西准噶尔别鲁阿嘎希花岗闪长岩年代学、地球化学特征及岩石成因

杨钢; 肖龙; 王国灿; 高睿; 贺新星; 张雷; 周佩

doi:10.3799/dqkx.2015.066

西准噶尔别鲁阿嘎希花岗闪长岩年代学、地球化学特征及岩石成因

doi: 10.3799/dqkx.2015.066

杨钢^{1, 2,},
肖龙^2, ,,
王国灿^{2, 3},
高睿^{2, 4},
贺新星^{2, 5},
张雷^{2, 6},
周佩²

1.
中国地震局地震研究所地震预警湖北省重点实验室，湖北武汉 430071
2.
中国地质大学地球科学学院，湖北武汉 430074
3.
中国地质大学地质过程与矿产资源国家重点实验室，湖北武汉 430074
4.
成都理工大学地球科学学院，四川成都 610059
5.
江苏省地质调查研究院，江苏南京 210018
6.
湖北省地质矿业开发有限责任公司，湖北武汉 430022

基金项目:

中国地质调查局项目 1212011220245

新疆1∶25万铁厂沟镇幅(L45C002001)与克拉玛依市幅(L45C003001)区调修测项目 1212011120502

详细信息

作者简介:
杨钢(1987-)，男，助理工程师，从事岩石学和地震地质学研究.E-mail：2639297557@qq.com

通讯作者:
肖龙，E-mail：longxiao@cug.edu.cn

中图分类号: P534
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出版历程
- 收稿日期: 2014-09-20
- 刊出日期: 2015-05-15

Geochronological, Geochemical and Petrogenesis of Bieluagaxi Granodioritic Pluton in Western Junggar

Yang Gang^{1, 2
,},
Xiao Long^{2
, ,},
Wang Guocan^{2, 3},
Gao Rui^{2, 4},
He Xinxing^{2, 5},
Zhang Lei^{2, 6},
Zhou Pei²

1.
Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
4.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
5.
Geological Survey of Jiangsu Province, Nanjing 210018, China
6.
Hubei Geological & Mining Exploration Co., Ltd., Wuhan 430022, China

摘要

摘要: 为更深入了解西准噶尔晚古生代岩浆活动和构造背景，对位于西准噶尔中部的别鲁阿嘎希岩体开展了年代学、地球化学以及Sr-Nd同位素研究，讨论了岩石成因、源区性质和构造背景.别鲁阿嘎希花岗闪长岩为钙碱性系列岩石，岩浆锆石结晶年龄为318.7±3.3 Ma.其具相对高的MgO(Mg^#=49~59)、Ni、Cr含量，富集大离子亲石元素(如K、Rb、Sr和Ba)、亏损高强场元素(如Nb、Ta、Ti)，轻重稀土元素分异不明显.Sr-Nd同位素特征显示，其有较低的初始Sr比值(0.704 297~0.704 399)，较高的ε_Nd(t)值(5.8~6.5).通过综合分析，认为在晚石炭世早期，达尔布特洋壳(板片)俯冲至地幔楔下部，俯冲洋壳板片脱水所产生的流体在上升过程中与地幔楔共同作用，底侵加热由亏损地幔形成不久的年轻地壳(由洋壳和岛弧组成)，使其部分熔融形成了别鲁阿嘎希分异I型花岗岩.
- 别鲁阿嘎希岩体 /
- 地质年代学 /
- 地球化学 /
- Sr-Nd同位素 /
- 西准噶尔 /
- 地层学
Abstract: For a better understanding of the petrogenesis and tectonic environment of the acidic intrusive rocks in Western Junggar, a study is carried out on Bieluagaxi granodioritic pluton located in the Central part of West Junggar. Its petrogenesis, magma source, tectonics setting based on petrography, zircon LA-ICP-MS U-Pb ages, whole-rock major and trace elements, and Sr-Nd isotopic compositions are discussed in detail. LA-ICP-MS U-Pb zircon data of the granodiorite give weighted ages of 318.7±3.3 Ma. Bieluagaxi granodiorite is calc-alkaline suite with high MgO(Mg^#=49-59), Ni and Cr contents. Bieluagaxi granodiorite is strongly enriched in large ion lithophile elements (LILEs, e.g. K, Rb, Sr and Ba), but it displays depletion of high field strength elements (HFSEs, e.g. Nb, Ta and Ti). In terms of Sr-Nd isotopic compositions, granodiorite has low initial ⁸⁷Sr/⁸⁶Sr ratios (0.704 297-0.704 399) and high positive ε_Nd(t) (5.8-6.5). Therefore, we suggest that the early Late Carboniferous Bieluagaxi granodioritic pluton has been generated in a subduction setting, the mantle wedge began to partially melt due to the upward fluid from the dehydration of subducting oceanic slab, resulting in the asthenospheric mafic magma underplating the lower crust. Then, the lower juvenile basaltic crust derived from the depleted mantle underwent partial melting to generate the I type granites of the Bieluagaxi granodioritic pluton.
- Bieluagaxi granodioritic pluton /
- geochronology /
- geochemistry /
- Sr-Nd isotope /
- western Junggar /
- stratigraphy

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图 1 西准噶尔地区地质简图

据苏玉平等(2006)、安芳和朱永峰(2007)和尹继元等(2012)修改

Fig. 1. Geological sketch of the western Junggar region

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图 2 别鲁阿嘎希岩体地质简图

1.库鲁木迪组上亚组上岩性段；2.库鲁木迪组上亚组中岩性段；3.库鲁木迪组上亚组下岩性段；4.花岗闪长岩；5.碱长花岗岩；6.岩墙；7.断层；8.采样点.据金成伟和徐永生(1997)以及尹继元等(2012)

Fig. 2. Geological sketch of the Bieluagaxi pluton

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图 3 各岩性镜下特征

a.正交偏光下花岗闪长岩花岗结构特征; b.单片光下花岗闪长岩花岗结构特征；c.正交偏光下闪长岩特征；d.单片光下酸性、与中性岩浆混合特征；e.单片光下石英闪长岩特征；f.正交偏光下具角闪石斑晶闪长玢岩特征；Qz.石英；Pl.斜长石；Kf.碱性长石；Am.角闪石

Fig. 3. Microphotographs of different rock types

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图 4 别鲁阿嘎希花岗闪长岩岩墙与寄主岩石野外特征(a~d)以及部分锆石CL图像和年龄值(e)

a.岩墙呈楔状侵入寄主岩石；b.酸性与中性岩浆混合带；c.不同岩相的石英闪长岩中微粒闪长岩包体；d.闪长岩墙捕获花岗闪长岩

Fig. 4. Field geological observation (a-d), representative CL images and ages of zircons (e) for the Bieluagaxi granodiorite

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图 5 别鲁阿嘎希花岗闪长岩中锆石U-Pb谐和图

Fig. 5. U-Pb concordia data of zircons for the Bieluagaxi granodiorite

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图 6 别鲁阿嘎希花岗闪长岩(Na₂O+K₂O)-SiO₂、SiO₂-AR、Na₂O-K₂O、A/NK-A/CNK、Rb/Ba-(Zr+Ce+Y)和(Na₂O+K₂O)/CaO-(Zr+Ce+Y)图解

数据来源：准噶尔I型花岗岩范围据Chen and Jahn(2004)；图a底图据Middlemost(1994)；图b底图据Peccerillo and Taylor(1976)；图e和f底图据Whalen et al.(1987)；I-I.I-I型花岗岩; S-S.S-S型花岗岩; A-A.A-A型花岗岩; FG.FG分异型I, S或M型花岗岩; OGT.OGT分异型I、S和M型花岗岩

Fig. 6. (Na₂O+K₂O)-SiO₂, SiO₂-AR, Na₂O-K₂O, A/NK-A/CNK, Rb/Ba-(Zr+Ce+Y) and (Na₂O+K₂O)/CaO-(Zr+Ce+Y) relationships of the Bieluagaxi granodiorite

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图 7 别鲁阿嘎希花岗闪长岩微量元素原始地幔标准化蛛网(a)和球粒陨石标准化REE分布模式(b)

球粒陨石标准化值和原始地幔标准化值据Sun and McDonough(1989)；引文据尹继元等(2012)

Fig. 7. Primitive mantle-normalized trace element spider diagram (a) and Chondrite-normalized REE patterns (b) for the Bieluagaxi granodiorite

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图 8 别鲁阿嘎希花岗闪长岩R₂-R₁(a)和Rb-Y+Nb(b)判别

图a底图据Bachelor and Bowden(1985); 图b底图据Pearce et al.(1984).1.地幔分异花岗岩; 2.碰撞前花岗岩; 3.碰撞后隆起花岗岩; 4.晚造山花岗岩; 5.非造山花岗岩; 6.同碰撞花岗岩; 7.后造山花岗岩.WPG.板内花岗岩; VAG.弧花岗岩; Syn-OLG.同碰撞花岗岩; ORG.洋脊花岗岩, 引文据尹继元等(2012)

Fig. 8. R₂-R₁ (a) and Rb-Y+Nb (b) discriminant diagrams of Bieluagaxi granodiorite

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表 1 别鲁阿嘎希花岗闪长岩中锆石LA-ICP-MS U-Pb定年数据

Table 1. LA-ICP-MS zircon U-Pb data for the Bieluagaxi granodiorite

测试点号	元素含量(10^-6)			Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U
测试点号	Pb	Th	U	Th/U	比值	1σ	比值	1σ	比值	1σ	年龄(Ma)	1σ	年龄(Ma)	1σ	年龄(Ma)	1σ
BL2.01	35	193	652	0.30	0.058 56	0.002 34	0.407 09	0.015 55	0.050 58	0.000 65	550	87	347	11	318	4
BL2.02	75	537	1 220	0.44	0.052 59	0.002 40	0.360 04	0.016 05	0.049 63	0.000 54	322	101	312	12	312	3
BL2.03	28	154	520	0.30	0.051 83	0.003 25	0.356 89	0.021 51	0.050 25	0.000 72	280	144	310	16	316	4
BL2.04	33	236	600	0.39	0.053 27	0.002 51	0.363 38	0.016 83	0.049 69	0.000 71	339	106	315	13	313	4
BL2.05	59	414	1 014	0.41	0.058 01	0.003 58	0.403 81	0.023 57	0.051 04	0.000 87	532	137	344	17	321	5
BL2.06	60	384	973	0.39	0.055 86	0.003 21	0.392 28	0.021 41	0.051 38	0.000 81	456	123	336	16	323	5
BL2.07	31	177	566	0.31	0.053 74	0.002 12	0.386 91	0.015 50	0.052 04	0.000 73	361	61	332	11	327	4
BL2.08	36	205	642	0.32	0.052 69	0.002 33	0.378 75	0.016 46	0.052 01	0.000 64	322	100	326	12	327	4
BL2.09	49	353	890	0.40	0.053 55	0.001 99	0.375 52	0.013 76	0.050 54	0.000 66	354	85	324	10	318	4
BL2.10	50	229	795	0.29	0.051 41	0.001 69	0.367 91	0.012 03	0.051 36	0.000 58	257	71	318	9	323	4
BL2.11	32	180	576	0.31	0.052 86	0.002 58	0.370 07	0.016 94	0.050 59	0.000 82	324	111	320	13	318	5
BL2.12	29	170	526	0.32	0.053 56	0.003 56	0.368 86	0.024 48	0.049 48	0.001 28	354	150	319	18	311	8
BL2.13	71	551	1 231	0.45	0.052 61	0.002 58	0.370 30	0.019 20	0.050 16	0.001 15	322	113	320	14	316	7

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表 2 别鲁阿嘎希花岗闪长岩主量元素(%)和微量元素(10^-6)组成

Table 2. Major (%) and trace elements (10^-6) compositions for the Bieluagaxi granodiorite

样号	BL1	BL2	BL3	BL4
SiO₂	64.2	64.3	64.5	63.8
TiO₂	0.48	0.42	0.49	0.48
Al₂O₃	15.6	17.3	16.4	17.1
FeO	3.65	2.92	3.28	3.33
Fe₂O₃	0.50	0.51	0.48	0.62
MgO	3.34	1.84	2.25	2.28
MnO	0.09	0.07	0.09	0.09
CaO	4.61	4.22	4.39	4.28
K₂O	1.70	2.25	2.29	2.39
Na₂O	3.52	4.23	3.78	4.09
P₂O₅	0.11	0.13	0.13	0.15
H₂O⁺	1.96	1.43	1.49	1.19
CO₂	0.06	0.24	0.24	0.08
Total	99.82	99.86	99.81	99.88
Mg^#	59	49	52	51
AR	1.69	1.86	1.83	1.87
La	13.0	16.3	16.2	16.1
Ce	27.2	32.6	32.2	39.0
Pr	3.30	3.73	3.67	3.76
Nd	12.3	13.7	13.5	14.9
Sm	2.79	2.87	2.93	2.99
Eu	0.89	0.93	0.88	0.94
Gd	2.56	2.43	2.59	2.58
Tb	0.41	0.37	0.42	0.40
Dy	2.56	2.26	2.53	2.35
Ho	0.54	0.45	0.48	0.46
Er	1.49	1.28	1.42	1.42
Tm	0.24	0.21	0.22	0.23
Yb	1.56	1.36	1.40	1.37
Lu	0.25	0.21	0.22	0.22
Y	14.0	12.6	13.7	12.7
Zr	103	101	103	125
Nb	4.23	3.83	4.80	3.67
Ba	480	603	681	680
Hf	3.50	3.12	3.35	3.98
Ta	0.53	0.42	0.50	0.27
Li	25.5	18.7	23.8	29.3
Sc	14.60	9.86	11.90	10.80
Cr	102.0	46.2	56.4	54.8
Co	14.2	8.90	10.8	10.6
Ni	41.9	15.9	20.4	18.1
Rb	33.1	47.9	44.8	51.8
Cs	1.38	1.92	2.42	3.42
Pb	9.52	12.0	10.8	9.42
Th	3.65	5.72	7.25	5.40
U	0.66	0.71	0.89	0.79
Sr	319	357	341	348
V	84.1	37.0	51.6	46.6
∑REE	83.03	91.35	92.27	99.45
LREE	61.99	72.60	71.93	80.26
HREE	21.05	18.75	20.34	19.19
LREE/HREE	2.95	3.87	3.54	4.18
(La/Yb)_N	6.0	8.6	8.3	8.4
Nb/Ta	8	9	10	13
Zr/Hf	29	32	31	32
Rb/Sr	0.10	0.13	0.13	0.15
注：(La/Yb)_N为La/Nb对球粒陨石标准化的值.

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表 3 别鲁阿嘎希花岗闪长岩Sr-Nd同位素分析结果

Table 3. The Sr-Nd isotopic compositions of Bieluagaxi granodiorite

样号	⁸⁷Rb/⁸⁶Sr	⁸⁷Sr/⁸⁶Sr±2σ	¹⁴⁷Sm/¹⁴⁴Nd	¹⁴³Nd/¹⁴⁴Nd±2σ	(⁸⁷Sr/⁸⁶Sr)_i	(¹⁴³Nd/¹⁴⁴Nd)_i	ε_Nd(t)	T_2DM(Ma)
BL2	0.388 537	0.706 161±8	0.126 689	0.512 787±5	0.704 399	0.512 523	5.8	610
BL4	0.431 488	0.706 254±4	0.121 195	0.512 814±5	0.704 297	0.512 561	6.5	550
注：误差为2σ；Nd和Sr同位素初始值根据318.7 Ma计算.

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