四川石棉县大水沟岩片绿片岩锆石SHRIMP U-Pb年代学及其地质意义

阮林森; 赵鹏大; 胡光道; 杨晓勇; 侯立玮; 陈陵康; 赵陕兰

doi:10.3799/dqkx.2013.067

四川石棉县大水沟岩片绿片岩锆石SHRIMP U-Pb年代学及其地质意义

doi: 10.3799/dqkx.2013.067

1.
中国地质大学资源学院, 湖北武汉 430074
2.
安徽省地质矿产勘查局313地质队, 安徽六安 237000
3.
中国科学技术大学地球与空间科学学院, 安徽合肥 230026
4.
四川省地质调查院, 四川成都 610084
5.
江西理工大学资源与环境工程学院, 江西赣州 341000
6.
陕西省地质矿产局区域地质矿产研究院, 陕西西安 712000

基金项目:

中国地质调查局"我国三稀金属资源战略调查四川三稀资源综合研究与重点评价" 1212011220814

详细信息

作者简介:
阮林森(1969-), 男, 工程师, 博士研究生, 研究方向矿产普查与勘探.E-mail: linsenruan@163.com

中图分类号: P539.2
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出版历程
- 收稿日期: 2013-02-23
- 刊出日期: 2013-07-01

SHRIMP U-Pb Dating of Greenschist from Dashuigou Schiefer, Shimian County, Shichuan Province and Its Geological Significance

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
No. 313 Geological Team, Bureau of Geology and Mineral Exploration of Anhui Province, Liu'an 237000, China
3.
School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
4.
Geological Survey of Shichuan Province, Chengdu 610084, China
5.
Faculty of Resource and Environmental Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, China
6.
Institute of Regional Geology and Mineral, Bureau of Geology and Mineral Exploration, Xi'an 712000, China

摘要

摘要: 大水沟岩片位于安宁河深大断裂带中段, 川西松潘甘孜造山带与扬子地台结合部位, 因其特殊的构造位置和赋存碲矿床而备受重视.运用SRHIMP U-Pb定年技术对大水沟绿片岩进行年龄测试, 来确定大水沟岩片的形成时代, 为大水沟周缘石棉-冕宁一带乃至川西扬子地台西缘的构造岩浆演化提供有益信息, 同时为大水沟碲铋矿床的形成时代提供线索.大水沟原岩恢复表明其应当有相当部分为沉积岩, 运用SHRIMP U-Pb定年从中获得的5种不同年龄段具有内部结构、外观特征的锆石差异.2467~2358Ma年龄的残留碎屑岩浆锆石说明扬子地台西缘存在太古代-古元古代的物源搬运; 790.5~762.5Ma的岩浆锆石与新元古代早期Rodinia超大陆裂解、地幔柱上涌时的岩浆事件有关; 696.8~642.9Ma锆石年龄反映了大水沟周缘碰撞造山和后造山期岩浆活动和变质作用; 伴随峨眉地裂大规模基性岩浆活动, 在大水沟近源很可能有262.0~220.0Ma碱性杂岩的侵入; 典型热液增生锆石216.5~167.1Ma年龄揭示了该区中侏罗世大规模的岩浆期后热液活动.大水沟岩片可能为异地推覆系统, 岩浆锆石年龄和热液增生锆石年龄限制了大水沟岩片总体定位于220.0~167.1Ma之间.
- 大水沟岩片 /
- 原岩 /
- 地质年代学 /
- 岩浆活动 /
- 热液锆石 /
- 岩石学
Abstract: Located at the central of the Anning River discordogenic fault, the binding site of the Songpan-Ganze orogenic belt and the Yangtze block, Dashuigou schiefer has attracted increasing attention of researchers regarding to its special tectonic site and the occurred tellurium deposit. In order to provide chronologic evidences for reconstructing tectonic and magmatic geochronic evolution of areas around Dashuigou and the western margin of the Yangtze block in Shichuan, as well as for locating time of Dashuigou schiefer, zircon ages of the greenschist from Dashuigou were determined by SHRIMP U-Pb dating technique. Five age groups of the zircons with different characteristics of inner texture and cosmetics are obtained and subdivided from the greenschist of Dashuigou schiefer which should contain great proportions of sediments in the protolith. Ages of 2467-2430Ma from remained detrital magma zircons shows the mass transportation of Archaean-early proterozoic basement, whereas ages of 790.5-762.5Ma probably represent the magmatic event around Dashuigou on the background of Rodinia crack and upwelling mantle in early neoproterozoic. Metamorphism and magmation generated by orogenics and post orogenics are documented by ages of 696.8-642.9Ma from the magmatic zircons. Zircons of 262.0-220.0Ma ages are inferred to have been originated from alkalic rock nearby related to the Emeishan movement.216.5-167.1Ma ages of typical new growth and re-crystallized zircons caused by hydrothermal alteration reveal the post-magmatic hydrothermal activity. Dashuigou schiefer is probably allochthonic thrust sheet, and ages from magma zircons and those thermal genetics bound its general locating time to the interval from 220.0Ma to 167.1Ma.
- Dashuigou schiefer /
- protolith /
- geochronology /
- magmation /
- thermal zircons /
- petrology

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图 1 大水沟区域构造略图(据喻安光等改编，1998)

1.T-P₁.三叠系-二叠系下统；2.S₁-S_2-3.志留系通化群；3.γ₅²侏罗纪二长花岗岩；4.γ₂²早震旦世中粒二长花岗岩；5.Ar-Pt康定杂岩；F1.滨东滑脱韧性剪切带；F2.西油坊逆冲推覆韧性剪切带；F3.拉谷盆子滑脱韧性剪切带；F4.野鸡洞逆冲推覆韧性剪切带；Ⅰ.洪坝构造岩片；Ⅱ.大水沟构造岩片；Ⅲ.蟹螺构造岩片；Ⅳ.岩勒构造岩片；Ⅴ.挖角坝构造岩片

Fig. 1. Tectonic and geologic map of the Dashuigou region

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图 2 区分正副变质岩的A-C-FM图(据王仁民等，1987)

A.铝质系数；C.钙质系数；FM.镁系数

Fig. 2. A-C-FM Diagram for differing orthorock

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图 3 岩石类型La/Tb-∑REE判别图解(据Allegre, 1978)

Fig. 3. La/Yb-∑REE discriminant diagram of rock types

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图 4 区分正副变质岩的Zr/TiO₂-Ni和Rfm-Rfl-Rv图解(a.据Wenchester et al., 1980; b.据王仁民等，1987)

Fig. 4. Zr/TiO₂-Ni diagram and Rfm-Rfl-Rv diagram for differing orthorock from pararock

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图 5 大水沟绿片岩锆石阴极发光图(图下方为细粒斜长角闪片岩中8颗锆石的反射光照片)

Fig. 5. Zircon CL images for greenshcist in Dashuigou

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图 6 锆石年龄谐和图

a.N1锆石4点；b.N2热液锆石

Fig. 6. Zircon U-Pb concordia diagram

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图 7 12颗高Th、U锆石加权平均年龄

Fig. 7. Weighted age of 12 zircons with abnormally high Th and U

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图 8 N2锆石39个测点的协和年龄

Fig. 8. Zircon U-Pb Concordia diagram of 39 spots from sample N2

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表 1 大水沟绿片岩主量(%)和微量元素(μg/g)分析结果

Table 1. Major (%) and trace elements (μg/g) analyses of green schist, Dashuigou

样号名称	H1片岩	H2片岩	H3片岩	H4片岩	H5片岩
SiO₂	45.45	44.02	39.20	39.64	37.89
TiO₂	1.70	1.70	1.35	1.48	1.85
Al₂O₃	14.46	17.49	16.88	16.16	18.06
Fe₂O₃	3.80	4.67	3.16	3.26	2.86
FeO	10.84	8.17	9.75	9.01	11.98
MnO	0.26	0.22	0.20	0.20	0.21
MgO	7.26	7.97	8.14	7.73	9.37
CaO	7.57	10.15	9.64	10.69	7.49
Na₂O	1.77	2.47	1.67	1.66	1.68
K₂O	0.80	0.31	2.38	2.39	2.35
P₂O₅	0.30	0.37	0.16	0.32	0.26
H₂O⁺	1.91	1.91	1.85	1.58	2.67
H₂O^-	0.06	0.06	0.13	0.11	0.19
S	0.15	0.15	0.18	0.20	0.10
CO₂	3.14	0.65	4.04	4.87	1.57
Total	99.47	100.31	98.74	99.30	98.53
Cs	4.37	4.01	4.07	4.34	4.00
Rb	41.90	14.34	29.30	252.09	118.43
Sr	215.00	201.05	128.00	199.00	219.60
Ba	269.00	250.44	289.00	315.39	348.92
Ga	28.34	19.45	21.97	20.88	25.56
Nb	18.30	16.20	6.21	17.14	17.92
Ta	1.66	1.20	1.22	1.36	1.36
Zr	134.00	94.00	78.90	113.00	101.00
Hf	3.36	13.00	3.45	2.70	4.40
Th	6.05	1.85	4.41	1.48	1.69
V	325.50	285.10	306.27	254.90	378.80
Cr	175.80	162.80	188.50	229.00	173.70
Co	58.90	54.94	47.70	26.26	61.89
Ni	90.30	89.17	103.73	123.20	98.82
B	4.10	3.50	3.67	4.20	3.30
Li	24.40	22.86	22.20	41.56	41.36
Sc	41.57	37.45	39.65	38.19	43.31
U	1.55	1.45	0.69	0.52	0.58
Cu	21.45	19.46	44.02	61.42	51.18
Zn	272.44	177.15	156.27	145.55	146.10
Pb	28.90	36.18	27.03	24.81	20.08
La	15.50	19.46	11.20	18.47	21.18
Ce	36.30	34.78	26.60	30.59	36.90
Pr	4.79	4.76	3.28	4.28	4.96
Nd	20.20	20.71	12.90	17.91	21.21
Sm	4.51	5.51	3.23	4.68	5.29
Eu	1.51	1.55	1.40	1.90	1.95
Gd	3.70	4.55	2.58	3.96	4.27
Tb	0.77	1.10	0.50	0.99	0.96
Dy	4.95	6.68	2.93	6.32	5.68
Ho	0.90	1.42	0.55	1.31	1.17
Er	2.58	3.71	1.60	3.38	3.12
Tm	0.40	0.58	0.25	0.54	0.48
Yb	2.35	3.17	1.43	2.91	2.52
Lu	0.35	0.41	0.24	0.40	0.34
Y	23.50	39.78	14.30	38.63	33.86
REE	122.31	148.14	82.99	136.27	143.89
LREE	82.81	86.76	58.61	77.84	91.48
HREE	16.00	21.60	10.08	19.81	18.54
LR/HR	5.18	4.02	5.81	3.93	4.93

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表 2 大水沟岩片绿片岩锆石SHRIMP U-Pb年龄分析结果

Table 2. Analytical data of SHRIMP U-Pb isotope of zircon grains from greenshcist, in Dashuigou schiefer

样点编号	U(10^-6)	Th(10^-6)	²³²Th/²³⁸U	²⁰⁶Pb_c(%)	²⁰⁶Pb^*(10^-6)	²⁰⁶Pb/²³⁸U(Ma)	1δerr	²⁰⁸Pb/²³²Th(Ma)	1δerr	²⁰⁷Pb/²⁰⁶Pb(Ma)	1δ err	²⁰⁷Pb^/²⁰⁶Pb^	err (%)	²⁰⁷Pb^*/²³⁵U	err (%)	²⁰⁶Pb^*/²³⁸U	err (%)	err corr
G3784-2#-27.1	56	53	0.97	3.23	6.5	790.5	13.0	599	43	34	261	0.0467	10.9	0.84	11.0	0.1305	1.7	0.158
G3784-2#-12	56	78	1.43	2.10	6.3	780.0	8.2	694	26	309	173	0.0525	7.6	0.93	7.7	0.1286	1.1	0.146
G3784-2#-1-2.1	82	148	1.87	1.45	8.9	762.5	6.6	677	23	548	105	0.0585	4.8	1.01	4.9	0.1256	0.9	0.187
G3784-2#-18.1	44	61	1.43	2.54	4.4	696.4	9.2	569	27	299	227	0.0523	10.0	0.82	10.1	0.1141	1.4	0.138
G3784-2#-1-1.1	106	118	1.15	1.08	10.4	689.4	6.0	607	14	444	86	0.0558	3.9	0.87	4.0	0.1129	0.9	0.229
G3784-2#-6.1	136	96	0.73	1.10	13.4	688.7	4.9	567	28	504	77	0.0573	3.5	0.89	3.6	0.1127	0.8	0.210
G3784-2#-10	301	160	0.55	0.46	29.0	682.4	3.8	608	12	603	37	0.0600	1.7	0.92	1.8	0.1117	0.6	0.330
G3784-2#-9	266	149	0.58	0.41	25.1	669.0	4.3	619	16	538	51	0.0582	2.3	0.88	2.4	0.1094	0.7	0.281
G3784-2#-31.2	304	191	0.65	0.14	27.9	653.3	3.7	617	9	649	30	0.0613	1.4	0.90	1.5	0.1066	0.6	0.391
G3784-2#-32.2	248	130	0.54	0.32	22.8	651.8	4.1	598	12	604	38	0.0600	1.7	0.88	1.9	0.1064	0.7	0.356
G3784-2#-14.1	435	201	0.48	0.30	39.6	647.1	3.3	595	14	581	26	0.0594	1.2	0.86	1.3	0.1056	0.5	0.414
G3784-2#-8.1	199	247	1.28	0.72	18.1	642.9	4.0	600	10	646	47	0.0612	2.2	0.88	2.3	0.1049	0.7	0.287
G3784-2#-33.2	176	84	0.49	0.74	9.6	392.4	6.7	574	21	586	99	0.0595	4.6	0.51	4.9	0.0628	1.8	0.360
G3784-2#-23.1	285	84	0.31	0.87	13.9	353.1	14.2	346	22	336	70	0.0532	3.1	0.41	5.2	0.0563	4.1	0.800
G3784-2#-5.1	148	205	1.42	3.30	5.5	262.0	2.7	223	10	-841	510	0.0334	17.8	0.19	17.8	0.0415	1.1	0.059
G3784-2#-7.1	72	116	1.66	3.89	2.6	260.9	4.5	222	13	64	157	0.0313	25.3	0.18	25.4	0.0413	1.8	0.070
G3784-2#-22.1	176	291	1.71	1.26	6.3	260.9	2.1	240	6	-1036	757	0.0473	6.6	0.27	6.7	0.0413	0.8	0.125
G3784-2#-11	100	191	1.96	3.50	3.6	256.5	3.5	195	22	-522	603	0.0375	22.5	0.21	22.6	0.0406	1.4	0.061
G3784-2#-25.1	227	441	2.00	1.77	8.0	255.3	2.0	234	5	-231	192	0.0419	7.6	0.23	7.7	0.0404	0.8	0.104
G3784-2#-20.1	104	199	1.98	3.68	3.7	255.2	4.0	222	14	-1048	683	0.0311	22.8	0.17	22.8	0.0404	1.6	0.070
G3784-2#-21.1	166	529	3.30	1.92	5.8	252.6	2.4	228	6	-128	217	0.0437	8.8	0.24	8.9	0.0400	1.0	0.110
G3784-2#-16.1	46	74	1.67	2.30	1.6	249.6	7.1	222	13	-301	551	0.0408	21.6	0.22	21.8	0.0395	2.9	0.134
G3784-2#-17.1	210	428	2.11	1.00	7.1	247.9	1.8	226	4	152	103	0.0491	4.4	0.27	4.5	0.0392	0.8	0.169
G3784-2#-13.1	228	664	3.01	1.67	7.8	247.8	2.1	221	3	-116	170	0.0439	6.9	0.24	6.9	0.0392	0.9	0.125
G3784-2#-3.1	204	598	3.03	1.71	6.9	245.0	2.0	210	3	-204	207	0.0424	8.2	0.23	8.3	0.0387	0.8	0.099
G3784-2#-15.1	954	1691	1.83	0.34	31.2	240.2	1.2	211	5	114	57	0.0483	2.4	0.25	2.5	0.0380	0.5	0.203
G3784-2#-24.1	533	1471	2.85	0.91	16.9	232.3	1.3	228	4	-87	94	0.0444	3.8	0.22	3.9	0.0367	0.6	0.150
G3784-2#-26.1	1556	3617	2.40	0.25	48.6	229.6	1.0	203	2	193	25	0.0500	1.1	0.25	1.2	0.0363	0.5	0.389
G3784-2#-28.1	1822	4576	2.60	0.17	56.6	228.4	1.0	202	2	238	21	0.0509	0.9	0.25	1.0	0.0361	0.4	0.449
G3784-2#-19.1	909	2596	2.95	0.58	28.2	227.1	1.1	196	3	89	49	0.0478	2.1	0.24	2.1	0.0359	0.5	0.238
G3784-2#-37.1	799	1423	1.84	0.32	23.9	220.0	1.7	198	2	174	42	0.0496	1.8	0.24	1.9	0.0347	0.8	0.403
G3784-2#-35.1	3411	1022	0.31	0.45	100.5	216.5	0.9	216	4	273	22	0.0517	1.0	0.24	1.1	0.0342	0.4	0.409
G3784-2#-30.1	5209	293	0.06	0.54	130.9	184.9	1.2	230	20	215	25	0.0504	1.1	0.20	1.3	0.0291	0.7	0.518
G3784-2#-31.1	4596	241	0.05	0.22	112.4	180.5	1.6	221	9	164	18	0.0493	0.8	0.19	1.2	0.0284	0.9	0.762
G3784-2#-29.1	4479	52	0.01	0.14	105.5	174.1	1.8	115	30	133	17	0.0487	0.7	0.18	1.3	0.0274	1.0	0.825
G3784-2#-32.1	3838	134	0.04	0.14	89.3	172.0	0.8	172	10	157	17	0.0492	0.7	0.18	0.9	0.0270	0.5	0.564
G3784-2#-33.1	4455	182	0.04	0.16	103.6	172.0	1.1	172	11	173	18	0.0495	0.8	0.18	1.0	0.0270	0.7	0.651
G3784-2#-34.1	4952	183	0.04	0.19	114.9	171.5	0.7	180	13	115	20	0.0483	0.8	0.18	0.9	0.0270	0.4	0.457
G3784-2#-36.1	5356	211	0.04	0.17	121.1	167.1	1.8	150	10	150	17	0.0490	0.7	0.18	1.3	0.0263	1.1	0.832
G3784-1#-1.1	145	317	2.26	1.15	10.9	533.0	4.0	477	10	259	111	0.0514	4.9	0.61	4.9	0.0862	0.8	0.158
G3784-1#-2.1	37	40	1.11	9.08	0.7	127.0	5.2	88	24							0.0199	4.1
G3784-1#-3.1	200	107	0.56	0.28	58.7	1892.7	9.9	1649	23	2430	9	0.1576	0.5	7.42	0.8	0.3412	0.6	0.761
G3784-1#-4.1	193	103	0.55	1.44	7.5	282.6	2.4	233	16	-17	181	0.0457	7.5	0.28	7.5	0.0448	0.9	0.116
G3784-1#-5.1	193	101	0.54	0.25	61.7	2030.7	11.0	2217	31	2400	9	0.1548	0.5	7.90	0.8	0.3703	0.6	0.765
G3784-1#-6.1	522	456	0.90	3.61	19.1	259.5	1.7	169	10	-38	180	0.0453	7.4	0.26	7.5	0.0411	0.7	0.092
G3784-1#-7.1	509	451	0.92	0.39	118.6	1542.5	6.8	1436	15	2358	9	0.1511	0.5	5.63	0.7	0.2703	0.5	0.695
G3784-1#-8.1	141	73	0.53	0.63	45.6	2049.7	15.7	1790	57	2467	16	0.1611	0.9	8.32	1.3	0.3743	0.9	0.686
注：(1)1#为上部细粒斜长角闪片岩中的N1锆石，2#为下部阳起石斜长角闪片岩中的N2锆石；(2)²⁰⁶Pb_c表示普通²⁰⁶Pb占总²⁰⁶Pb的百分比，²⁰⁶Pb^*表示放射性²⁰⁶Pb的含量.

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