额尔古纳地块新元古代岩浆作用与微陆块构造属性：来自侵入岩锆石U-Pb年代学、地球化学和Hf同位素的制约

赵硕; 许文良; 唐杰; 李宇; 郭鹏

doi:10.3799/dqkx.2016.550

额尔古纳地块新元古代岩浆作用与微陆块构造属性：来自侵入岩锆石U-Pb年代学、地球化学和Hf同位素的制约

doi: 10.3799/dqkx.2016.550

吉林大学地球科学学院，吉林长春 130061

基金项目:

吉林大学研究生创新基金资助项目 2016102

中国地质大学(武汉)地质过程与矿产资源国家重点实验室开放基金项目 GPMR201503

教育部博士点基金项目 20120061110048

国家自然科学基金项目 41272077

详细信息

作者简介:
赵硕(1987-)，博士生，矿物学、岩石学、矿床学专业.E-mail: zhaoshuo14@mails.jlu.edu.cn

通讯作者:
许文良, E-mail: xuwl@jlu.edu.cn

中图分类号: P597
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出版历程
- 收稿日期: 2016-02-21
- 刊出日期: 2016-11-15

Neoproterozoic Magmatic Events and Tectonic Attribution of the Erguna Massif:Constraints from Geochronological, Geochemical and Hf Isotopic Data of Intrusive Rocks

College of Earth Sciences, Jilin University, Changchun 130061, China

摘要

摘要: 对额尔古纳地块新元古代花岗岩进行了锆石LA-ICP-MS U-Pb年代学、岩石地球化学和锆石Hf同位素研究，以便对其新元古代岩浆作用历史与微陆块构造属性给予制约.所测花岗质岩石中锆石的CL图像特征和Th/U比值(0.17~1.46) 显示其为岩浆成因.测年结果并结合前人定年结果，可以判定额尔古纳地块上至少存在~929 Ma、~887 Ma、~850 Ma、~819 Ma、~792 Ma、~764 Ma和~738 Ma岩浆事件.岩石地球化学特征显示，~887 Ma花岗岩为一套后碰撞花岗岩类；而850~737 Ma花岗质岩石整体上属于A-型花岗岩，也有部分岩体(漠河、阿木尔、碧水和室韦岩体)显示I-型花岗岩特征.锆石Hf同位素特征反映这些花岗岩的源区既有中-新元古代(T_DM2=884~1 563 Ma)新增生地壳物质的部分熔融，同时伴有少量古老地壳物质的混染，也有残留的古老中基性下地壳物质的部分熔融.综合研究区新元古代侵入岩的地球化学特征，同时对比新元古代全球构造热事件，认为额尔古纳地块上新元古代岩浆活动记录了Rodinia超大陆形成和演化过程中的地壳响应：927~880 Ma的岩浆作用应是Rodinia超大陆汇聚造山的产物；而850~737 Ma的岩浆作用应是对Rodinia超大陆快速裂解的记录.通过岩浆事件对比发现，额尔古纳地块与邻近的西伯利亚南缘微陆块(如中蒙古地块和图瓦地块)具有亲缘性，而与塔里木板块和华南板块至少在新元古代岩浆活动上具有一定的相似性，而明显区别于华北板块和西伯利亚板块.
- 额尔古纳地块 /
- 新元古代 /
- 岩浆作用 /
- 年代学 /
- 地球化学 /
- 构造属性
Abstract: This paper presents LA-ICP-MS zircon U-Pb dating, major and trace elements, and Hf isotope data of the Neoproterozoic granitoids in the Erguna Massif with the aim of constraining the Neoproterozoic tectonic evolution and tectonic attribution of the Erguna Massif. Zircons from these granitoids are of magmatic origin in accordance with CL images and high Th/U ratios (0.17-1.46). The zircon dating results, together with previously published age data, demonstrate that the Neoproterozoic magmatisms in the Erguna Massif can be subdivided into seven stages: about 929 Ma, about 887 Ma, about 850 Ma, about 819 Ma, about 792 Ma, about 764 Ma and about 738 Ma. Geochemically, about 887 Ma granites are similar to those of post-collisional granites, whereas 850-737 Ma granitoids are similar generally to A-type granites, except for some samples (collected from Mohe, Amuer, Bishui and Shiwei plutons) which are similar to I-type granites. Zircon Hf isotopic compositions indicate that their primary magmas could have originated not only by partial melting of a depleted lower crust that accreated during the Meso-Neoproterozoic (T_DM2=884-1 563 Ma), with a contribution of ancient crustal material in their petrogenesis, but also by partial melting of the residual ancient mafic crustal material. These geochemical data, combined with the published data and the global magmatic-tectonic-thermal events, indicate that Neoproterozoic magmatic events within the Erguna Massif recorded crustal evolution as a result of the assembly and breakup of the Rodinia supercontinent: magmatisms between 927 Ma and 880 Ma were the result of collision-orogeny during the stage of assembly of the Rodinia supercontinent, whereas the 850-737 Ma magmatisms recorded the breakup of the Rodinia supercontinent. The Erguna Massif has an affinity to the adjacent massifs (e.g. Central Mongolia and Tuva massifs) near the southern margin of the Siberian block, and is similar to the Tarim and South China blocks at least in terms of these Neoproterozoic magmatic events, but obviously different from the North China and Siberian blocks.
- Erguna massif /
- Neoproterozoic /
- magmatism /
- geochronology /
- geochemistry /
- tectonic attribution

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图 1 研究区地质及构造简图

a.中国东北地区构造简图(据Wu et al., 2007修改)(① 喜桂图-塔源断裂，② 贺根山-黑河断裂，③ 索伦-西拉木伦-长春缝合带，④ 嘉荫-牡丹江断裂，⑤ 伊通-依兰断裂，⑥ 敦化-密山断裂)；b.研究区地质简图(内蒙古自治区地质矿产局，1991；黑龙江省地质矿产局，1993)

Fig. 1. Detailed geological map of the study area and tectonic sketch map of NE China

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图 2 研究区新元古代侵入岩样品显微照片

Af.碱性长石；Bi.黑云母；Pl.斜长石；Q.石英

Fig. 2. Microphotographs showing textures for the Neoproterozoic intrusive rocks

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图 3 研究区新元古代侵入岩部分锆石阴极发光图像

Fig. 3. CL images of the selected zircons from the Neoproterozoic intrusive rocks in the study area

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图 4 研究区新元古代侵入岩锆石U-Pb年龄谐和图

Fig. 4. Zircon U-Pb concordia diagrams for the Neoproterozoic intrusive rocks in the Erguna Massif

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图 10 新远古代岩浆事件统计频数

图a据本文、Wu et al.(2011)、佘宏全等(2012)、孙立新等(2012)、Gou et al.(2013)、Tang et al.(2013)、张丽等(2013)和赵硕等(2016)；图b据Izokh et al.(1998)、Kuzmichev et al.(2001)、Ritsk et al.(2001)、Sklyarov et al.(2003)和Gladkochub et al.(2007)；图c据Long et al.(2011)和Rojas-Agramonte et al.(2011)；图d据Li et al.(2003)、Lin et al.(2007)和Charvet et al.(2013)

Fig. 10. Relative-age-probability diagram summarizing the Neoproterozoic magmatic events

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图 5 研究区新元古代侵入岩的TAS图

碱性系列和亚碱性系列分界线据Irvine and Baragar (1971)，灰色投影点据已报道额尔古纳地块新元古代侵入岩地化数(孙立新等，2012；Gou et al., 2013；Tang et al., 2013)

Fig. 5. Plot of total alkali versus SiO₂ (TAS) for the Neoproterozoic intrusive rocks in the Erguna Massif

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图 6 (a)研究区新元古代侵入岩的K₂O-SiO₂图；(b)研究区新元古代侵入岩的A/NK-A/CNK图

图例同图 5

Fig. 6. Plots of K₂O versus SiO₂ (a) and A/CNK versus A/NK (b) for the Neoproterozoic intrusive rocks in the Erguna Massif

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图 7 研究区新元古代侵入岩的球粒陨石标准化稀土元素配分型式(a)和原始地幔标准化微量元素蛛网图(b)

球粒陨石和原始地幔元素值分别据Boynton(1984)和Sun and McDonough(1989)；阴影部分据孙立新等(2012)、Tang et al.(2013)和Gou et al.(2013)；图例同图 5

Fig. 7. Chondrite-normalized REE patterns (a) and primitive-mantle-normalized trace element spidergrams (b) for the Neoproterozoic intrusive rocks in the Erguna Massif

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图 8 研究区新元古代侵入岩的Hf同位素组成和锆石年龄关系

图例同图 5

Fig. 8. Correlations between Hf isotopic compositions and ages of zircons from the Neoproterozoic intrusive rocks

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图 9 研究区新元古代侵入岩的TFeO/MgO-(Zr+Nb+Ce+Y)和(Na₂O+K₂O)/CaO-(Zr+Nb+Ce+Y)图

据Whalen et al.(1987)；A.A型花岗岩；FG.分异的花岗岩；OGT.未分异的M、I、S型花岗岩; 图例同图 5

Fig. 9. Plots of TFeO/MgO versus Zr+Nb+Ce+Y and (Na₂O+K₂O)/CaO versus Zr+Nb+Ce+Y for the Neoproterozoic intrusive rocks in the Erguna Massif

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表 1 额尔古纳地块新元古代侵入岩的岩石学特征

Table 1. Petrography of the Neoproterozoic intrusive rocks in the Erguna Massif

样品号	采样点坐标	采样点位置	岩体名称	岩石类型	新鲜面颜色	结构	构造	矿物组成(%)
样品号	采样点坐标	采样点位置	岩体名称	岩石类型	新鲜面颜色	结构	构造	Q	Af	Pl	Bi	副矿物
12ER28-1	122°04′18.3″E 52°04′20.0″N	满归镇北约3 km处	满归岩体	黑云母二长花岗岩	肉红色	似斑状	片麻状	28	35	25	10	2
13ER13-1	122°05′33.0″E 52°03′26.4″N	满归镇北东约5 km处	满归岩体	碱长花岗岩	肉红色	似斑状	片麻状	25	50	10	13	2
14ER17-1	122°21′32.5″E 53°04′47.0″N	漠河县城北约15 km处	漠河岩体	黑云母二长花岗岩	灰白色	中细粒半自形	片麻状	20	40	30	7	3
14ER11-1	123°39′57.6″E 52°26′39.6″N	碧水镇北约30 km处	碧水岩体	碱长花岗岩	肉红色	中粗粒半自形	块状	25	65	5	3	2
14ER13-1	123°10′26.8″E 52°41′08.2″N	阿木尔镇南约15 km处	阿木尔岩体	花岗闪长岩	灰白色	中细粒半自形	片麻状	25	15	50	8	2
12ER14-1	120°15′37.5″E 51°18′41.3″N	室韦镇东约30 km处	室韦岩体	黑云母二长花岗岩	灰黑色	似斑状	片麻状	30	35	25	8	2
12ER7-1	119°15′12.5″E 50°29′30.7″N	五卡村北约10 km处	五卡岩体	碱长花岗岩	灰白色	细粒半自形	片麻状	35	45	10	8	2

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表 2 额尔古纳地块新元古代侵入岩锆石LA-ICP-MS U-Pb定年数据

Table 2. LA-ICP-MS zircon U-Pb dating data for the Neoproterozoic intrusive rocks in the Erguna Massif

点号	²³²Th(10 ^-6)	²³⁸U(10 ^-6)	Th/U	Pb(10 ^-6)	同位素比值						年龄(Ma)
					²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U
					比值	1σ	比值	1σ	比值	1σ	年龄(Ma)	1σ	年龄(Ma)	1σ	年龄(Ma)	1σ
12ER28-1
1	2 564	20 920	0.12	3 093	0.069 50	0.001 50	1.112 62	0.023 74	0.114 85	0.001 00	914	30	759	11	701	6
2	2 803	13 867	0.20	2 560	0.069 55	0.001 42	1.111 50	0.023 19	0.114 68	0.001 19	915	26	759	11	700	7
3	2 597	8 011	0.32	1 984	0.067 60	0.001 45	1.334 86	0.033 82	0.141 46	0.002 20	856	28	861	15	853	12
4	949	4 854	0.20	947	0.067 94	0.001 73	1.327 85	0.035 23	0.140 32	0.001 81	867	34	858	15	846	10
5	919	5 425	0.17	1 009	0.067 55	0.001 65	1.333 49	0.032 55	0.141 38	0.001 34	855	35	860	14	852	8
6	3 404	12 192	0.28	2 638	0.069 88	0.001 55	1.066 48	0.023 54	0.109 44	0.001 11	925	29	737	12	670	6
7	3 255	16 600	0.20	2 431	0.075 36	0.001 83	1.009 37	0.024 79	0.096 05	0.001 38	1 078	27	709	13	591	8
8	4 256	15 513	0.27	2 768	0.071 38	0.001 62	1.116 57	0.024 76	0.111 62	0.000 96	968	31	761	12	682	6
9	1 813	9 545	0.19	1 804	0.066 91	0.001 66	1.320 90	0.039 84	0.140 56	0.002 75	835	32	855	17	848	16
10	4 098	14 752	0.28	2 554	0.070 49	0.002 34	1.139 66	0.037 20	0.114 82	0.001 24	943	49	772	18	701	7
11	2 280	16 642	0.14	2 599	0.067 40	0.001 81	1.114 36	0.030 14	0.118 17	0.001 20	850	39	760	14	720	7
12	385	1 846	0.21	367	0.066 21	0.002 49	1.295 72	0.050 43	0.140 79	0.002 18	813	55	844	22	849	12
13	2 174	9 481	0.23	1 861	0.067 66	0.001 91	1.323 46	0.040 15	0.140 78	0.002 11	858	38	856	18	849	12
14	1 539	24 871	0.06	2 981	0.06 893	0.001 58	1.092 64	0.026 00	0.113 75	0.001 06	897	34	750	13	694	6
15	2 527	6 419	0.39	1 734	0.070 26	0.001 70	1.568 08	0.038 15	0.160 20	0.001 48	936	35	958	15	958	8
13ER12-1
1	1 153	2 371	0.49	1 061	0.067 00	0.000 85	1.303 91	0.016 67	0.140 28	0.000 71	838	18	847	7	846	4
2	1 035	5 121	0.20	1 306	0.067 20	0.000 82	1.310 53	0.017 52	0.140 60	0.000 99	844	16	850	8	848	6
3	847	1 979	0.43	735	0.067 22	0.000 92	1.304 45	0.018 81	0.139 99	0.000 99	845	18	848	8	845	6
4	563	2 322	0.24	651	0.067 39	0.000 96	1.382 02	0.020 98	0.147 86	0.001 00	850	20	881	9	889	6
5	221	674	0.33	244	0.068 83	0.001 18	1.413 38	0.025 13	0.148 49	0.001 34	894	22	895	11	892	8
6	730	2 312	0.32	856	0.068 71	0.001 06	1.412 42	0.022 60	0.148 43	0.001 17	890	20	894	10	892	7
7	902	887	1.02	685	0.067 41	0.001 05	1.311 77	0.020 98	0.140 45	0.001 01	850	21	851	9	847	6
8	575	1 596	0.36	525	0.068 17	0.000 89	1.298 81	0.018 05	0.137 41	0.000 93	874	18	845	8	830	5
9	528	2 631	0.20	642	0.068 02	0.000 85	1.361 36	0.018 25	0.144 30	0.001 00	869	17	872	8	869	6
10	944	2 813	0.34	970	0.068 04	0.000 99	1.360 78	0.020 81	0.144 14	0.001 10	870	19	872	9	868	6
11	730	2 413	0.30	763	0.068 36	0.001 03	1.360 32	0.021 25	0.143 27	0.001 03	880	20	872	9	863	6
12	687	3 528	0.19	874	0.068 07	0.001 06	1.351 84	0.020 61	0.143 30	0.001 06	871	19	868	9	863	6
13	1 332	910	1.46	1 049	0.068 77	0.001 00	1.413 93	0.020 84	0.148 08	0.000 97	892	20	895	9	890	5
14	1 168	3 100	0.38	1 135	0.067 71	0.000 83	1.393 85	0.019 19	0.148 12	0.001 17	860	16	886	8	890	7
15	446	2 852	0.16	559	0.068 47	0.000 83	1.282 15	0.015 82	0.134 73	0.000 80	883	16	838	7	815	5
16	587	3 609	0.16	764	0.067 65	0.000 82	1.273 04	0.015 81	0.135 43	0.000 92	858	15	834	7	819	5
13ER13-1
1	964	5 040	0.19	1 311	0.068 56	0.001 10	1.388 52	0.019 81	0.146 88	0.001 06	886	34	884	8	883	6
2	699	3 133	0.22	794	0.068 27	0.000 81	1.331 65	0.016 69	0.140 43	0.000 93	877	15	860	7	847	5
3	531	1 567	0.34	570	0.069 42	0.000 92	1.469 37	0.019 59	0.152 85	0.001 23	911	15	918	8	917	7
4	1 135	4 965	0.23	1354	0.067 62	0.000 90	1.322 04	0.018 39	0.140 79	0.000 94	857	18	855	8	849	5
5	982	4 197	0.23	1 199	0.068 52	0.001 00	1.336 20	0.020 18	0.140 74	0.001 14	884	18	862	9	849	6
6	629	2 045	0.31	750	0.069 69	0.000 92	1.481 38	0.023 09	0.153 26	0.001 46	919	17	923	9	919	8
7	923	3 905	0.24	1 147	0.070 69	0.001 34	1.35817	0.023 98	0.139 34	0.000 97	948	40	871	10	841	5
8	484	2 890	0.17	741	0.068 23	0.001 52	1.320 74	0.027 17	0.140 40	0.001 21	875	47	855	12	847	7
9	882	3 001	0.29	1 014	0.068 72	0.001 45	1.393 89	0.027 22	0.147 10	0.001 17	890	45	886	12	885	7
10	1 080	3 010	0.36	1 048	0.074 47	0.001 13	1.445 63	0.022 87	0.140 29	0.001 19	1 054	19	908	9	846	7
11	633	2 310	0.27	710	0.068 55	0.000 92	1.394 93	0.020 21	0.146 82	0.001 15	885	17	887	9	883	6
12	840	3 138	0.27	876	0.069 86	0.000 88	1.413 75	0.020 21	0.146 01	0.001 26	924	16	895	9	879	7
13	885	2 606	0.34	932	0.070 39	0.000 86	1.433 18	0.017 65	0.146 85	0.000 82	940	16	903	7	883	5
14	1 856	3 381	0.55	1 678	0.070 28	0.000 85	1.429 72	0.019 82	0.146 69	0.001 27	936	15	901	8	882	7
15	732	3 008	0.24	892	0.071 09	0.000 87	1.510 62	0.020 98	0.153 01	0.001 19	960	16	935	8	918	7
14ER17-1
1	2 145	5 077	0.42	1 693	0.071 71	0.001 31	1.487 04	0.029 08	0.149 25	0.001 44	978	24	925	12	897	8
2	2 080	6 603	0.32	1 507	0.066 15	0.001 11	1.157 08	0.021 52	0.125 88	0.001 22	811	23	781	10	764	7
3	846	3 631	0.23	664	0.064 77	0.001 22	1.019 13	0.019 14	0.113 29	0.000 66	767	30	713	10	692	4
4	915	4 479	0.20	890	0.065 69	0.001 30	1.193 66	0.026 28	0.130 58	0.001 33	797	29	798	12	791	8
5	2 521	6 909	0.36	1 758	0.066 64	0.001 40	1.208 71	0.025 88	0.130 62	0.001 15	827	30	805	12	791	7
6	1 680	6 332	0.27	1 108	0.065 05	0.001 39	0.993 97	0.022 51	0.109 79	0.001 03	776	32	701	11	672	6
7	1 898	6 517	0.29	1 278	0.066 61	0.001 39	1.031 56	0.020 89	0.111 51	0.000 78	825	31	720	10	682	5
8	1 229	5 004	0.25	1 073	0.065 23	0.001 17	1.187 29	0.021 34	0.130 99	0.001 08	782	24	795	10	794	6
9	3 433	9 324	0.37	2 143	0.066 21	0.001 07	1.202 74	0.022 28	0.130 46	0.001 44	813	21	802	10	790	8
10	1 099	5 064	0.22	1 000	0.067 28	0.001 20	1.079 11	0.019 45	0.115 14	0.000 88	846	25	743	9	703	5
11	1 283	4 976	0.26	1 074	0.063 45	0.001 24	1.157 21	0.022 93	0.130 94	0.001 16	723	27	781	11	793	7
12	1 877	5 531	0.34	1 363	0.064 57	0.001 28	1.163 42	0.023 11	0.129 36	0.001 08	760	28	784	11	784	6
13	1 871	6 116	0.31	1 444	0.063 66	0.001 12	1.156 47	0.022 49	0.130 58	0.001 50	730	23	780	11	791	9
14	2 268	5 696	0.40	1 533	0.063 80	0.001 08	1.156 55	0.020 18	0.130 56	0.001 31	735	21	780	10	791	7
14ER11-1
1	1 217	3 221	0.38	1 014	0.065 05	0.001 13	1.189 32	0.021 58	0.131 31	0.001 32	776	22	796	10	795	8
2	720	1 966	0.37	607	0.064 49	0.001 16	1.181 74	0.021 23	0.131 53	0.001 03	758	25	792	10	797	6
3	396	781	0.51	313	0.065 48	0.001 50	1.202 49	0.027 78	0.131 96	0.001 21	790	33	802	13	799	7
4	490	1 058	0.46	393	0.063 38	0.001 33	1.155 74	0.023 63	0.131 03	0.001 13	721	29	780	11	794	6
5	1 029	1 952	0.53	921	0.068 13	0.001 52	1.395 15	0.028 45	0.147 47	0.001 32	872	27	887	12	887	7
6	2 444	8 149	0.30	2 170	0.065 39	0.001 25	1.192 60	0.025 91	0.130 77	0.001 80	787	24	797	12	792	10
7	714	1 170	0.61	530	0.065 00	0.001 58	1.180 11	0.027 75	0.130 49	0.001 18	774	34	791	13	791	7
8	2 159	5 595	0.39	1 753	0.065 01	0.001 17	1.190 48	0.022 07	0.131 36	0.001 24	775	23	796	10	796	7
9	617	1 312	0.47	503	0.066 40	0.001 41	1.207 95	0.025 71	0.130 54	0.001 06	819	31	804	12	791	6
10	780	1 463	0.53	614	0.064 23	0.001 42	1.180 55	0.026 85	0.131 97	0.001 16	749	33	792	13	799	7
11	1 653	4 453	0.37	1 402	0.065 20	0.001 17	1.193 66	0.022 80	0.131 40	0.001 12	781	26	798	11	796	6
12	371	1 509	0.25	370	0.063 97	0.001 73	1.159 34	0.031 14	0.130 59	0.001 31	741	40	782	15	791	7
13	374	1 075	0.35	347	0.065 74	0.001 52	1.190 38	0.029 07	0.130 49	0.001 34	798	34	796	13	791	8
14	1 931	3 685	0.52	1 415	0.062 46	0.00142	1.14574	0.02943	0.132 00	0.001 62	690	34	775	14	799	9
15	638	1 045	0.61	482	0.064 00	0.001 69	1.159 63	0.032 91	0.130 83	0.001 59	742	39	782	15	793	9
14ER13-1
1	220	621	0.35	99	0.065 75	0.001 35	1.188 73	0.028 09	0.131 20	0.001 80	799	27	795	13	795	10
2	398	735	0.54	121	0.065 31	0.001 24	1.168 80	0.026 64	0.129 60	0.001 50	784	29	786	12	786	9
3	300	805	0.37	129	0.067 65	0.001 27	1.224 20	0.024 64	0.131 20	0.001 30	858	26	812	11	795	7
4	155	691	0.22	104	0.065 99	0.001 21	1.190 49	0.025 67	0.130 58	0.001 45	806	27	796	12	791	8
5	119	366	0.33	58	0.065 68	0.001 31	1.183 82	0.024 16	0.130 57	0.001 04	796	29	793	11	791	6
6	169	557	0.30	83	0.065 69	0.001 36	1.191 27	0.030 64	0.131 18	0.002 09	797	29	797	14	795	12
7	215	625	0.34	97	0.064 78	0.001 33	1.173 68	0.028 18	0.131 33	0.001 96	767	27	788	13	795	11
8	207	523	0.40	85	0.064 38	0.001 25	1.158 63	0.023 09	0.130 48	0.001 08	754	28	781	11	791	6
9	100	175	0.57	29	0.063 17	0.001 68	1.140 05	0.033 54	0.130 85	0.001 60	714	42	773	16	793	9
10	195	630	0.31	92	0.060 94	0.001 27	1.104 06	0.028 17	0.131 07	0.002 02	637	30	755	14	794	12
11	157	442	0.36	70	0.062 39	0.001 26	1.130 81	0.024 84	0.131 27	0.001 33	688	30	768	12	795	8
12	51	287	0.18	43	0.062 81	0.001 26	1.137 98	0.024 19	0.131 26	0.001 45	702	27	772	11	795	8
13	122	520	0.24	80	0.063 38	0.001 2	1.149 68	0.024 2	0.131 05	0.001 3	721	28	777	11	794	7

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表 3 额尔古纳地块新元古代侵入岩的主量元素(%)和微量元素(10^-6)的分析结果

Table 3. Major (%) elements and trace elements (10^-6) data for the Neoproterozoic intrusive rocks in the Erguna Massif

年龄	~850 Ma								~790 Ma								~762 Ma				~737 Ma
样品	12ER28-2	12ER28-3	12ER28-4	12ER28-5	13ER13-1	13ER13-3	13ER13-4	13ER13-5	14ER17-1	14ER17-2	14ER17-3	14ER17-4	14ER11-1	14ER11-3	14ER13-4	14ER13-5	12ER14-2	12ER14-3	12ER14-4	12ER14-6	12ER7-1	12ER7-2	12ER7-4	12ER7-6
SiO₂	71.60	70.97	71.35	71.03	70.87	69.13	75.15	72.34	73.94	73.96	73.60	73.78	74.84	73.69	68.70	67.93	70.40	71.68	66.88	71.54	77.18	77.59	77.95	77.93
TiO₂	0.39	0.41	0.37	0.37	0.40	0.37	0.32	0.32	0.16	0.16	0.14	0.14	0.19	0.20	0.40	0.43	0.36	0.38	0.59	0.40	0.15	0.15	0.13	0.14
Al₂O₃	13.70	14.08	14.36	14.36	14.25	15.09	11.62	13.84	14.07	14.02	14.29	14.29	13.22	13.78	15.88	14.67	14.74	14.41	15.60	14.17	11.56	11.29	11.10	11.36
TFe₂O₃	2.95	3.01	2.92	2.79	3.08	2.92	2.62	2.60	1.42	1.32	1.34	1.05	1.35	1.41	2.45	4.12	2.22	2.59	3.37	2.36	1.84	1.81	1.79	1.71
MnO	0.05	0.05	0.05	0.04	0.04	0.04	0.04	0.04	0.03	0.03	0.03	0.02	0.02	0.01	0.04	0.07	0.03	0.03	0.07	0.03	0.02	0.02	0.02	0.00
MgO	0.68	0.68	0.61	0.61	0.71	0.66	0.57	0.57	0.34	0.34	0.30	0.30	0.27	0.27	0.85	1.51	0.70	0.75	1.53	0.70	0.02	0.02	0.02	0.02
CaO	1.72	2.00	2.05	1.82	1.96	1.64	1.46	1.48	1.20	1.09	1.16	1.18	1.05	0.81	1.86	3.54	2.43	2.43	3.15	3.04	0.31	0.29	0.32	0.24
Na₂O	3.06	3.22	3.26	3.26	3.38	3.22	2.41	2.85	3.61	3.61	3.54	3.41	3.08	2.92	3.44	2.54	3.27	3.11	3.20	3.16	3.53	3.40	3.41	3.56
K₂O	4.22	4.35	4.12	4.43	4.02	5.19	4.40	5.10	4.07	4.18	4.41	4.45	4.61	5.60	4.35	3.84	3.81	3.23	3.77	3.23	4.81	4.74	4.61	4.48
P₂O₅	0.11	0.12	0.11	0.10	0.12	0.12	0.10	0.10	0.04	0.04	0.03	0.04	0.03	0.03	0.09	0.09	0.10	0.10	0.16	0.11	0.01	0.01	0.01	0.01
LOI	1.40	0.84	0.82	1.06	1.42	1.34	0.92	0.96	0.58	0.62	0.62	0.70	0.84	0.72	1.40	1.02	1.30	1.10	1.32	1.18	0.48	0.50	0.42	0.20
Total	99.94	99.73	100.02	99.89	100.35	99.84	99.63	100.30	99.62	99.48	99.54	99.58	99.64	99.62	99.68	99.94	99.40	99.87	99.72	100.02	99.91	99.87	99.79	99.65
Mg^#	31	31	29	30	31	31	30	30	32	34	31	36	28	28	41	42	38	36	47	37	1.8	1.8	1.8	1.9
Na₂O/K₂O	0.73	0.74	0.79	0.74	0.84	0.62	0.55	0.56	0.89	0.86	0.80	0.77	0.67	0.52	0.79	0.66	0.86	0.96	0.85	0.98	0.73	0.72	0.74	0.79
A/CNK	1.08	1.03	1.06	1.07	1.06	1.09	1.02	1.07	1.12	1.13	1.12	1.14	1.11	1.12	1.16	0.99	1.06	1.11	1.04	1.00	1.00	1.00	0.99	1.02
Li	20.8	35.9	32.0	24.5	16.1	14.6	19.7	20.5	17.7	16.7	21.4	21.6	17.1	8.85	35.1	34.9	7.91	9.02	17.7	8.21	1.23	1.25	1.37	1.76
Be	2.29	2.56	2.49	2.38	2.36	2.02	1.67	1.94	2.21	2.25	2.87	2.95	2.90	2.04	2.53	2.48	2.25	2.31	3.28	2.23	18.7	12.4	11.3	14.1
Sc	5.55	6.47	6.20	5.42	6.30	5.85	5.40	5.44	2.56	2.47	2.58	2.44	0.96	1.06	2.71	14.46	4.15	4.08	17.20	4.82	0.68	0.60	0.72	0.75
V	23.6	25.7	24.0	22.2	25.4	24.7	21.2	21.4	9.34	9.85	8.52	8.37	9.40	14.1	17.0	72.1	27.6	28.4	44.7	30.4	0.49	0.58	0.50	0.63
Cr	7.05	6.46	6.06	8.95	9.71	7.56	7.38	7.74	1.17	1.31	1.21	1.21	1.61	1.10	5.38	30.7	5.51	5.67	21.50	6.01	0.19	0.14	0.61	0.32
Co	4.64	4.80	4.56	4.24	5.09	4.73	4.25	4.18	1.19	1.27	0.97	1.26	1.49	1.44	2.88	7.69	3.14	3.32	6.61	3.42	0.10	0.09	0.09	0.09
Ni	3.28	3.47	3.09	4.84	4.64	3.94	3.69	3.78	0.97	0.92	0.91	1.08	1.33	1.21	2.10	5.55	1.20	1.39	9.80	1.39	0.18	0.10	1.29	0.18
Cu	2.76	1.54	1.59	3.35	3.19	7.62	5.93	18.7	2.38	4.37	1.75	0.92	4.08	1.51	0.73	2.30	2.07	1.97	3.12	9.38	1.72	1.43	4.14	4.19
Zn	45.6	50.6	48.0	43.3	46.7	44.4	41.7	41.6	34.3	30.4	28.9	31.9	19.1	16.3	64.8	53.6	39.2	41.8	66.1	45.8	165.0	102.0	141.0	52.9
Ga	17.1	19.0	19.2	17.8	19.5	19.2	15.5	17.6	17.3	16.9	17.5	17.3	15.9	15.9	20.6	17.8	17.7	17.6	20.3	18.1	33.5	32.3	32.2	34.4
Rb	188	195	188	189	168	200	173	200	139	143	166	177	143	165	134	149	90.7	87.1	119	89.7	321	302	307	236
Sr	122	132	129	123	185	161	133	155	374	344	309	292	204	203	382	227	579	558	748	568	6.64	5.84	5.77	8.26
Y	24.2	32.4	36.0	28.1	24.6	24.7	30.0	31.9	13.6	13.9	14.3	11.6	8.83	7.44	13.9	39.4	9.12	11.2	30.2	15.4	172	165	136	196
Zr	211	240	239	204	253	234	233	210	96.4	99.3	86.6	90.2	116	149	162	146	176	151	162	220	567	526	658	677
Nb	23.1	23.9	24.2	20.1	21.1	21.8	16.7	20.6	7.26	7.53	7.98	8.38	5.49	5.17	10.4	8.81	5.94	6.58	18.3	8.41	57.5	63.2	54.5	84.8
Sn	3.79	5.58	5.53	5.05	3.18	3.05	2.61	3.38	1.01	1.36	2.15	2.10	1.08	0.96	2.46	2.53	1.15	1.85	3.90	2.37	2.98	2.99	4.02	15.90
Cs	5.04	3.71	3.40	4.59	4.53	4.17	4.23	4.02	2.36	2.69	3.74	3.86	0.99	0.94	2.01	5.05	2.90	4.00	1.97	3.69	4.60	3.12	6.58	1.39
Ba	575	550	515	524	461	742	577	695	1058	1021	880	951	567	757	863	567	1752	1457	1574	1459	5.16	5.60	4.63	14.10
La	49.5	46.0	52.1	45.7	58.1	57.2	92.2	71.4	19.6	21.9	19.0	17.8	29.2	34.8	28.2	39.4	29.3	34.2	53.8	37.7	66.5	63.9	62.9	60.4
Ce	90.2	82.8	96.0	83.8	113	110	174	140	37.9	39.2	34.9	35.3	48.3	63.0	43.0	76.6	54.8	63.6	105	71.3	154	145	142	135
Pr	9.72	8.95	10.30	9.05	11.4	11.2	17.6	13.9	3.84	4.10	3.79	3.73	4.70	5.69	5.09	8.57	5.96	6.92	11.8	7.79	20.0	18.5	17.6	17.6
Nd	34.5	31.1	36.6	32.0	38.8	37.0	58.1	46.6	13.5	14.8	13.9	13.6	16.0	18.5	19.4	33.7	20.4	23.4	43.0	27.0	81.8	75.4	69.4	74.6
Sm	6.29	5.78	6.54	5.76	6.62	6.61	9.49	7.95	2.81	3.07	3.02	3.32	2.45	2.55	3.98	7.50	3.15	3.47	7.55	4.32	24.2	21.3	18.6	24.5
Eu	0.83	0.85	0.83	0.82	0.98	1.01	0.86	0.91	0.55	0.50	0.52	0.64	1.00	1.02	1.05	1.13	1.08	1.11	1.71	1.27	0.22	0.18	0.18	0.27
Gd	4.80	5.26	5.57	4.45	5.08	5.06	6.79	5.93	2.22	2.62	2.55	2.83	1.58	1.61	3.11	6.74	2.05	2.31	5.87	3.03	27.1	24.2	19.7	31.5
Tb	0.70	0.85	0.89	0.71	0.74	0.74	0.96	0.81	0.35	0.38	0.41	0.41	0.24	0.23	0.45	1.09	0.27	0.32	0.86	0.41	4.76	4.28	3.47	5.84
Dy	3.98	5.13	5.33	4.21	4.11	4.12	4.70	4.77	2.22	2.38	2.39	2.20	1.39	1.26	2.57	6.70	1.47	1.56	4.82	2.14	29.8	26.5	21.4	34.7
Ho	0.78	0.99	1.11	0.86	0.83	0.82	0.89	0.91	0.46	0.46	0.48	0.38	0.28	0.25	0.47	1.31	0.27	0.29	0.92	0.41	5.86	5.31	4.27	6.57
Er	2.05	3.06	3.17	2.44	2.29	2.17	2.53	2.57	1.41	1.43	1.32	1.02	0.83	0.75	1.20	3.59	0.82	0.84	2.76	1.22	16.2	14.8	12.2	17.5
Tm	0.29	0.45	0.47	0.39	0.34	0.36	0.38	0.40	0.23	0.23	0.21	0.16	0.15	0.13	0.19	0.54	0.12	0.14	0.39	0.19	2.27	2.02	1.78	2.45
Yb	1.85	3.06	2.90	2.57	2.26	2.23	2.36	2.71	1.57	1.52	1.45	1.00	1.00	0.94	1.15	3.26	0.83	0.93	2.68	1.22	13.9	12.7	11.9	15.1
Lu	0.26	0.44	0.40	0.34	0.35	0.34	0.35	0.41	0.25	0.23	0.22	0.15	0.15	0.15	0.19	0.47	0.14	0.14	0.40	0.18	1.76	1.60	1.61	1.79
Hf	5.48	6.42	6.59	5.49	7.01	6.28	6.41	5.87	2.78	2.96	2.48	2.79	3.22	3.89	4.59	4.19	4.72	4.14	4.52	6.00	18.5	17.6	20.7	30.4
Ta	1.68	2.12	2.42	1.90	1.46	1.46	1.23	1.66	0.54	0.41	0.56	0.71	0.59	0.41	0.87	0.67	0.38	0.47	1.55	0.65	4.09	4.50	4.20	8.89
Tl	1.09	1.11	1.07	1.04	1.01	1.18	1.00	1.19	1.14	1.17	1.32	1.49	0.80	0.93	0.81	0.82	0.94	0.87	1.27	0.92	2.34	2.23	2.33	1.46
Pb	25.9	30.1	28.9	26.8	25.2	31.3	23.3	28.7	37.5	37.2	39.6	50.8	20.6	20.6	35.9	20.2	22.6	20.7	33.0	20.7	23.4	14.0	23.8	33.7
Th	20.4	21.2	28.6	16.7	28.8	27.9	43.0	32.7	11.4	13.6	13.7	13.7	9.44	11.7	8.97	17.9	8.53	10.1	19.6	10.9	30.1	35.3	32.6	50.4
U	2.93	4.08	3.89	2.21	2.76	2.57	4.55	2.41	1.62	1.68	2.80	1.88	2.15	1.69	1.65	2.02	1.36	1.33	2.97	1.84	7.29	7.28	8.04	12.1
δEu	0.44	0.46	0.41	0.48	0.50	0.51	0.31	0.39	0.65	0.53	0.56	0.63	1.46	1.44	0.88	0.48	1.22	1.13	0.76	1.02	0.03	0.02	0.03	0.03
LREE	191	175	202	177	228	223	352	281	78.1	83.5	75.2	74.4	102	126	101	167	115	133	223	149	347	324	311	312
HREE	14.7	19.2	19.8	16.0	16.0	15.8	19.0	18.5	8.71	9.26	9.03	8.15	5.62	5.32	9.33	23.7	5.97	6.53	18.7	8.80	102	91.4	76.3	115
LREE/HREE	13.0	9.12	10.2	11.1	14.3	14.1	18.6	15.2	8.97	9.02	8.33	9.13	18.1	23.6	10.8	7.04	19.2	20.3	11.9	17.0	3.41	3.55	4.07	2.71
ΣREE	206	195	222	193	244	239	371	299	86.8	92.7	84.2	82.6	107	131	110	191	121	139	242	158	448	416	387	428
(La/Yb)_N	18.0	10.1	12.1	12.0	17.3	17.3	26.3	17.7	8.40	9.71	8.85	12.0	19.7	25.0	16.5	8.16	23.8	24.8	13.5	20.8	3.23	3.39	3.56	2.70
注：LOI.烧失量；Mg^#=100×Mg/(Mg+Fe_total²⁺)；A/CNK=mole[Al₂O₃/(CaO+Na₂O+K₂O)]；δEu=2×(Eu/0.0735)/[(Sm/0.195)+(Gd/0.259)]；LREE=La+Ce+Pr+Nd+Sm+Eu；HREE=Gd+Tb+Dy+Ho+Er+Tm+Yb+Lu；ΣREE=LREE+HREE；(La/Yb)_N=(La/0.310)/(Yb/0.209).

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表 4 额尔古纳地块新元古代侵入岩的锆石Lu-Hf同位素的分析结果

Table 4. Lu-Hf isotopic data for the Neoproterozoic igneous rocks in the Erguna Massif

样品号	¹⁷⁶Yb/¹⁷⁷Hf	误差	¹⁷⁶Lu/¹⁷⁷Hf	误差	¹⁷⁶Hf/¹⁷⁷Hf	误差	ε_Hf(0)	ε_Hf(t)	误差	T_DM1(Hf)	T_DM2(Hf)	f_Lu/Hf
12ER28-1 (850 Ma)
12ER28-1-01	0.063 650	0.001 214	0.002 539	0.000 044	0.282 149	0.000 010	-22.0	-4.7	0.4	1 619	1 880	-0.92
12ER28-1-02	0.046 993	0.000 484	0.001 915	0.000 019	0.282 125	0.000 009	-22.9	-5.2	0.3	1 627	1 909	-0.94
12ER28-1-03	0.062 718	0.000 420	0.002 507	0.000 014	0.282 142	0.000 009	-22.3	-4.9	0.3	1 628	1 893	-0.92
12ER28-1-04	0.060 510	0.000 399	0.002 364	0.000 012	0.282 126	0.000 009	-22.8	-5.4	0.3	1 645	1 920	-0.93
12ER28-1-05	0.055 588	0.000 677	0.002 230	0.000 021	0.282 136	0.000 009	-22.5	-5.0	0.3	1 625	1 897	-0.93
12ER28-1-06	0.047 412	0.000 720	0.001 924	0.000 030	0.282 125	0.000 008	-22.9	-5.2	0.3	1 628	1 909	-0.94
13ER12-1 (846 Ma)
13ER12-1-01	0.051 687	0.001 081	0.001 888	0.000 042	0.282 154	0.000 032	-21.9	-4.2	1.1	1 584	1 998	-0.94
13ER12-1-02	0.055 839	0.000 772	0.002 110	0.000 031	0.282 202	0.000 027	-20.2	-2.7	0.9	1 525	1 899	-0.94
13ER12-1-03	0.058 545	0.000 856	0.002 156	0.000 036	0.282 165	0.000 025	-21.5	-4.0	0.9	1 581	1 984	-0.94
13ER13-1 (846 Ma)
13ER13-1-01	0.050 153	0.000 335	0.001 846	0.000 010	0.282 115	0.000 022	-23.2	-5.6	0.8	1 638	2 083	-0.94
13ER13-1-02	0.054 364	0.000 590	0.001 881	0.000 016	0.282 166	0.000 019	-21.4	-3.8	0.7	1 566	1 970	-0.94
13ER13-1-03	0.069 760	0.000 977	0.002 347	0.000 027	0.282 124	0.000 021	-22.9	-5.5	0.8	1 647	2 080	-0.93
13ER13-1-04	0.056 827	0.000 361	0.002 037	0.000 009	0.282 111	0.000 020	-23.4	-5.8	0.7	1 652	2 098	-0.94
13ER13-1-05	0.043 573	0.000 431	0.001 519	0.000 011	0.282 129	0.000 023	-22.7	-4.9	0.8	1 604	2 041	-0.95
14ER17-1 (791 Ma)
14ER17-1-01	0.044 015	0.000 265	0.001 768	0.000 009	0.282 517	0.000 009	-9.0	7.5	0.3	1 061	1 160	-0.95
14ER17-1-02	0.058 751	0.001 183	0.002 112	0.000 034	0.282 533	0.000 012	-8.4	7.9	0.4	1 047	1 138	-0.94
14ER17-1-03	0.034 320	0.000 790	0.001 417	0.000 033	0.282 509	0.000 009	-9.3	7.4	0.3	1 063	1 166	-0.96
14ER17-1-04	0.033 895	0.001 537	0.001 396	0.000 064	0.282 539	0.000 010	-8.2	8.5	0.3	1 019	1 107	-0.96
14ER11-1 (795 Ma)
14ER11-1-01	0.019 903	0.000 039	0.000 827	0.000 002	0.282 443	0.000 008	-11.6	5.5	0.3	1 138	1 277	-0.98
14ER11-1-02	0.021 030	0.000 322	0.000 854	0.000 013	0.282 462	0.000 009	-10.9	6.2	0.3	1 112	1 239	-0.97
14ER11-1-03	0.019 422	0.000 540	0.000 798	0.000 020	0.282 437	0.000 009	-11.8	5.3	0.3	1 145	1 287	-0.98
14ER11-1-04	0.022 558	0.000 351	0.000 933	0.000 015	0.282 454	0.000 009	-11.2	5.8	0.3	1 126	1 258	-0.97
14ER11-1-05	0.024 507	0.000 182	0.001 016	0.000 007	0.282 422	0.000 009	-12.4	4.7	0.3	1 173	1 322	-0.97
14ER11-1-06	0.021 396	0.000 285	0.000 939	0.000 011	0.282 450	0.000 009	-11.4	5.7	0.3	1 132	1 266	-0.97
14ER11-1-07	0.028 497	0.000 626	0.001 158	0.000 025	0.282 458	0.000 010	-11.1	5.8	0.3	1 127	1 257	-0.97
14ER11-1-08	0.023 574	0.000 160	0.000 954	0.000 007	0.282 434	0.000 008	-11.9	5.1	0.3	1 154	1 297	-0.97
14ER11-1-09	0.088 909	0.002 982	0.003 514	0.000 105	0.282 490	0.000 011	-10.0	5.7	0.4	1 154	1 262	-0.89
14ER11-1-10	0.016 945	0.000 622	0.000 747	0.000 028	0.282 438	0.000 008	-11.8	5.4	0.3	1 142	1 283	-0.98
14ER13-1 (793 Ma)
14ER13-1-01	0.046 618	0.001 822	0.001 847	0.000 070	0.282 360	0.000 011	-14.6	2.0	0.4	1 289	1 470	-0.94
14ER13-1-02	0.044 892	0.001 261	0.001 788	0.000 049	0.282 362	0.000 010	-14.5	2.1	0.4	1 284	1 464	-0.95
14ER13-1-03	0.040 103	0.001 173	0.001 613	0.000 046	0.282 360	0.000 010	-14.6	2.1	0.4	1 281	1 464	-0.95
14ER13-1-04	0.027 661	0.000 567	0.001 137	0.000 022	0.282 340	0.000 010	-15.3	1.6	0.3	1 292	1 488	-0.97
13ER41-1 (794 Ma)
13ER41-1-01	0.037 100	0.000 564	0.001 342	0.000 019	0.282 370	0.000 027	-14.2	2.6	0.9	1 258	1 436	-0.96
13ER41-1-02	0.028 488	0.000 292	0.001 038	0.000 009	0.282 263	0.000 024	-18.0	-1.0	0.9	1 397	1 636	-0.97
13ER41-1-03	0.038 222	0.001 016	0.001 489	0.000 042	0.282 379	0.000 026	-13.9	2.9	0.9	1 249	1 422	-0.96
13ER41-1-04	0.031 888	0.000 424	0.001 161	0.000 018	0.282 329	0.000 021	-15.7	1.3	0.8	1 309	1 510	-0.97
13ER41-1-05	0.031 103	0.000 047	0.001 167	0.000 002	0.282 302	0.000 024	-16.6	0.3	0.9	1 347	1 563	-0.96
13ER41-1-06	0.036 852	0.000 287	0.001 413	0.000 010	0.282 307	0.000 025	-16.4	0.4	0.9	1 348	1 559	-0.96
13ER43-1 (794 Ma)
13ER43-1-01	0.036 470	0.000 197	0.001 326	0.000 006	0.282 332	0.000 022	-15.6	1.3	0.8	1 311	1 509	-0.96
13ER43-1-02	0.017 360	0.000 109	0.000 659	0.000 003	0.282 342	0.000 023	-15.2	2.0	0.8	1 274	1 470	-0.98
13ER43-1-03	0.012 876	0.000 191	0.000 527	0.000 008	0.282 299	0.000 022	-16.7	0.5	0.8	1 328	1 550	-0.98
13ER43-1-04	0.021 992	0.000 039	0.000 833	0.000 003	0.282 325	0.000 023	-15.8	1.3	0.8	1 303	1 508	-0.97
13ER43-1-05	0.027 936	0.000 071	0.001 053	0.000 003	0.282 286	0.000 024	-17.2	-0.2	0.8	1 365	1 590	-0.97
13ER43-1-06	0.023 833	0.000 224	0.000 906	0.000 009	0.282 285	0.000 024	-17.2	-0.2	0.9	1 361	1 588	-0.97
13ER44-1 (794 Ma)
13ER44-1-01	0.029 196	0.000 152	0.001 134	0.000 006	0.282 286	0.000 023	-17.2	-0.2	0.8	1 368	1 592	-0.97
13ER44-1-02	0.015 668	0.000 155	0.000 605	0.000 005	0.282 298	0.000 025	-16.8	0.4	0.9	1 333	1 555	-0.98
13ER44-1-03	0.016 969	0.000 180	0.000 647	0.000 006	0.282 314	0.000 025	-16.2	1.0	0.9	1 312	1 524	-0.98
13ER44-1-04	0.020 126	0.000 210	0.000 769	0.000 007	0.282 316	0.000 022	-16.1	1.0	0.8	1 313	1 523	-0.98
13ER44-1-05	0.018 255	0.000 036	0.000 684	0.000 001	0.282 309	0.000 026	-16.4	0.8	0.9	1 319	1 534	-0.98
13ER44-1-06	0.020 967	0.000 189	0.000 786	0.000 006	0.282 345	0.000 021	-15.1	2.0	0.7	1 273	1 467	-0.98
12ER7-1 (737 Ma)
12ER7-1-01	0.085 806	0.001 340	0.002 153	0.000 029	0.282 545	0.000 018	-8.0	7.2	0.9	1 032	1 136	-0.94
12ER7-1-02	0.105 054	0.000 468	0.002 653	0.000 008	0.282 601	0.000 017	-6.1	8.9	0.8	964	1 040	-0.92
12ER7-1-03	0.075 178	0.001 018	0.001 958	0.000 016	0.282 670	0.000 018	-3.6	11.7	0.9	845	884	-0.94
12ER7-1-04	0.103 477	0.000 913	0.002 842	0.000 022	0.282 641	0.000 019	-4.6	10.2	0.9	910	967	-0.91

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