桂北圆石山早侏罗世A型花岗岩的岩石成因及意义

贾小辉; 王晓地; 杨文强; 牛志军

doi:10.3799/dqkx.2014.003

桂北圆石山早侏罗世A型花岗岩的岩石成因及意义

doi: 10.3799/dqkx.2014.003

中国地质调查局武汉地质矿产研究所, 湖北武汉 430223

基金项目:

中国地质调查局基础地质综合研究项目《南岭成矿带基础地质综合研究》 1212011085356

详细信息

作者简介:
贾小辉(1980-), 助理研究员, 从事岩石学、地球化学相关研究. E-mail: jxh1226@126.com

中图分类号: P581
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出版历程
- 收稿日期: 2013-07-30
- 刊出日期: 2014-01-01

The Early Jurassic A-Type Granites in Northern Guangxi, China: Petrogenesis and Implications

Wuhan Institute of Geology and Mineral Resources, China Geological Survey, Wuhan 430223, China

摘要

摘要: 桂北圆石山花岗岩中发育大量镁铁质包体.LA-ICP-MS锆石U-Pb定年结果显示, 花岗岩形成于早侏罗世(179±2 Ma).花岗岩的地球化学特征表现为硅含量均一, 富碱更富钾、相对富铁而贫镁, 具有高的10⁴×Ga/A1比值和Zr+Nb+Ce+Y含量, 属于A型花岗岩.圆石山花岗岩具有比较均一的Sr、Nd同位素组成(I_Sr＝0.701 7~0.710 8, ε_Nd(t)＝-7.77~-4.55).镁铁质包体则显示了稍低的I_Sr值(0.705 0~0.707 1)和稍高的ε_Nd(t)值(-4.87~-2.63).花岗岩的锆石原位Hf同位素组成为: (¹⁷⁶Hf/¹⁷⁷Hf)_i=0.282 62~0.282 70, ε_Hf(t)=-1.68~1.17, 相应的Hf同位素两阶段模式年龄T_DM2变化于1.25~1.43 Ga之间.圆石山花岗岩可能是在伸展环境下由低成熟度的下地壳物质部分熔融所形成.自早侏罗世(~200 Ma)以来, 伸展作用是华南内陆构造背景的主体, 多期次的玄武质岩浆底侵作用可能是燕山期伸展作用的直接诱因.华南内陆早侏罗世时期可能仍处于板内“后碰撞”环境.
- 早侏罗世 /
- A型花岗岩 /
- 玄武质底侵 /
- 伸展作用 /
- 岩石学 /
- 地球化学
Abstract: The Yuanshishan granites have large amounts of mafic enclaves. This paper presents new zircon LA-ICP-MS U-Pb age, and the age analysis shows that the granites were generated in Early Jurassic (179±2 Ma). These granites are characterized by uniform silicon contents, enriched in alkali contents and more enriched in K contents, and enriched in iron and depleted in magnesium contents, with high 10⁴×Ga/A1 values and Zr+Nb+Ce+Y contents. The granites belong to A-type granite. The Yuanshishan granites have homogeneous Sr-Nd isotope compositions (I_Sr＝0.701 7 to 0.710 8, ε_Nd(t)＝-7.77 to - 4.55). Mafic enclaves show lower I_sr(0.705 0 to 0.707 1) and higher ε_Nd(t)(- 4.87 to -2.63) values. In situ zircons Hf isotope compositions from these granites have limited ranges (¹⁷⁶Hf/¹⁷⁷Hf)_i=0.282 62 to 0.282 70), ε_Hf(t) = -1.68 to 1.17, and T_DM2 =1.25 to 1.43 Ga. We suggest that the Yuanshishan granites were likely generated by partial melting of newly underplated basaltic lower crust in extension setting. Since Early Jurassic (~200 Ma), extension has been the major subject of the tectonic background in the interior of the South China. Multistage basaltic magma underplating is direct inducement to the Yanshanian extension. During the Early Jurassic, the South China interior was most likely in post-collisional setting.
- Early Jurassic /
- A-type granite /
- basaltic magma underplating /
- extension /
- petrology /
- geochemistry

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图 1 桂北恭城圆石山地质略图(a)及区域构造地质简图(b)(底图据广西地质矿产勘查开发局, 恭城瑶族自治县幅1∶5万区域(G49E019012)地质调查报告, 1999)

Fig. 1. Sketch geological map of Yuanshishan (a) and sketch geological setting map (b) of the Gongcheng area, northern Guangxi

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图 2 圆石山花岗岩锆石U-Pb年龄谐和图

Fig. 2. The U-Pb concordant diagrams for the representative zircons of the Yuanshishan granites

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图 3 SiO₂ vs. K₂O(a)(Peccerillo and Taylor, 1976)和A/CNK vs. A/NK(b)

Fig. 3. SiO₂ vs. K₂O diagrams (a) and A/CNK vs. A/NK diagrams (b) for the Yuanshishan granites

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图 4 圆石山花岗岩稀土元素分布模式(a)和原始地幔标准化微量元素蜘蛛网(b)

Fig. 4. The chondrite-normalized rare earth elements (REE) (a) and the primitive mantle-normalized multi-element diagrams (b) of the Yuanshishan granites

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图 5 10⁴×Ga/Al vs. Zr、Nb、Ce、Y图解(Whalen et al., 1987)

Fig. 5. 10⁴×Ga/Al vs. Zr, Nb, Ce, Y diagrams for the Yuanshishan granites

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图 6 圆石山花岗岩锆石的ε_Hf(t)频谱图(a)和T_DM2频谱图(b)

Fig. 6. The frequence diagrams for ε_Hf(t) (a) and T_DM2 ages (b) of the zircons from the Yuanshishan granites

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图 7 Zr+Nb+Ce+Y vs. FeO^T/MgO(a)和Zr+Nb+Ce+Y vs. (K₂O+Na₂O)/CaO(b)图解(Whalen et al., 1987)

Fig. 7. Zr+Nb+Ce+Y vs. FeO^T/MgO diagrams(a) and Zr+Nb+Ce+Y vs. (K₂O+Na₂O)/CaO diagrams for the Yuanshishan granites(b)

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图 8 Al₂O₃ vs. FeO^T/(FeO^T+MgO)图解(a)和Al₂O₃/(K₂O/Na₂O) vs. FeO^T/(FeO^T+MgO)图解(b)(Dall'Agnol and de'Oliveira, 2007)

Fig. 8. Al₂O₃ vs. FeO^T/(FeO^T+MgO) diagrams(a) and Al₂O₃/(K₂O/Na₂O) vs. FeO^T/(FeO^T+MgO) diagrams (b) for the Yuanshishan granites

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表 1 圆石山花岗岩LA-ICP-MS锆石U-Pb同位素分析数据

Table 1. LA-ICP-MS U-Pb isotope for zircons of the Yuanshishan granites

点号	Th/U	Th(10^-6)	U(10^-6)	比值(经普通铅校正过的)						年龄(经普通铅校正过的)(Ma)
点号	Th/U	Th(10^-6)	U(10^-6)	²⁰⁷Pb/²⁰⁶Pb	±1σ	²⁰⁷Pb/²³⁵U	±1σ	²⁰⁶Pb/²³⁸U	±1σ	²⁰⁷Pb/²⁰⁶Pb	±1σ	²⁰⁷Pb/²³⁵U	±1σ	²⁰⁶Pb/²³⁸U	±1σ
1	0.34	414	1 214	0.047 77	0.001 0	0.192 09	0.004 1	0.029 06	0.000 2	88	49	178	3	185	1
2	0.37	291	791	0.049 99	0.002 0	0.212 10	0.008 8	0.030 72	0.000 2	195	97	195	7	195	1
3	0.15	517	3 559	0.047 30	0.000 7	0.209 62	0.003 5	0.032 01	0.000 3	64	34	193	3	203	2
4	0.42	351	842	0.051 21	0.001 4	0.198 21	0.005 4	0.028 01	0.000 2	250	62	184	5	178	1
5	0.43	155	358	0.053 28	0.003 2	0.204 65	0.012 0	0.027 86	0.000 4	341	139	189	10	177	2
6	0.33	261	802	0.053 97	0.006 2	0.204 88	0.023 2	0.027 53	0.000 3	370	261	189	20	175	2
7	0.68	391	577	0.061 31	0.001 2	0.674 46	0.013 4	0.079 56	0.000 6	650	41	523	8	494	3
8	0.38	195	514	0.049 91	0.001 7	0.220 29	0.007 3	0.032 06	0.000 3	191	76	202	6	203	2
9	0.29	358	1 248	0.054 03	0.003 0	0.235 08	0.012 4	0.031 55	0.000 5	372	126	214	10	200	3
10	0.22	390	1 764	0.064 11	0.000 9	0.572 21	0.020 3	0.063 33	0.001 8	745	47	459	13	396	11
11	0.51	552	1 087	0.079 24	0.001 0	1.956 51	0.033 3	0.178 21	0.002 2	1 178	24	1 101	11	1 057	12
12	0.21	661	3 117	0.049 57	0.001 0	0.194 99	0.003 8	0.028 41	0.000 2	175	43	181	3	181	1
13	0.28	908	3 269	0.046 28	0.000 7	0.182 63	0.003 1	0.028 48	0.000 2	12	31	170	3	181	1
14	0.33	1 926	5 859	0.047 42	0.001 1	0.184 00	0.004 2	0.028 09	0.000 2	70	50	171	4	179	1
15	0.42	288	690	0.047 30	0.001 3	0.176 90	0.005 1	0.027 04	0.000 3	65	61	165	4	172	2
16	0.30	233	777	0.049 65	0.001 7	0.192 29	0.005 9	0.028 18	0.000 3	179	70	179	5	179	2
17	0.42	342	824	0.046 84	0.001 3	0.177 35	0.004 6	0.027 50	0.000 2	41	54	166	4	175	1
18	0.42	804	1 918	0.050 21	0.001 7	0.179 12	0.005 6	0.025 91	0.000 2	205	72	167	5	165	1

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表 2 圆石山花岗岩锆石的Lu-Hf同位素分析结果

Table 2. Lu-Hf isotopic results for zircons of the Yuanshishan granites

点号	¹⁷⁶Yb/¹⁷⁷Hf	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Hf/¹⁷⁷Hf	1σ	T(Ma)	ε_Hf(t)	1σ	T_Hf1(Ga)	T_Hf2(Ga)
01	0.023 623 1	0.000 64	0.282 68	0.000 013	185	0.82	0.5	0.80	1.29
02	0.019 189 8	0.000 53	0.282 67	0.000 011	195	0.53	0.4	0.82	1.32
03	0.037 283 0	0.000 97	0.282 75	0.000 010	203	3.52	0.4	0.71	1.14
04	0.028 904 5	0.000 80	0.282 68	0.000 012	178	0.60	0.4	0.80	1.29
05	0.015 244 8	0.000 44	0.282 68	0.000 011	177	0.44	0.4	0.80	1.30
06	0.022 838 5	0.000 65	0.282 62	0.000 013	175	-1.68	0.5	0.89	1.44
07	0.027 042 1	0.000 74	0.282 21	0.000 010	494	-9.16	0.3	1.46	2.34
08	0.018 991 9	0.000 55	0.282 67	0.000 011	203	1.74	0.4	0.78	1.26
09	0.020 045 5	0.000 57	0.282 62	0.000 009	200	-0.94	0.3	0.88	1.42
10	0.024 360 6	0.000 68	0.282 50	0.000 011	396	-0.01	0.4	1.01	1.63
11	0.030 998 2	0.000 88	0.282 09	0.000 012	1 178	1.33	0.4	1.63	2.61
12	0.030 248 4	0.000 83	0.282 69	0.000 010	181	0.81	0.4	0.80	1.28
13	0.032 045 2	0.000 91	0.282 69	0.000 012	181	0.83	0.4	0.80	1.28
14	0.052 384 5	0.001 46	0.282 70	0.000 009	179	1.17	0.3	0.79	1.25
15	0.017 786 9	0.000 51	0.282 63	0.000 010	172	-1.33	0.4	0.87	1.41
16	0.017 479 9	0.000 50	0.282 69	0.000 012	179	1.01	0.4	0.78	1.27
17	0.018 840 3	0.000 56	0.282 65	0.000 009	175	-0.63	0.3	0.85	1.37
18	0.026 798 1	0.000 76	0.282 69	0.000 010	165	0.75	0.3	0.79	1.27

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表 3 圆石山花岗岩主量元素(%)和微量元素(10^-6)分析结果

Table 3. Chemical compositions of the Yuanshishan granites

样品	花岗岩							镁铁质包体
样品	N035-1	N035-2	N035-3	N035-4	N035-8	N036-1	N036-2	N035-5	N035-6	N035-7	N035-9
SiO₂	71.07	73.36	70.30	70.99	74.06	72.92	72.99	59.31	62.37	60.07	56.12
Al₂O₃	14.62	13.48	14.88	14.72	13.05	13.84	13.47	16.02	12.16	16.61	15.87
Fe₂O₃	0.66	0.05	0.15	1.35	1.15	0.91	0.10	0.88	0.13	0.67	1.66
FeO	2.06	2.68	3.07	1.79	1.70	1.64	2.69	9.32	9.00	6.86	7.87
CaO	0.94	1.01	1.11	1.12	1.06	0.90	0.91	2.94	2.77	4.09	4.42
MgO	0.22	0.22	0.27	0.26	0.25	0.17	0.18	1.33	4.29	2.02	2.53
K₂O	6.67	5.53	6.11	5.81	5.01	5.46	5.73	3.56	4.10	2.66	3.18
Na₂O	3.20	3.10	3.38	3.38	3.16	3.36	3.29	3.64	2.20	3.80	3.30
TiO₂	0.150	0.150	0.200	0.190	0.166	0.122	0.120	0.910	0.990	1.080	1.480
P₂O₅	0.04	0.04	0.06	0.06	0.06	0.03	0.03	0.41	0.32	0.52	0.56
MnO	0.05	0.04	0.05	0.05	0.05	0.04	0.05	0.19	0.16	0.12	0.19
Total	99.68	99.66	99.59	99.72	99.71	99.39	99.56	98.51	98.49	98.51	97.18
Li	108.0	99.2	120.0	114.0	112.0	122.0	120.0	575.0	459.0	268.0	350.0
Be	10.10	9.05	9.42	10.60	8.05	7.19	7.36	16.00	7.55	5.72	10.20
Sc	5.67	5.96	6.98	7.30	6.78	6.19	6.21	24.30	20.90	10.40	15.40
V	11.30	10.70	12.40	12.50	12.30	9.03	9.59	64.70	117.00	109.00	160.00
Cr	19.90	17.40	12.20	6.92	7.32	12.80	20.50	9.75	338.0	0.87	14.60
Co	2.30	2.39	2.36	2.47	2.08	1.59	2.12	10.00	27.20	13.20	18.00
Ni	6.80	3.23	3.61	3.21	2.99	3.09	3.97	5.23	138.00	5.18	7.61
Cu	7.43	6.19	6.72	6.00	4.94	5.65	9.02	7.95	9.64	22.30	24.80
Zn	46.9	43.1	53.0	52.8	50.6	34.8	42.1	281.0	247.0	156.0	197.0
Ga	29.1	28.1	30.7	28.9	27.1	28.0	27.8	37.3	29.2	27.0	34.0
Rb	388	436	403	390	362	406	426	676	719	392	565
Sr	55.7	95.6	87.3	69.9	71.0	52.6	58.6	61.0	143.0	404.0	401.0
Y	61.9	70.4	68.8	63.3	48.0	79.6	95.2	109.0	82.1	62.7	88.6
Zr	172	183	198	180	148	136	165	531	278	311	311
Nb	51.4	37.0	40.0	40.1	48.0	44.1	49.2	92.2	71.0	43.2	70.1
Mo	1.17	1.04	1.18	1.20	0.73	0.58	0.55	0.28	1.22	1.00	1.88
Cd	0.07	0.18	0.08	0.10	0.06	0.11	0.15	0.34	0.18	0.40	0.26
In	0.11	0.09	0.09	0.12	0.10	0.06	0.06	0.41	0.27	0.17	0.38
Sb	0.58	0.56	0.81	0.84	0.65	0.51	0.59	0.25	0.23	0.36	0.72
Cs	36.1	36.5	41.5	42.7	38.0	21.4	22.2	131.0	139.0	32.4	78.4
Ba	537	525	778	423	333	316	357	491	387	898	801
La	51.3	59.8	49.9	55.0	57.6	44.0	44.2	37.8	49.7	51.3	65.7
Ce	114.0	123.0	105.0	116.0	117.0	93.1	93.7	82.1	105.0	94.1	120.0
Pr	13.2	15.3	12.7	14.0	14.8	11.7	11.7	11.6	13.2	12.7	16.1
Nd	52.5	60.6	50.5	53.9	59.2	47.9	48.7	52.4	56.6	54.3	67.7
Sm	13.2	14.4	13.0	13.6	14.2	13.0	13.8	18.8	15.7	12.5	16.6
Eu	0.840	0.790	1.070	0.780	0.680	0.650	0.640	0.470	0.799	1.790	2.060
Gd	11.3	12.0	11.4	11.1	11.4	12.2	13.1	19.5	14.7	11.2	15.9
Tb	2.13	2.35	2.34	2.07	1.96	2.52	2.68	3.98	2.92	2.18	2.94
Dy	12.2	13.3	13.1	11.8	11.1	15.0	17.0	21.9	16.8	12.7	17.4
Ho	2.25	2.49	2.39	2.12	1.84	2.89	3.33	3.88	3.05	2.26	3.22
Er	6.31	7.03	6.87	6.01	4.98	8.01	9.51	10.10	8.10	6.35	8.67
Tm	1.10	1.21	1.20	1.03	0.82	1.40	1.67	1.74	1.33	1.06	1.45
Yb	6.32	7.18	6.73	6.14	4.39	8.06	9.84	9.95	7.30	5.83	8.04
Lu	0.95	1.11	1.06	0.97	0.64	1.21	1.51	1.51	1.09	0.90	1.24
Hf	7.03	7.45	8.11	7.23	6.23	5.80	7.52	14.10	8.72	7.74	8.57
Ta	6.05	5.22	5.14	5.04	5.89	7.06	6.93	8.15	5.81	3.26	6.66
W	5.60	3.25	3.41	5.68	7.15	3.43	4.32	2.54	2.71	2.09	6.33
Tl	2.52	2.07	2.30	2.18	1.94	2.32	2.49	4.52	4.58	2.40	3.43
Pb	42.6	37.4	42.2	38.7	36.6	42.2	47.1	31.1	10.8	17.3	16.6
Bi	0.24	0.88	0.35	0.60	0.52	0.25	0.25	0.59	0.17	0.40	2.41
Th	35.1	40.0	39.3	39.3	39.8	38.7	40.5	14.9	26.9	17.6	24.6
U	14.30	13.50	14.20	12.70	18.30	12.00	13.40	6.43	8.70	12.10	12.70
10⁴×Ga/Al	3.76	3.94	3.90	3.71	3.92	3.82	3.90	4.40	4.53	3.07	4.05
Zr+Nb+Ce+Y	399	413	411	399	361	352	403	814	536	511	589
T(℃)	814	820	824	816	799	796	811	852	773	775	745

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表 4 圆石山花岗岩Sr-Nd同位素分析结果

Table 4. Sr-Nd isotopic compositions of the Yuanshishan granites

样品号	Sm(10^-6)	Nd(10^-6)	¹⁴⁷Sm/¹⁴⁴Nd	¹⁴³Nd/¹⁴⁴Nd	2σ	T(Ma)	ε_Nd(t)	T_DM2(Ga)
N035-2	14.4	60.6	0.144 6	0.512 272	0.000 007	178.5	-5.95	1.46
N035-4	13.6	53.9	0.153 6	0.512 354	0.000 007	178.5	-4.55	1.34
N036-1	13.0	47.9	0.165 2	0.512 203	0.000 012	178.5	-7.77	1.61
N036-2	13.8	48.7	0.172 5	0.512 307	0.000 007	178.5	-5.90	1.45
N035-5	18.8	52.4	0.218 4	0.512 414	0.000 005	178.5	-4.87	1.37
N035-6	15.7	56.6	0.168 8	0.512 382	0.000 007	178.5	-4.36	1.33
N035-7	12.5	54.3	0.140 1	0.512 437	0.000 007	178.5	-2.63	1.19

样品号	Rb(10^-6)	Sr(10^-6)	⁸⁷Rb/⁸⁶Sr	⁸⁷Sr/⁸⁶Sr	2σ		T(Ma)	(⁸⁷Sr/⁸⁶Sr)_i
N035-2	436	95.6	12.862	0.740 035	0.000 013		178.5	0.707 3
N035-4	390	69.9	15.734	0.741 760	0.000 008		178.5	0.701 7
N036-1	406	52.6	21.767	0.759 676	0.000 010		178.5	0.704 2
N036-2	426	58.6	20.501	0.763 087	0.000 014		178.5	0.710 8
N035-5	676	61.0	31.252	0.785 050	0.000 009		178.5	0.705 4
N035-6	719	143.0	14.179	0.743 271	0.000 010		178.5	0.707 1
N035-7	392	404.0	2.736	0.711 940	0.000 011		178.5	0.705 0
注: T_DM值采用(Depaolo et al., 1991)两阶段模式年龄.

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