotopic compositions of Kulabiye gabbro

样品编号	ZK4002-14-3	ZK4003-14-1	ZK4003-14-7	ZK4003-15-2
t（Ma）	278	278	278	278
Rb	12.4	10.7	10.6	11.3
Sr	617	640	695	607
⁸⁷Rb/⁸⁶Sr	0.0863	0.070 9	0.132 8	0.081 0
⁸⁷Sr/⁸⁶Sr	0.704 292	0.704 234	0.704 638	0.704 306
2σ	0.000 004	0.000 004	0.000 005	0.000 004
（⁸⁷Sr/⁸⁶Sr）_i	0.703 948	0.703 952	0.704 109	0.703 983
Sm	7.86	7	7.78	7.81
Nd	34.4	31.8	34.9	35
¹⁴⁷Sm/¹⁴⁴Nd	0.133 1	0.133 3	0.126 6	0.138 3
¹⁴³Nd/¹⁴⁴Nd	0.512 815	0.512 816	0.512 78	0.512 816
2σ	0.000 008	0.000 007	0.000 009	0.000 007
（¹⁴³Nd/¹⁴⁴Nd）_i	0.512 571	0.512 572	0.512 548	0.512 563
ε_Nd（t）	5.73	5.74	5.28	5.56
T_DM（Ma）	637	637	651	679

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表 4 库拉比也含矿岩辉长岩锆石Lu⁃Hf同位素分析结果

Table 4. Lu⁃Hf isotopic composition of zircons from Kulabiye gabbro

样品点号	t（Ma）	¹⁷⁶Yb/¹⁷⁷Hf	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Hf/¹⁷⁷Hf	2σ	ε_Hf(0)	ε_Hf(t)	2σ	T_DM1	f_Lu/Hf
KL1-01	278	0.057 1	0.002 1	0.283 018	0.000 027	8.7	14.4	1.0	341	‒0.94
KL1-02	270	0.045 3	0.001 6	0.282 939	0.000 020	5.9	11.6	0.7	450	‒0.95
KL1-03	276	0.058 8	0.002 1	0.282 959	0.000 025	6.6	12.3	0.9	428	‒0.94
KL1-04	282	0.047 0	0.001 6	0.282 948	0.000 020	6.2	12.1	0.7	438	‒0.95
KL1-06	284	0.059 4	0.002 0	0.282 970	0.000 023	7.0	12.9	0.8	411	‒0.94
KL1-07	284	0.029 7	0.001 0	0.282 919	0.000 022	5.2	11.3	0.8	472	‒0.97
KL1-08	277	0.039 1	0.001 4	0.282 851	0.000 023	2.8	8.6	0.8	574	‒0.96
KL1-09	279	0.059 7	0.002 1	0.282 952	0.000 028	6.4	12.1	1.0	437	‒0.94
KL1-10	278	0.043 7	0.001 6	0.283 001	0.000 030	8.1	13.9	1.0	361	‒0.95
KL1-11	281	0.029 2	0.001 0	0.283 015	0.000 022	8.6	14.6	0.8	336	‒0.97
KL1-12	285	0.071 5	0.002 5	0.282 940	0.000 027	5.9	11.7	1.0	460	‒0.93
KL1-15	284	0.022 1	0.000 8	0.283 027	0.000 025	9.0	15.1	0.9	318	‒0.97
KL1-16	274	0.029 4	0.001 0	0.283 020	0.000 022	8.8	14.6	0.8	329	‒0.97
KL1-17	281	0.103 0	0.003 5	0.283 010	0.000 030	8.4	14.0	1.1	367	‒0.89
KL1-18	275	0.057 5	0.002 0	0.283 034	0.000 026	9.3	14.9	0.9	317	‒0.94
KL1-19	272	0.044 4	0.001 5	0.282 957	0.000 026	6.6	12.3	0.9	423	‒0.95
KL1-22	278	0.032 6	0.001 2	0.282 990	0.000 024	7.7	13.6	0.8	374	‒0.96
KL1-23	272	0.042 8	0.001 7	0.282 985	0.000 027	7.5	13.2	1.0	386	‒0.95
KL1-24	272	0.041 7	0.001 5	0.282 961	0.000 021	6.7	12.4	0.8	418	‒0.95
KL1-25	282	0.062 7	0.002 2	0.282 956	0.000 022	6.5	12.3	0.8	433	‒0.93

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表 5 新疆北部主要铜镍矿床年代学统计

Table 5. Chronological statistics of main Cu-Ni deposits in northern Xinjiang

地区	矿床名称	定年对象	定年方法	年龄（Ma）	资料来源
东准噶尔	喀拉通克铜镍矿	Y1岩体辉长岩	LA-ICP-MS锆石U-Pb	274~287	韩宝福等，2004
		Y3岩体苏长岩	SHRIMP锆石U-Pb	283.3±1.3	焦建刚等，2014
		Y5岩体辉长岩	SHRIMP锆石U-Pb	320.5±2.5	冯延清，2018
		G21岩体辉长岩	SHRIMP锆石U-Pb	281.1±1.5	冯延清，2018
		Y1岩体矿石	Re-Os	290.2±6.9	张作衡等，2005
		Y2岩体矿石	Re-Os	282.5±4.8	张作衡等，2005
		Y1岩体东部矿石	Re-Os	305±15	Han et al., 2007
	科克别克提铜镍矿床	辉长岩	LA-ICP-MS锆石U-Pb	290~291	张永和徐兴旺，2019
		辉长岩	LA-ICP-MS锆石U-Pb	330.3±0.7	单立华等，2018
		闪长岩	LA-ICP-MS锆石U-Pb	328.9±0.6	裴圣良等，2020
	库拉比也铜镍矿床	辉长岩	LA-ICP-MS锆石U-Pb	278±2.2	本文
东天山	黄山铜镍矿	辉橄岩	SHRIMP锆石U-Pb	283.8±3.4	秦克章等，2002
	黄山东铜镍矿	矿石	Re-Os	282±20	毛景文等，2002
	黄山东铜镍矿	辉长岩	SHRIMP锆石U-Pb	274±3	韩宝福等，2004
	香山铜镍矿	辉长岩	SHRIMP锆石U-Pb	285±1.2	秦克章等，2002
	白石泉铜镍矿	辉橄岩	LA-ICP-MS锆石U-Pb	281.2±0.9	毛启贵等，2006
	天宇铜镍矿	辉橄岩	LA-ICP-MS锆石U-Pb	290.2±3.4	唐冬梅等，2009
	黄山南铜镍矿	辉长岩	SIMS锆石U-Pb	278~282	Mao et al., 2016
	香山西矿床	辉长岩	SIMS锆石U-Pb	278.6~279.6	Shi et al., 2019
	路北铜镍矿	辉长岩	LA-ICP-MS锆石U-Pb	277.8~287.9	赵冰冰等，2018
	月牙湾铜镍矿	辉长岩	LA-ICP-MS锆石U-Pb	281~282	Sun et al., 2019

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参考文献(95)

Anderson, D. L., 1994. Komatiites and Picrites: Evidence that the 'Plume' Source is Depleted. Earth and Planetary Science Letters, 128(3-4): 303-311. https://doi.org/10.1016/0012⁃821X(94)90152⁃X
Chen, B., Jahn, B. M., 2002. Geochemical and Isotopic Studies of the Sedimentary and Granitic Rocks of the Altai Orogen of Northwest China and Their Tectonic Implications. Geological Magazine, 139(1): 1-13. https://doi.org/10.1017/s0016756801006100
Ding, R. F., Wei, X. F., Pan, D., et al., 2014. Geological Characteristics and Prospecting of AKETASI Gold Deposit in Fuyun County, Xinjiang. Mineral Deposits, 33(S1): 923-924 (in Chinese).
Dong, Y. G., Zhu, S. H., Rui, X. J., et al., 1994. The Ore⁃Forming Geochemistry and Genesis of Salbulak Gold Deposit, Xinjiang. Volcanology & Mineral Resources, 15(4): 21-34 (in Chinese with English abstract).
Feng, J., Zhang, Z. C., 2009. Geochemistry of the Intermediate⁃Acid Porphyries on Southern Margin of the Altay Mountains and Its Implications for Petrogenesis. Geological Review, 55(1): 58-72 (in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.2009.01.007
Feng, Y. Q., 2018. Copper Nickel Mineralization and Geodynamic Setting of Late Paleozoic Mafic Pluton in Karatonk, Xinjiang (Dissertation). Chang'an University, Xi'an (in Chinese with English abstract).
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
Han, B. F., Ji, J. Q., Song, B., et al., 2004. SHRIMP Zircon U⁃Pb Ages of Kalatongke No. 1 and Huangshandong Cu⁃Ni⁃Bearing Mafic⁃Ultramafic Complexes, North Xinjiang, and Geological Implications. Chinese Science Bulletin, 49(22): 2324-2328 (in Chinese with English abstract). doi: 10.1360/csb2004-49-22-2324
Han, B. F., Ji, J. Q., Song, B., et al., 2006. Late Paleozoic Vertical Growth of Continental Crust around the Junggar Basin, Xinjiang, China (PartⅠ): Timing of Post⁃Collisionai Plutonism. Acta Petrologica Sinica, 22(5): 1077-1086 (in Chinese with English abstract).
Han, B. F., Wang, S. G., Jahn, B. M., et al., 1997. Depleted⁃Mantle Source for the Ulungur River A⁃Type Granites from North Xinjiang, China: Geochemistry and Nd⁃Sr Isotopic Evidence, and Implications for Phanerozoic Crustal Growth. Chemical Geology, 138(3-4): 135-159. https://doi.org/10.1016/S0009⁃2541(97)00003⁃X
Han, C. M., Xiao, W. J., Cui, B., et al., 2006. Major Types and Characteristics of Late Paleozoic Copper Deposits in North Xinjiang, Northwest China. Acta Geologica Sinica, 80(1): 74-89 (in Chinese with English abstract). doi: 10.3321/j.issn:0001-5717.2006.01.009
Han, C. M., Xiao, W. J., Zhao, G. C., et al., 2006. Major Types, Characteristics and Geodynamic Mechanism of Upper Paleozoic Copper Deposits in Northern Xinjiang, Northwestern China. Ore Geology Reviews, 28(3): 308-328. https://doi.org/10.1016/j.oregeorev.2005.04.002
Han, C. M., Xiao, W. J., Zhao, G. C., et al., 2007. Re⁃Os Dating of the Kalatongke Cu⁃Ni Deposit, Altay Shan, NW China, and Resulting Geodynamic Implications. Ore Geology Reviews, 32(1-2): 452-468. https://doi.org/10.1016/j.oregeorev.2006.11.004
Hawkesworth, C. J., Gallagher, K., Hergt, J. M., et al., 1993. Trace Element Fractionation Processes in the Generation of Island Arc Basalts. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 342(1663): 179-193. https://doi.org/10.1098/rsta.1993.0013
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). doi: 10.3969/j.issn.1000-0569.2007.10.025
Hu, A. Q., Jahn, B. M., Zhang, G. X., et al., 2000. Crustal Evolution and Phanerozoic Crustal Growth in Northern Xinjiang: Nd Isotopic Evidence. Part I. Isotopic Characterization of Basement Rocks. Tectonophysics, 328(1-2): 15-51. https://doi.org/10.1016/S0040⁃1951(00)00176⁃1
Jiao, J. G., Wang, Y., Qian, Z. Z., et al., 2014. Tentative Discussion on Rock⁃Forming and Ore⁃Forming Mechanism of Kalatongke Cu⁃Ni Sulfide Deposit and Chronology of Kalatongke Y9 Intrusion. Mineral Deposits, 33(4): 675-688 (in Chinese with English abstract). doi: 10.3969/j.issn.0258-7106.2014.04.001
Li, D., He, D. F., Santosh, M., et al., 2014. Petrogenesis of Late Paleozoic Volcanics from the Zhaheba Depression, East Junggar: Insights into Collisional Event in an Accretionary Orogen of Central Asia. Lithos, 184-187: 167-193. https://doi.org/10.1016/j.lithos.2013.10.003
Li, J. Y., 2004. Late Neoproterozoic and Paleozoic Tectonic Framework and Evolutionof Eastern Xinjiang, NW China. Geological Review, 50(3): 304-322 (in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.2004.03.015
Liang, P., Chen, H. Y., Hollings, P., et al., 2016. The Paleozoic Tectonic Evolution and Metallogenesis of the Northern Margin of East Junggar, Central Asia Orogenic Belt: Geochronological and Geochemical Constraints from Igneous Rocks of the Qiaoxiahala Fe⁃Cu Deposit. Journal of Asian Earth Sciences, 130: 23-45. https://doi.org/10.1016/j.jseaes.2016.08.001
Liang, X. R., Wei, G. J., Li, X. H., et al., 2003. Precise Measurement of ¹⁴³Nd/¹⁴⁴Nd and Sm/Nd Ratios Using Multiple Collectors Inductively Coupled Plasma Mass Spectrometer (MC ICPMS). Geochimica, 32(1): 91-96 (in Chinese with English abstract). doi: 10.3321/j.issn:0379-1726.2003.01.013
Liu, W., Liu, X. J., Liu, L. J., 2013. Underplating Generated A⁃ and I⁃Type Granitoids of the East Junggar from the Lower and the Upper Oceanic Crust with Mixing of Mafic Magma: Insights from Integrated Zircon U⁃Pb Ages, Petrography, Geochemistry and Nd⁃Sr⁃Hf Isotopes. Lithos, 179: 293-319. https://doi.org/10.1016/j.lithos.2013.08.009
Liu, X. J., Liu, W., 2014. Source Characteristics and Tectonic Setting of the Early and Middle Devonian Volcanic Rocks in the North Junggar, Northwest China: Insights from Nd⁃Sr Isotopes and Geochemistry. Lithos, 184-187: 27-41. https://doi.org/10.1016/j.lithos.2013.10.015
Long, L. L., Wang, Y. W., Du, A. D., et al., 2011. Molybdenite Re⁃Os Age of Xilekuduke Cu⁃Mo Deposit in Xinjiang and Its Geological Significance. Mineral Deposits, 30(4): 635-644 (in Chinese with English abstract). doi: 10.3969/j.issn.0258-7106.2011.04.004
Mao, J. W., Yang, J. M., Han, C. M., et al., 2002. Metallogenic Systems of Polymetallic Copper and Gold Deposits and Related Metallogenic Geodynamic Model in Eastern Tianshan, Xinjiang. Earth Science, 27(4): 413-424 (in Chinese with English abstract). doi: 10.3321/j.issn:1000-2383.2002.04.010
Mao, Y. J., Qin, K. Z., Tang, D. M., et al., 2016. Crustal Contamination and Sulfide Immiscibility History of the Permian Huangshannan Magmatic Ni⁃Cu Sulfide Deposit, East Tianshan, NW China. Journal of Asian Earth Sciences, 129: 22-37. https://doi.org/10.1016/j.jseaes.2016.07.028
Mao, Q. G., Xiao, W. J., Han, C. M., et al., 2006. Zircon U⁃Pb Age and the Geochemistry of the Baishiquan Mafic⁃Ultramafic Complex in the Eastern Tianshan, Xinjiang Province: Constraints on the Closure of the Paleo⁃Asian Ocean. Acta Petrologica Sinica, 22(1): 153-162 (in Chinese with English abstract).
McClay, K. R., 1983. Structural Evolution of the Sullivan Fe⁃Pb⁃Zn⁃Ag Orebody, Kimberley, British⁃Columbia, Canada. Economic Geology, 78(7): 1398-1424. https://doi.org/10.2113/gsecongeo.78.7.1398
Middlemost, E. A. K., 1994. Naming Materials in the Magma/Igneous Rock System. Earth⁃Science Reviews, 37(3-4): 215-224. https://doi.org/10.1016/0012⁃8252(94)90029⁃9
Pei, S. L., Ding, R. F., Shan, L. H., et al., 2020. Zircon U⁃Pb Geochronology and Geochemistry of the Kekebieketi Basic Complex in Fuyun, Xinjiang and the Geological Significance. Earth Science Frontiers, 27(4): 184-198 (in Chinese with English abstract).
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). doi: 10.3969/j.issn.1000-8845.2002.04.002
Ripley, E. M., Li, C. S., 2013. Sulfide Saturation in Mafic Magmas: Is External Sulfur Required for Magmatic Ni⁃Cu⁃(PGE) Ore Genesis? Economic Geology, 108(1): 45-58. https://doi.org/10.2113/econgeo.108.1.45
Rollinson, H., 1993. Using Geochemical Data: Evaluation, Presentation, Interpretation. Longman Scientific and Technical, London.
Scherer, E. E., Cameron, K. L., Blichert⁃Toft, J., 2000. Lu⁃Hf Garnet Geochronology: Closure Temperature Relative to the Sm⁃Nd System and the Effects of Trace Mineral Inclusions. Geochimica et Cosmochimica Acta, 64(19): 3413-3432. https://doi.org/10.1016/S0016⁃7037(00)00440⁃3
Seat, Z., Beresford, S. W., Grguric, B. A., et al., 2009. Reevaluation of the Role of External Sulfur Addition in the Genesis of Ni⁃Cu⁃PGE Deposits: Evidence from the Nebo⁃Babel Ni⁃Cu⁃PGE Deposit, West Musgrave, Western Australia. Economic Geology, 104(4): 521-538. https://doi.org/10.2113/gsecongeo.104.4.521
Shan, L. H., Ding, R. F., Wei, X. F., et al., 2018. SHRIMP Zircon U⁃Pb Dating for Rocks and Its Geological Significance in Kekebieketi District of Fuyun County, Xinjiang. Mineral Exploration, 9(5): 777-792 (in Chinese with English abstract). doi: 10.3969/j.issn.1674-7801.2018.05.002
Shi, Y., Wang, Y. W., Wang, J. B., et al., 2019. Petrogenesis and Metallogenesis of the Yaxi Gabbroic Intrusion Associated with Fe⁃Ti⁃V⁃P Ores in Eastern Tianshan, NW China. Ore Geology Reviews, 111: 103000. https://doi.org/10.1016/j.oregeorev.2019.103000
Si, C. Q., Liu, W., Liu, X. J., 2022. Generation Mechanism of Carboniferous Arc Magma and Cumulate Column in Middle Arc Crust, Hadanxun of Northeast Junggar. Earth Science, 47(1): 325-341 (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, Y., Wang, J. B., Lü, X. Q., et al., 2019. Geochronology, Petrogenesis and Tectonic Implications of the Newly Discovered Cu⁃Ni Sulfide⁃Mineralized Yueyawan Gabbroic Complex, Kalatag District, Northwestern Eastern Tianshan, NW China. Ore Geology Reviews, 109: 598-614. https://doi.org/10.1016/j.oregeorev.2019.05.009
Tang, D. M., Qin, K. Z., Sun, H., et al., 2009. Lithological, Chronological and Geochemical Characteristics of Tianyu Cu⁃Ni Deposit: Constraints on Source and Genesis of Mafic⁃Ultramafic Intrusions in Eastern Xinjiang. Acta Petrologica Sinica, 25(4): 817-831 (in Chinese with English abstract).
Tang, H. J., Meng, G. X., Wang, Z. L., et al., 2020. Zircon U⁃Pb Geochronology of the Newly Discovered Kulabiye Cu⁃Ni Sulfide⁃Mineralized Gabbroic Complex, East Junggar Basin in Xinjiang, China. China Geology (English Edition), (3): 490-492. https://doi.org/10.31035/cg2020045
Tang, H. J., Meng, G. X., Wu, Z. H., et al., 2022. Petrogenesis and Tectonic Implications of A⁃Type Granites in Zhaheba in the East Junggar Region of Xinjiang, China: Evidence from Geochronology, Geochemistry and Sr⁃Nd Isotopic Compositions. Acta Geologica Sinica ⁃ English Edition, 96(3): 938-953. https://doi.org/10.1111/1755⁃6724.14802
Tang, H. J., Meng, G. X., Yang, Y. Q., et al., 2018. Geological and Geochemical Features of the Permian Bimodal Volcanic Rocks in the Qiakurtu Area, Eastern Junggar Basin, Xinjiang, and Their Tectonic Significance. Geological Review, 64(6): 1393-1412 (in Chinese with English abstract).
Taylor, S. R., McLennan, S. M., 1985. The Continental Crust: Its Composition and Evolution. The Journal of Geology, 94(4): 57-72.
Wan, B., Xiao, W. J., Han, C. M., et al., 2014. Re⁃Os Molybdenite Age of the Cu⁃Mo Skarn Ore Deposit at Suoerkuduke in East Junggar, NW China and Its Geological Significance. Ore Geology Reviews, 56: 541-548. https://doi.org/10.1016/j.oregeorev.2013.02.011
Wang, J. B., Xu, X., 2006. Post⁃Collisional Tectonic Evolution and Metallogenesis in Northern Xinjiang, China. Acta Geologica Sinica, 80(1): 23-31 (in Chinese with English abstract).
Wang, T., Jahn, B. M., Kovach, V. P., et al., 2009. Nd⁃Sr Isotopic Mapping of the Chinese Altai and Implications for Continental Growth in the Central Asian Orogenic Belt. Lithos, 110(1-4): 359-372. https://doi.org/10.1016/j.lithos.2009.02.001
Wang, X., Cao, J., Zhang, G. Z., 2021. Origin of Ore⁃Forming Magmas Associated with Ni⁃Cu Sulfide Deposits in Orogenic Belts: Case Study of Permian Huangshannan Magmatic Ni⁃Cu Sulfide Deposit, East Tianshan, NW China. Earth Science, 46(11): 3829-3849 (in Chinese with English abstract).
Wei, G. J., Liang, X. R., Li, X. H., et al., 2002. Precise Measurement of Sr Isotopic Composition of Liquid and Solid Base Using (LP)MC ICPMS. Geochimica, 31(3): 295-299 (in Chinese with English abstract). doi: 10.3321/j.issn:0379-1726.2002.03.011
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
Wilson, B. M., 1989. Igneous Petrogenesis a Global Tectonic Approach. Springer, Dordrecht. https://doi.org/10.1007/978⁃1⁃4020⁃6788⁃4
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).
Xiao, W. J., Han, C. M., Yuan, C., et al., 2006. Unique Carboniferous⁃Permian Tectonic⁃Metallogenic Framework of Northern Xinjiang (NW China): Constraints for the Tectonics of the Southern Paleoasian Domain. Acta Petrologica Sinica, 22(5): 1062-1076 (in Chinese with English abstract).
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., Yuan, C., et al., 2009. Paleozoic Multiple Subduction⁃Accretion Processes of the Southern Altaids. American Journal of Science, 309(3): 221-270. https://doi.org/10.2475/03.2009.02
Xue, C. J., Zhao, Z. F., Wu, G. G., et al., 2010. The Multiperiodic Superimposed Porphyry Copper Mineralization in Central Asian Tectonic Region: a Case Study of Geology, Geochemistry and Chronology of Halasu Copper Deposit, Southeastern Altai, China. Earth Science Frontiers, 17(2): 53-82 (in Chinese with English abstract).
Yan, S. H., Teng, R. L., Wang, Y. T., et al., 2006. ⁴⁰Ar/³⁹Ar Dating of the Bu'ergen Gold⁃Bearing Shear Zone on the Southern Margin of the Altay Mountains, Xinjiang, and Its Significance. Geology in China, 33(3): 648-655 (in Chinese with English abstract).
Zhang, Q., Pan, G. Q., Li, C. D., et al., 2007. Does Fractional Crystallization Occur in Granitic Magma? Some Crucial Questions on Granite Study (2). Acta Petrologica Sinica, 23(6): 1239-1251 (in Chinese with English abstract).
Zhang, Y., Xu, X. W., 2019. The Keke Gabbro in Qinghe County of Xinjiang: Records from Partial Meltingmagma of the Oxidized Mantle Wedge. Acta Geologica Sinica, 93(5): 1037-1054 (in Chinese with English abstract).
Zhang, Z. C., Mao, J. W., Cai, J. H., et al., 2008. Geochemistry of Picrites and Associated Lavas of a Devonian Island Arc in the Northern Junggar Terrane, Xinjiang (NW China): Implications for Petrogenesis, Arc Mantle Sources and Tectonic Setting. Lithos, 105(3-4): 379-395. https://doi.org/10.1016/j.lithos.2008.05.013
Zhang, Z. C., Zhou, G., Kusky, T. M., et al., 2009. Late Paleozoic Volcanic Record of the Eastern Junggar Terrane, Xinjiang, Northwestern China: Major and Trace Element Characteristics, Sr⁃Nd Isotopic Systematics and Implications for Tectonic Evolution. Gondwana Research, 16(2): 201-215. https://doi.org/10.1016/j.gr.2009.03.004
Zhang, Z. H., Chai, F. M., Du, A. D., et al., 2005. Re⁃Os Dating and Ore⁃Forming Material Tracing of the Karatungk Cu⁃Ni Sulfide Deposit in Northern Xinjiang. Acta Petrologica et Mineralogica, 24(4): 285-293 (in Chinese with English abstract).
Zhao, B. B., Deng, Y. F., Zhou, T. F., et al., 2018. Petrogenesis of the Baixintan Ni⁃Cu Sulfide⁃Bearing Mafic⁃Ultramafic Intrusion, East Tianshan: Evidence from Geochronology, Petrogeochemistry and Sr⁃Nd Isotope. Acta Petrologica Sinica, 34(9): 2733-2753 (in Chinese with English abstract).
丁汝福, 卫晓锋, 潘东, 等, 2014. 新疆富蕴县阿克塔斯金矿地质特征及找矿前景. 矿床地质, 33(S1): 923-924.
董永观, 朱韶华, 芮行健, 等, 1994. 新疆萨尔布拉克金矿矿床地球化学及矿床成因. 火山地质与矿产, 15(4): 21-34. https://www.cnki.com.cn/Article/CJFDTOTAL-HSDZ199404002.htm
冯京, 张招崇, 2009. 阿尔泰山南缘中‒酸性斑岩的地球化学特征及其岩石成因探讨. 地质论评, 55(1): 58-72. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200901009.htm
冯延清, 2018. 新疆喀拉通克晚古生代镁铁质岩体铜镍成矿作用与地球动力学背景(博士学位论文). 西安: 长安大学.
韩宝福, 季建清, 宋彪, 等, 2004. 新疆喀拉通克和黄山东含铜镍矿镁铁‒超镁铁杂岩体的SHRIMP锆石U⁃Pb年龄及其地质意义. 科学通报, 49(22): 2324-2328. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB20042200C.htm
韩宝福, 季建清, 宋彪, 等, 2006. 新疆准噶尔晚古生代陆壳垂向生长(Ⅰ): 后碰撞深成岩浆活动的时限. 岩石学报, 22(5): 1077-1086. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605003.htm
韩春明, 肖文交, 崔彬, 等, 2006. 新疆北部晚古生代铜矿床主要类型和地质特征. 地质学报, 80(1): 74-89. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200601010.htm
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
焦建刚, 王勇, 钱壮志, 等, 2014. 新疆喀拉通克铜镍硫化物矿床Y9岩体年代学与成岩成矿机制探讨. 矿床地质, 33(4): 675-688. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201404001.htm
李锦轶, 2004. 新疆东部新元古代晚期和古生代构造格局及其演变. 地质论评, 50(3): 304-322. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200403015.htm
梁细荣, 韦刚健, 李献华, 等, 2003. 利用MC⁃ICPMS精确测定¹⁴³Nd/¹⁴⁴Nd和Sm/Nd比值. 地球化学, 32(1): 91-96. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200301012.htm
龙灵利, 王玉往, 杜安道, 等, 2011. 新疆希勒库都克铜钼矿床辉钼矿Re⁃Os年龄及其地质意义. 矿床地质, 30(4): 635-644. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201104005.htm
毛景文, 杨建民, 韩春明, 等, 2002. 东天山铜金多金属矿床成矿系统和成矿地球动力学模型. 地球科学, 27(4): 413-424. http://www.earth-science.net/article/id/1140
毛启贵, 肖文交, 韩春明, 等, 2006. 新疆东天山白石泉铜镍矿床基性‒超基性岩体锆石U⁃Pb同位素年龄、地球化学特征及其对古亚洲洋闭合时限的制约. 岩石学报, 22(1): 153-162. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200601016.htm
裴圣良, 丁汝福, 单立华, 等, 2020. 新疆富蕴科克别克提基性杂岩体锆石U⁃Pb年代学、地球化学及其地质意义. 地学前缘, 27(4): 184-198.
秦克章, 方同辉, 王书来, 等, 2002. 东天山板块构造分区、演化与成矿地质背景研究. 新疆地质, 20(4): 302-308. https://www.cnki.com.cn/Article/CJFDTOTAL-XJDI200204002.htm
单立华, 丁汝福, 卫晓锋, 等, 2018. 新疆富蕴县科克别克提一带岩体SHRIMP锆石U⁃Pb年龄及其地质意义. 矿产勘查, 9(5): 777-792. https://www.cnki.com.cn/Article/CJFDTOTAL-YSJS201805003.htm
司翠芹, 刘伟, 刘秀金, 2022. 东北准噶尔哈旦逊石炭纪弧岩浆及堆晶柱形成机制. 地球科学, 47(1): 325-341. doi: 10.3799/dqkx.2021.044
唐冬梅, 秦克章, 孙赫, 等, 2009. 天宇铜镍矿床的岩相学、锆石U⁃Pb年代学、地球化学特征: 对东疆镁铁‒超镁铁质岩体源区和成因的制约. 岩石学报, 25(4): 817-831. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200904008.htm
汤贺军, 孟贵祥, 杨岳清, 等, 2018. 新疆东准噶尔恰库尔图地区二叠纪双峰式火山岩地质地球化学特征及构造意义. 地质论评, 64(6): 1393-1412. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201806007.htm
王京彬, 徐新, 2006. 新疆北部后碰撞构造演化与成矿. 地质学报, 80(1): 23-31. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200601002.htm
王旋, 曹俊, 张盖之, 2021. 造山带铜镍硫化物矿床的岩浆起源: 以东天山黄山南铜镍矿床为例. 地球科学, 46(11): 3829-3849. doi: 10.3799/dqkx.2021.015
韦刚健, 梁细荣, 李献华, 等, 2002. (LP)MC⁃ICPMS方法精确测定液体和固体样品的Sr同位素组成. 地球化学, 31(3): 295-299. https://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200203010.htm
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
肖文交, 韩春明, 袁超, 等, 2006. 新疆北部石炭纪‒二叠纪独特的构造‒成矿作用: 对古亚洲洋构造域南部大地构造演化的制约. 岩石学报, 22(5): 1062-1076. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605002.htm
薛春纪, 赵战锋, 吴淦国, 等, 2010. 中亚构造域多期叠加斑岩铜矿化: 以阿尔泰东南缘哈腊苏铜矿床地质、地球化学和成岩成矿时代研究为例. 地学前缘, 17(2): 53-82. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201002012.htm
闫升好, 滕荣丽, 王义天, 等, 2006. 新疆布尔根含金剪切带的⁴⁰Ar/³⁹Ar年龄及其地质意义. 中国地质, 33(3): 648-655. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200603022.htm
张旗, 潘国强, 李承东, 等, 2007. 花岗岩结晶分离作用问题: 关于花岗岩研究的思考之二. 岩石学报, 23(6): 1239-1251. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200706001.htm
张永, 徐兴旺, 2019. 新疆青河县科克辉长岩体: 氧化地幔楔部分熔融岩浆的记录. 地质学报, 93(5): 1037-1054. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201905004.htm
张作衡, 柴凤梅, 杜安道, 等, 2005. 新疆喀拉通克铜镍硫化物矿床Re⁃Os同位素测年及成矿物质来源示踪. 岩石矿物学杂志, 24(4): 285-293. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200504004.htm
赵冰冰, 邓宇峰, 周涛发, 等, 2018. 东天山白鑫滩含铜镍矿镁铁‒超镁铁岩体的岩石成因: 年代学、岩石地球化学和Sr⁃Nd同位素证据. 岩石学报, 34(9): 2733-2753. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201809015.htm

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新疆东准噶尔库拉比也铜镍矿床含矿岩体的成因及构造意义: 年代学、岩石地球化学和Sr⁃Nd⁃Hf同位素证据

doi: 10.3799/dqkx.2022.128

作者简介:
汤贺军（1987—），男，博士，高级工程师，主要从事矿产资源勘查及矿床学研究.ORCID：0000⁃0002⁃0720⁃3682.E⁃mail：tanghejungeo@163.com

通讯作者:
孟贵祥，ORCID：0000⁃0002⁃4473⁃057X. E⁃mail: mgxlw@126.com

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Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes

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新疆东准噶尔库拉比也铜镍矿床含矿岩体的成因及构造意义: 年代学、岩石地球化学和Sr⁃Nd⁃Hf同位素证据

doi: 10.3799/dqkx.2022.128

作者简介: 汤贺军（1987—），男，博士，高级工程师，主要从事矿产资源勘查及矿床学研究.ORCID：0000⁃0002⁃0720⁃3682.E⁃mail：tanghejungeo@163.com

通讯作者: 孟贵祥，ORCID：0000⁃0002⁃4473⁃057X. E⁃mail: mgxlw@126.com

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Genesis and Tectonic Significance of Ore Bearing Rock Mass in Kulabiye Cu⁃Ni Deposit, East Junggar, Xinjiang: Evidence from Chronology, Geochemistry and Sr⁃Nd⁃Hf Isotopes

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作者简介:
汤贺军（1987—），男，博士，高级工程师，主要从事矿产资源勘查及矿床学研究.ORCID：0000⁃0002⁃0720⁃3682.E⁃mail：tanghejungeo@163.com

通讯作者:
孟贵祥，ORCID：0000⁃0002⁃4473⁃057X. E⁃mail: mgxlw@126.com