宁镇地区安基山侵入岩SHRIMP锆石U-Pb年龄及其地质意义

曾键年; 李锦伟; 陈津华; 陆建培

doi:10.3799/dqkx.2013.006

宁镇地区安基山侵入岩SHRIMP锆石U-Pb年龄及其地质意义

doi: 10.3799/dqkx.2013.006

1.
中国地质大学资源学院, 湖北武汉 430074
2.
浙江省地质调查院, 浙江杭州 311203

基金项目:

中国地质调查局资源评价项目 1212010781014

中国地质调查局资源评价项目 1212010660404

中国地质大学地质过程与矿产资源国家重点实验室开放基金 MGMR2001-1

详细信息

作者简介:
曾键年(1956-), 男, 教授, 主要研究方向为矿床学、矿床地球化学和成矿规律与成矿预测.E-mail: 1178911300@qq.com

中图分类号: P612
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出版历程
- 收稿日期: 2012-04-02
- 刊出日期: 2013-01-15

SHRIMP Zircon U-Pb Dating of Anjishan Intrusive Rocks in Ningzhen District, Jiangsu, and Its Geological Significance

1.
Faculty of Earth Resources, China University of Geosciences, Wanhan 430074, China
2.
Zhejiang Institute of Geological Survey, Hangzhou 311203, China

摘要

摘要: 对宁镇地区安基山岩体主要岩石类型花岗闪长斑岩的SHRIMP锆石U-Pb定年结果表明, 安基山岩体的花岗闪长斑岩SHRIMP锆石U-Pb年龄为(106.9±0.9)Ma, 代表了岩体形成年龄, 岩体形成于早白垩世晚期; 安基山岩体的形成明显晚于铜陵等地高钾钙碱性中酸性侵入岩形成时代, 揭示出宁镇地区中酸性钙碱性岩浆活动及其成矿响应是中生代长江中下游成矿带大规模岩浆活动的另一期成岩成矿事件; 宁镇地区铜多金属成矿作用在时间、空间和成因上与107 Ma左右的钙碱性中酸性岩浆活动有密切的联系, 区内成岩成矿作用是一个连续的过程; 宁镇地区钙碱性中酸性岩浆活动的地球动力学背景对应中国东部中生代岩石圈拆沉减薄事件; 长江中下游地区岩石圈拆沉从130 Ma左右开始, 可能一直持续到107 Ma以后.
- 安基山岩体 /
- 锆石U-Pb定年 /
- 地质年代学 /
- 地球动力学背景 /
- 宁镇地区
Abstract: The SHRIMP zircon U-Pb dating of granodiorite-porphyry, the main rock type of Anjishan rock mass yields the age of 106.9±0.9 Ma, as the formation age of the Anjishan rock mass, which shows that the Anjishan rock mass formed in the late Early Cretaceous. Anjishan rock mass is younger than the high-K calc-alkaline intermediate-acidic intrusive rocks in Tongling and other districts and it illustrates that the intermediate-acidic intrusive rocks in Ningzhen District belongs to another diagenetic event in the middle to lower Yangtze metallogenic belt's Mesozoic large magmatism. The Ningzhen District's Cu-polymetallic mineralization is closely related with the 107 Ma calc-alkaline intermediate-acidic magmatism in time, space and origin. The petrogenesis- mineralization has been a continuous process in this district. The geodynamics background of the Ningzhen District's calc-alkaline intermediate-acidic magmatism corresponds to the Mesozoic lithospheric delamination thinning event in Eastern China. It demonstrates that the middle to lower Yangtze lithosphere delamination began at about130 Ma, and lasted to 107 Ma or later.
- Anjishan rock mass /
- zircon U-Pb dating /
- geochoronolog /
- geodynamics background /
- Ningzhen district

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图 1 宁镇地区大地构造位置及地质简图

1.断裂；2.推测断裂；3.中酸性侵入岩体；4.宁镇区；根据夏嘉生(2000)和许继峰等(2001)资料修编

Fig. 1. Location of tectonics and sketch geologic map of Ningzhen region

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图 2 样品10NW04显微镜下特征

d(对角线长)为2.24 mm；a.斜长石斑晶的聚片双晶，正交偏光；b.角闪石斑晶碳酸盐化和绿泥石化，单偏光

Fig. 2. Characteristics of the sample 10NW04 in microscope

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图 3 安基山岩体花岗闪长斑岩分析锆石的阴极发光(CL)图像

Fig. 3. Cathodo luminescence (CL) images of selected zircons from granodiorite porphyry of Anjishan intrusion

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图 4 安基山岩体花岗闪长斑岩锆石U-Pb谐和曲线图

Fig. 4. U-Pb concordia curve diagram of zircons from granodiorite porphyry of Anjishan intrusion

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表 1 样品10NW04主量(%)、微量元素(10^-6)分析结果

Table 1. Analysis in major elements (%) and trace elements (10^-6) of sample 10NW04

SiO₂	TiO₂	Al₂O₃	Fe₂O₃	FeO	MnO	MgO	CaO	Na₂O	K₂O	P₂O₅	∑	Na₂O/K₂O
64.75	0.48	15.20	1.53	2.48	0.05	1.97	4.22	4.59	2.69	0.26	98.22	1.71
Co	Ni	Cr	V	Cu	Pb	Zn	Rb	Sr	Ba	Zr	Hf	Nb
9.5	19.2	30.6	74.4	38.2	12.3	37.6	40.1	966.0	1 838.0	76.8	2.6	15.2
Ta	Th	U	Sc
1.1	11.2	2.7	4.8
La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb
38.8	75.6	7.47	25.1	4.1	1.39	3.42	0.41	2.06	0.33	0.91	0.11	0.89
Lu	Y	∑REE	L/H	La_N/Yb_N	δEu	δCe
0.13	8.6	160.72	18.46	31.27	1.13	1.09
测试单位：湖北省地质实验研究所.

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表 2 安基山岩体样品10NW04的SHRIMP锆石U-Pb分析结果

Table 2. SHRIMP U-Pb analysis of zircons from sample 10NW04 of Anjishan intrusion

分析点号	²⁰⁶Pb_c(%)	U(10^-6)	Th(10^-6)	²³²Th/²³⁸U	²⁰⁶Pb^*(10^-6)	²⁰⁷Pb/²⁰⁶Pb	误差(±%)	²⁰⁶Pb/²³⁸U	误差(±%)	²⁰⁷Pb/²³⁵U	误差(±%)	²⁰⁶Pb/²³⁸U(Ma)	误差(1σ)	²⁰⁷Pb/²⁰⁶Pb(Ma)	误差(1σ)
1.1	1.53	461	292	0.65	6.7	0.056 6	2.9	0.016 6	1.5	0.11	3.6	105.9	1.6	-104	244
2.1	2.24	216	104	0.50	2.3	0.066 6	3.9	0.016 8	2.4	0.11	6.0	107.4	2.6	115	370
3.1	2.49	395	232	0.61	5.9	0.059 1	3.1	0.016 8	2.0	0.11	4.3	107.7	2.1	-447	388
4.1	4.50	237	105	0.46	3.6	0.065 7	3.9	0.016 6	2.2	0.10	6.5	106.3	2.3	-1 368	1 360
5.1	3.21	170	62	0.38	2.5	0.074 5	4.4	0.016 4	2.3	0.12	6.8	104.6	2.4	113	562
6.1	3.72	237	123	0.54	3.4	0.073 3	3.8	0.016 1	2.1	0.10	6.6	102.7	2.1	-182	548
7.1	1.25	315	141	0.46	4.6	0.063 5	6.9	0.016 9	1.7	0.13	8.3	107.9	1.8	345	225
8.1	1.25	334	126	0.39	4.9	0.056 9	3.7	0.016 9	1.7	0.12	4.6	108.1	1.8	-132	324
9.1	2.40	364	186	0.53	5.2	0.060 8	3.2	0.016 4	2.6	0.11	4.8	104.5	2.7	-280	372
9.2	1.16	313	139	0.46	4.7	0.058 8	3.4	0.017 4	1.8	0.11	4.8	111.2	2.0	167	259
10.1	1.99	297	166	0.58	4.3	0.062 9	3.5	0.016 6	2.1	0.11	5.2	105.9	2.2	30	314
11.1	2.31	311	165	0.55	4.7	0.056 3	3.5	0.017 1	1.7	0.12	4.1	109.1	1.8	-543	421
12.1	1.74	333	227	0.71	4.9	0.057 2	3.3	0.016 9	1.8	0.10	4.6	108.1	1.9	-171	340
13.1	1.30	207	100	0.50	3.1	0.063 5	4.9	0.017 1	1.9	0.12	6.4	109.0	2.0	326	230
14.1	2.03	371	172	0.48	5.3	0.059 0	3.3	0.016 4	1.9	0.11	4.6	105.0	2.0	-206	541
15.1	1.31	418	257	0.64	6.2	0.057 7	3.2	0.017 0	1.7	0.12	4.1	108.7	1.8	48	236
16.1	1.06	300	140	0.48	4.5	0.064 6	4.3	0.017 1	1.7	0.11	6.4	109.2	1.8	453	168
17.1	2.73	198	88	0.46	2.9	0.072 9	4.1	0.016 4	2.3	0.12	6.1	105.0	2.4	227	504
18.1	5.22	260	178	0.71	3.8	0.086 5	3.1	0.016 2	2.9	0.10	6.8	103.3	2.9	-130	1 094
19.1	1.08	373	266	0.74	5.3	0.057 9	3.2	0.016 4	1.5	0.11	4.0	104.9	1.6	151	123
注：误差为1σ；Pb_c和Pb^*分别代表普通铅和放射成因铅；假设²⁰⁶Pb/²³⁸U-²⁰⁸Pb/²³²Th年龄谐合校正普通铅.

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表 3 九瑞、安庆和铜陵地区主要钙碱性岩体同位素年龄

Table 3. The isotopic ages of major calc-alkaline rock in Jiurui, Anqing and Tongling areas

岩浆岩体	年龄(Ma)	测定方法	资料来源	岩浆岩体	年龄(Ma)	测定方法	资料来源
安庆月山	138.7±0.5	锆石U-Pb	张乐骏等，2008	铜陵铜官山	137.5±1.1	锆石U-Pb	徐夕生等，2004
庐江沙溪	134.0±1.5	锆石U-Pb	曾键年等，2010	铜陵凤凰山	144.2±2.3	锆石U-Pb	吴淦国等，2008
铜陵冬瓜山	135.5±2.2	锆石U-Pb	徐晓春等，2008	铜陵鸡冠石	135.5±4.4	锆石U-Pb	楼亚儿和杜杨松，2006
铜陵新桥	140.4±2.2	锆石U-Pb	王彦斌等，2004b	九瑞城门山	140.6±1.6	锆石U-Pb	蒋少涌，2008^*
铜陵胡村	140.0±2.6	锆石U-Pb	徐晓春等，2008	九瑞武山	145.6±3.9	锆石U-Pb	蒋少涌等，2008
*.学术会议交流资料.

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