云开地块印支期变质-深熔作用:混合岩、片麻岩锆石U-Pb年代学和Hf同位素证据

柯贤忠; 周岱; 龙文国; 王晶; 徐德明; 田洋; 金巍

doi:10.3799/dqkx.2018.574

云开地块印支期变质-深熔作用:混合岩、片麻岩锆石U-Pb年代学和Hf同位素证据

doi: 10.3799/dqkx.2018.574

中国地质调查局武汉地质调查中心, 湖北武汉 430205

基金项目:

中国地质调查局项目 DD20160031

中国地质调查局项目 12120114039201

中国地质调查局项目 12120113066400

中国地质调查局项目 DD20160035

详细信息

作者简介:
柯贤忠(1984-), 男, 助理研究员, 博士, 主要从事区域地质调查及研究工作

中图分类号: P597
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出版历程
- 收稿日期: 2017-10-16
- 刊出日期: 2018-07-15

Indosinian Metamorphism and Anatexis in Yunkai Massif: Evidences from Zircon Geochronology and Hf Isotopes of Migmatites and Gneisses

Wuhan Center of China Geological Survey, Wuhan 430205, China

摘要

摘要: 云开地块中生代构造演化是华南地区的研究热点之一.通过对云开地块变质基底中的混合岩、片麻岩（5个样品）和花岗岩（1个样品）开展锆石LA-ICP-MS U-Pb定年，获得440.3±3.3 Ma、230.2±2.9 Ma、230.7±1.3 Ma、459.5±2.7 Ma、431.5±4.3 Ma、229.2±5.4 Ma、229.7±2.7 Ma 7组变质（深熔）或岩浆年龄和2组（样品1432-1和ID7-3）碎屑锆石年龄，碎屑锆石年龄范围均为太古代-新元古代，且具有~1.0 Ga年龄主峰，与天堂山岩群和云开群碎屑锆石年龄谱相似.区域资料表明云开地块天堂山岩群和云开群具有相似的物质组成，均形成于早古生代-新元古代，存在变质程度和物质面貌的差异；在加里东期构造-热事件的基础上，广泛叠加了印支期区域变质（深熔）-构造-流体作用影响.4个样品中（1431-1、1432-1、D116-3和ID7-3）锆石原位Lu-Hf同位素组成显示，加里东期变质和深熔锆石Lu/Hf同位素组成基本一致，应继承了原岩的同位素组成特征.印支期变质和深熔锆石Lu/Hf同位素组成不同，可能主要由变质作用和深熔作用的差异所致.以古-中元古代为主的地壳物质参与了加里东期和印支期变质-深熔作用，在加里东期和印支期深熔作用过程中，均有少量幔源物质的加入，印支期幔源物质的贡献相对显著.
- 锆石U-Pb年代学 /
- Hf同位素 /
- 变质-深熔作用 /
- 印支期 /
- 云开地块 /
- 地球化学
Abstract: The Mesozoic tectonic evolution in Yunkai massif has always been one of hot topics in South China. Zircons from five metamorphic rocks including migmatite and gneiss and one granite from the metamorphic basement in Yunkai massif were measured by the LA-ICP-MS U-Pb dating method, yielding 7 metamorphic (anatectic) or magmatic ages (440.3±3.3 Ma, 230.2±2.9 Ma, 230.7±1.3 Ma, 459.5±2.7 Ma, 431.5±4.3 Ma, 229.2±5.4 Ma, 229.7±2.7 Ma) and 2 groups of detrital ages. Both the detrital zircons showed Archaean-Neoproterozoic age range with~1.0 Ga age peaks, which were similar with those of the Tiantangshan Group and the Yunkai Group. Together with the regional data, it was concluded that the Tiantangshan Group and the Yunkai Group, which were analogous in provenance and formed in Early Palaeozoic-Neoproterozoic, were broadly overprinted by the Indosinian metamorphism (anatexis)-deformation-fluid activities after the Caledonian tectonic-thermal events, resulting in differences in metamorphic grade and appearance. In situ zircon Lu-Hf isotopic analysis from four samples show that both the isotopic compositions of Caledonian metamorphic and anatectic zircons were similar with each other, which was ascribed to inheriting the compositions of provenance rocks, whereas the different isotopic compositions of Indosinian metamorphic and anatectic zircons could have been caused by individual mechanism of metamorphic and anatectic processes. It was inferred that the dominant Paleo-Mesoproterozoic crustal material played important role in the metamorphism and anatexis processes in Caledonian and Indosinian, and a few mantle-derived material was added in the anatectic processes in Caledonian and Indosinian with relatively remarkable contribution of mantle-derived material in Indosinian.
- zircon U-Pb geochronology /
- Hf isotopes /
- metamorphism-anatexis /
- Indosinian /
- Yunkai massif /
- geochemistry

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图 1 云开地区地质简图及采样位置

图a据Wang et al.(2013b)；图b据邱元禧等(2006)；Chen et al.(2017)

Fig. 1. Simplified geological map of the Yunkai region and the sampling localities

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图 2 变质岩宏观和微观照片

a, f.眼球状混合片麻岩(1431-1)；b, g.条带状混合片麻岩(1432-1)；c, h.混合岩(D116-3)；d.花岗质片麻岩(15BR04)；e.条带状混合岩(ID7-3)、花岗岩脉(ID7-5)；i.条带状混合岩(ID7-3)；j.花岗岩脉(ID7-5)；Qz.石英；Pl.斜长石；Kfs.钾长石；Mic.微斜长石；Bt.黑云母；Mus.白云母

Fig. 2. Macro- and micro-photographs of the metamorphic rocks in Yunkai massif

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图 3 云开地块变质岩典型锆石阴极发光(CL)图像

Fig. 3. Cathodoluminescence (CL) images of representative zircons from the metamorphic rocks in Yunkai massif

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图 4 云开地块变质岩锆石U-Pb谐和图

Fig. 4. Concordia diagrams of zircon U-Pb data for the metamorphic rocks in Yunkai massif

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图 5 样品D116-3变质锆石与深熔锆石Th/U值(a)和稀土配分曲线(b)

Fig. 5. Th/U ratios and REE distribution pattern of the metamorphic and anatectic zircons from sample D116-3

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图 6 云开地区变质岩锆石Hf同位素图解

a.t-ε_Hf图解；b. ¹⁷⁶Lu/¹⁷⁷Hf-¹⁷⁶Hf/¹⁷⁷Hf图解；c.ε_Hf和T_DM2分布直方图

Fig. 6. Hf isotopic diagrams of zircon from metamorphic rocks in Yunkai region

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图 7 云开地区印支期不同类型变质年龄分布直方图

Fig. 7. Histograms of differetnt types of Indosinian metamorphic age in Yunkai region

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表 1 云开地块变质岩LA-ICP-MS锆石U-Th-Pb同位素分析结果

Table 1. Zircon U-Th-Pb isotopic compositions of metamorphic rocks in Yunkai massif

点号	位置	Th (10^-6)	U (10^-6)	Th/ U	同位素比值						表面年龄(Ma)						谐和度 (%)
点号	位置	Th (10^-6)	U (10^-6)	Th/ U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	谐和度 (%)
1431-1(眼球状混合片麻岩)，核-边结构为主，少量核-幔-边结构
1	m	80	286	0.28	0.055 7	0.002 4	0.554 5	0.024 6	0.071 9	0.000 9	443	129	448	16.1	448	5.3	99
2	c	152	271	0.56	0.057 7	0.002 5	0.556 1	0.023 3	0.069 6	0.000 7	517	94.4	449	15.2	434	4.2	96
3	c	89	347	0.26	0.057 4	0.002 2	0.569 8	0.021 5	0.071 5	0.000 7	506	83.3	458	13.9	445	4.3	97
4	c	172	335	0.51	0.058 1	0.002 5	0.582 9	0.024 5	0.072 3	0.000 9	532	99.1	466	15.7	450	5.3	96
5	c	59	313	0.19	0.057 2	0.002 2	0.565 2	0.021 8	0.070 9	0.000 7	502	85.2	455	14.1	442	4.5	97
6	c	49	305	0.16	0.056 2	0.002 4	0.534 1	0.022 9	0.068 8	0.000 9	461	96.3	435	15.2	429	5.4	98
7	c	93	368	0.25	0.058 3	0.002 1	0.553 4	0.020 0	0.068 5	0.000 7	543	77.8	447	13.1	427	4.2	95
8	c	115	218	0.53	0.056 2	0.002 5	0.551 3	0.024 7	0.071 3	0.000 9	461	100.0	446	16.1	444	5.5	99
9	c	882	606	1.45	0.059 1	0.002 2	0.582 2	0.021 4	0.071 3	0.000 9	572	81.5	466	13.7	444	5.3	95
10	c	60	304	0.20	0.056 4	0.002 9	0.541 1	0.027 7	0.069 3	0.001 0	478	119	439	18.3	432	5.8	98
11	c	76	181	0.42	0.060 8	0.003 4	0.584 5	0.032 9	0.070 7	0.001 2	632	119	467	21.1	440	7.3	94
12	c	65	200	0.33	0.052 9	0.002 9	0.494 7	0.026 4	0.068 0	0.000 8	324	124	408	17.9	424	5.0	96
13	c	61	573	0.11	0.057 1	0.002 2	0.553 3	0.021 3	0.069 9	0.000 8	494	83.3	447	13.9	436	4.6	97
14	c	61	330	0.19	0.057 5	0.002 2	0.570 4	0.022 2	0.071 6	0.000 8	509	78.7	458	14.4	446	4.9	97
15	c	91	428	0.21	0.057 3	0.001 8	0.559 6	0.017 7	0.070 5	0.000 7	502	70.4	451	11.5	439	4.2	97
16	r	20	237	0.08	0.058 3	0.002 7	0.581 1	0.027 1	0.071 9	0.000 8	539	101	465	17.4	448	5.1	96
17	c	125	237	0.53	0.071 5	0.003 6	0.679 6	0.035 0	0.068 4	0.000 8	972	103	527	21.2	426	4.9	79
18	c	44	220	0.20	0.058 8	0.003 0	0.573 5	0.029 8	0.070 2	0.000 9	561	139	460	19.2	438	5.6	94
19	c	59	374	0.16	0.060 0	0.002 5	0.595 3	0.025 4	0.071 4	0.000 8	611	95.4	474	16.2	445	4.9	93
20	c	54	274	0.20	0.055 2	0.002 5	0.553 4	0.024 7	0.072 3	0.000 8	420	102	447	16.1	450	4.5	99
21	c	84	472	0.18	0.055 2	0.002 0	0.540 1	0.019 6	0.070 5	0.000 7	420	81.5	439	12.9	439	4.2	99
22	r	0	12.6	0.01	0.000 0	0.000 0	0.376 6	0.223 2	0.040 2	0.002 4			325	165	254	15	75
23	c	54	262	0.20	0.058 5	0.002 6	0.564 8	0.024 7	0.069 9	0.000 8	550	96.3	455	16.0	436	4.6	95
24	c	69	255	0.27	0.055 2	0.002 5	0.553 4	0.025 5	0.072 5	0.000 8	420	102	447	16.7	451	5.0	99
25	c	72	344	0.21	0.055 7	0.002 3	0.550 6	0.022 7	0.071 7	0.000 8	439	92.6	445	14.9	446	4.6	99
26	r	59	97	0.61	0.075 0	0.004 9	0.730 1	0.047 6	0.071 2	0.001 1	1 069	132	557	27.9	443	6.8	77
1432-1(条带状混合片麻岩)，核-幔-边结构为主
1	r	6	642	0.01	0.051 5	0.001 8	0.256 0	0.008 5	0.036 0	0.000 4	265	79.6	231	6.9	228	2.5	98
2	c	182	354	0.51	0.101 2	0.001 7	3.895 3	0.067 7	0.277 5	0.002 2	1 656	31.8	1 613	14.1	1 579	10.9	97
3	c	142	229	0.62	0.078 1	0.001 8	1.856 4	0.041 0	0.171 8	0.001 5	1 150	44.4	1 066	14.6	1 022	8.1	95
4	m	4	421	0.01	0.051 7	0.002 1	0.265 1	0.011 0	0.037 0	0.000 4	272	96.3	239	8.8	234	2.3	98
5	r	176	290	0.61	0.147 1	0.002 7	8.255 9	0.146 3	0.404 6	0.003 0	2 313	31.2	2 259	16.1	2 190	14.0	96
6	c	514	2 784	0.18	0.093 4	0.001 7	1.865 4	0.040 4	0.143 3	0.001 7	1 496	35.2	1 069	14.3	863	9.3	78
7	c	567	629	0.90	0.074 3	0.001 6	1.779 9	0.038 4	0.172 4	0.001 5	1 050	47.2	1 038	14.0	1 025	8.2	98
8	r	62	646	0.10	0.078 0	0.001 9	1.741 4	0.044 1	0.160 5	0.001 8	1 147	48.1	1 024	16.3	960	10.0	93
9	r	2	272	0.01	0.058 1	0.003 2	0.287 2	0.015 4	0.035 9	0.000 4	532	122	256	12.2	227	2.7	88
10	c	557	894	0.62	0.133 7	0.002 6	6.623 6	0.124 6	0.356 1	0.002 5	2 147	33.3	2 062	16.6	1 964	12.1	95
11	c	328	1 292	0.25	0.069 6	0.001 3	1.428 1	0.027 3	0.147 5	0.001 1	917	38.9	901	11.4	887	6.3	98
12	r	2.46	322	0.01	0.045 7	0.002 5	0.227 2	0.012 2	0.036 3	0.000 4			208	10.1	230	2.7	89
13	c	69	563	0.12	0.140 1	0.002 5	7.334 8	0.131 9	0.375 9	0.003 0	2 228	30.1	2 153	16.1	2 057	13.9	95
14	r	3	332	0.01	0.046 3	0.002 5	0.228 4	0.012 0	0.036 0	0.000 4	16.8	125.915	209	9.9	228	2.3	91
15	r	15	384	0.04	0.055 5	0.002 0	0.504 9	0.023 7	0.064 8	0.002 1	432	81.5	415	16.0	405	12.9	97
16	c	74	70	1.06	0.200 1	0.004 7	14.352 1	0.332 2	0.516 8	0.005 2	2 827	38.9	2 773	22.1	2 685	22.3	96
17	c	362	800	0.45	0.060 0	0.001 5	0.830 1	0.020 8	0.099 3	0.000 9	606	53.7	614	11.6	610	5.1	99
18	r	70	289	0.24	0.068 1	0.002 9	0.939 3	0.035 8	0.100 6	0.001 2	872	91.7	673	18.8	618	7.1	91
19	c	145	257	0.57	0.067 6	0.001 6	1.433 0	0.033 8	0.152 8	0.0014	857	50.5	903	14.1	917	7.6	98
20	r	102	401	0.25	0.067 3	0.001 5	1.231 6	0.027 9	0.132 0	0.001 4	856	46.3	815	12.7	799	7.9	98
21	c	76	323	0.23	0.066 5	0.001 4	1.469 4	0.031 1	0.159 2	0.001 2	833	44.4	918	12.8	953	6.9	96
22	c	629	439	1.43	0.067 3	0.001 4	1.549 2	0.032 1	0.166 1	0.001 3	856	-156.5	950	12.8	991	7.3	95
23	r	19	455	0.04	0.053 1	0.002 0	0.371 4	0.013 6	0.050 7	0.000 5	332	87.0	321	10.1	319	3.3	99
24	r	5	383	0.01	0.052 4	0.002 1	0.352 8	0.014 3	0.048 8	0.000 6	302	90.7	307	10.7	307	3.8	99
25	c	176	265	0.66	0.052 9	0.001 7	0.730 7	0.023 5	0.099 9	0.001 0	324	74.1	557	13.8	614	6.0	90
26	c	64	112	0.57	0.068 8	0.002 3	1.608 6	0.053 4	0.169 4	0.001 7	894	63.9	974	20.8	1 009	9.2	96
27	c	47	501	0.09	0.055 3	0.001 8	0.485 7	0.016 1	0.063 6	0.000 7	433	72.2	402	11.0	397	4.2	98
28	c	125	221	0.57	0.072 3	0.002 1	1.691 7	0.050 0	0.168 0	0.001 4	994	25.0	1 005	18.9	1 001	8.0	99
29	c	666	611	1.09	0.072 2	0.001 7	1.632 9	0.038 2	0.162 6	0.001 4	991	47.1	983	14.7	971	7.5	98
30	r	4	568	0.01	0.052 6	0.002 1	0.267 1	0.010 9	0.036 6	0.000 4	322	125.0	240	8.7	232	2.4	96
D116-3(混合岩)，核-边或核-幔-边结构
1	r	152	289	0.52	0.052 2	0.003 0	0.259 8	0.013 7	0.036 4	0.000 4	295	127	235	11.0	230	2.6	98
2	r	370	454	0.81	0.071 0	0.001 4	1.681 3	0.033 9	0.170 5	0.001 6	967	40.7	1 001	12.8	1 015	8.7	98
3	r	153	250	0.61	0.050 1	0.002 5	0.255 2	0.012 8	0.036 6	0.000 5	211	121	231	10.4	232	2.8	99
4	c	68	103	0.66	0.060 4	0.005 3	0.308 6	0.027 3	0.038 0	0.000 6	617	189	273	21.2	240	3.7	87
5	c	213	499	0.43	0.099 4	0.002 0	3.976 5	0.076 1	0.288 1	0.002 1	1 613	37.0	1 629	15.6	1 632	10.4	99
6	r	200	290	0.69	0.051 4	0.002 6	0.260 2	0.012 8	0.036 9	0.000 4	257	117	235	10.3	234	2.7	99
7	r	167	239	0.70	0.054 8	0.003 3	0.293 9	0.017 0	0.039 1	0.0004	467	133	262	13.3	247	2.7	94
8	r	100	235	0.42	0.054 0	0.002 9	0.269 2	0.014 0	0.036 8	0.000 5	372	129	242	11.2	233	3.0	96
9	r	55	334	0.16	0.050 4	0.002 5	0.250 1	0.012 2	0.035 9	0.000 4	213	114	227	10.0	227	2.4	99
10	r	71	199	0.36	0.193 9	0.007 0	1.430 0	0.057 2	0.052 9	0.000 7	2 776	59.3	902	23.9	332	4.5	7
11	c	197	862	0.23	0.050 8	0.001 5	0.257 2	0.007 5	0.036 6	0.000 3	235	70.4	232	6.1	232	1.9	99
12	r	7	821	0.01	0.0506	0.001 7	0.254 7	0.008 3	0.036 6	0.000 4	233	77.8	230	6.7	232	2.3	99
13	c	1 470	583	2.52	0.070 5	0.001 5	1.518 5	0.032 3	0.155 2	0.001 2	943	43.7	938	13.0	930	6.9	99
14	m	46	72.5	0.63	0.083 6	0.009 9	0.431 6	0.049 6	0.038 5	0.000 9	1 283	233	364	35.2	244	5.5	60
15	r	6	991	0.01	0.051 0	0.001 9	0.254 1	0.008 9	0.036 1	0.000 3	239	83.3	230	7.2	228	1.8	99
16	r	65	587	0.11	0.051 9	0.002 3	0.260 1	0.011 0	0.036 7	0.0004	280	106.5	235	8.8	232	2.7	98
17	r	6	918	0.01	0.051 5	0.001 8	0.256 0	0.008 6	0.036 1	0.000 3	261	75.0	231	7.0	228	2.2	98
18	c	33	574	0.06	0.069 5	0.001 7	1.282 5	0.030 1	0.133 0	0.001 1	922	48.9	838	13.4	805	6.0	96
19	r	29	902	0.03	0.054 8	0.001 7	0.290 0	0.010 2	0.037 9	0.000 5	467	70.4	259	8.1	240	3.2	92
20	c	133	214	0.62	0.073 8	0.002 0	1.644 9	0.044 4	0.160 7	0.001 4	1 035	59.7	988	17.1	961	7.8	97
21	c	353	46 083	0.01	0.297 0	0.010 3	1.835 1	0.057 6	0.045 2	0.000 7	3 455	54.7	1 058	20.7	285	4.2	-16
22	c	65	163	0.40	0.052 2	0.004 7	0.255 6	0.021 6	0.036 9	0.000 6	300	207	231	17.4	234	3.6	98
23	r	82	125	0.66	0.130 0	0.003 1	6.633 2	0.159 3	0.367 3	0.003 3	2 098	42.3	2 064	21.2	2 017	15.8	97
24	r	180	780	0.23	0.056 5	0.003 5	0.266 1	0.016 5	0.034 0	0.000 4	472	137	240	13.2	215	2.7	89
25	c	220	276	0.80	0.049 0	0.003 8	0.250 0	0.017 2	0.035 9	0.000 5	146	170	227	14.0	228	2.9	99
26	r	19	589	0.03	0.071 2	0.003 5	0.470 9	0.032 6	0.045 3	0.0014	965	100	392	22.5	286	8.5	68
27	r	194	306	0.63	0.050 6	0.003 2	0.252 6	0.015 4	0.036 6	0.000 5	233	144	229	12.5	232	3.1	98
28	r	72	150	0.48	0.050 2	0.005 4	0.251 3	0.025 9	0.036 2	0.000 6	211	224	228	21.0	229	3.6	99
29	r	10	1 038	0.01	0.111 5	0.004 6	0.556 1	0.024 4	0.035 7	0.000 4	1 824	75.2	449	15.9	226	2.3	33
30	c	82	228	0.36	0.160 9	0.003 1	10.185 5	0.199 1	0.456 7	0.003 6	2 466	32.4	2 452	18.2	2 425	15.8	98
31	r	132	265	0.50	0.052 7	0.003 3	0.262 8	0.016 0	0.037 1	0.000 5	322	143	237	12.9	235	3.1	99
15BR04(花岗质片麻岩)，核-边结构为主，少量核-幔-边结构
01	r	217	7 930	0.03	0.051 8	0.001 2	0.276 9	0.006 6	0.038 5	0.000 3	276	53.7	248	5.3	244	1.8	98
02	c	516	792	0.65	0.055 7	0.002 0	0.581 1	0.021 0	0.075 2	0.000 7	443	76.8	465	13.5	467	4.1	99
03	r	1 582	18 896	0.08	0.083 2	0.001 6	0.420 3	0.008 2	0.036 4	0.000 3	1 273	37.5	356	5.9	231	1.9	57
04	c	723	907	0.80	0.055 8	0.001 9	0.571 1	0.019 6	0.073 8	0.000 7	443	74.1	459	12.7	459	4.3	99
05	c	592	880	0.67	0.054 7	0.002 2	0.560 3	0.022 8	0.074 1	0.000 8	398	90.7	452	14.8	461	4.9	98
06	r	1 090	11 359	0.10	0.060 3	0.001 4	0.360 3	0.008 1	0.043 1	0.000 3	613	50.0	312	6.1	272	2.0	86
07	c	683	1 261	0.54	0.055 8	0.001 7	0.575 5	0.018 2	0.074 3	0.000 9	456	66.7	462	11.7	462	5.4	99
08	c	530	1 007	0.53	0.055 8	0.001 9	0.579 8	0.020 1	0.075 1	0.000 8	456	75.9	464	12.9	467	4.6	99
09	r	1 652	15 414	0.11	0.061 7	0.001 8	0.311 1	0.009 4	0.036 4	0.0004	665	63.0	275	7.3	230	2.2	82
10	c	523	1 152	0.45	0.073 1	0.002 5	0.675 9	0.023 8	0.066 9	0.000 9	1 017	68.5	524	14.4	417	5.5	77
11	c	512	1 060	0.48	0.058 3	0.002 0	0.684 5	0.023 0	0.085 0	0.000 8	543	74.1	529	13.8	526	4.7	99
12	c	356	889	0.40	0.057 3	0.001 8	0.579 2	0.018 1	0.073 1	0.000 8	502	66.7	464	11.7	455	4.7	97
13	c	1 092	1 519	0.72	0.055 2	0.001 4	0.562 0	0.014 9	0.073 5	0.000 6	420	57.4	453	9.7	457	3.5	99
14	c	661	930	0.71	0.055 0	0.001 6	0.557 0	0.016 2	0.073 2	0.000 7	413	64.8	450	10.6	455	4.0	98
15	c	344	519	0.66	0.053 5	0.002 0	0.539 8	0.020 1	0.073 4	0.0009	350	85.2	438	13.2	457	5.2	95
16	r	1 060	10 099	0.10	0.060 7	0.001 5	0.304 0	0.006 7	0.036 3	0.000 3	628	51.8	269	5.3	230	1.9	84
17	r	3 416	15 123	0.23	0.075 0	0.002 1	0.381 7	0.010 1	0.036 8	0.000 3	1 133	54.5	328	7.5	233	2.1	65
18	r	97	5 303	0.02	0.052 8	0.001 4	0.313 9	0.008 7	0.042 9	0.000 5	320	65.7	277	6.7	271	3.4	97
19	r	296	16 710	0.02	0.057 6	0.001 3	0.288 7	0.007 0	0.036 0	0.000 4	517	50.0	258	5.5	228	2.3	87
20	r	381	9 853	0.04	0.055 4	0.001 3	0.321 7	0.007 3	0.041 9	0.000 4	428	51.8	283	5.6	264	2.2	93
21	r	602	19 102	0.03	0.211 9	0.004 8	1.597 8	0.041 1	0.053 9	0.000 6	2 920	41.8	969	16.1	339	3.4	3
22	r	1 797	26 530	0.07	0.072 1	0.001 5	0.293 1	0.006 0	0.029 2	0.000 2	991	41.8	261	4.7	186	1.5	66
23	c	1 819	2 348	0.77	0.057 3	0.001 4	0.585 5	0.014 5	0.073 4	0.000 7	506	58.3	468	9.3	457	4.3	97
24	r	1 162	26 617	0.04	0.071 3	0.001 5	0.261 4	0.005 6	0.026 5	0.000 3	966	42.6	236	4.5	169	2.2	66
ID7-3(条带状混合岩)，核-边或核-幔-边结构
1	r	115	297	0.39	0.175 6	0.006 0	9.480 6	0.315 5	0.383 9	0.004 0	2 613	90	2 386	31	2 095	19	87
2	c	235	491	0.48	0.177 9	0.005 1	9.188 3	0.265 6	0.367 6	0.003 8	2 635	48	2 357	27	2 018	18	84
3	r	13	1 102	0.01	0.053 3	0.002 0	0.274 7	0.009 9	0.037 1	0.000 4	339	92	246	8	235	2	95
4	r	131	2 373	0.06	0.051 5	0.001 5	0.494 6	0.014 7	0.068 6	0.000 7	265	69	408	10	427	4	95
5	c	30	1 662	0.02	0.050 4	0.001 8	0.259 2	0.009 3	0.036 7	0.000 4	217	85	234	8	233	3	99
6	r	67	1 375	0.05	0.059 3	0.001 7	0.856 5	0.030 1	0.102 3	0.002 0	589	58	628	16	628	12	99
7	r	130	222	0.59	0.066 7	0.002 6	1.046 6	0.042 0	0.112 0	0.001 6	828	80	727	21	684	9	93
8	r	214	1 045	0.21	0.054 8	0.001 7	0.526 2	0.015 4	0.068 7	0.000 6	467	73	429	10	428	3	99
9	r	176	461	0.38	0.050 4	0.002 0	0.489 5	0.019 7	0.069 4	0.000 8	213	91	405	13	433	5	93
10	r	45	1 042	0.04	0.116 4	0.003 0	4.951 6	0.139 6	0.301 4	0.003 5	1 902	47	1 811	24	1 698	17	93
11	r	287	463	0.62	0.053 9	0.002 3	0.512 1	0.021 1	0.068 5	0.000 7	369	64	420	14	427	4	98
12	r	177	206	0.86	0.059 7	0.003 4	0.566 3	0.031 9	0.068 8	0.000 9	591	131	456	21	429	6	93
13	c	93	254	0.37	0.054 5	0.003 2	0.565 9	0.032 9	0.074 4	0.000 9	394	133	455	21	462	5	98
14	r	36	2 519	0.01	0.052 2	0.001 7	0.254 5	0.008 0	0.034 8	0.000 3	300	74	230	6	221	2	95
15	r	103	218	0.47	0.053 7	0.003 4	0.5383	0.035 4	0.071 7	0.001 3	367	143	437	23	446	8	97
16	c	381	1 148	0.33	0.074 6	0.001 8	1.815 9	0.043 9	0.173 6	0.001 4	1 057	49	1 051	16	1 032	8	98
17	c	118	271	0.44	0.057 6	0.003 1	0.566 3	0.030 6	0.070 6	0.000 9	522	121	456	20	440	6	96
18	r	449	607	0.74	0.059 8	0.002 2	0.576 6	0.020 6	0.069 3	0.000 7	594	77	462	13	432	4	93
19	c	156	484	0.32	0.070 9	0.002 2	1.602 9	0.048 3	0.161 4	0.001 7	955	62	971	19	965	9	99
20	r	276	645	0.43	0.096 1	0.002 9	3.545 5	0.103 1	0.263 6	0.002 3	1 550	57	1 537	23	1 508	12	98
21	c	10	670	0.02	0.055 2	0.003 2	0.283 5	0.018 0	0.036 7	0.000 9	420	130	253	14	232	5	91
22	r	31	2 248	0.01	0.052 3	0.001 7	0.263 0	0.008 5	0.036 0	0.000 3	298	69	237	7	228	2	96
23	r	91	506	0.18	0.072 6	0.002 1	1.468 1	0.040 6	0.145 2	0.001 2	1 011	58	917	17	874	7	95
24	c	217	265	0.82	0.092 4	0.002 6	3.341 2	0.092 6	0.259 1	0.002 3	1 476	53	1 491	22	1 485	12	99
25	r	23	2 020	0.01	0.048 6	0.0014	0.251 0	0.007 3	0.037 0	0.000 3	128	67	227	6	234	2	97
26	c	197	521	0.38	0.074 0	0.002 0	1.675 0	0.044 4	0.162 6	0.001 7	1 043	54	999	17	971	9	97
27	r	418	1 465	0.29	0.052 5	0.001 4	0.550 6	0.015 6	0.075 3	0.000 8	306	63	445	10	468	5	95
28	r	111	116	0.96	0.057 4	0.003 5	0.976 4	0.059 0	0.124 3	0.001 8	509	137	692	30	755	10	91
29	r	215	566	0.38	0.052 4	0.002 1	0.496 4	0.020 2	0.067 7	0.000 7	306	89	409	14	422	4	96
30	c	326	461	0.71	0.069 1	0.002 0	1.524 3	0.043 9	0.158 3	0.001 4	903	59	940	18	947	8	99
31	r	88	2 692	0.03	0.053 5	0.001 4	0.507 9	0.012 8	0.068 2	0.000 6	350	53	417	9	425	3	98
32	m	23	592	0.04	0.057 9	0.001 9	0.762 7	0.025 1	0.094 7	0.000 9	528	74	576	14	583	5	98
33	r	89	2 138	0.04	0.055 9	0.001 4	0.520 0	0.013 4	0.066 8	0.000 6	456	56	425	9	417	3	97
34	r	7	618	0.01	0.056 1	0.002 8	0.325 3	0.016 2	0.041 9	0.000 7	454	109	286	12	264	4	92
35	c	443	523	0.85	0.056 7	0.002 1	0.541 3	0.020 0	0.069 0	0.000 7	480	83	439	13	430	4	97
36	r	89	1 464	0.06	0.058 1	0.001 9	0.558 2	0.018 6	0.069 0	0.000 6	532	75	450	12	430	4	95
37	r	102	212	0.48	0.062 6	0.002 9	1.005 9	0.047 5	0.116 1	0.001 5	694	100	707	24	708	9	99
38	c	173	203	0.85	0.070 2	0.002 8	1.595 8	0.061 8	0.165 2	0.001 8	1 000	82	969	24	986	10	98
39	r	186	328	0.57	0.061 9	0.002 7	0.600 1	0.026 9	0.069 9	0.000 8	733	94	477	17	436	5	90
40	r	10	1 245	0.01	0.053 5	0.001 7	0.487 4	0.015 3	0.065 6	0.000 5	350	70	403	10	409	3	98
41	c	190	295	0.64	0.060 4	0.0028	0.588 3	0.026 6	0.071 1	0.000 8	620	100	470	17	443	5	94
42	r	5	416	0.01	0.055 4	0.003 2	0.275 0	0.015 2	0.036 4	0.000 4	428	126	247	12	231	3	93
ID7-5(花岗岩脉)，核-边结构
1	r	92	1 103	0.08	0.050 4	0.001 8	0.255 8	0.008 8	0.036 6	0.000 4	213	86.1	231	7	232	2	99
2	c	78	1 323	0.06	0.067 3	0.001 8	1.130 8	0.030 2	0.120 6	0.001 2	856	55.6	768	14	734	7	95
3	r	41	668	0.06	0.056 1	0.001 9	0.545 1	0.020 3	0.069 6	0.001 1	454	69.4	442	13	434	7	98
4	r	23.5	973	0.02	0.050 0	0.002 0	0.248 2	0.009 6	0.035 8	0.000 3	195	92.6	225	8	227	2	99
5	r	140	436	0.32	0.064 3	0.002 5	0.624 4	0.027 9	0.069 2	0.001 8	750	83.3	493	17	431	11	86
6	r	102	1 068	0.10	0.050 2	0.0018	0.261 5	0.009 6	0.037 4	0.000 4	211	85.2	236	8	237	2	99
7	r	295	1 157	0.26	0.050 0	0.001 8	0.244 0	0.008 6	0.035 1	0.000 3	195	83.3	222	7	222	2	99
8	r	415	833	0.50	0.050 8	0.002 1	0.252 8	0.010 5	0.035 8	0.000 4	232	98.1	229	9	227	2	99
9	r	340	1 456	0.23	0.050 3	0.001 8	0.248 1	0.008 4	0.035 6	0.000 4	209	81.5	225	7	225	2	99
10	r	305	1 450	0.21	0.050 6	0.001 8	0.255 7	0.009 1	0.036 3	0.000 3	220	50.9	231	7	230	2	99
11	c	433	1 140	0.38	0.056 0	0.002 0	0.273 8	0.009 6	0.035 4	0.000 3	450	79.6	246	8	224	2	90
12	r	212	6 335	0.03	0.054 1	0.001 7	0.264 5	0.009 1	0.035 2	0.000 5	376	76.8	238	7	223	3	93
13	r	298	653	0.46	0.056 2	0.002 7	0.289 8	0.013 9	0.037 4	0.000 4	461	106	258	11	237	3	91
14	r	229	524	0.44	0.052 8	0.003 0	0.263 5	0.015 0	0.036 3	0.000 4	320	134	238	12	230	3	96
15	r	235	611	0.38	0.052 0	0.002 7	0.262 6	0.014 0	0.036 6	0.000 4	283	150	237	11	232	3	97
16	r	932	3 530	0.26	0.053 2	0.002 2	0.271 3	0.011 7	0.036 9	0.000 4	339	94.4	244	9	233	2	95
17	r	256	580	0.44	0.053 9	0.003 0	0.276 6	0.015 9	0.037 3	0.000 5	369	132	248	13	236	3	95
18	r	108	851	0.13	0.062 9	0.002 3	0.614 4	0.024 9	0.070 7	0.001 4	706	75.0	486	16	440	8	90
19	r	239	606	0.39	0.049 1	0.002 4	0.255 0	0.012 5	0.037 5	0.000 4	154	115	231	10	237	3	97
20	r	147	308	0.48	0.051 0	0.003 8	0.257 5	0.018 9	0.036 5	0.000 5	239	203	233	15	231	3	99
注：c.锆石核部；m.锆石幔部；r.锆石边部.

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表 2 云开地块变质岩锆石Lu-Hf同位素分析结果

Table 2. Zircon Lu-Hf isotopic compositions of metamorphic rocks in Yunkai massif

点号	年龄(Ma)	¹⁷⁶Hf/¹⁷⁷Hf	2σ	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Yb/¹⁷⁷Hf	ε_Hf(t)	T_DM1(Ma)	T_DM2(Ma)	f_Lu/Hf
1431-1(眼球状混合片麻岩)
01	448	0.282 468	0.000 015	0.001 753	0.046 160	-1.4	1 132	1 520	-0.95
02	434	0.282 294	0.000 018	0.001 041	0.026 061	-7.7	1 355	1 905	-0.97
03	445	0.282 437	0.000 020	0.001 418	0.037 749	-2.5	1 167	1 585	-0.96
04	450	0.282 624	0.000 016	0.002 280	0.059 929	4.0	921	1 178	-0.93
05	442	0.282 428	0.000 015	0.001 235	0.031 850	-2.8	1 173	1 603	-0.96
06	429	0.282 437	0.000 016	0.001 495	0.038 807	-2.8	1 168	1 594	-0.95
07	427	0.282 591	0.000 017	0.002 563	0.068 942	2.3	977	1 268	-0.92
08	444	0.282 320	0.000 015	0.000 879	0.022 018	-6.5	1 313	1 837	-0.97
09	444	0.282 639	0.000 032	0.002 762	0.072 882	4.2	912	1 157	-0.92
10	432	0.282 499	0.000 015	0.001 887	0.048 346	-0.7	1 091	1 461	-0.94
11	440	0.282 342	0.000 013	0.000 860	0.021 631	-5.8	1 282	1 790	-0.97
12	424	0.282 478	0.000 012	0.001 527	0.039 823	-1.5	1 111	1 507	-0.95
13	436	0.282 563	0.000 016	0.002 470	0.062 280	1.5	1 016	1 326	-0.93
14	446	0.282 588	0.000 017	0.002 427	0.063 446	2.6	978	1 264	-0.93
15	439	0.282 566	0.000 022	0.002 209	0.057 846	1.7	1 003	1 312	-0.93
16	448	0.282 472	0.000 014	0.001 320	0.032 147	-1.2	1 113	1 502	-0.96
17	426	0.282 350	0.000 016	0.001 316	0.033 605	-5.9	1 286	1 789	-0.96
18	438	0.282 485	0.000 015	0.001 825	0.048 092	-1.1	1 110	1 488	-0.95
19	445	0.282 417	0.000 017	0.001 223	0.031 860	-3.1	1 188	1 625	-0.96
20	450	0.282 496	0.000 015	0.002 040	0.053 560	-0.5	1 101	1 461	-0.94
21	439	0.282 416	0.000 021	0.001 765	0.046 068	-3.4	1 207	1 641	-0.95
23	436	0.282 439	0.000 015	0.001 318	0.034 035	-2.6	1 160	1 583	-0.96
24	451	0.282 492	0.000 014	0.001 525	0.039 717	-0.4	1 091	1 460	-0.95
25	446	0.282 521	0.000 015	0.001 872	0.049 339	0.4	1 059	1 403	-0.94
26	443	0.282 448	0.000 014	0.001 409	0.037 540	-2.1	1 150	1 560	-0.96
1432-1(条带状混合片麻岩)
01	228	0.281 936	0.000 048	0.000 262	0.006 999	-24.6	1 816	2 816	-0.99
02	1 656	0.281 558	0.000 014	0.000 564	0.014 335	-6.8	2 346	2 772	-0.98
03	1 150	0.281 836	0.000 014	0.000 407	0.009 754	-8.0	1 960	2 464	-0.99
04	234	0.282 257	0.000 018	0.000 224	0.006 124	-13.1	1 377	2 098	-0.99
05	2 313	0.281 723	0.000 016	0.002 010	0.049 768	11.6	2 203	2 143	-0.94
06	863	0.281 635	0.000 012	0.001 300	0.034 471	-21.9	2 285	3 117	-0.96
07	1 050	0.282 242	0.000 022	0.001 906	0.050 251	3.1	1 461	1 692	-0.94
08	960	0.282 154	0.000 016	0.000 704	0.018 665	-1.1	1 537	1 890	-0.98
09	227	0.282 011	0.000 028	0.000 268	0.006 986	-22.0	1 715	2 652	-0.99
12	230	0.282 312	0.000 015	0.000 143	0.003 990	-11.3	1 299	1 978	-1.00
13	2 228	0.281 222	0.000 011	0.000 296	0.008 632	-5.5	2 781	3 128	-0.99
14	228	0.282 298	0.000 012	0.000 514	0.013 413	-11.8	1 330	2 012	-0.98
15	405	0.282 260	0.000 015	0.000 405	0.009 098	-9.3	1 379	1 987	-0.99
16	2 827	0.280 883	0.000 032	0.000 268	0.007 300	-3.8	3 229	3 482	-0.99
17	610	0.282 382	0.000 016	0.000 797	0.021 576	-0.7	1 223	1 595	-0.98
19	917	0.282 145	0.000 024	0.001 189	0.031 299	-2.7	1 569	1 955	-0.96
21	953	0.282 619	0.000 016	0.001 040	0.025 766	15.0	898	866	-0.97
22	991	0.281 988	0.000 013	0.000 902	0.023 044	-6.5	1 775	2 248	-0.97
25	614	0.282 390	0.000 022	0.000 594	0.014 459	-0.2	1 206	1 571	-0.98
26	1 009	0.282 023	0.000 016	0.000 779	0.020 820	-4.7	1 720	2 153	-0.98
27	397	0.282 409	0.000 015	0.000 778	0.021 401	-4.3	1 185	1 663	-0.98
28	1 001	0.282 178	0.000 014	0.000 746	0.019 867	0.6	1 505	1 812	-0.98
29	971	0.282 690	0.000 020	0.003 444	0.094 073	16.4	852	793	-0.90
30	232	0.282 251	0.000 017	0.000 115	0.003 486	-13.3	1 381	2 111	-1.00
D116-3(混合岩)
01	230	0.282 818	0.000 017	0.001 068	0.027 294	6.5	616	847	-0.97
02	1 015	0.282 234	0.000 013	0.001 093	0.030 814	2.7	1 441	1 694	-0.97
03	232	0.282 753	0.000 021	0.001 374	0.035 760	4.2	715	996	-0.96
05	1 612	0.281 877	0.000 017	0.000 671	0.017 897	3.5	1 917	2 103	-0.98
06	234	0.282 923	0.000 016	0.001 621	0.042 230	10.2	474	612	-0.95
07	247	0.282 619	0.000 011	0.000 416	0.010 888	-0.1	884	1 281	-0.99
08	233	0.282 542	0.000 012	0.000 229	0.006 513	-3.0	985	1 459	-0.99
09	227	0.282 537	0.000 017	0.000 726	0.016 422	-3.4	1 005	1 480	-0.98
11	232	0.282 571	0.000 030	0.001 173	0.028 255	-2.2	969	1 404	-0.96
12	232	0.282 420	0.000 014	0.000 977	0.023 338	-7.5	1 177	1 743	-0.97
15	228	0.282 401	0.000 035	0.001 627	0.038 922	-8.4	1 224	1 793	-0.95
17	228	0.282 330	0.000 027	0.001 035	0.026 165	-10.8	1 304	1 946	-0.97
20	961	0.282 257	0.000 015	0.000 612	0.015 639	2.6	1 391	1 655	-0.98
22	234	0.282 516	0.000 011	0.000 128	0.003 789	-4.0	1 019	1 518	-1.00
27	232	0.282 683	0.000 010	0.000 806	0.022 699	1.8	803	1 150	-0.98
28	229	0.282 432	0.000 020	0.000 132	0.003 970	-7.0	1 135	1 710	-1.00
31	235	0.282 617	0.000 018	0.000 565	0.016 434	-0.4	890	1 295	-0.98
ID7-3(条带状混合岩)
01	2613	0.281 283	0.000 013	0.001 097	0.024 874	4.1	2 755	2 839	-0.97
03	235	0.282 155	0.000 011	0.000 090	0.002 561	-16.7	1 511	2 324	-1.00
04	427	0.282 397	0.000 014	0.001 344	0.035 268	-4.3	1 221	1 684	-0.96
05	233	0.282 212	0.000 010	0.000 016	0.000 532	-14.7	1 431	2 198	-1.00
08	428	0.282 513	0.000 009	0.002 136	0.050 505	-0.4	1 079	1 437	-0.94
09	433	0.282 375	0.000 008	0.000 956	0.023 856	-4.8	1 239	1 723	-0.97
11	427	0.282 341	0.000 012	0.000 791	0.019 131	-6.1	1 280	1 798	-0.98
12	429	0.282 325	0.000 011	0.000 962	0.023 720	-6.6	1 308	1 836	-0.97
14	221	0.282 190	0.000 024	0.000 275	0.006 514	-15.8	1 471	2 257	-0.99
15	446	0.282 399	0.000 010	0.001 095	0.026 459	-3.7	1 210	1 664	-0.97
17	440	0.282 392	0.000 010	0.001 256	0.029 347	-4.1	1 224	1 685	-0.96
21	232	0.281 691	0.000 030	0.000 452	0.011 587	-33.2	2 158	3 356	-0.99
22	228	0.282 128	0.000 008	0.000 161	0.004 703	-17.8	1 551	2 389	-1.00
25	234	0.282 216	0.000 021	0.000 147	0.004 027	-14.5	1 430	2 189	-1.00
27	468	0.282 392	0.000 011	0.001 212	0.030 833	-3.5	1 223	1 668	-0.96
29	422	0.282 360	0.000 013	0.001 060	0.025729	-5.6	1 263	1 764	-0.97
33	417	0.282 310	0.000 013	0.001 162	0.027 958	-7.5	1 337	1 881	-0.96
35	430	0.282 490	0.000 014	0.002 036	0.049 664	-1.1	1 109	1 485	-0.94
36	430	0.282 201	0.000 012	0.000 822	0.020 732	-11.0	1 477	2 111	-0.98
39	436	0.282 402	0.000 012	0.001 227	0.029 842	-3.9	1 210	1 665	-0.96
40	409	0.282 271	0.000 010	0.000 735	0.019 771	-8.9	1 376	1 965	-0.98
41	443	0.282 361	0.000 011	0.001 050	0.025 305	-5.1	1 261	1 749	-0.97
42	231	0.282 238	0.000 033	0.000 022	0.000 762	-13.8	1 395	2 140	-1.00

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表 3 云开地区印支期变质年龄统计表

Table 3. Summary of Indosinian metamorphic ages in Yunkai region

样号	岩性	采样位置	数据来源	定年方法	年龄(Ma)	成因分类
1432-1	混合片麻岩	信宜			230.2±2.9	区域变质
D116-3	混合岩	罗定			229.6±2.1	(或深熔)
D116-3	混合岩	罗定	本文	LA-ICPMS锆石U-Pb	231.3±1.6	作用
ID7-3	条带状混合岩	高州			229.2±5.4	流体活动
15BR04	花岗质片麻岩	北流炳荣			244.0±1.8
GD-131	基性麻粒岩	钦州那蒙			238.0±8.0
GD-132	基性麻粒岩	钦州大寺		SHRIMP锆石U-Pb	244.0±7.0
GD-4	含石榴子石角闪岩	高州谢鸡	Wang et al., 2012	SHRIMP锆石U-Pb	230.0±6.0
YK-13	斜长角闪岩	容县黎村			248.0±6.0
YK-9A	混合岩化角闪岩	信宜金垌			221.0±4.0
09YK-8B	正片麻岩	信宜	Wang et al., 2011	LA-ICPMS锆石U-Pb	203.0±10.0
09YK-12	正片麻岩	容县黎村	Wang et al., 2011		239.0±6.0
02YK-42	正片麻岩	电白	Wang et al., 2007d	SHRIMP锆石U-Pb	236.0±3.0
L114	矽线石榴堇青片麻岩	云开	Wan et al., 2010	SHRIMP锆石U-Pb	242.0±8.0
GZ-0307	片麻状混合岩	高州云炉	Wang et al., 2013b	LA-ICPMS锆石U-Pb	241.0±3.0
GZ-08	正片麻岩	高州云炉		LA-ICPMS锆石U-Pb	238.0±4.0
GZ-03	紫苏花岗岩	高州云炉	Chen et al., 2012	电子探针独居石U-Th-Pb	231.0±9.0
23GX-11	副片麻岩	高州云炉		电子探针独居石U-Th-Pb	237.0±13.0
23GX04	黑云母片麻岩	高州	Chen et al., 2017	LA-ICPMS锆石U-Pb	229.0±10.0	区域变质
11GD04	黑云母片麻岩	高州	Chen et al., 2017	LA-ICPMS锆石U-Pb	245.0±5.0	(或深熔)
11GD01	片麻状花岗岩	高州			233.0±4.0	作用
11GDGZA1	片麻状花岗岩	高州			233.0±5.0
23GX04	黑云母片麻岩	高州			237.0±3.0
23GX05-2	黑云母片麻岩	高州			234.0±5.0
23GX15	二云母片麻岩	高州			236.0±4.0
11GD06	二云母片麻岩	高州	Chen et al., 2017	电子探针独居石U-Th-Pb	240.0±4.0
11GD07	片麻状花岗岩	高州	Chen et al., 2017	电子探针独居石U-Th-Pb	233.0±11.0
23GX13-2	黑云母片麻岩	高州			~240.0
23GX14	石榴石电气石片岩	高州			236.0±8.0
11GD03	石榴石电气石片岩	高州			244.0±11.0
11GD04	黑云母片麻岩	高州			236.0±5.0
11GD05	黑云母片麻岩	高州			239.0±6.0
--	泥质麻粒岩	钦州旧州	赵亮等，2010	LA-ICPMS锆石U-Pb	253.0±3.0
hdt-2	基性麻粒岩	钦州大龟山	彭松柏等，2004	SHRIMP锆石U-Pb	248.0±6.0
Datong 1	糜棱岩	合浦			213.0±4.0
Datong 2	糜棱岩	合浦	Zhang and Cai, 2009	白云母Ar-Ar	212.0±3.0
Hetai 1	糜棱岩	北流	Zhang and Cai, 2009	白云母Ar-Ar	199.0±1.0
Hetai 2	糜棱岩	北流			195.0±1.0
02YK-27	糜棱状花岗岩	信宜			230.0±1.0
02YK-30	花岗质糜棱岩	信宜白石			225.0±1.0
02YK-38	糜棱状片麻岩	高州			222.0±1.0
02YK-74	糜棱状副片麻岩	信宜			228.0±1.0
02YK-39	糜棱状混合岩	高州谢鸡			225.0±1.0
02YK-09	糜棱状片麻岩	阳春			208.0±1.0
02YK-12	糜棱状片麻岩	阳春	Wang et al., 2007c	黑云母Ar-Ar	209.0±1.0
02YK-15	糜棱岩	阳春永宁			212.0±1.0	构造变形
02YK-56	花岗质糜棱岩	博白			219.0±1.0
02YK-64	糜棱岩	容县黎村			211.0±1.0
02YK-80	糜棱状花岗岩	罗定榃滨			209.0±1.0
02YK-26	糜棱状片麻岩	信宜钱排			214.0±1.0
02YK-31	糜棱状花岗岩	信宜白石			217.0±1.0
G13Y1	片岩	罗定泗纶	彭少梅等，1996	白云母Ar-Ar	249.0±3.0
G03Y1	片理化片麻状花岗岩	阳春	彭少梅等，1996	白云母Ar-Ar	229.0±2.0
G13Y1	混合岩	罗定泗纶			250.0±3.0
G12Y2	石英片岩质糜棱岩	分界	邵建国等，1995	白云母Ar-Ar	255.0±3.0
G03Y1	糜棱状花岗岩	永宁			229.0±3.0
Jiangshan1	绢云母千糜岩	防城江山	丁汝鑫等，2015	绢云母Ar-Ar	244.8±0.6
Jiangshan2	绢云母千糜岩				203.9±1.7
14HT060	糜棱岩	河台金矿	焦骞骞等，2017	LA-ICPMS锆石U-Pb	240.1±4.1	流体活动
14HT111	糜棱岩	河台金矿	焦骞骞等，2017	LA-ICPMS锆石U-Pb	204.1±4.3

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