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
计量
- 文章访问数: 5871
- HTML全文浏览量: 628
- PDF下载量: 1557
- 被引次数: 0
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

HTML全文

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 全尺寸图片幻灯片

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

下载: 导出CSV

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.

下载: 导出CSV

参考文献(67)

Allègre, C.J., Minster, J.F., 1978. Quantitative Models of Trace Element Behavior in Magmatic Processes. Earth and Planetary Science Letters, 38(1): 1-25. doi: 10.1016/0012-821X(78)90123-1
Chen, Y.C., Mao, J.W., Luo, Y.N., et al., 1996. Geology and Geochemistry of the Dashuiguo Te-(Au) Deposit, Sichuan Province. Atomic Energy Press, Beijing, 23-28 (in Chinese).
Du, L.L., Geng, Y.S., Yang, C.H., et al., 2005. Geochemistry and SHRIMP U-Pb Zircon Chronology of Basalts from the Yanbian Group in the Western Yangtze Block. Acta Geologica Sinica, 79(6): 805－812(in Chinese with English abstract). http://www.researchgate.net/publication/279606357/download
Guo, J.Q., You, Z.P., Wang, D.K., 1997. Deformed and Metamorphic Features of Dashuigou Microlithon, Shimian, in the Western Margin of Yangtze Landmass. Acta Geologic Shichuan, 17(3): 1997(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SCDB199703001.htm
Hoskin, P.W.O., Black, L.P., 2000. Metamorphic Zircon Formation by Solid-State Recrystallization of Protolith Igneous Zircon. Journal of Metamorphic Geology, 18(4): 423-439. doi:10.1046/ j.1525-1314.2000.00266.x
Hou, L.W., 1999. Type and Origin of the Core Complexes and the Domal Deformational-Metamorphic Bodies in the Western Margin of the Yangtze Craton. Acta Geologic Sichuan, 16(1): 6-10(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SCDB601.001.htm
Hu, J.M., Meng, Q.R., Shi, Y.R., et al., 2005. SHRIMP U-Pb Dating of Zircons from Granitoid Bodies in the Songpan-Ganzi Terrane and Its Implications. Acta Petrologica Sinica, 21(3): 867-880(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200503027.htm
Li, Z.X., Li, X.H., Zhou, H., et al., 2002. Grenvillian Continental Collision in South China: New SHRIMP U-Pb Zircon Results and Implications for the Configuration of Rodinia. Geology, 30(2): 163-166. doi: 10.1130/0091-7613(2002)030<0163:GCCISC
Li, W. X, Li, X.H., Li, Z.X., 2008. Middle Neoproterozoic Syn-Rifting Volcanic Rocks in Guangfeng, South China: Petro-Genesis and Tectonic Significance. Geological Magazine, 145(4): 475-489. doi: 10.1017/S0016756808004561
Li, X.H., Zhou, H.W., Li, Z.X., et al., 2002. Petro-Genesis of Neo-Proterozoic Bimodal Volcanic in Western Shichuan and Its Tectonic Implications: Geo-Chemical and Sm-Nd Isotopic Constrains. Scientia Geologica Sinica, 37(3): 264-276(in Chinese with English abstract).
Li, Z.X., Li, X.H., Kinny. P.D., et al., 1999. The Breakup of Rodinia: Did it Start With a Mantle Plume Beneath South China? Earth and Planetary Science Letters, 173(3): 171-181. doi:10.1016 /S0012-821X(99)00240-X
Li, Z.X., Li, X.H., Kinney, P.D., et al., 2003. Geochronology of Neoproterozoic Syn-Rift Magmatism in the Yangtze Craton, South China and Correlations with other Continents: Evidence for a Mantle Superplume that Broke-Up Rodinia. Precambrian Research, 122(1-4): 85-109. doi: 10.1016/S0301-9268 (02)00208-5
Liati, A., Gebauer, D., Wysoczanski, R., 2002. U-Pb SHRIMP-Dating of Zircon Domains from UHP Garnet-Rich Mafic Rocks and Late Pegmatoids in the Rhodope Zone (N Greece): Evidence for Early Cretaceous Crystallization and Late Cretaceous Metamorphism. Chemical Geology, 184(3-4): 281-299. doi: 10.1016/S0009-2541 (01)00367-9
Lin, G.C., 2010. Zircon U-Pb Age and Petrochemical Characteristics of Shimain Granite in Western Shichuan: Petrogenesis and Tectonic Significance. Earth Science—Journal of China University of Geosciences, 35(4): 612-620(in Chinese with English abstract).
Lin, G.C., Li, X.H., Li, W.X., 2006. SHRIMP U-Pb Zircon Geochronology Geochemistry and Nd-Hf Isotope of Neoproterozoic Magmatic Rocks in Western Sichuan: Petrogenesis and Tectonic Significance. Science China (Series D): Earth Sciences, 36(7): 630-645 (in Chinese).
Lin, Q.C., Xia, B., Zhang, Y.Q., 2006. Zircon SHRIMP U-Pb Dating of the Cida Alkali Complex in the Dechang Area, Southern Sichuan, China. Geological Bulletin of China, 25(3): 588-597(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-bulletin-china_thesis/0201252289562.html
Ling, W.L., Gao, S., Zhang, B.R., et al. 2003. Neoproterozoic Tectonic Evolution of the Northwestern Yangtze Craton, South China: Implications for Amalgamation and Break-Up of the Rodinia Supercontinent. Precambrian Research, 122(1-4): 111-140. doi: 10.1016/S0301-00222-X
Liu, F.L., Xu, Z.Q., Song, B., 2003. Determination of UHP and Retrograde Metamorphic Ages of the Sulu Terrane: Evidence from SHRIMP U-Pb Dating of Zircons on Gneissic Rocks. Acta Geologica Sinica, 77(2): 229-238(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200302018.htm
Liu, J.D., Zhang, C.J., Liu, X.F., et al., 2004. Metallogenic Regularities and Exploring Direction of the Southwest Yangtze Landmass. Geological Publishing House, Beijing, 178-189(in Chinese).
Pidgeon, R.T., 1992. Recrystallization of Oscillatory Zoned Zircon: Some Geochronological and Petrological Implications. Contributions to Mineralogy and Petrology, 110(4): 463－472. doi: 10.1007/BF00344081
Shaw, D.M., 1972. The Origin of Apeley Gneiss, Ontaria, Canada. Journal of Earth Science, 9: 18-35. doi: 10.1139/e72-002
Stacey, J.S. Kramers, J.D., 1975. Approximation of Terrestrial Lead Isotope Evolution by a Two-Stage Model. Earth and Planetary Science Letters, 26(2): 207-228. doi:10.1016 /0012-821X(75)90088-6
Song, B., Zhang, Y.H., Wan, Y.S., et al., 2002. Mount Making and Procedure of the SHRIMP Dating. Geological Review (Suppl. ), 48: 26-30(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP2002S1006.htm
Tomaschek, F., Kennedy, A.K., Villa, I.M., et al., 2003. Zircons from Syros, Cyclades, Greece Recrystallization and Mobilization of Zircon during High Pressure Metamorphism. Journal of Petrology, 44(11): 1977-2002. doi: 10.1093/petrology/egg067
Vavra, G., Schmid, R., Gebauer, D., 1999. Internal Morphology, Habit and U-Th-Pb Microanalysis of Amphibolite to Granulite Facies Zircon: Geochronology of the Ivrea Zone (Southern Alps). Contributions to Mineralogy and Petrology, 134(4): 380-404. doi: 10.1007/s004100050492
Wang, K.M., Kan, Z.Z., 2001. Geological Response to Formation of the Rodinia Supercontinent in Western Margin of the Yangtze Platform. Geological and Mineral Resources of South China, 4: 22-27 (in Chinese with English abstract). http://www.researchgate.net/publication/283360993_Geological_response_to_formation_of_the_Rodinia_supercontinent_in_western_margin_of_the_Yangtze_platform
Wang, R.C., Shen, W.Z., Xu, S.J., et al., 1995. Isotopic Geology of the Dashuigou Te-Deposit, Shimian County, Sichuan Province. Journal of Nanjing University (Natural Sciences), 31(4): 617-624 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-NJDZ504.013.htm
Wang, R.M., He, G.P., Chen, Z.Z., et al., 1987. Graphic Method for Protolith Metamorphic Rocks. Geological Publishing House, Beijing, 9-60(in Chinese).
Wenchester, J.A., Park, R.G., Holland, J.G., 1980. The Geochemistry of Lewisian Semipelitic Schists from the Gairloch District, Western Ross. Scottish Journal of Geology, 16: 165-179. doi: 10.1144/sjg16020165
Wu, G.Y., 1990. Precambrian Tectonic Evolution of Kangding-Luding Area, Western Sichuan. Geotectonica et Metallogenia, 44(3): 239-246(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK199003006.htm
Wu, Y.B., Zheng, Y.F., 2004. Study of Genesis Mineralogy of Zircon and Its Constrain on U-Pb Age. Chinese Science Bulletin, 49(16): 1589-1604(in Chinese). doi: 10.1360/csb2004-49-16-1589
Xia, B., Liu, H.Y., Zhang, Y. Q, 2004. SHRIMP Dating of Agpaitic Alklic Rocks in Panxi Rift Zone and Its Geologic Implications: Examples for Hongge, Baima and Jijie Rock Bodies. Geotectoinc et Metallogenia, 28: 149-154(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK200402005.htm
Xu, S.J., Shen, W.Z., Wang, R.C., et al., 1998. Zircon U-Pb Dating of Ore-Bearing Amphibolite in Dashuigou Tellurium Deposit. Chinese Science Bulletin, 43(8): 883-885 (in Chinese). doi: 10.1360/csb1998-43-8-883
Yan, D.P., Zhou, M.F., Song, H.L., et al., 2002. Where was South China Located in the Reconstruction of Rodinia? Earth Science Frontiers, 9(4): 249-256(in Chinese with English abstract). http://www.researchgate.net/publication/284875270_where_was_south_china_located_in_the_reconstruction_of_rodinia
Yin, J.Z., Chen, Y.C., Zhou, J.X., 1996. The Geological and Geochemical Characteristics of the Host Rocks Dashuigou Independent Tellurium Ore Deposit in Shimian County, Sichuan Province. Journal of Changchun University of Earth Sciences, 26(3): 322-326(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ603.013.htm
Yin, J.Z., Chen, Y.C., Zhou, J.X., et al., 1995. The First and Independent Tellurium Deposit Metallogenetic Ages. Chinese Science Bulletin, 4(8): 766-767 (in Chinese).
Yu, A.G., Chen, Y.L., Yang, M.W., et al., 1998. Discovery of Micropaleontological Fossils in the Metamorphic Rocks in Dashuigou, Shimian. Acta Geologic Shichuan, 16(1): 6-10(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SCDB804.001.htm
Yu, A.G., Guo, J.Q., 1998. Tectonic Framework on the Western Margin of the Yangtze Platform. Regional Geology of China, 18(4): 248-250(in Chinese with English abstract). http://www.researchgate.net/publication/313564751_Tectonic_framework_on_the_western_margin_of_the_Yangtze_Platform
Zhang, Z.C., 2009. A Discussion on Some Important Problems Concerning the Emeishan Large Igneous Province. Geology in China, 36(3): 634-646 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200903012.htm
Zhou, J.X., Chen, Z.Y., 2007. Studying of Zircon Cathodoluminescence by Electron Probe. Press of University of Electronic Science and Technology of China, Chengdu, 34-123(in Chinese).
Zhou, M.F., Yan, D.P., Kennedy, A.K., et al., 2002. SHRIMP U-Pb Zircon Geochronological and Geochemical Evidence for Neoproterozoic Arc-Magmatism along the Western Margin of the Yangtze Block, South China. Earth Planet Science Letter, 196(1-2): 51-67. doi:10.1016 /S0012-821X(01)00595-7
陈毓川, 毛景文, 骆耀南, 等, 1996. 四川大水沟碲(金)矿床地质和地球化学. 北京: 原子能出版社, 23-28.
杜利林, 耿元生, 杨崇辉, 等, 2005. 扬子地台西缘盐边群玄武质岩石地球化学特征及SHRIMP锆石U-Pb年龄. 地质学报, 79(6): 805－812. doi: 10.3321/j.issn:0001-5717.2005.06.009
郭建强, 游再平, 王大可, 1997. 扬子陆块西缘石棉大水沟岩片变形变质特征. 四川地质学报, (3): 168-173. https://www.cnki.com.cn/Article/CJFDTOTAL-SCDB199703001.htm
侯立玮, 1999. 扬子克拉通西缘弯状变形变质体的类型与成因. 四川地质学报, 16(1): 6-10. https://www.cnki.com.cn/Article/CJFDTOTAL-SCDB601.001.htm
胡健民, 孟庆任, 石玉若, 等2005. 松潘甘孜地体内花岗岩锆石SHRIMP U-Pb定年及其构造意义. 岩石学报, 21(3): 867-880. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503027.htm
李献华, 周汉文, 李正祥, 等, 2002. 川西新元古代双峰式火山岩成因的微量元素和Sm和Nd同位素制约及其大地构造意义. 地质科学, 37(3): 264-276. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200203001.htm
林广春, 2010. 川西石棉花岗岩的锆石U-Pb年龄和岩石地球化学特征: 岩石成因与构造意义. 地球科学——中国地质大学学报, 35(4): 612-620. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201004014.htm
林广春, 李献华, 李武显, 2006. 川西新元古代基性岩墙群的SHRIMP锆石U-Pb年龄、元素和Nd-Hf同位素地球化学: 岩石成因与构造意义. 中国科学(D辑): 地球科学, 36(7): 630-645. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200607003.htm
林清茶, 夏斌, 张玉泉, 2006. 川南德昌地区茨达碱性岩锆石SHRIMP U-Pb定年. 地质通报, 25(3): 588-597. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200603009.htm
刘福来, 徐志琴, 宋彪, 2003. 苏鲁地体超高压和退变质时代的厘定: 来自片麻岩锆石微区SHRIMP U-Pb定年的证据. 地质学报, 77(2): 229-238. doi: 10.3321/j.issn:0001-5717.2003.02.011
刘家铎, 张成江, 刘显凡等, 2004. 扬子地台西南缘成矿规律与找矿方向. 北京: 地质出版社, 178-189.
宋彪, 张玉海, 万渝生, 等, 2002. 锆石SHRIMP样品靶、制作、年龄测定及有关现象讨论. 地质评论, 48(增刊): 26-30. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2002S1006.htm
王康明, 阚泽忠, 2001. 扬子地台西缘对Rodinia形成期地质影响. 华南地质与矿产, 4: 22-27. doi: 10.3969/j.issn.1007-3701.2001.04.007
王汝成, 沈渭洲, 徐士进, 等, 1995. 四川石棉大水沟碲矿床的同位素地质研究. 南京大学学报自然科学版, 31(4): 617-624. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ504.013.htm
王仁民, 贺高平, 陈珍珍, 等, 1987. 变质岩原岩图解判别法. 北京: 地质出版社, 10-67.
吴根耀, 1990. 川西康定-泸定地区前寒武纪大地构造演化——一个地壳多次活化"动""定"递进的实例. 大地构造与成矿学, 44(3): 239-246. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK199003006.htm
吴元保, 郑永飞, 2004. 锆石成因矿物学研究及其对U-Pb年龄解释的制约. 科学通报, 49(16): 1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002
夏斌, 刘红英, 张玉泉, 2004. 攀西古裂谷钠质碱性岩锆石SHRIMP U-Pb年龄及地质意义—以红格、白马和鸡街岩体为例. 大地构造与成矿学, 2(6): 149-154. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200402005.htm
徐士进, 沈渭洲, 王汝成, 等, 1998. 大水沟碲矿含矿斜长角闪岩的锆石U-Pb定年. 科学通报: 4 3(8): 883-885. doi: 10.3321/j.issn:0023-074X.1998.08.023
颜丹平, 周美夫, 宋鸿林等, 2002. 华南在Rodinia古陆中位置的讨论—扬子地块西缘变质一岩浆杂岩证据及其与Seychelles地块的对比. 地学前缘, 9(4): 249-256. doi: 10.3321/j.issn:1005-2321.2002.04.004
银剑钊, 陈毓川, 周建雄, 1996. 世界首例独立碲矿床赋矿围岩的地质地球化学研究. 长春地质学院学报, 26(3): 322-326. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ603.013.htm
银剑钊, 陈毓川, 周建雄, 等, 1995. 世界首例独立碲矿的成矿年龄, 科学通报, 4(8): 766-767. doi: 10.3321/j.issn:0023-074X.1995.08.028
喻安光, 陈玉禄, 杨明文等, 1998. 石棉大水沟变质岩系中微古植物化石的发现. 四川地质学报, 18(4): 248-250. https://www.cnki.com.cn/Article/CJFDTOTAL-SCDB804.001.htm
喻安光, 郭建强, 1998. 扬子地台西缘构造格局. 中国区域地质, 17(3): 256-261. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD803.005.htm
张招崇, 2009. 关于峨眉山大火成岩省一些重要问题的探讨. 中国地质, 36(3): 634-644. doi: 10.3969/j.issn.1000-3657.2009.03.010
周建雄, 陈振宇, 2007. 电子探针下锆石阴极发光的研究. 成都: 电子科技大学出版社, 34-123.