华北-西伯利亚板块对接带早白垩纪的裂解: 来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据

李益龙; 周汉文; 钟增球; 尹淑苹; 李福林

doi:10.3799/dqkx.2010.107

华北-西伯利亚板块对接带早白垩纪的裂解: 来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据

doi: 10.3799/dqkx.2010.107

李益龙^{1, 2,},
周汉文^{1, 2, ,},
钟增球^{1, 2},
尹淑苹³,
李福林¹

1.
中国地质大学地球科学学院, 湖北武汉 430074
2.
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
3.
中国地质科学院地质研究所, 北京 100037

基金项目:

国家重点基础研究"973"项目 2007CB411307

中国地质调查局项目 1212010510507

详细信息

作者简介:
李益龙(1983-), 男, 博士生, 研究方向为变质岩石学.E-mail: yilong_l@yahoo.com.cn

通讯作者:
周汉文, E-mail: hwzhou@cug.edu.cn

中图分类号: P597
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- 被引次数: 0
出版历程
- 收稿日期: 2010-05-26
- 刊出日期: 2010-11-01

Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia

LI Yi-long^{1, 2
,},
ZHOU Han-wen^{1, 2
, ,},
ZHONG Zeng-qiu^{1, 2},
YIN Shu-ping³,
LI Fu-ling¹

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

摘要

摘要: 在内蒙古林西县西拉木伦断裂带内发育规模较大的中性岩墙群, 岩墙多呈NE3°~5°近直立侵入.对岩石进行了锆石LA-ICP-MS U-Pb定年和详细的岩石地球化学特征研究.锆石LA-ICP-MS U-Pb年龄为132.2±2.2Ma, 岩石侵位于早白垩世.岩石地球化学特征显示岩石具有高钾钙碱性系列-钾玄岩系列的过渡特征, 形成于板内拉张环境, 岩浆源区具有壳幔混源的特征, 是早期俯冲洋壳遭受幔源岩浆底侵作用的结果.岩墙的产状受左旋剪切机制控制, 该机制可能主要与太平洋板块相对亚洲板块的向北运动有关.
- 中性岩墙群 /
- 锆石LA-ICP-MS U-Pb定年 /
- 地球化学 /
- 西拉木伦断裂带 /
- 内蒙古
Abstract: A large scale of intermediate dykes developed in Xar Moron fault belt in Linxi county, Inner-Mongolia, with NE3° to 5° angle of strike and nearly vertical trend. LA-ICP-MS zircon U-Pb dating method and whole rock geochemistry test were applied. It is indicated that the intermediate dykes emplaced in Lower Cretaceous with LA-ICP-MS zircon U-Pb age of 132.2±2.2Ma. The whole rock geochemistry of the dykes reveals transition characteristics between high potassium calc-alkaline series and shoshonite series. They formed in intraplate extensional background and sourced from crust-mantle magmatic mixing, which result from the mantle magma underplating below the early subducted oceanic crust. The strike of the dykes was chronically controlled by a sinistral shear mechanism in the area, which might be related to the northward movement of Pacific plate to Asian plate.
- intermediate dykes /
- LA-ICP-MS zircon U-Pb dating /
- geochemistry /
- Xar Moron fault belt /
- Inner-Mongolia

HTML全文

图 1 研究区构造格局略图

Fig. 1. Structure delineation of the research area

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图 2 内蒙古林西县双井地区地质简图

1.双井片岩；2.花岗质片麻岩；3.志留系西别河组；4.杏树洼蛇绿岩；5.二叠系哲斯组；6.中生代侵入岩；7.中生代火山岩；8.第三系玄武岩；9.第四系；10.断层；11.村庄；12.岩墙采样点

Fig. 2. Geological map of Shuangjing area in Linxi County, Inner-Mongolia

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图 3 林西县中性岩墙群单颗粒锆石CL图像(a)和LA-ICP-MS锆石U-Pb谐和图(b)

圆圈表示剥蚀激光束对应的位置，直径为24μm

Fig. 3. Representative CL images (a) and LA-ICP-MS U-Pb concordia diagram (b) of zircons from the intermediate dykes in Linxi County

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图 4 林西县中性岩墙群的分类图解

a.全碱-SiO₂图解(MacDonald and Katsura, 1964)；b.AFM图解(Irvine and Baragar, 1971)

Fig. 4. Classification of the intermediate dykes in Linxi County

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图 5 林西县中性岩墙群的系列判别

a.K₂O-SiO₂图解(Morrison, 1980)；b.Th/Yb-Ta/Yb图解(Müller and Groves, 1995)

Fig. 5. Rock series Discriminant of the intermediate dykes in Linxi County

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图 6 林西县中性岩墙群微量元素原始地幔标准化蛛网图(a)和稀土元素球粒陨石标准化分布模式(b)

标准值采用Sun and McDonough (1989)推荐值

Fig. 6. Primitive-mantle normalized trace elements distribution patterns (a) and Chondrite normalized REE distribution patterns (b) of the intermediate dykes in Linxi County

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图 7 林西县中性岩墙群的构造背景判别图

a.FeO_t-MgO-Al₂O₃图解(Pearce et al., 1977)；b.TiO₂-K₂O-P₂O₅图解(Pearce et al., 1975)

Fig. 7. Tectonic discriminant diagrams for intermediate dykes in Linxi County

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表 1 林西县中性岩墙群(8878)的LA-ICP-MS锆石U-Pb分析结果

Table 1. LA-ICP-MS zircon U-Pb analytic data for intermediate dykes (8878) in Linxi County

锆石点号		8878-1	8878-2	8878-3	8878-4	8878-5	8878-6	8878-7	8878-8
组成	Pb(10^-6)	18.45	3.32	2.17	6.22	6.03	6.84	12.55	17.69
	Th(10^-6)	364.79	88.04	36.95	185.40	206.70	175.80	386.57	345.24
	U(10^-6)	628.84	110.37	73.28	181.22	203.55	215.55	411.52	629.92
	Th/U	0.58	0.80	0.50	1.02	1.02	0.82	0.94	0.55
含量比值	²⁰⁷Pb/²⁰⁶Pb	0.04945	0.05201	0.05064	0.05181	0.05033	0.05087	0.05216	0.05025
	1σ	0.00099	0.00238	0.00323	0.00431	0.00189	0.00314	0.00237	0.00101
	²⁰⁷Pb/²³⁵U	0.14472	0.14615	0.14656	0.14537	0.14199	0.13987	0.14694	0.14606
	1σ	0.00279	0.00652	0.00916	0.01189	0.00520	0.00846	0.00648	0.00284
	²⁰⁶Pb/²³⁸U	0.02123	0.02038	0.02099	0.02035	0.02046	0.01994	0.02043	0.02108
	1σ	0.00021	0.00027	0.00033	0.00031	0.00024	0.00025	0.00023	0.00021
	²⁰⁸Pb/²³²Th	0.00661	0.00665	0.00691	0.00640	0.00620	0.00628	0.00642	0.00668
	1σ	0.00008	0.00013	0.00023	0.00006	0.00010	0.00006	0.00005	0.00008
年龄(Ma)	²⁰⁷Pb/²⁰⁶Pb	169	286	224	277	210	235	292	207
	1σ	27	78	115	190	63	143	106	27
	²⁰⁷Pb/²³⁵U	137	139	139	138	135	133	139	138
	1σ	2	6	8	11	5	8	6	3
	²⁰⁶Pb/²³⁸U	135	130	134	130	131	127	130	134
	1σ	1	2	2	2	2	2	1	1
	²⁰⁸Pb/²³²Th	133	134	139	129	125	127	129	135
	1σ	2	3	5	1	2	1	1	2

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表 2 林西县中性岩墙群的主量元素分析结果及处理后数据(%)

Table 2. Compositions of major elements and conversion data of the intermediate dykes from Linxi County

样品	SiO₂	Al₂O₃	Fe₂O₃	FeO	CaO	MgO	Na₂O	K₂O	TiO₂	MnO	P₂O₅	H₂O⁺	CO₂	Total
8878-2	52.91	14.91	3.64	3.90	6.31	3.25	2.78	2.77	1.40	0.09	0.48	2.97	4.34	99.75
8878-3	52.86	15.02	2.68	4.85	6.14	3.41	2.81	3.10	1.43	0.15	0.50	2.95	3.75	99.65
8878-4	53.27	15.33	2.07	5.40	5.56	3.38	3.79	2.28	1.48	0.11	0.51	2.90	3.55	99.63
8878-5	54.49	16.72	3.06	3.50	5.53	2.84	3.45	2.88	1.01	0.10	0.42	2.44	2.86	99.30
8878-6	53.30	15.40	2.52	5.00	5.59	3.42	3.81	2.37	1.50	0.11	0.51	3.05	3.06	99.64
8878-7	55.33	14.92	3.31	4.10	4.68	3.28	3.78	3.64	1.62	0.09	0.76	2.51	1.68	99.70

换算后
样品	SiO₂	Al₂O₃	Fe₂O₃	FeO	CaO	MgO	Na₂O	K₂O	TiO₂	MnO	P₂O₅	FeO_t	σ	Mg^#
8878-2	57.24	16.13	3.94	4.22	6.83	3.52	3.01	3.00	1.51	0.10	0.52	7.76	2.53	44.67
8878-3	56.87	16.16	2.88	5.22	6.61	3.67	3.02	3.34	1.54	0.16	0.54	7.81	2.91	45.57
8878-4	57.17	16.45	2.22	5.80	5.97	3.63	4.07	2.45	1.59	0.12	0.55	7.79	2.99	45.34
8878-5	57.97	17.79	3.26	3.72	5.88	3.02	3.67	3.06	1.07	0.11	0.45	6.65	3.03	44.74
8878-6	56.99	16.47	2.69	5.35	5.98	3.66	4.07	2.53	1.60	0.12	0.55	7.77	3.12	45.62
8878-7	57.93	15.62	3.47	4.29	4.90	3.43	3.96	3.81	1.70	0.09	0.80	7.41	4.04	45.23

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表 3 林西县中性岩墙群的微量元素分析结果(10^-6)

Table 3. Compositions of trace elements of the intermediate dykes in Linxi County

元素	8878-2	8878-3	8878-4	8878-5	8878-6	8878-7
Be	1.68	1.95	1.63	1.35	1.64	1.86
Sc	14.80	15.20	15.00	9.28	15.30	12.70
V	140.00	144.00	149.00	114.00	152.00	124.00
Cr	43.30	39.50	31.10	1.87	32.80	63.50
Co	19.90	20.90	20.60	16.00	21.00	19.90
Ni	10.60	9.92	9.13	3.51	8.97	27.00
Cu	29.40	28.40	22.50	15.40	17.60	32.80
Zn	188.00	200.00	146.00	113.00	130.00	173.00
Ga	19.70	20.00	20.20	20.70	20.90	22.40
Rb	92.70	91.50	62.20	75.10	63.40	77.10
Sr	321	483	646	1048	640	608
Y	19.2	20.1	20.1	18.1	20.4	24.7
Zr	226	236	239	174	247	354
Nb	11.00	11.60	12.20	8.03	12.10	21.60
Sn	1.72	1.67	1.65	1.24	1.66	2.18
Cs	4.96	3.58	2.32	2.92	2.55	3.83
Ba	727	1585	1715	4169	1681	1109
La	36.1	38.7	35.6	36.1	36.7	59.7
Ce	72.3	76.8	78.0	67.8	81.8	128
Pr	9.40	10.1	10.2	8.82	10.4	16.3
Nd	37.3	40.1	40.1	34.7	41.6	62.0
Sm	6.98	7.41	7.30	5.89	7.75	10.5
Eu	1.84	2.17	2.09	1.97	2.14	2.51
Gd	5.37	5.73	5.70	4.43	5.86	7.37
Tb	0.73	0.79	0.80	0.60	0.82	1.01
Dy	3.90	4.13	4.25	3.22	4.25	5.11
Ho	0.69	0.73	0.72	0.60	0.75	0.90
Er	1.83	1.90	1.96	1.58	1.95	2.33
Tm	0.25	0.28	0.27	0.22	0.27	0.32
Yb	1.46	1.58	1.54	1.39	1.60	1.96
Lu	0.23	0.25	0.24	0.21	0.25	0.28
Hf	5.38	5.77	5.73	4.16	5.92	8.15
Ta	0.65	0.70	1.51	0.50	0.71	1.08
Pb	196.00	221.00	103.00	73.30	56.80	53.40
Th	4.51	4.70	4.50	3.34	4.52	3.95
U	1.25	1.22	1.13	0.85	1.13	1.26
Eu^*	0.88	0.98	0.95	1.13	0.93	0.94
Ce^*	0.94	0.93	0.99	0.90	1.01	1.00
(La/Yb)_n	17.77	17.59	16.63	18.65	16.48	16.31
(La/Gd)_n	5.83	5.86	5.42	7.07	5.42	5.55
(Dy/Yb)_n	1.79	1.75	1.85	1.55	1.78	1.77

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