湘桂边界越城岭岩基北部印支期花岗岩锆石U-Pb年代学和地球化学特征

程顺波; 付建明; 崔森; 卢友月; 马丽艳; 刘阿睢

doi:10.3799/dqkx.2018.178

湘桂边界越城岭岩基北部印支期花岗岩锆石U-Pb年代学和地球化学特征

doi: 10.3799/dqkx.2018.178

程顺波^1,2,,
付建明^1,2,
崔森^1,2, ,,
卢友月^1,2,
马丽艳^1,2,
刘阿睢^1,2

1.
中国地质调查局武汉地质调查中心, 湖北武汉 430205
2.
中国地质调查局花岗岩成岩成矿研究中心, 湖北武汉 430205

基金项目:

中地质调查局项目 121201009000150012

中地质调查局项目 121201009000150002

详细信息

作者简介:
程顺波(1983-), 男, 助理研究员, 从事华南地质过程与成矿作用研究

通讯作者:
崔森

中图分类号: P597
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- 被引次数: 0
出版历程
- 收稿日期: 2018-03-15
- 刊出日期: 2018-07-15

Zircon U-Pb Chronology, Geochemistry of the Indonesian Granitic Rocks from Northern Yuechengling Batholith in Guangxi-Hunan Junction

Cheng Shunbo^{1,2
,},
Fu Jianming^1,2,
Cui Sen^{1,2
, ,},
Lu Youyue^1,2,
Ma Liyan^1,2,
Liu A'sui^1,2

1.
Wuhan Center of Chinese Geological Survey, Wuhan 430205, China
2.
Research Center of Granitic Diagenesis and Mineralization, Chinese Geological Survey, Wuhan 430205, China

摘要

摘要: 湘桂边界越城岭岩基北部印支期花岗岩时空分布和岩石成因目前还不明确.以该时期花岗岩为研究对象，进行了岩石学、锆石U-Pb年代学、地球化学和Nd-Hf同位素组成研究.研究结果显示，印支期花岗岩主要分布在湘桂边界以北区域，形成时代236~222 Ma.岩性以含电气石的二长花岗岩为主，副矿物组合为锆石、（斜）黝帘石、磷灰石、石榴石，并具有高硅、富碱，贫钙、镁和磷，弱-强过铝质的地球化学特征.早阶段花岗岩源岩主要为变质杂砂岩，可能混入了少许新生地壳组分；晚阶段花岗岩源岩由不同比例的变质泥质岩石和变质杂砂岩组成.花岗岩具有负且稳定的锆石ε_Nd（t）值（-9.3~-10.6）和ε_Hf（t）值（-5.4~-11.9），反映源区平均地壳存留年龄为1.8 Ga左右.花岗质岩浆的形成受控于华南印支期后造山加厚地壳背景下变沉积岩中云母类矿物的脱水熔融过程，其运移和就位与岩基旁侧深大断裂的松弛调整密切相关.
- 锆石U-Pb年代学 /
- 地球化学 /
- Nd-Hf同位素 /
- 印支期 /
- 湘桂边界
Abstract: The temporal and spatial distribution of Indonesian granitoid in northern Yuechengling batholith is still uncertained. In this paper, a compilation of petrology, zircon U-Pb chronology, geochemistry and Nd-Hf isotopes was used on the granitoid to solve this uncertainty. The result shows Indonesian granitoid spreads in north area of the border with the age of 236-222 Ma, and mainly consists of medium to fine grained tourmaline-bearing monzogranites, with accessory minerals assemblage of zircon, zoisite (and/or clinozoisite), apatite and garnet. The granitic samples have characteristics of high SiO₂, alkaline, low CaO, MgO, P₂O₅ contents, and weak to strong peraluminous (A/CNK=1.07-1.17), with enrichment of Rb, Th, U and strong depletion of Ba, Sr, Eu, Nb, Ti elements. Source of early stage of Indonesian granitic rocks mainly consisting of metagreywackes, with small amount of new crustal component. Those of late stage are inhomogeneous mixing of metagreywackes and metapelites. Granitic rocks of both stage have stable high negative ε_Nd(t)(-9.3——10.6) and ε_Hf(t) (-5.4——11.9) ratios with source's average crustal residence age of ca 1.8 Ga. Integrated with Indonesian tectonic involvement of South China, formation of granitic magma is perhaps due to dehydration melting of mica-riched metasediments during post-orogenic thickened crust environment, migration and emplacement of the magma is controlled by relaxation of deep fault adjacent to the batholith.
- zircon U-Pb chronology /
- geochemistry /
- Nd-Hf isotope /
- Indosinian /
- Guangxi-Hunan junction

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图 1 越城岭-苗儿山岩基大地构造位置

底图据Wang et al.(2007b)

Fig. 1. Tectonic location of Yuechengling-Miaoershan batholiths

下载: 全尺寸图片幻灯片

图 2 越城岭-苗儿山岩基地质简图

1.地质界线；2.涟源-资源断裂；3.元古界；4.古生界；5.中生界；6.花岗岩；7.钨矿床(点)；8.钨锡矿床(点)；9.钨铜矿床(点)；10.采样地点；11.花岗岩年代及方法；12.晋宁期花岗岩；13.加里东期第Ⅰ阶段花岗岩；14.加里东期第Ⅱ阶段花岗岩；15.印支期花岗岩；16.工作区.LA为LA-ICP-MS；SH为SHRIMP；TIMS为热电离质谱法；SIMS为二次离子质谱法.年代学数据据赵葵东等(2006)、谢晓华等(2008)、柏道远等(2010, 2014, 2015)、石少华等(2010)、伍静等(2012)、杨振(2012)、Chu et al.(2012)、程顺波等(2013, 2016)、Zhao et al.(2013)、寇晓虎等(2014)、张迪等(2015)、陈文迪等(2016)、杜云等(2017)

Fig. 2. Geological sketch of Yuechengling-Miaoershan batholiths

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图 3 越城岭岩基北部印支期花岗岩岩石学和矿物学照片

a.晚阶段细粒二长花岗岩岩株侵入到早阶段中细粒少斑二长花岗岩中(14D504)；b.晚阶段细粒二长花岗岩岩脉侵入到早阶段中粒斑状花岗岩中(14D686)；c.早阶段中细粒含斑二长花岗岩中电气石石英钾长石伟晶岩团块(14D545)；d.早阶段中粒斑状二长花岗岩显微照片(14D529)(+)；e.晚阶段细粒正长花岗岩显微照片(14D561)(+)；f.样品14D561副矿物含石榴石(-).Tou.电气石；Pl.斜长石；Kf.正长石；Ms.白云母；Q.石英；Gr.石榴子石；+为正交偏光，-为单偏光

Fig. 3. Photographs of Indosinian granitic rocks of northern Yuechengling batholiths, and their micrographs under microscope

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图 4 越城岭岩基北部印支期花岗岩样品锆石LA-ICP-MS U-Pb年龄谐和图及代表性锆石阴极发光照片

束斑大小30 μm

Fig. 4. LA-ICP-MS U-Pb zircon concordia age plots and cathodoluminescence (CL) images of samples of Indonesian granites from northern Yuechengling batholith

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图 5 越城岭岩基北部印支期花岗岩样品的SiO₂-K₂O图解(a)和A/CNK-A/NK图解(b)

Fig. 5. SiO₂-K₂O diagram (a) and A/CNK-A/NK diagram (b) of Indosinian granitic samples of northern Yuechengling batholith

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图 6 越城岭岩基北部印支期花岗岩样品的微量元素蜘网图解(a)和稀土元素配分图解(b)

原始地幔和球粒陨石标准值据Sun and McDonough(1989)

Fig. 6. Primitive mantle-normalized spider diagram (a) and chondrite-normalized REE patterns (b) of Indosinian granitic samples of northern Yuechengling batholith

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图 7 越城岭岩基北部印支期花岗岩样品的ε_Nd(t)-t关系

底图据沈渭洲等(1994)

Fig. 7. ε_Nd(t)-t diagram of various granitic rocks of Indonesian granitic samples from northern Yuechengling batholith

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图 8 越城岭岩基北部印支期花岗岩样品ε_Hf(t)和T_DM2^Hf直方图

Fig. 8. Histograms of ε_Hf(t) and Hf modal ages of zircons from Caledonian granitic rocks of northern Yuechengling batholith

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图 9 越城岭岩基北部印支期花岗岩样品C/MF-A/MF图解图解

据Altherr et al.(2000)

Fig. 9. Diagram of C/MF vs A/MFof Indonesian granitic rocks of northern Yuechengling batholith

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表 1 越城岭-苗儿山岩基成岩期次简表

Table 1. Diagenetic stage of Yuechenging-Miaoershan batholiths

成岩期次	位置	产出形式	岩性组合	形成时间	参考文献
晋宁期	苗儿山岩体西北部猫儿界、叶溪江和报木坪等地	小型岩株	片麻状花岗闪长岩、二长花岗岩和花岗斑岩	811~806 Ma	李福顺和周厚祥，2002；柏道远等，2010；刘伟等，2011
加里东期	越城岭、苗儿山岩体大部	大型岩基	花岗闪长岩、(含电气石)二长花岗岩	438~381 Ma	Zhao et al., 2013；程顺波等，2016及其引用文献
印支期	越城岭北部，中部戈洞坪等.苗儿山南部油麻岭、杨桥岭，中部香草坪、豆榨山等地	岩基和中小型岩株	(含电气石)二长花岗岩、正长花岗岩	236~211 Ma	谢晓华等，2008；石少华等，2010；伍静等，2012；程顺波等，2013；寇晓虎等，2014以及本文

下载: 导出CSV

表 2 越城岭岩基北部印支期花岗岩样品锆石U-Th-Pb同位素分析结果

Table 2. U-Th-Pb isotopic analysis of zircons from Indonesian granites from northern Yuechengling batholith

分析点	Pb^*(10^-6)	Th(10^-6)	U(10^-6)	Th/U比值	²⁰⁷Pb/²⁰⁶Pb比值	1σ(10^-5)	²⁰⁷Pb/²³⁵U比值	1σ(10^-5)	²⁰⁶Pb/²³⁸U比值	1σ(10^-5)	²⁰⁷Pb/²³⁵U年龄(Ma)	1σ	²⁰⁶Pb/²³⁸U年龄(Ma)	1σ
中粒斑状二长花岗岩样品(14D529)(坐标110°54′52″E、26°27′11″N)
1	82.5	461	2 653	0.17	0.050 25	104	0.237 56	465	0.034 11	40	216	4	216	2
2	29.6	607	803	0.76	0.052 03	176	0.247 88	764	0.034 74	55	225	6	220	3
3	11.4	290	280	1.03	0.055 99	492	0.265 22	2 159	0.035 97	101	239	17	228	6
4	9.8	210	258	0.81	0.054 90	448	0.254 76	1 948	0.034 55	99	230	16	219	6
5	5.5	124	146	0.85	0.057 80	441	0.257 47	1 563	0.034 65	117	233	13	220	7
6	16.6	278	472	0.58	0.051 92	245	0.245 86	1 031	0.035 23	63	223	8	223	4
7	21.0	229	634	0.36	0.057 59	264	0.271 70	1 214	0.034 37	66	244	10	218	4
8	29.3	174	911	0.19	0.051 83	158	0.247 07	734	0.034 48	45	224	6	219
9	61.9	231	1 960	0.12	0.052 13	138	0.253 65	602	0.035 34	51	230	5	224	3
10	59.1	189	1 881	0.10	0.050 83	142	0.248 89	672	0.035 35	46	226	5	224	3
11	49.1	180	1 475	0.12	0.053 42	211	0.266 43	1 017	0.036 01	69	240	8	228	4
12	33.7	188	1 018	0.18	0.054 04	188	0.260 90	823	0.035 27	51	236	7	223	3
13	31.6	284	826	0.34	0.052 94	221	0.286 24	1 185	0.039 94	97	256	9	252	6
14	101.0	322	3 083	0.10	0.052 55	157	0.257 99	64	0.035 68	69	233	5	226	4
15	93.0	165	2 879	0.06	0.051 45	143	0.253 86	644	0.035 78	56	230	5	227	4
16	24.3	177	726	0.24	0.052 90	224	0.249 25	102	0.034 56	59	226	8	219	4
17	45.3	126	1 403	0.09	0.051 94	161	0.251 43	746	0.035 20	48	228	6	223	3
18	13.1	274	323	0.85	0.053 45	531	0.252 77	2 255	0.035 50	130	229	18	225	8
19	20.8	244	592	0.41	0.053 75	247	0.257 04	1 071	0.035 44	68	232	9	225	4
20	24.7	156	749	0.21	0.051 81	194	0.244 50	866	0.034 72	61	223	7	220	4
中粗粒斑状二长花岗岩样品(14D548)(坐标110°58′38″E、26°27′02″N)
1	18.3	97	537	0.18	0.052 60	215	0.255 85	962	0.035 77	63	231	8	227	4
2	32.5	390	936	0.42	0.051 44	168	0.243 57	741	0.034 64	50	221	6	219	3
3	27.4	158	789	0.20	0.053 07	247	0.262 24	987	0.036 26	77	236	8	230	5
4	18.6	174	517	0.34	0.054 89	249	0.266 25	1 040	0.036 10	94	240	8	229	6
5	22.8	92	708	0.13	0.052 24	159	0.251 79	771	0.035 18	56	228	6	223	4
6	23.0	122	712	0.17	0.051 35	152	0.242 50	703	0.034 44	45	220	6	218	3
7	33.6	240	1 008	0.24	0.050 99	188	0.242 93	802	0.034 78	57	221	7	220	4
8	17.8	149	528	0.28	0.051 97	193	0.248 44	904	0.035 08	54	225	7	222	3
9	54.5	248	1 659	0.15	0.052 62	128	0.255 98	609	0.035 25	44	231	5	223	3
10	20.7	157	612	0.26	0.052 45	205	0.253 27	945	0.035 29	62	229	8	223	4
11	53.3	258	1 551	0.17	0.052 16	158	0.254 10	691	0.035 48	45	230	6	225	3
12	26.9	463	669	0.69	0.054 52	440	0.260 58	1816	0.035 85	142	235	15	227	9
13	60.4	268	1 806	0.15	0.050 79	120	0.243 69	561	0.034 77	44	221	5	220	3
14	29.0	359	769	0.47	0.054 08	280	0.262 64	1 267	0.035 41	71	237	10	224	4
15	26.4	237	746	0.32	0.051 38	160	0.248 10	716	0.035 33	52	225	6	224	3
16	53.8	347	1 573	0.22	0.054 35	150	0.262 07	677	0.035 11	45	236	5	222	3
17	65.2	185	1 945	0.10	0.053 95	141	0.260 58	703	0.034 85	48	235	6	221	3
18	118.0	481	3 442	0.14	0.051 20	95	0.249 48	462	0.035 14	39	226	4	223	2
19	21.2	124	607	0.20	0.051 80	330	0.248 22	1 448	0.034 95	57	225	12	221	4
20	88.1	469	2 560	0.18	0.053 55	131	0.259 68	617	0.035 03	42	234	5	222	3
细粒少斑二长花岗岩样品(14D503)(坐标111°01′36″E、26°25′01″N)
1	36.3	1 160	809	1.43	0.051 28	346	0.242 36	1 577	0.034 26	69	220	13	217	4
2	134.0	378	3 623	0.10	0.069 97	174	0.364 46	1 048	0.037 43	53	316	8	237	3
3	129.0	493	3 721	0.13	0.051 17	119	0.258 10	5 799	0.036 57	54	233	5	231	3
4	27.2	378	749	0.50	0.053 86	247	0.252 85	1 120	0.034 32	68	229	9	218	4
5	99.3	499	2 088	0.24	0.131 60	378	0.692 11	2 092	0.037 92	54	534	13	240	3
6	87.8	478	2 454	0.19	0.054 55	143	0.272 29	6 633	0.036 19	53	245	5	229	3
7	22.7	289	622	0.46	0.050 00	200	0.238 08	921	0.035 09	59	217	7	222	4
8	42.3	303	606	0.50	0.055 75	192	0.498 50	1 606	0.065 16	86	411	11	407	5
9	131.0	358	3 738	0.10	0.053 44	127	0.268 52	593	0.036 48	44	242	5	231	3
10	40.5	445	1 036	0.43	0.053 34	393	0.265 10	1 871	0.036 38	100	239	15	230	6
11	45.0	368	1 261	0.29	0.054 26	207	0.257 43	886	0.035 25	58	233	7	223	4
12	448.0	469	8 667	0.05	0.120 23	513	0.781 75	3 871	0.045 61	86	586	22	288	5
13	23.3	369	559	0.66	0.053 82	456	0.272 99	2 535	0.036 48	128	245	20	231	8
14	43.6	232	1 187	0.20	0.052 60	281	0.264 39	1 234	0.036 81	95	238	10	233	6
15	137.0	551	3 994	0.14	0.053 27	100	0.265 75	581	0.035 94	52	239	5	228	3
16	73.4	404	2 066	0.20	0.050 91	177	0.260 35	951	0.036 75	57	235	8	233	4
17	80.0	642	2 300	0.28	0.053 42	143	0.258 87	704	0.034 96	52	234	6	221	3
18	68.1	458	1 947	0.23	0.052 47	166	0.261 80	792	0.036 10	61	236	6	229	4
19	28.7	265	817	0.32	0.053 37	196	0.263 95	962	0.036 16	68	238	8	229	4
20	49.8	1 162	1 189	0.98	0.053 21	152	0.270 09	733	0.036 92	59	243	6	234	4
细粒正长花岗岩样品(14D561)(坐标110°54′03″E、26°25′48″N)
1	128.0	994	3 717	0.27	0.066 46	167	0.325 66	735	0.035 58	43	286	6	225	3
2	12.8	206	357	0.58	0.053 08	226	0.251 45	1 105	0.034 72	68	228	9	220	4
3	20.0	198	590	0.34	0.051 20	189	0.244 89	881	0.034 87	51	222	7	221	3
4	100.0	328	3 106	0.11	0.052 17	174	0.252 28	882	0.034 94	58	228	7	221	4
5	167.0	321	5 253	0.06	0.051 81	87	0.255 11	442	0.035 61	38	231	4	226	2
6	26.9	224	815	0.27	0.051 87	170	0.244 55	786	0.034 22	53	222	6	217	3
7	31.5	201	960	0.21	0.053 29	231	0.254 10	1 099	0.034 56	63	230	9	219	4
8	20.1	161	629	0.26	0.044 04	243	0.200 20	994	0.033 52	68	185	8	212	4
9	39.1	397	528	0.75	0.055 86	183	0.525 79	1 711	0.068 73	112	429	11	429	7
10	26.8	253	794	0.32	0.054 27	190	0.262 79	1 047	0.034 84	51	237	8	221	3
11	57.9	201	1 681	0.12	0.051 09	150	0.247 23	754	0.035 06	53	224	6	222	3
12	57.4	460	1 563	0.29	0.053 29	137	0.259 57	617	0.035 53	48	234	5	225	3
13	25.8	287	677	0.42	0.051 43	259	0.242 95	1 157	0.034 69	82	221	9	220	5
14	63.0	405	1 737	0.23	0.050 80	177	0.239 40	832	0.034 07	48	218	7	216	3
15	37.2	190	1 010	0.19	0.051 48	277	0.245 77	1 426	0.034 39	70	223	12	218	4
16	21.9	210	536	0.39	0.051 45	224	0.255 28	1 106	0.036 07	60	231	9	228	4
17	104.0	68	747	0.09	0.065 75	162	1.163 47	2 599	0.128 00	152	784	12	776	9
18	38.8	268	1 063	0.25	0.051 28	265	0.225 41	1 082	0.032 13	58	206	9	204	4
19	35.9	355	839	0.42	0.050 96	229	0.249 88	1 145	0.035 59	77	226	9	225	5
20	123.0	290	3 161	0.09	0.051 36	130	0.247 24	594	0.034 92	40	224	56	221	3
注：Pb^*代表放射性成因铅.

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表 3 越城岭岩基北部印支期花岗岩样品的主量元素(%)和微量元素(10^-6)分析结果

Table 3. Major elements (%) and trace elements (10^-6) of Indosinian granitic samples from northern Yuechengling batholith

期次	早阶段					晚阶段
样品号	14D529	14D548	14D503	462^*	464^*	14D504	14D561-1
SiO₂	74.71	74.46	72.98	74.66	73.66	75.63	74.52
TiO₂	0.173	0.223	0.288	0.230	0.250	0.216	0.149
Al₂O₃	12.74	12.74	13.48	12.95	13.69	12.30	13.37
Fe₂O₃	0.356	0.217	0.966	0.330	0.600	0.602	0.645
FeO	2.55	2.64	2.10	1.45	1.23	2.23	1.68
MnO	0.078	0.071	0.064	0.050	0.040	0.081	0.064
MgO	0.360	0.472	0.546	0.450	0.490	0.420	0.332
CaO	0.914	1.150	1.490	0.960	0.900	0.788	0.939
K₂O	4.54	4.72	4.62	5.17	5.08	4.34	4.90
Na₂O	3.04	2.83	2.94	2.82	2.75	2.79	3.06
P₂O₅	0.082	0.100	0.098	0.070	0.120	0.092	0.085
灼失	0.118	0.037	0.103	0.730	1.060	0.234	0.037
∑	99.66	99.66	99.68	99.87	99.87	99.72	99.78
FeO^T	2.87	2.84	2.97	1.75	1.77	2.77	2.26
A/CNK	1.10	1.07	1.07	1.08	1.17	1.15	1.11
CaO/Na₂O	0.30	0.41	0.51	0.34	0.33	0.28	0.31
Al₂O₃/TiO₂	73.64	57.13	46.81	56.30	54.76	56.94	89.73
Rb	558	497	364	501	416	484	500
Sr	29.9	44.6	71.8	39.9	50.6	22.1	37.4
Ba	95.3	171.0	266.0	171.0	221.00	58.7	155.0
U	21.4	14.7	25.6			12.9	5.0
Th	31.5	30.8	33.5	39.7	35.1	23.0	19.2
Nb	21.4	15.9	14.4	19.6	14.7	16.6	13.8
Ta	7.72	4.44	2.81	3.40	2.52	4.43	4.52
Zr	112.0	130.0	142.0	149.0	129.0	99.5	97.8
Hf	4.87	4.97	5.16	5.38	4.52	4.11	4.18
Y	29.7	21.7	32.8	35.7	30.0	26.9	18.0
Nb/Ta	2.77	3.58	5.12	5.76	5.83	3.75	3.05
Zr/Hf	23.00	26.16	27.52	27.70	28.54	24.21	23.40
La	28.9	30.2	45.5	40.8	44.4	27.0	25.5
Ce	71.9	73.8	103.0	95.6	100.0	64.2	61.9
Pr	7.22	7.29	10.00	10.60	11.10	6.61	6.06
Nd	24.6	25.2	33.2	37.4	39.1	22.5	20.7
Sm	5.50	5.19	6.60	8.23	8.02	4.96	4.39
Eu	0.260	0.370	0.660	0.432	0.538	0.190	0.31
Gd	4.76	4.37	5.82	6.84	6.52	4.30	3.61
Tb	0.92	0.78	1.04	1.08	1.00	0.82	0.64
Dy	5.82	4.48	6.50	6.43	5.55	5.21	3.74
Ho	1.19	0.89	1.35	1.19	1.04	1.05	0.74
Er	3.37	2.52	3.74	3.34	2.95	2.99	2.02
Tm	0.60	0.42	0.60	0.54	0.45	0.53	0.35
Yb	4.06	2.75	3.70	3.59	2.85	3.54	2.28
Lu	0.540	0.370	0.480	0.516	0.391	0.470	0.300
∑REE	159.64	158.63	222.19	216.58	223.91	144.37	132.54
(La/Yb)_N	5.11	7.88	8.82	8.15	11.17	5.47	8.02
δEu	0.15	0.23	0.32	0.17	0.22	0.12	0.23
注：*样品寇晓虎等(2014).

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表 4 越城岭岩基北部印支期花岗岩样品的Sm-Nd同位素组成

Table 4. Sm-Nd isotopic compositions of Indonesian granitic samples from northern Yuechengling batholith

时代	样号	成岩期次	t(Ma)	(¹⁴⁷Sm/¹⁴⁴Nd)_m	(¹⁴³Nd/¹⁴⁴Nd)_m	ε_Nd(t)	(¹⁴³Nd/¹⁴⁴Nd)_i	T_DM(Ga)	T_DM2(Ga)	f_Sm/Nd
印支期	14D529-1	早阶段	222	0.115 1	0.512 045	-9.3	0.511 878	1.71	1.75	-0.41
	14D548	早阶段	222	0.133 5	0.512 026	-10.2	0.511 832	2.14	1.82	-0.32
	14D503	早阶段	227	0.136 4	0.512 038	-10.0	0.511 835	2.19	1.81	-0.31
	14D504	晚阶段	222	0.133 1	0.512 017	-10.3	0.511 824	2.14	1.84	-0.32
	14D561-1	晚阶段	222	0.130 7	0.512 000	-10.6	0.511 810	2.11	1.86	-0.34

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表 5 越城岭岩基北部印支期花岗岩样品锆石Hf同位素分析结果

Table 5. MC-ICP-MS Hf isotopic analysis of zircons from Indonesian granitic rocks of northern Yuechengling batholith

	¹⁷⁶Hf/¹⁷⁷Hf比值	2σ(10^-6)	¹⁷⁶Lu/¹⁷⁷Hf比值	¹⁷⁶Yb/¹⁷⁷Hf比值	t(Ma)	ε_Hf(t)	2σ	T_DM2(Ma)	2σ	f_Lu/Hf
14D529中粒斑状二长花岗岩
1	0.282 345	10	0.001 047	0.039 851	216	-10.5	0.4	1 913	46	-0.97
2	0.282 385	8	0.001 312	0.056 730	220	-9.1	0.3	1 824	37	-0.96
3	0.282 417	9	0.000 691	0.028 108	228	-7.7	0.3	1 742	40	-0.98
4	0.282 465	8	0.000 594	0.027 083	219	-6.1	0.3	1 639	37	-0.98
5	0.282 444	9	0.000 747	0.032 394	220	-6.9	0.3	1 686	39	-0.98
6	0.282 337	9	0.001 057	0.040 007	223	-10.7	0.3	1 927	42	-0.97
7	0.282 329	7	0.001 325	0.052 851	218	-11.1	0.2	1 949	30	-0.96
8	0.282 446	8	0.000 786	0.037 774	219	-6.8	0.3	1 684	34	-0.98
9	0.282 374	9	0.001 470	0.060 459	224	-9.4	0.3	1 848	40	-0.96
10	0.282 341	8	0.001 622	0.057 732	224	-10.6	0.3	1 923	36	-0.95
11	0.282 366	8	0.001 370	0.049 643	228	-9.6	0.3	1 862	37	-0.96
12	0.282 356	8	0.001 212	0.055 329	223	-10.0	0.3	1 885	37	-0.96
13	0.282 368	7	0.001 552	0.070 197	252	-9.0	0.3	1 845	33	-0.95
14	0.282 409	8	0.000 876	0.039 117	226	-8.0	0.3	1 762	38	-0.97
15	0.282 391	7	0.001 379	0.055 278	227	-8.7	0.3	1 806	32	-0.96
16	0.282 451	8	0.000 697	0.027 186	219	-6.7	0.3	1 673	36	-0.98
17	0.282 463	8	0.000 913	0.035 409	223	-6.2	0.3	1 645	36	-0.97
18	0.282 396	9	0.001 369	0.047 421	225	-8.6	0.3	1 796	39	-0.96
19	0.282 146	10	0.004 480	0.154 253	225	-17.9	0.3	2 379	43	-0.87
20	0.282 390	7	0.001 137	0.052 076	220	-8.9	0.3	1 811	32	-0.97
14D503细粒少斑二长花岗岩
1	0.282 307	10	0.001 531	0.075 226	217	-11.9	0.3	2 001	44	-0.95
2	0.282 350	10	0.001 286	0.057 883	237	-9.9	0.3	1 892	42	-0.96
3	0.282 351	8	0.001 587	0.062 218	231	-10.1	0.3	1895	38	-0.95
4	0.282 487	10	0.000 547	0.026 019	218	-5.4	0.3	1 591	43	-0.98
5	0.282 298	8	0.000 964	0.040 256	240	-11.7	0.3	2 003	33	-0.97
6	0.282 373	8	0.001 491	0.054 791	229	-9.3	0.3	1 846	37	-0.96
7	0.282 438	11	0.000 602	0.028 837	222	-7.0	0.4	1 699	48	-0.98
8	0.282 363	9	0.000 429	0.018 505	407	-5.6	0.3	1 750	39	-0.99
9	0.282 298	8	0.001 450	0.061 492	231	-11.9	0.3	2 013	37	-0.96
10	0.282 426	9	0.000 700	0.032 060	230	-7.3	0.3	1 721	41	-0.98
11	0.282 430	8	0.001 230	0.046 437	223	-7.4	0.3	1 721	37	-0.96
13	0.282 391	8	0.001 056	0.038 332	231	-8.6	0.3	1 801	38	-0.97
14	0.282 403	9	0.000 675	0.026 493	233	-8.1	0.3	1 771	38	-0.98
15	0.282 372	8	0.001 802	0.063 456	228	-9.4	0.3	1 853	36	-0.95
17	0.282 332	8	0.001 369	0.050 538	221	-10.9	0.3	1 942	34	-0.96
18	0.282 304	8	0.001 314	0.052 672	229	-11.7	0.3	1 998	37	-0.96
19	0.282 434	8	0.000 933	0.038 990	229	-7.1	0.3	1 706	35	-0.97
20	0.282 315	9	0.001 635	0.072 530	234	-11.3	0.3	1 974	41	-0.95

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