新疆西准噶尔玛依勒山地区阔依塔斯杂岩体地球化学特征及锆石U-Pb年龄

靳松; 荣桂林; 张兆祎; 李天刚; 彭朝晖; 吴立昂

新疆西准噶尔玛依勒山地区阔依塔斯杂岩体地球化学特征及锆石U-Pb年龄

1. 中国地质大学地球科学学院, 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;
2. 河北省地质调查院, 河北石家庄 050081

基金项目:

本文由教育部科技项目博士点基金(20130145120016)

中央高校基本科研业务费专项资金优秀青年基金(CUGL120280)和新疆国土资源厅地质调查项目(XJQDZ2008-01和XJQDZ2008-03)联合资助。

详细信息

作者简介:
靳松,男,1982年生,博士,工程师,主要从事岩石地球化学和区域地质矿产调查的研究;E-mail:js521@163.com。

中图分类号: P597.3;P588.12⁺1~2
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出版历程
- 收稿日期: 2015-01-12
- 修回日期: 2015-08-24
- 网络出版日期: 2023-09-26
- 刊出日期: 2016-02-24

Geochemical characteristics and zircon U-Pb ages of the Kuoyitasi complex body from Mayileshan area in western Junggar, Xinjiang

1. Faculty of Earth Science, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, Hubei, China;
2. Hebei Institute of Geological Survey, Shijiazhuang 050081, Hebei, China

Funds:

Supported by Science and Technology Project Doctoral Fund (No. 20130145120016), Central College Basic Scientific Research Business Expenses Special Funds for Outstanding Youth (No. CUGL120280), Survey Projects of Xinjiang Bureau of Land and Resources(No. XJQDZ2008-01, No. XJQDZ2008-03).

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摘要

摘要: 新疆西准噶尔北部广泛发育中酸性侵入岩,其形成时代为晚石炭世-早二叠世,岩石类型为辉石闪长岩、石英闪长岩和花岗闪长岩。阔依塔斯杂岩体的形成年龄为(297±2)Ma,SiO₂为52.40%~67.53%;高Al₂O₃,14.92%~17.85%;里特曼指数(δ)小于3.3,介于1.47~1.98;富钠贫钾,K₂O/Na₂O为0.15~0.49;铁高而镁低,FeO^T/MgO为1.01~1.69。其稀土配分模式右倾,轻重稀土分馏明显,具有微弱铕正异常。地球化学和年代学特征表明:岩体形成于后碰撞演化的晚期阶段,这一时间早于东准噶尔后碰撞的时间(二叠纪末)。该杂岩体主体可能为幔源岩浆底侵镁铁质下地壳,导致发生部分熔融的产物。
- 西准噶尔 /
- 晚石炭世-早二叠世 /
- 后碰撞 /
- 岩石成因 /
- LA-ICP-MS锆石定年
Abstract: There are large-scale intermediate-acid intrusive rocks distributed in the north of western Junggar, Xinjiang. The rocks formed during late Carboniferous to early Permian. The typical plutons include pyroxene diorite, quartz diorite and granodiorite. The Kuoyitasi intrusion is among one of them. It has SiO₂ values of 52.40%-67.53%, high Al₂O₃ content (14.92%-17.85%) and Na content, and low K and MgO content. Rittman values (δ) of the samples vary from 1.47 to 1.98, and the FeO^T/MgO values are between 1.01 and 1.69. The REE patterns are characterized by LREE enrichment and slight Eu anomalies with obvious fractionation between LREE and HREE. The geochemical characteristics suggest that the Kuoyitasi intrusion formed in a post-collisional extensional tectonic environment, and should be formed earlier than the collision time of east Junggar terrain. The rocks were probably derived from partial melting of the lower crust which was intruded by mafic magmas.
- western Junggar /
- Late-Early Pamir /
- Carboniferous /
- post-collision /
- petrogenesis

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图 1 新疆西准噶尔玛依勒山地区地质图

Figure 1. Geological sketch map of Mayileshan region in western Junggar, Xinjiang

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图 2 阔依塔斯杂岩体岩石学特征

a—石英闪长岩中含大量角闪闪长岩包体，同时可见大量后期钾长石细脉；b—花岗闪长岩内各类包体；c—花岗闪长岩中辉石闪长岩包体(内又有角闪闪长岩包体)；d—角闪岩包体；e—花岗闪长岩与辉长闪长岩间脉动接触；f—辉长闪长岩镜下照片；g—石英闪长岩镜下照片；h—花岗闪长岩镜下照片

Figure 2. Petrologic characteristics of Kuoyitasi complex body

a-Plenty of amphibole diorite inclusions in quartz diorite, with large quantities of late K-feldspar veinlits; b-Various inclusions in granodiorite; c- Gabbro diorite inclusions in granodiorite (with amphibole diorite inclusions); d-Diorite inclusion; e-Pulsation contact between granodiorite and gabbro diorite; f-Microphotograph of gabbro diorite; g- Microphotograph of quartz diorite; h- Microphotograph of granodiorite

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图 3 西准噶尔阔依塔斯杂岩体主量元素图解(a-TAS图解; b-SiO₂-K₂O图解)

Figure 3. Main elements diagram of Kuoyitasi complex body in west Junggar (a-TAS diagram ;b-SiO₂-K₂O diagram)

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图 4 西准噶尔阔依塔斯杂岩体岩石类型判别图(a-AR-SiO₂图解; b-A/CNK-A/NK图解)

Figure 4. Rock type discrimination diagram for Kuoyitasi complex body in west Junggar (a- AR-SiO₂ diagram b-A/NK-A/NCK diagram)

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图 5 西准噶尔阔依塔斯杂岩体稀土(a)和微量元素(b)元素配分型式图

Figure 5. REE and trace element patterns of Kuoyitasi complex body in west Junggar

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图 6 西准噶尔阔依塔斯杂岩体锆石CL图像

Figure 6. CL images of zircons from Kuoyitasi complex body in west Junggar

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图 7 西准噶尔阔依塔斯杂岩体中锆石U-Pb谐和图

Figure 7. U-Pb concordia diagram of zircons from Kuoyitasi complex body in west Junggar

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图 8 西准噶尔阔依塔斯杂岩体岩石成因判别图(a—Al-Na-K-Ca-Fe+Mg图解; b—A/MF-C/MF图解：A—变泥质岩的部分熔融; B—变杂砂岩的部分熔融; C—基性岩的部分熔融)

Figure 8. Genesis discrimination diagram of Kuoyitasi complex body in west Junggar (a-Al-Na-K-Ca-Fe+Mg diagram; b-A/MF-C/MF diagram)

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表 1 西准噶尔阔依塔斯杂岩体主量元素(%)、微量和稀土元素(10^-6)分析结果

Table 1 Analyses of major elements, trace elements and REE from Kuoyitasi complex body in west Junggar

样品号	P10YQ1	P10YQ2	P10YQ4	TP11YQ3	P10YQ3
岩性	辉长闪长岩	辉长闪长岩	辉长闪长岩	石英闪长岩	花岗闪长岩
SiO₂	52.4	52.76	54.6	61.64	67.53
TiO₂	0.76	0.85	0.8	0.55	0.46
Al₂O₃	15.88	17.85	17.45	16.4	14.92
Fe₂O₃	4.82	2.4	6.1	1.11	1.74
FeO	2.18	4.72	2.11	3.95	1.76
MnO	0.11	0.12	0.14	0.1	0.05
MgO	7.14	5.68	5.82	3.26	2.17
CaO	6.74	8.71	7.82	3.59	3.56
Na₂O	3.66	3.85	3.69	5.15	4.05
K₂O	1.25	0.58	0.61	1.04	1.99
P₂O₅	0.18	0.25	0.2	0.14	0.13
烧失量	1.36	1.53	0.7	2.15	1.37
H₂O⁺	0.94	0.93	0.59	1.72	1.06
H₂O^-	0.18	0.21	0.17	0.15	0.2
Total	99.48	99.29	100.04	100.95	99.73
K₂H₂O⁺/Na₂H₂O⁺	0.34	0.15	0.17	0.2	0.49
Na₂H₂O⁺+K₂H₂O⁺	4.91	4.43	4.3	6.19	6.04
A/NK	2.15	2.56	2.59	1.71	1.69
A/CKN	0.81	0.78	0.83	1.02	0.98
δ	1.76	1.87	1.55	1.98	1.47
Rb	26.9	9	10.3	32.24	68.06
Ba	444	282	347	496	643
Th	2.4	1.3	1.1	9.49	9.42
Nb	2.9	3.1	2.5	12.54	11.66
Ta	0.24	0.22	0.2	0.98	0.91
Sr	635	840	703	226	189
Zr	92	86	94	357.7	336.14
Hf	4.9	3.6	4.1	8.7	8.21
Y	14.4	14.6	13.8	24.4	22.54
Sc	20.8	26.1	22.7	4.36	4.26
Cr	192	142	206	29.2	49.2
Co	29	30	32
P	949	1263	1052	685	770
La	9.86	8.24	9.28	22.09	25.87
Ce	20.9	18.6	20.2	47.43	51.06
Pr	2.95	2.74	3.01	7.16	7.08
Nd	13.4	14	14.2	27.34	25.77
Sm	2.92	3.26	3.13	4.98	5.49
Eu	0.96	1.08	1.17	1.2	1.18
Gd	2.72	3.13	2.96	4.55	4.29
Tb	0.48	0.54	0.49	0.78	0.73
Dy	2.72	3.08	2.86	4.66	4.22
Ho	0.54	0.57	0.542	0.9	0.81
Er	1.5	1.6	1.44	2.57	2.33
Tm	0.23	0.23	0.23	0.46	0.42
Yb	1.43	1.43	1.4	3.04	2.86
Lu	0.21	0.23	0.23	0.43	0.4
ΣREE	60.73	58.67	61.14	127.6	132.52
LREE/HREE	5.18	4.43	5.03	6.34	7.25
δEu	1.03	1.02	1.15	0.76	0.72
(La/Yb)_N	4.95	4.13	4.75	5.22	6.49
(La/Sm)_N	2.18	1.63	1.91	2.86	3.04
(Gd/Yb)_N	1.57	1.81	1.75	1.24	1.24

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表 2 阔依塔斯杂岩体CIPW标准矿物及岩石化学参数一览表

Table 2 Analyses of CIPW and chemical parameters of rock from Kuoyitasi complex body

样品号	P10YQ1	P10YQ2	P10YQ4	TP11YQ3	P10YQ3
岩性	辉长闪长岩	辉长闪长岩	辉长闪长岩	石英闪长岩	花岗闪长岩
Q	5.41	1.71	4.76	13.4	25.37
Au	23.47	30.39	29.55	17.43	16.94
Ab	31.32	33.33	31.55	44.96	34.85
Or	7.47	3.51	3.64	6.34	11.96
Ne	0	0	0	0	0
C	0	0	0	0.63	0
Di	7.32	9.77	6.72	0	0.13
Hy	19.73	15.63	18.06	14.17	7.56
Ol	0	0	0	0	0
Cs	0	0	0	0	0
Il	1.46	1.65	1.54	1.08	0.89
Mt	3.39	3.42	3.72	1.66	2
Ap	0.42	0.59	0.47	0.33	0.31
Zr	0	0	0	0	0
合计	100	100	100.01	100	100.01
DI	44.2	38.55	39.95	64.7	72.18
A/CNK	0.809	0.783	0.833	1.017	0.976
SI	37.98	32.98	32.38	22.47	18.59
A.R	1.55	1.4	1.41	1.9	1.97
σ	1.76	1.87	1.55	1.98	1.47
R1	1986	1839	1971	1941	2532
R2	1403	1600	1483	895	795
F1	0.54	0.5	0.53	0.62	0.66
F2	-1.49	-1.55	-1.53	-1.48	-1.34
F3	-2.54	-2.56	-2.53	-2.6	-2.56
A/MF	0.58	0.74	0.68	1.07	1.46
C/MF	0.45	0.66	0.56	0.43	0.63

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表 3 西准噶尔阔依塔斯杂岩体LA-ICP-MS锆石U-Pb同位素测试结果

Table 3 Zircon U-Pb isotopic data obtained by LA-ICP-MS from Kuoyitasi complex body in west Junggar

测点号	含量/10^-6			Th/U	同位素比值						表面年龄/Ma
测点号	²⁰⁷Pb/²⁰⁶Pb	lσ	²⁰⁷Pb/²³⁵U	Th/U	lσ	²³⁸Pb/²³⁸U	lσ	²⁰⁷Pb/²⁰⁶Pb	lσ	²⁰⁷Pb/²³⁵U	lσ	²³⁸Pb/²³⁸U	lσ
01	3	38	45	0.84	0.0546	0.0017	0.3617	0.0059	0.0481	0.0006	395	71	314	5	303	4
02	5	65	80	0.82	0.0514	0.0009	0.3397	0.0036	0.0480	0.0006	257	41	297	3	302	4
03	3	41	49	0.82	0.0513	0.0012	0.3304	0.0050	0.0467	0.0005	256	55	290	4	294	3
04	4	25	52	0.49	0.0525	0.0010	0.3398	0.0038	0.0470	0.0009	306	44	297	3	296	6
05	7	80	109	0.74	0.0527	0.0012	0.3524	0.0033	0.0485	0.0009	318	51	307	3	305	5
06	4	33	61	0.54	0.0524	0.0012	0.3468	0.0039	0.0480	0.0009	304	50	302	3	302	5
07	4	49	62	0.78	0.0530	0.0010	0.3470	0.0040	0.0475	0.0006	330	44	302	4	299	4
08	4	47	60	0.78	0.0537	0.0015	0.3508	0.0046	0.0474	0.0006	359	62	305	4	298	4
09	4	38	61	0.63	0.0541	0.0014	0.3430	0.0040	0.0460	0.0006	376	57	299	3	290	4
10	4	33	57	0.57	0.0541	0.0011	0.3448	0.0040	0.0462	0.0009	377	47	301	3	291	6
11	5	56	80	0.71	0.0547	0.0011	0.3505	0.0038	0.0465	0.0008	399	43	305	3	293	5
12	5	58	86	0.67	0.0510	0.0012	0.3273	0.0053	0.0466	0.0006	240	56	288	5	293	4
13	6	93	109	0.86	0.0543	0.0009	0.3507	0.0031	0.0469	0.0005	381	38	305	3	295	3
14	5	22	56	0.38	0.0512	0.0015	0.3378	0.0043	0.0479	0.0006	249	69	295	4	301	4
15	9	113	155	0.73	0.0532	0.0016	0.3491	0.0027	0.0476	0.0010	339	66	304	2	299	6
16	5	47	76	0.61	0.0525	0.0012	0.3423	0.0041	0.0473	0.0007	307	54	299	4	298	4
17	5	38	72	0.53	0.0530	0.0012	0.3356	0.0038	0.0459	0.0005	327	51	294	3	290	3
18	5	39	75	0.53	0.0527	0.0012	0.3451	0.0042	0.0475	0.0009	315	52	301	4	299	5

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