新疆东准噶尔地区老君庙岩群时代厘定、原岩恢复及对基底的指示意义

杨硕; 刘阁; 靳刘圆; 郑海峰; 王盛栋

新疆东准噶尔地区老君庙岩群时代厘定、原岩恢复及对基底的指示意义

1.
新疆地质调查院, 新疆乌鲁木齐 830000

2.
中国地质科学院地球物理地球化学勘查研究所, 河北廊坊 065000

基金项目:
中央返还两权价款项目（编号：A16-1-LQ17）和中国地质调查局项目《中国新疆区域地质调查片区总结与服务产品开发》（编号：DD20160345-04）、《新疆矿产资源调查成果综合集成与服务产品开发》（编号：DD20160346）

详细信息

作者简介: 杨硕(1988-), 男, 硕士, 构造地质学专业, 从事区域地质调查工作。E-mail:yangshxs@126.com

中图分类号: P534.41;P597⁺.3

收稿日期: 2018-07-20

修回日期: 2018-10-22

刊出日期: 2020-01-25

Dating and reconstruction of protoliths of the Laojunmiao Group and its indications for basement in eastern Junggar, Xinjiang

1.
Institute of Gelogical Surveyof Xinjiang, Urumqi 830000, Xinjiang, China

2.
Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, Hebei, China

Received Date: 20 July 2018

Revised Date: 22 October 2018

Publish Date: 25 January 2020

摘要

摘要:
老君庙岩群出露于准噶尔盆地东北緣，发育一套高绿片岩相-角闪岩相变质岩，其形成时代和构造背景长期以来存在争议。对钾长糜棱片岩进行锆石U-Pb定年，结果显示老君庙岩群年龄值主要集中在500~54OMa之间，少数为新元古代早期（740~920Ma），根据最年轻的峰值年龄（约520Ma）将老君庙岩群时代重新厘定为早寒武世。利用岩石地球化学特征对老君庙岩群进行原岩恢复，显示其具有大陆壳的特征，原岩建造类似复理石建造，其形成的构造环境应属陆緣海环境。关于准噶尔盆地基底属性的问题一直没有定论，通过本次研究，结合区域资料，认为东准噶尔地区存在前寒武基底。
- 老君庙岩群 /
- 锆石U-Pb /
- 原岩恢复 /
- 东准噶尔 /
- 基底
Abstract:
The Laojunmiao Group which is exposed on the northeastern margin of the Runggar basin consists of metamorphic complex of high greenschist facies to amphibolite facies. Its formation age and tectonic setting has been controversial for a long time. Zircon U-Pb dating of K-feldspar mylonite schist yielded a number of ages which are mostly concentrated on 500~544Ma with, a few belonging to early Neoproterozoic(740~920Ma).According to the youngest peak age(~520Ma), the age of Laojunmiao Group is redefined as early Cambrian.The lithogeochemical characteristics of Laojunmiao Group show that it has the characteristics of the continental crust, the protoliths formation is similar to a set of flysch formation and its tectonic environment should belong to the continental margin sea.As the problem in regard of the basement properties of funggar basin has not been conclusive yet, the results of this study in combination with, regional data can prove the existence of Precambrian basement in Eastern Junggar.
- Laojunmiao Group /
- zircon U-Pb /
- reconstruction of protoliths /
- Eastern Junggar /
- basement

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图 1 研究区地质简图(据参考文献①修改)

Figure 1.

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图 2 老君庙岩群锆石阴极发光(CL)图像、测点及年龄

Figure 2.

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图 3 老君庙岩群锆石U-Pb谐和图(a)及年龄概率分布直方图(b)

Figure 3.

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图 4 老君庙岩群稀土元素配分模式图(球粒陨石标准化值据参考文献[25])

Figure 4.

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图 5 老君庙岩群微量元素蛛网图(原始地幔标准化值据参考文献[26])

Figure 5.

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图 6 老君庙岩群Si-((al+fm)-(c+alk))图解^[27]

Figure 6.

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图 7 老君庙岩群log(SiO₂/Al₂O₃)-log(Na₂O/K₂O)图解^[28]

Figure 7.

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图 8 东准噶尔地区碎屑锆石年龄统计(不含大于1000Ma的数据)

Figure 8.

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表 1 老君庙岩群LA-ICP-MS锆石U-Th-Pb测年结果

Table 1. Data of LA-ICP-MS U-Th-Pb dating of zircons from Laojunmiao Group

测点号	含量/10^-6			Th/U	同位素比值						年龄/Ma
测点号	Pb	Th	U	Th/U	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/2³⁵U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁶Pb/²³⁸U	1σ
1	27	16	58	0.28	0.1474	0.0023	1.610	0.062	0.0793	0.0031	886.2	12.9
2	184	255	449	0.57	0.0853	0.0010	0.688	0.014	0.0585	0.0013	527.9	5.8
3	117	146	255	0.57	0.0852	0.0013	0.772	0.047	0.0701	0.0080	527.2	7.8
4	148	189	636	0.30	0.0826	0.0005	0.674	0.012	0.0590	0.0010	511.7	3.3
5	455	479	369	1.30	0.1214	0.0009	1.098	0.020	0.0655	0.0012	738.5	5.4
6	194	147	279	0.52	0.1509	0.0013	1.494	0.030	0.0716	0.0014	906.0	7.4
7	193	283	358	0.79	0.0834	0.0007	0.643	0.015	0.0558	0.0013	516.3	4.3
8	119	168	259	0.65	0.0833	0.0008	0.684	0.020	0.0597	0.0017	515.5	4.8
9	185	261	328	0.80	0.0845	0.0008	0.703	0.016	0.0601	0.0013	523.1	4.5
10	131	189	284	0.66	0.0843	0.0009	0.724	0.019	0.0622	0.0016	521.9	5.4
11	301	196	846	0.23	0.1531	0.0012	1.560	0.025	0.0735	0.0011	918.3	6.6
12	162	209	409	0.51	0.0857	0.0011	0.729	0.021	0.0618	0.0017	529.9	6.5
13	167	149	303	0.49	0.1318	0.0012	1.202	0.027	0.0660	0.0015	798.4	6.9
14	176	91	824	0.11	0.1523	0.0012	1.497	0.026	0.0711	0.0013	913.7	6.8
15	125	191	236	0.81	0.0825	0.0012	0.692	0.063	0.0593	0.0039	510.8	7.4
16	167	241	362	0.67	0.0804	0.0008	0.705	0.022	0.0632	0.0019	498.6	4.9
17	152	98	317	0.31	0.1401	0.0024	1.589	0.046	0.0812	0.0017	845.1	13.7
18	182	265	422	0.63	0.0841	0.0008	0.681	0.014	0.0585	0.0012	520.6	4.8
19	85	113	255	0.44	0.0841	0.0009	0.688	0.020	0.0594	0.0018	520.7	5.8
20	305	428	818	0.52	0.0854	0.0007	0.688	0.014	0.0582	0.0012	528.3	4.3
21	112	144	302	0.48	0.0865	0.0010	0.748	0.034	0.0633	0.0034	534.9	5.9
22	138	187	333	0.56	0.0837	0.0009	0.704	0.021	0.0610	0.0019	517.9	5.5
23	150	108	342	0.32	0.1521	0.0013	1.496	0.030	0.0713	0.0015	912.5	7.5
24	114	153	284	0.54	0.0870	0.0009	0.736	0.031	0.0614	0.0026	537.7	5.6
25	101	92	129	0.71	0.1430	0.0018	1.381	0.037	0.0702	0.0019	861.7	10.3
26	167	738	218	3.39	0.1376	0.0016	1.373	0.033	0.0723	0.0017	831.1	8.9

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表 2 老君庙岩群主量、微量及稀土元素组成

Table 2. Compositions of major, trace and rare earth elements in Laojunmiao Group

样品号	QY-1	QY-2	QY-3	QY-4	QY-5	QY-6	QY-7	QY-8	QY-9	QY-10	QY-11	QY-12	QY-13
SiO₂	69.75	69.0	70.15	62.92	62.21	61.69	64.58	66.25	77.48	63.36	79.87	62.79	60.79
TiO₂	0.29	0.35	0.31	0.71	0.66	0.58	0.38	0.39	0.50	0.48	0.11	0.77	0.77
Al₂O₃	13.47	15.31	13.74	15.33	14.20	12.11	9.36	9.81	8.13	10.48	3.52	12.37	12.97
Fe₂O₃	0.81	1.03	0.88	1.38	1.72	0.96	0.71	0.58	1.12	1.40	0.67	0.90	1.67
FeO	1.35	1.78	1.62	4.60	3.97	4.24	2.90	3.24	1.90	2.74	1.28	5.00	4.39
MnO	0.05	0.05	0.04	0.09	0.09	0.11	0.10	0.11	0.07	0.13	0.10	0.09	0.09
MgO	1.00	1.74	0.89	4.09	3.71	3.70	2.65	2.81	1.15	2.85	0.85	3.70	4.10
CaO	2.64	0.71	2.76	1.62	3.66	5.96	7.15	5.53	2.59	6.78	6.65	3.48	3.83
Na₂O	5.86	6.49	5.96	2.70	3.36	3.06	2.60	3.08	3.49	3.44	1.20	2.90	2.31
K₂O	0.74	0.72	0.69	2.51	1.74	1.18	0.87	0.61	0.29	0.57	0.15	1.06	1.74
P₂O₅	0.07	0.09	0.08	0.17	0.17	0.15	0.12	0.11	0.16	0.13	0.07	0.18	0.19
烧失量	3.23	3.23	1.86	3.55	4.39	6.21	7.53	6.19	3.12	7.17	5.97	5.31	5.85
合计	99.4	100.7	99.2	100.2	100.3	100.4	99.3	99.1	100.2	99.8	100.3	99.1	99.2
Rb	26.9	29.6	24.1	89.2	53.1	39.2	34.6	25.5	13.6	22.4	6.5	44.5	74.1
Sr	121.5	223	178.5	188	300	277	243	169.5	101.5	186.5	143.5	114	139
Ba	65.9	93.7	83.1	491	469	303	196	159	77.4	159	158	191	352
Th	6.13	7.2	6.21	9.23	7.92	7.4	4.92	5.8	11.9	6.38	2.51	12.55	14.45
U	0.95	1.24	1.16	2.65	2.19	2.38	0.95	1.18	3.23	0.9	0.43	1.68	2.51
Nb	5.8	4.5	3.7	8.8	7.8	6.7	4.5	4.9	7.4	5.5	1.8	8.6	9
Ta	0.2	0.1	0.2	0.4	0.6	0.4	0.42	0.43	0.64	0.47	0.16	0.68	0.72
Zr	80	113	80	163	151	168	85	101	299	133	34	240	252
Hf	2.4	3.4	2.5	4.6	4.1	4.7	2.3	2.7	7.5	3.5	0.9	6.3	6.4
P	285.5	367.1	326.3	693.4	693.4	611.8	489.5	448.7	652.6	530.3	285.5	734.2	775
Ti	2320	2800	2480	5680	5280	4640	3040	3120	4000	3840	880	6160	6160
La	17.6	18.8	13.2	24.6	23.3	21.3	15	16.8	27.1	19.3	5.2	32	37.5
Ce	30.7	34.7	24.2	51.8	48.5	44.1	31.3	33.4	56.5	38.9	10.9	68.6	77.9
Pr	3.24	3.61	2.58	5.92	5.7	5.1	3.52	3.79	6.33	4.47	1.37	7.43	8.29
Nd	11.4	12.6	9.1	23.1	22	20.5	13.9	14.9	24.7	17.7	5.7	29	32.1
Sm	1.94	2.05	1.55	4.92	4.96	4.08	2.7	2.98	4.89	3.47	1.26	5.39	6.08
Eu	0.5	0.57	0.44	1.13	1.2	0.99	0.63	0.65	0.93	0.81	0.25	1.09	1.24
Gd	1.55	1.61	1.21	4.46	4.46	3.81	2.42	2.57	4.56	3.19	1.3	4.44	5.23
Tb	0.2	0.25	0.2	0.74	0.73	0.59	0.36	0.38	0.71	0.47	0.19	0.61	0.73
Dy	1.18	1.26	1.07	4.46	4.11	3.36	2.26	2.45	4.7	2.91	1.27	3.79	4.51
Ho	0.22	0.25	0.21	0.95	0.82	0.67	0.48	0.51	0.98	0.61	0.29	0.79	0.86
Er	0.59	0.71	0.6	2.72	2.37	1.89	1.37	1.48	2.92	1.71	0.92	2.27	2.5
Tm	0.09	0.11	0.09	0.44	0.35	0.28	0.2	0.22	0.44	0.27	0.15	0.36	0.37
Yb	0.6	0.73	0.6	2.63	1.87	1.39	1.51	2.77	1.71	2.45	1.13	2.45	2.52
Lu	0.1	0.11	0.1	0.41	0.34	0.3	0.21	0.22	0.41	0.27	0.21	0.37	0.4
Y	6.5	6.7	6.4	24.5	21.1	18	13.5	14	31.4	17	9	22.9	25.8
∑REE	76.4	84.1	61.6	153	142.2	126.8	89.2	95.9	169.3	112.8		181.5	206
LR/HR	5.93	6.17	4.87	2.69	2.89	3.12	3.02	3.11	2.46	3.01		3.78	3.8
Ce_N/Yb_N	13.23	12.3	10.43	5.09	5.65	6.1	5.82	5.72	5.28	5.88		7.24	8.0
δEu	0.85	0.93	0.95	0.72	0.77	0.76	0.74	0.7	0.59	0.73		0.66	0.66
Rb_N/Yb_N	14.76	13.35	13.22	11.16	7.87	6.9	8.19	5.56	1.62	4.31		5.98	9.68
(al+fm)- (c+alk)	22	47	22	47	24	2	-17	-5	12	-10		24	23
Si尼格里值	507	522	497	445	399	378	421	474	803	396		455	413
注：QY-1~QY-6为白云母钾长糜棱片岩；QY-7、QY-9、QY-10和QY-13为斜长绿泥石英片岩；QY-8为斜长二云母石英片岩；QY-11为石英脉；QY-12为黑云母斜长片岩；数据由广州澳实分析检测公司测试；主量元素含量单位为%，微量和稀土元素含量单位为10^-6

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