胶东范家庄地区晚侏罗世低镁埃达克质花岗岩成因及构造背景

刘晓阳; 谭俊; 王怀洪; 王勇军; 甘觐荣; 王治华; 张铭

doi:10.3799/dqkx.2018.376

胶东范家庄地区晚侏罗世低镁埃达克质花岗岩成因及构造背景

doi: 10.3799/dqkx.2018.376

刘晓阳^1, ,,
谭俊^1, ,,
王怀洪^2,3,
王勇军^2,3,4,
甘觐荣¹,
王治华¹,
张铭¹

1.
中国地质大学资源学院, 湖北武汉 430074
2.
山东省煤田地质规划勘察研究院, 山东济南 250100
3.
中国地球物理学会煤田地球物理重点实验室, 山东济南 250100
4.
山东省煤田地质局第一勘探队, 山东枣庄

基金项目:

山东省煤田地质局2017年度科研专项基金项目鲁煤地科字（2017）2号

详细信息

作者简介:
刘晓阳(1993-), 男, 博士研究生, 主要从事矿床及矿产勘查研究工作

通讯作者:
谭俊

中图分类号: P581
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出版历程
- 收稿日期: 2018-12-03
- 刊出日期: 2020-02-15

Petrogenesis and Tectonic Setting of the Late Jurassic Low-Mg Adakitic Granites in the Fanjiazhuang Area, Jiaodong Peninsula

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Shandong Provincial Research Institute of Coal Geology Planning and Exploration, Jinan 250100, China
3.
Key Laboratory of Coalfield Geophysics, Geophysical Society of China, Jinan 250100, China
4.
The First Prospecting Team of Shandong Coal Geology Bureau, Zaozhuang 277000, China

摘要

摘要: 胶东地区广泛发育一系列晚侏罗世岩浆作用产生的埃达克质岩，其成因机制及构造背景研究为揭示胶东地区中生代构造演化提供了重要证据.选取出露于胶东苏鲁地区的范家庄花岗岩进行锆石U-Pb年龄、全岩主微量元素和Sr-Nd-Pb同位素组成分析，探讨了岩石成因及成岩构造背景.锆石U-Pb年龄结果表明范家庄花岗岩侵位于晚侏罗世（161±2 Ma）.岩石主微量数据具有富硅（SiO₂=68.94%~71.00%）、高铝（Al₂O₃>15.17%）、低镁（MgO=0.32%~0.41%）；高Sr、低Y、Yb含量以及高（La/Yb）_N（>38.59）比值的特点，同位素测试结果显示相对高的（⁸⁷Sr/⁸⁶Sr）_i比值（0.709 28~0.711 41）、相对较低的ε_Nd（t）值（-20.5~-14.1）和高放射性Pb同位素组成（²⁰⁶Pb/²⁰⁴Pb）_t=16.853~17.207，（²⁰⁷Pb/²⁰⁴Pb）_t=15.436~15.495，（²⁰⁸Pb/²⁰⁴Pb）_t=37.340~37.629.综合分析认为，范家庄岩体属于低镁埃达克质岩，产于增厚下地壳部分熔融，源区以扬子板块下地壳组分为主，混合有华北板块下地壳成分.晚侏罗世伊泽奈奇板块俯冲形成的弧后拉张环境诱发重力不稳定或者岩石圈伸展造成加厚的造山带垮塌，软流圈上涌的导致加厚地壳部分熔融可能是形成胶东范家庄低镁埃达克岩的地球动力学背景.
- 地球化学 /
- Sr-Nd-Pb同位素 /
- 低镁埃达克质岩 /
- 晚侏罗世 /
- 范家庄 /
- 胶东
Abstract: A series of late Jurassic adakitic rocks are widely developed in the Jiaodong Peninsula, eastern China, and their petrogenesis and tectonic setting provide important evidence for Mesozoic tectonic evolution in Jiaodong area. In this study, we investigate the bulk-rock major element, trace element and Sr-Nd-Pb isotopes of the granitoid exposed in the Fanjiazhuang area. LA-ICP-MS zircon U-Pb dating results yield a weighted mean ²⁰⁶Pb/²³⁸U age of 161±2 Ma for the Fanjiazhuang granitoid. Geochemical data indicate that the intrusion is characterized by high SiO₂(68.94%-71.00%), Al₂O₃(>15.17%), Sr but low MgO(0.32%-0.41%), Y and Yb contents, and high Sr/Y and La/Yb ratios. The rocks exhibit high initial ⁸⁷Sr/⁸⁶Sr ratios (0.709 28 to 0.711 41), low ε_Nd(t) (-20.5 to -14.1) and they are characterized by high radiogenic Pb isotopic compositions with (²⁰⁶Pb/²⁰⁴Pb)_t=16.853-17.207, (²⁰⁷Pb/²⁰⁴Pb)_t=15.436-15.495, (²⁰⁸Pb/²⁰⁴Pb)_t=37.340-37.629. The elemental and isotopic data suggest that the late Jurassic low-Mg adakitic granites in Fanjiazhuang area were derived from the partial melting of the thickened lower crust. The results show that the magma sources were dominated by lower crust of the Yangtze Block and with subordinate lower crust of the North China Block. The Izanagi plate subduction was the most likely geodynamic force for formation of the Jurassic Fanjiazhuang low-Mg adakatic granite in the Jiaodong Peninsula.
- geochemistry /
- Sr-Nd-Pb isotopes /
- low-Mg adakitic /
- Late Jurassic /
- Fanjiazhuang /
- Jiaodong Peninsula

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图 1 胶东地区区域地质简图(a), 范家庄地区地质简图(b)

据高太忠等(1999); 陈海燕(2010)修改

Fig. 1. Geological map of the Jiaodong area (a) and geological map of the Fanjiazhuang area(b)

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图 2 范家庄花岗岩宏观及镜下照片

Qtz.石英; Pl.斜长石; Afs.碱性长石; Bt.黑云母; Ms.白云母; Spn.榍石; Ser.绢云母

Fig. 2. The wild and the microscopic photos of the Fanjiazhuang granite

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图 3 范家庄花岗岩样品(FJZ10-6)锆石CL图

实线圈代表U-Pb同位素分析测试点

Fig. 3. Cathodoluminescence images for zircons of sample FJZ10-6

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图 4 范家庄花岗岩样品(FJZ10-6)U-Pb年龄协和图(a)和加权平均年龄图(b)

Fig. 4. Zircon U-Pb concordia diagram (a) and histogram of weighted average age (b)

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图 5 范家庄花岗岩TAS图解

Fig. 5. Total alkalis vs. silica(TAS) diagram

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图 6 (a) K₂O-SiO₂关系; (b)A/NK-A/CNK关系

Fig. 6. (a)K₂O vs. SiO₂ diagram, (b)A/NK-A/CNK diagram

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图 7 原始地幔标准化微量元素蛛网图(a)和球粒陨石标准化稀土元素配分图

球粒陨石及原始地幔标准化数据据Sun and McDonough (1989), 大陆下地壳成分引自(Rudnick and Gao, 2003), 大别造山带低镁埃达克质岩引自(刘质彬, 2017)

Fig. 7. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace elements spider diagram (b) for Fanjiazhuang granite

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图 8 埃达克质岩Sr/Y vs. Y和((La/Yb)_N vs. Yb_N判别图解

图a据Ma et al. (2013)修改

Fig. 8. Adakitic trace elemental discrimination diagrams for Fanjiazhuang granite

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图 9 范家庄花岗岩Dy/Yb-Dy图解(a), La/Sm-La图解(b), MgO-SiO₂图解(c)与TiO₂-SiO₂图解(d)

c, d.底图据Wang et al. (2007)和Moyen(2009)修改

Fig. 9. Dy/Yb vs. Dydiagram(a), La/Sm-La diagram (b), MgO vs. SiO₂ diagram (c) and TiO₂ vs. SiO₂ diagram for Fanjiazhuang granite

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图 10 范家庄花岗岩εNd(t)- (⁸⁷Sr/⁸⁶Sr)_i图解

图据Yang et al. (2012b)修改

Fig. 10. Initial ⁸⁷Sr/⁸⁶Sr vs. εNd(t) value for Fanjiazhuang granite.

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图 11 范家庄花岗岩²⁰⁷Pb/²⁰⁴Pb(t)- ²⁰⁶Pb/²⁰⁴Pb(t)和²⁰⁸Pb/²⁰⁴Pb(t)- ²⁰⁶Pb/²⁰⁴Pb(t),

图据Yang et al. (2012a)修改, 蚌埠地区荆山及西庐山岩体引自(杨德彬, 2009).

Fig. 11. Initial ²⁰⁷Pb/²⁰⁴Pb and ²⁰⁸Pb/²⁰⁴Pb vs. initial²⁰⁶ Pb/²⁰⁴Pb diagrams for the Fanjiazhuang granite

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图 12 伊泽奈奇板块与太平洋板块相互关系复原图(a)及胶东范家庄埃达克质岩演化模式图(b)

图a据肖庆辉等(2010)修改

Fig. 12. Restoration map of the Izanagi plate and the Pacific plate (a); Geodymanic model for the generation and emplacement of the Fanjiazhuang granite in the Shandong Peninsula(b)

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表 1 胶东范家庄地区花岗岩(FJZ10-6)锆石LA-ICP-MS U-Pb定年分析结果

Table 1. LA-ICP-MS zircon U-Pb dating results of The Fanjiazhuang granite sample(FJZ10-6) from Shandong Peninsula

分析点号	Th	U	Th/U	U-Th-Pb同位素比值				同位素年龄(Ma)
分析点号	10^-6	10^-6	Th/U	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
FJZ10-6-02	534	844	0.63	0.173 2	0.013 2	0.025 5	0.000 5	162	11	162	3
FJZ10-6-03	371	892	0.42	0.180 4	0.011 5	0.025 3	0.000 5	168	10	161	3
FJZ10-6-04	273	461	0.59	0.183 1	0.017 9	0.025 1	0.000 6	171	15	160	4
FJZ10-6-07	161	272	0.59	0.186 7	0.018 6	0.026 3	0.000 7	174	16	167	4
FJZ10-6-08	141	186	0.76	0.178 1	0.016 4	0.024 7	0.000 7	166	14	157	4
FJZ10-6-09	594	1 859	0.32	0.180 5	0.009 8	0.025 2	0.000 4	168	8	160	3
FJZ10-6-10	296	1 228	0.24	0.183 4	0.012 1	0.025 6	0.000 5	171	10	163	3
FJZ10-6-11	121	704	0.17	0.195 3	0.016 6	0.025 9	0.000 5	181	14	165	3
FJZ10-6-12	176	413	0.43	0.180 8	0.017 0	0.025 0	0.000 5	169	15	159	3
FJZ10-6-13	649	1 931	0.34	0.180 5	0.007 9	0.025 7	0.000 4	168	7	164	3
FJZ10-6-14	2 364	4 718	0.50	0.182 2	0.007 7	0.024 8	0.000 3	170	7	158	2
FJZ10-6-15	734	2 336	0.31	0.176 1	0.010 9	0.024 7	0.000 3	165	9	157	2

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表 2 胶东范家庄地区花岗岩石主量元素(%)、微量及稀土元素(10^-6)分析结果

Table 2. Major(%) and trace element (10^-6) compositions of the Fanjiazhuang granite from Shandong Peninsula

岩性	范家庄花岗岩
样品号	FJZ10-1	FJZ10-2	FJZ10-3	FJZ10-4	FJZ10-5	FJZ10-6	FJZ10-8	FJZ10-9
SiO₂	70.6	70.72	71.00	70.19	68.94	70.74	70.91	69.70
TiO₂	0.25	0.23	0.26	0.26	0.26	0.21	0.27	0.29
Al₂O₃	15.52	15.17	15.56	15.60	15.74	15.46	16.33	15.82
Fe₂O₃^T	2.63	2.96	2.54	2.92	2.79	2.37	1.79	1.88
MnO	0.04	0.05	0.04	0.05	0.04	0.04	0.03	0.03
MgO	0.36	0.41	0.35	0.38	0.37	0.32	0.36	0.38
CaO	1.98	1.74	1.94	1.86	2.00	1.84	2.08	2.04
Na₂O	4.36	4.15	4.29	4.31	4.39	4.20	4.31	4.31
K₂O	4.00	4.15	4.11	4.05	3.97	4.28	3.82	4.13
P₂O₅	0.06	0.06	0.06	0.06	0.06	0.05	0.06	0.06
LOI	0.22	0.41	0.33	0.48	0.31	0.27	0.30	0.24
Total	100.02	100.05	100.48	100.16	98.87	99.78	100.25	98.87
A/CNK	1.03	1.05	1.03	1.05	1.04	1.04	1.09	1.04
Na₂O+K₂O	8.36	8.30	8.40	8.36	8.36	8.48	8.13	8.44
K₂O/Na₂O	0.92	1.00	0.96	0.94	0.90	1.02	0.89	0.96
Mg#	21	22	21	20	21	21	29	28
La	50.82	44.67	42.58	51.39	49.43	48.26	48.81	56.04
Ce	87.12	79.06	70.70	88.81	84.28	80.81	83.03	95.22
Pr	7.78	7.86	7.34	9.00	9.14	8.33	8.24	9.42
Nd	26.16	23.36	22.40	27.25	26.12	24.39	26.54	30.90
Sm	3.49	3.60	3.47	3.75	3.76	3.02	3.58	4.42
Eu	0.88	0.96	0.93	0.96	1.01	0.79	1.01	1.23
Gd	2.32	2.48	2.32	2.24	2.46	1.66	2.11	2.71
Tb	0.31	0.34	0.33	0.33	0.33	0.22	0.31	0.45
Dy	1.35	1.71	1.62	1.37	1.50	0.72	1.69	2.36
Ho	0.27	0.34	0.32	0.28	0.29	0.13	0.33	0.45
Er	0.76	0.90	0.84	0.84	0.86	0.42	0.97	1.22
Tm	0.11	0.13	0.11	0.13	0.12	0.05	0.13	0.19
Yb	0.63	0.83	0.78	0.74	0.78	0.40	0.80	0.99
Lu	0.09	0.10	0.09	0.11	0.12	0.06	0.11	0.13
∑REE	182.11	166.34	153.84	187.22	180.19	169.27	177.66	205.74
LREE/HREE	30.14	23.33	22.96	29.97	26.93	45.14	26.55	23.19
Sr/Y	102.7	76.8	85.9	101.7	108.5	206.1	106.6	81.7
(La/Yb)_N	57.6	38.6	39.2	49.7	45.6	87.6	43.8	40.7
Eu/Eu*	0.89	0.93	0.94	0.94	0.95	0.97	1.04	1.01
Sc	8.67	8.29	7.98	6.96	6.70	6.40	1.95	2.11
V	4.9	8.2	6.4	8.9	7.9	7.3	6.4	6.7
Cr	31.3	27.0	11.1	18.7	18.1	16.8	0.6	1.1
Co	254.11	237.27	231.7	181.22	176.82	186.84	1.49	1.56
Ni	30.4	28.2	23.4	22.5	20.5	23.2	0.7	1.0
Rb	90	101	87	91	84	84	92	93
Sr	911	849	898	946	995	874	1010	1045
Y	8.87	11.05	10.45	9.30	9.17	4.24	9.47	12.80
Zr	199	195	192	214	206	186	198	215
Nb	4.88	12.70	6.68	6.89	7.23	3.78	7.50	8.84
Ba	1 767	1 978	1 714	1 963	2 002	1 869	2 730	2 877
Hf	4.23	4.78	4.24	5.00	4.87	4.75	4.84	5.14
Ta	1.26	1.86	1.28	1.17	1.13	0.99	0.48	0.62
Pb	23.4	31.0	23.0	26.7	27.0	28.3	29.5	29.6
Th	9.81	9.10	7.81	10.05	10.19	9.16	9.02	10.30
U	0.73	1.09	0.81	1.02	1.14	0.88	1.30	0.97
注：LOI.烧失量; Mg^#=100 × Mg²⁺/(Mg²⁺+0.9 ×Fe₂O₃^T); A/CNK = Al₂O₃/(CaO+Na₂O+K₂O)摩尔比

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