额尔古纳地块玻乌勒山地区新元古代斜长角闪岩-片麻状花岗岩的成因及其地质意义

杨华本; 刘玉; 郑吉林; 梁中恺; 王晓勇; 唐雪峰; 苏燕平

额尔古纳地块玻乌勒山地区新元古代斜长角闪岩-片麻状花岗岩的成因及其地质意义

武警黄金第三支队, 黑龙江哈尔滨 150086

基金项目:
中国地质调查局项目《黑龙江1∶5 万碧州公社、大乌苏、玻乌勒山、沙兰山幅区域地质矿产调查》（编号：1212011220666）

详细信息

作者简介: 杨华本(1986-),男,硕士,工程师,从事区域地质调查工作。E-mail:yanghuaben@163.com

中图分类号: P534.3;P588.12⁺1

收稿日期: 2015-12-09

修回日期: 2016-07-01

刊出日期: 2017-03-25

Petrogenesis and geological significance of Neoproterozoic amphibolite and granite in Bowuleshan area, Erguna massif, Northeast China

No.3 Gold Geological Party, CAPF, Harbin 150086, Heilongjiang, China

Received Date: 09 December 2015

Revised Date: 01 July 2016

Publish Date: 25 March 2017

摘要

摘要:
对大兴安岭北段额尔古纳地块东南缘玻乌勒山地区新元古代斜长角闪岩和片麻状花岗岩进行了LA-ICP-MS 锆石UPb定年和岩石地球化学分析，讨论额尔古纳地块的演化及其与Rodinia 超大陆聚合事件的关系。斜长角闪岩的锆石阴极发光图像显示核边结构，获得核部年龄904±4Ma 和边部年龄803~886Ma；片麻状花岗岩的锆石呈自形-半自形，发育岩浆成因的振荡环带，U-Pb 年龄为915±3Ma，表明其形成于新元古代。片麻状花岗岩SiO₂=61.85%~67.63%，Mg^#=36.9-47.9，Na₂O+K₂O=4.21%~9.29%，A/CNK=0.89~1.01，属于偏铝质系列。岩石富集轻稀土元素和大离子亲石元素，亏损高场强元素Nb、Ta 和Ti，具弱的Eu 负异常、低的初始Sr 比值和正的ε_Nd(t)值，暗示片麻状花岗岩为年轻的初生地壳物质熔融形成。斜长角闪岩贫硅、Mg#较高，Ni、Cr、Co 含量较高，Zr/Hf、Nb/Ta 和Th/U 值低，具有平坦的稀土元素配分模式，与正常型洋中脊玄武岩相似，具有亏损地幔性质，同时富集大离子亲石元素Rb、Ba、K、Sr 和Pb，亏损高场强元素Nb、Ta、Ti 等，记录了消减带岩浆作用的信息，表明其为活动大陆边缘经过岛弧岩浆抽提的亏损地幔源区发生重新熔融形成。结合区域上新元古代岩浆事件的纪录，认为额尔古纳地块新元古代早期岩浆事件是Rodinia 超大陆聚合事件的响应，后期变质事件可能与Rodinia 超大陆裂解有关。
- 斜长角闪岩 /
- 片麻状花岗岩 /
- 额尔古纳地块 /
- 新元古代
Abstract:
In this paper, the authors discuss LA-ICP-MS zircon U-Pb ages, major and trace element analyses for Neoproterozoic Bowuleshan amphibolite and gneissic granite on the southeastern margin of Erguna massif, northern Da Hinggan Mountains. The purpose is to elucidate the tectonic history of the Erguna massif and its relationship to the assemblage of the Rodinia supercontinent. Zircons collected from amphibolite exhibit core-rim structure in CL images, the U-Pb dating yielded the age of 904±4Ma for magmatic core and 889~915Ma for metamorphic rim. Zircons collected from gneissic granite are euhedral-subhedral in form, and display fine-scale oscillatory growth zoning in CL images, implying a magmatic origin. The dating age is 915±3Ma. Zircon U-Pb dating demonstrates that these rocks were emplaced during the Neoproterozoic. The Neoproterozoic gneissic granite in the Erguna massif has SiO₂=61.85%~67.63%, Mg^#=36.9~47.9, Na₂O+K₂O=4.21%~9.29%, and A/CNK=0.89~1.01, suggesting metaluminous characteristics, Moreover, the Neoproterozoic granitoids are enriched in LREEs and LILEs, and depleted in HREEs and high field strength elements (HFSEs, Nb, Ta, and Ti), with Eu negative anomalies (δEu=0.77~0.80) and low initial Sr isotope ratios and positive values for the ε_Nd(t) value (3.52), which implies that their primary magmas were derived from partial melting of an original crust. In contrast, the Neoproterozoic amphibolite has low SiO₂ (45.22%~49.16%), relatively high Mg#, high Ni, Cr, low Zr/Hf, Nb/Ta and Th/ U ratios, and Co content. The flat REE patterns are analogous to features of N-type MORB from the depleted mantle source, but are characterized by enrichment of LILEs (Rb, Ba, K, Sr and Pb) and depletion of HFSEs such as Nb, Ta and Ti; it records magmatic processes of subduction zone, and indicates that amphibolite was derived from partial melting of depleted mantle wedge with igneous activity in continental arcs, on the active continental margin. On such a basis, in combination with the regional characteristics of Neoproterozoic magmatic events, the authors have reached the conclusion that the Early Neoproterozoic magmatic events of the Erguna massif occurred in the context of the assembly of the Rodinia supercontinent, and later metamorphic events might correspond to the breakup of the Rodinia supercontinent.
- amphibolite /
- gneissic granite /
- Erguna massif /
- Neoproterozoic

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图 1 中国东北地区构造简图（a）及大兴安岭玻乌勒山地区地质简图（b）（图a 据参考文献[1]，图b 据参考文献1 2 修改）

Figure 1.

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图 2 大兴安岭玻乌勒山片麻状花岗岩（a）和斜长角闪岩（b）显微照片

Figure 2.

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图 3 玻乌勒山片麻状花岗岩（a）和斜长角闪岩（b）代表性锆石CL 图像

Figure 3.

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图 4 玻乌勒山片麻状花岗岩（a）和斜长角闪岩（b）锆石U-Pb 年龄谐和图

Figure 4.

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图 5 玻乌勒山片麻状花岗岩与斜长角闪岩TAS 图^[11](a)和SiO₂-K₂O 图^[12](b)

Figure 5.

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图 6 玻乌勒山斜长角闪岩-片麻状花岗岩球粒陨石标准化稀土元素曲线(a、c)及原始地幔标准化微量元素蛛网图(b、d)(球粒陨石标准化值、原始地幔标准化值、OIB 及N-MORB 据参考文献[13])

Figure 6.

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图 7 玻乌勒山斜长角闪岩A-K 相关图解(a)^[14]、Si-((al+fm)-(c+alk))图解(b)^[15]、Nb/Y-SiO₂图解(c)^[16]和AI-CCPI 图解(d)^[17]

Figure 7.

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图 8 玻乌勒山斜长角闪岩微量元素成分构造判别图

Figure 8.

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表 1 玻乌勒山片麻状花岗岩和斜长角闪岩的LA-ICP-MS 锆石U-Th-Pb 同位素分析结果

Table 1. LA-ICP-MS zircon U-Th-Pb data of the Bowuleshangneissic granite and meta-gabbro

分析点	元素含量/10^-6		Th/U	同位素比值						年龄/Ma
	元素含量/10^-6			206Pb/238U		207Pb/235U		207Pb/206Pb		206Pb/238U		207Pb/235U
	Pb	U		测值	1σ	测值	1σ	测值	1σ	测值	1σ	测值	1σ
SPM4TC07，片麻状花岗岩，²⁰⁶Pb/²³⁸U表面年龄加权平均值为915±3Ma，MSWD=0.15；北纬51°50.034′、东经124°56.083′
1	10	61	0.719	0.1515	0.0016	1.446	0.043	0.0693	0.0021	909	9	908	27
2	8	48	0.455	0.1519	0.0017	1.453	0.062	0.0694	0.0029	912	10	911	39
3	26	155	0.656	0.1519	0.0015	1.454	0.02	0.0694	0.0009	912	9	911	13
4	12	68	0.611	0.1524	0.0016	1.456	0.03	0.0693	0.0014	915	9	913	19
5	32	164	1.337	0.1529	0.0017	1.451	0.019	0.0689	0.0008	917	10	911	12
6	15	95	0.521	0.1524	0.0017	1.46	0.029	0.0695	0.0014	915	10	914	18
7	12	77	0.259	0.1529	0.0023	1.458	0.035	0.0692	0.0016	917	14	914	22
8	15	85	0.892	0.1533	0.0016	1.473	0.026	0.0697	0.0012	919	10	920	16
9	17	98	0.708	0.1524	0.0015	1.47	0.03	0.07	0.0014	915	9	918	19
10	11	66	0.66	0.1547	0.0018	1.488	0.04	0.0698	0.0017	927	11	926	25
11	35	198	0.915	0.154	0.0017	1.49	0.017	0.0702	0.0007	924	10	926	11
12	14	90	0.559	0.1536	0.0016	1.477	0.025	0.0698	0.0011	921	10	921	16
13	15	89	0.668	0.153	0.0016	1.467	0.023	0.0696	0.001	918	10	917	14
14	14	86	0.788	0.1517	0.0015	1.463	0.025	0.0699	0.0012	911	9	915	16
15	18	108	0.737	0.1519	0.0016	1.466	0.024	0.07	0.0011	912	10	917	16
16	8	51	0.699	0.1517	0.0016	1.452	0.053	0.0694	0.0024	910	9	911	33
17	7	48	0.407	0.1519	0.0016	1.454	0.07	0.0695	0.0033	911	10	912	44
18	10	61	0.608	0.153	0.0016	1.473	0.053	0.0699	0.0025	918	9	920	34
19	11	66	0.609	0.1512	0.0015	1.455	0.055	0.0698	0.0026	908	9	912	35
20	21	141	0.168	0.1515	0.0018	1.469	0.024	0.0703	0.0009	910	11	918	15
21	12	75	0.559	0.1519	0.0016	1.474	0.035	0.0704	0.0017	912	10	920	22
22	12	83	0.14	0.1529	0.0019	1.469	0.032	0.0697	0.0014	917	11	918	20
23	16	100	0.457	0.1529	0.0016	1.482	0.028	0.0703	0.0013	917	10	923	18
24	10	65	0.459	0.1519	0.0016	1.475	0.058	0.0704	0.0027	912	10	920	36
25	51	339	0.258	0.1529	0.0015	1.468	0.016	0.0697	0.0007	917	9	918	10
26	8	47	0.49	0.1533	0.0016	1.474	0.079	0.0697	0.0037	920	10	920	49
27	8	47	0.54	0.1524	0.0016	1.459	0.062	0.0694	0.0029	915	10	914	39
28	15	93	0.548	0.1518	0.0018	1.47	0.025	0.0702	0.0011	911	11	918	16
29	15	93	0.688	0.1527	0.0015	1.463	0.028	0.0695	0.0013	916	9	915	18
30	11	70	0.552	0.1525	0.0016	1.465	0.03	0.0697	0.0014	915	9	916	19
31	15	94	0.538	0.1523	0.0017	1.46	0.025	0.0695	0.0011	914	10	914	16
32	28	199	0.027	0.1517	0.0016	1.45	0.023	0.0693	0.0009	910	10	910	15
33	5	32	0.416	0.1526	0.0018	1.453	0.065	0.0691	0.0031	915	11	911	41
34	8	50	0.612	0.1534	0.0017	1.468	0.046	0.0695	0.0022	920	10	918	29
35	13	83	0.456	0.1528	0.0015	1.471	0.03	0.0699	0.0014	917	9	919	19
36	15	98	0.489	0.1526	0.0017	1.461	0.023	0.0695	0.0011	915	10	915	15
37	37	232	0.53	0.1518	0.0018	1.455	0.018	0.0695	0.0006	911	11	912	12
38	19	135	0.012	0.1529	0.0016	1.48	0.024	0.0702	0.001	917	10	923	15
SPM4TC07，片麻状花岗岩，²⁰⁶Pb/²³⁸U表面年龄加权平均值为915±3Ma，MSWD=0.15；北纬51°50.034′、东经124°56.083′
39	5	44	0.01	0.1329	0.0014	1.332	0.064	0.0727	0.0034	805	9	860	41
40	71	385	1.427	0.1524	0.0016	1.472	0.014	0.0701	0.0005	914	10	919	9
41	12	75	0.433	0.1522	0.0017	1.459	0.032	0.0695	0.0016	913	10	914	20
42	34	220	0.364	0.1525	0.0019	1.468	0.019	0.0698	0.0006	915	11	917	12
43	17	103	0.769	0.1517	0.0015	1.45	0.022	0.0694	0.001	910	9	910	14
44	18	108	0.781	0.152	0.0016	1.465	0.021	0.0699	0.001	912	9	916	13
45	27	168	0.464	0.1523	0.0025	1.473	0.027	0.0702	0.0008	914	15	919	17
46	8	58	0.013	0.1521	0.0016	1.503	0.069	0.0717	0.0032	913	10	932	43
47	15	100	0.417	0.1526	0.0016	1.464	0.022	0.0696	0.0009	916	10	916	14
48	15	94	0.617	0.1521	0.0018	1.457	0.027	0.0695	0.0012	913	11	913	17
49	93	575	0.562	0.1524	0.0016	1.461	0.014	0.0695	0.0005	915	9	915	9
HQG，斜长角闪岩，²⁰⁶Pb/²³⁸U表面年龄加权平均值为904±4Ma，MSWD=0.54；北纬51°52.936′、东经124°51.364′
1	14	103	0.015	0.1501	0.0016	1.434	0.026	0.0692	0.0012	902	10	903	17
2	37	266	0.006	0.1507	0.0016	1.442	0.021	0.0694	0.0009	905	10	907	13
3	3	18	0.198	0.1491	0.003	1.423	0.186	0.0692	0.0095	896	18	899	117
4	1	8	0.129	0.1521	0.0027	1.465	0.252	0.0698	0.0137	913	16	916	158
5	2	13	0.061	0.1437	0.0022	1.349	0.196	0.0681	0.0104	866	13	867	126
6	13	107	0.025	0.1327	0.0016	1.204	0.036	0.0658	0.0019	803	9	803	24
7	7	50	0.122	0.1513	0.0016	1.451	0.038	0.0696	0.0017	908	9	910	24
9	1	10	0.111	0.1515	0.0027	1.46	0.218	0.0699	0.0109	909	16	914	137
8	10	70	0.085	0.1502	0.002	1.439	0.045	0.0695	0.0018	902	12	906	28
10	4	32	0.035	0.1421	0.0015	1.333	0.065	0.0681	0.0033	857	9	860	42
11	2	12	0.112	0.1478	0.0021	1.405	0.161	0.069	0.0082	889	12	891	103
12	32	224	0.059	0.1515	0.0023	1.46	0.033	0.07	0.0011	909	14	914	21
13	3	14	0.051	0.1823	0.0029	3.947	0.249	0.157	0.0098	1080	17	1623	103
14	18	131	0.013	0.15	0.0017	1.424	0.023	0.0689	0.001	901	10	899	15
15	2	12	0.068	0.1375	0.002	1.278	0.142	0.0674	0.0076	830	12	836	93
16	29	204	0.316	0.1509	0.0016	1.435	0.022	0.069	0.0009	906	10	904	14
17	6	45	0.052	0.1516	0.0019	1.461	0.05	0.0699	0.0024	910	12	915	31
18	2	18	0.054	0.1414	0.0018	1.329	0.101	0.0682	0.0052	852	11	858	65
19	2	11	0.062	0.1545	0.0023	1.504	0.179	0.0706	0.0084	926	14	932	111
20	12	87	0.041	0.1503	0.002	1.427	0.033	0.0689	0.0014	903	12	900	21
21	17	130	0.019	0.1379	0.0015	1.267	0.021	0.0666	0.001	833	9	831	14
22	32	228	0.004	0.151	0.0018	1.435	0.022	0.0689	0.0009	907	11	904	14
23	25	177	0.011	0.15	0.0017	1.433	0.023	0.0693	0.001	901	10	903	15
25	2	13	0.073	0.1509	0.0027	1.444	0.23	0.0695	0.0114	906	16	908	145
26	44	320	0.063	0.1463	0.0015	1.373	0.019	0.0681	0.0009	880	9	877	13
27	16	113	0.034	0.1511	0.0015	1.453	0.028	0.0698	0.0013	907	9	911	18
28	14	101	0.01	0.1514	0.0016	1.458	0.029	0.0698	0.0013	909	9	913	18
29	2	15	0.081	0.1518	0.002	1.465	0.138	0.07	0.0066	911	12	916	87
30	2	11	0.118	0.1593	0.0024	1.57	0.167	0.0715	0.0077	953	15	959	102
HQG，斜长角闪岩，²⁰⁶Pb/²³⁸U表面年龄加权平均值为904±4Ma，MSWD=0.54；北纬51°52.936′、东经124°51.364′
31	12	87	0.007	0.1488	0.0015	1.418	0.036	0.0692	0.0017	894	9	897	23
32	3	18	0.11	0.1381	0.0018	1.279	0.1	0.0672	0.0051	834	11	837	66
33	9	66	0.013	0.1521	0.0017	1.47	0.034	0.0702	0.0016	912	10	918	22
34	12	88	0.096	0.1474	0.0016	1.398	0.032	0.0688	0.0016	886	10	888	21
35	3	20	0.046	0.1525	0.002	1.462	0.092	0.0696	0.0044	915	12	915	58
36	2	12	0.077	0.1479	0.0021	1.403	0.162	0.0688	0.0082	889	13	891	103
37	5	38	0.037	0.1501	0.0016	1.433	0.05	0.0693	0.0024	902	10	903	32
38	2	11	0.139	0.1516	0.0023	1.462	0.188	0.07	0.0092	910	14	915	118
39	3	14	0.075	0.2001	0.0024	2.204	0.148	0.0799	0.0054	1176	14	1183	79
40	5	33	0.04	0.1508	0.0022	1.441	0.074	0.0693	0.0032	905	13	906	47
41	10	70	0.018	0.1483	0.0017	1.42	0.03	0.0695	0.0013	891	10	898	19
42	2	10	0.167	0.1507	0.0023	1.451	0.185	0.0699	0.0093	905	14	911	116

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表 2 玻乌勒山片麻状花岗岩与斜长角闪岩主量、微量、稀土元素和Sr-Nd 同位素分析结果

Table 2. Major, trace elements, REE and Sr-Nd isotopic compositionsfor Bowuleshan gneissic granite and amphibolite

样号岩性	PM5TC 3-1	PM4TC 07	PM5TC 04	PM25TC9	HQG1	HQG3	HQG4
样号岩性	片麻状花岗岩			斜长角闪岩
SiO₂	61.85	67.63	67.3	47.85	49.16	45.22	46.02
Al₂O₃	16.86	13.59	15.42	13.8	15.63	15.08	14.68
TiO₂	0.72	0.68	0.62	1.57	0.75	1.05	0.77
Fe₂O₃	3.1	2.67	1.56	4.12	4.64	4.41	4.52
FeO	1.46	3.09	1.84	9.13	6.44	6.39	5.58
CaO	2.85	4.77	1.94	10.99	10.39	11.98	13.54
MgO	1.4	1.88	1.33	7.22	6.34	10	9.56
K₂O	4.73	0.46	3.22	0.44	0.52	1.09	0.85
Na₂O	4.55	3.76	4.93	2.33	2.88	1.35	1.3
MnO	0.101	0.119	0.08	0.216	0.24	0.161	0.165
P₂O₅	0.294	0.162	0.179	0.141	0.065	0.049	0.033
LOI	1.83	1.11	1.35	2.03	2.8	3.02	2.78
总和	99.76	99.91	99.79	99.84	99.86	99.81	99.8
FeOT	4.25	5.49	3.25	12.84	10.62	10.36	9.65
A/CNK	0.95	0.89	1.02	0.57	0.65	0.6	0.53
Mg^#	36.9	37.8	42.3	50.1	51.5	63.2	63.8
SI	9.15	15.8	10.4	31.1	30.4	43	43.8
Rb/Sr	0.22	0.07	0.13	0.03	0.03	0.17	0.09
σ	4.58	0.72	2.74	1.58	1.88	2.68	1.52
Y	17.15	34.93	18.03	27.8	14.8	31.2	19.7
La	41.01	13.01	37.35	5.57	2.11	1.68	1.53
Ce	85.77	42.25	75.29	14.8	4.55	3.62	2.95
Pr	10.33	4.15	9.07	2.38	0.73	0.81	0.58
Nd	37.47	17.84	31.55	12.1	3.77	5.45	3.8
Sm	6.29	4.82	5.2	3.57	1.42	2.59	1.62
Eu	1.44	1.24	1.16	1.38	0.65	1.08	0.73
Gd	4.8	4.87	4.08	3.79	1.66	3.32	2.11
Tb	0.7	1.04	0.66	0.79	0.39	0.8	0.49
Dy	3.62	6.55	3.42	5.43	2.78	5.89	3.67
Ho	0.64	1.37	0.65	1.1	0.57	1.23	0.77
Er	1.98	4.4	2.05	2.94	1.61	3.47	2.16
Tm	0.31	0.73	0.36	0.5	0.29	0.58	0.37
Yb	1.96	4.49	2.25	3.2	1.8	3.59	2.26
Lu	0.52	0.54	0.29	0.43	0.25	0.52	0.31
Li	16.66	7.91	10.86	7.91	23.3	38.8	24.4
Be	2.95	2.36	2.14	0.52	0.57	0.35	0.48
Sc	8.06	20.21	5.28	44.2	45.4	47.6	33.9
V	61.6	64.5	53.9	335	338	313	221
Cr	8.6	20.3	8.8	337	112	353	442
Co	9.2	15.8	6.9	47.3	41.6	51.8	37.3
Ni	4.3	7.9	7.2	54.7	32.3	121	114
Ga	20.27	17.94	20.38	18.2	22.5	19.3	15.9
Rb	123.3	15.9	46.8	7.25	13.6	46.9	29.6
Sr	555.8	234.9	357.2	220	518	273	324
Zr	311.3	230.3	278.7	102	30.6	32.3	27.7
Nb	15.07	8.25	15.06	4.95	1.03	0.51	0.66
Mo	0.17	0.2	0.26	0.4	0.24	0.37	0.3
Ba	893.8	150.6	810.5	96.5	176	300	341
Hf	7.65	8.9	14.94	5.99	1.65	2.24	1.74
Ta	0.94	0.55	1.08	0.48	0.34	0.38	0.17
Pb	19.8	6	23.1	3.12	10.6	9.4	23.2
Th	8.93	5.11	14.52	0.38	0.17	0.11	0.13
U	1.6	0.7	2.01	0.15	0.087	0.086	0.1
Cl	44.7	93	63.8	57.9	37	79.9	51.9
F	530	290	408	412	360	564	480
ΣREE	214	142.24	191.42	85.75	37.36	65.83	43.05
LREE/HREE	5.75	1.41	5.02	0.87	0.55	0.3	0.35
(La/Yb)_N	8.38	2.57	13.58	1.4	0.9	0.35	0.52
δEu	0.8	0.78	0.77	1.14	1.29	1.13	1.2
⁸⁷Sr/⁸⁶Sr		0.704774
⁸⁷Sr/⁸⁶Sr(i)		0.703387
¹⁴³Nd/¹⁴⁴Nd		0.512657
ε_Nd(915Ma)		3.52
T_DM2(Ga)		1.28
注：A/CNK=（Al₂O₃）/（CaO⁺K₂O⁺Na₂O）；Mg^#=100×Mg²⁺/（Mg²⁺+Fe²⁺+Fe³⁺）；δEu=Eu_N/[（Gd_N+Sm_N）/2]；“_N”表示相对于球粒陨石标准化值；固结指数(SI)=MgO×100/(MgO+FeO+F₂O₃+Na₂O⁺K₂O)；主量元素含量单位为%，微量和稀土元素含量为10^-6

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参考文献(53)

[1]	Wu F Y, Zhao G C, Sun D Y, et al. The Hulan Group: Its role in the evolution of the Central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences, 2007, 30(3/4):542-556. https://www.researchgate.net/publication/223492632_The_Hulan_Group_Its_role_in_the_evolution_of_the_Central_Asian_Orogenic_Belt_of_NE_China
[2]	任纪舜, 牛宝贵, 刘志刚. 软碰撞、叠覆造山和多旋回缝合作用[J]. 地学前缘, 1999,(3):85-93. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199903010.htm
[3]	谢鸣谦. 拼贴板块构造及其驱动机理:中国东北及邻区的大地构造演化[M]. 北京:科学出版社, 2000.
[4]	孙广瑞, 李仰春, 张昱. 额尔古纳地块基底地质构造[J]. 地质与资源, 2002, 11(3):129-139. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200203000.htm
[5]	苗来成, 刘敦一, 张福勤,等. 大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMP U-Pb年龄[J]. 科学通报, 2007, 52(5):591-601. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200705018.htm
[6]	表尚虎, 郑卫政, 周兴福. 大兴安岭北部锆石U-Pb年龄对额尔古纳地块构造归属的制约[J]. 地质学报, 2012, 86(8):1262-1272. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201208010.htm
[7]	王洪波, 杨晓平. 大兴安岭北段新一轮国土资源大调查以来的主要基础地质成果与进展[J]. 地质通报, 2013, 32(2/3):525-532. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2013Z1025.htm
[8]	Liu Y, Hu Z, Gao S, et al. In situ, analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1/2):34-43. https://www.researchgate.net/profile/Yongsheng_Liu5/publication/222034389_In_situ_analysis_of_major_and_trace_elements_of_anhydrous_minerals_by_LA-ICP-MSLA-ICP-MS_without_applying_an_internal_standard/links/54067d610cf2c48563b2536f/In-situ-analysis-of-major-and-trace-elements-of-anhydrous-minerals-by-LA-ICP-MSLA-ICP-MS-without-applying-an-internal-standard.pdf
[9]	Liu Y, Gao S, Hu Z, et al. Continental and Oceanic Crust Recycling-induced Melt - Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths[J]. Journal of Petrology, 2010, 51(1/2):392-9.
[10]	Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LAICP-MS[J]. Science Bulletin, 2010, 55(15):1535-1546. doi: 10.1007/s11434-010-3052-4
[11]	Middlemost E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4): 215-224. http://www.oalib.com/references/7414805
[12]	Peccerillo A, Taylor S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to mineralogy and petrology, 1976, 58(1): 63-81. doi: 10.1007/BF00384745
[13]	Sun S S, Mcdonough W F. Chemical and Isotopic Systematics of Oceanic Basalts; Implications for Mantle Composition and Processes[J]. Geological Society London Special Publications, 1989, 42(1): 313-345. doi: 10.1144/GSL.SP.1989.042.01.19
[14]	周世泰. 恢复变质岩原岩的一种岩石化学方法[J]. 辽宁地质学报, 1981, (1):178-187.
[15]	Simonen A. Stratigraphy and sedimentation of the Svecofennidic, early Archeansupracrustal rocks in southwestern Finland[J]. Bulletin of the Geological Society of Finland, 1953, 160:1-64.
[16]	Winchester J A, Floyd P A. Geochemical discrimination of different magma series and their differentiation products using immobile elements[J]. Chemical Geology, 1977, 20(4):325-343. http://www.academia.edu/17797804/Geochemical_discrimination_of_different_magma_series_and_their_differentiation_products_using_immobile_elements
[17]	Large R R. The Alteration Box Plot: A Simple Approach to Understanding the Relationship between Alteration Mineralogy and Lithogeochemistry Associated with Volcanic-Hosted Massive Sulfide Deposits[J]. Economic Geology, 2001, 96(5):957-971. https://pangea.stanford.edu/research/ODEX/EG/papers/Abs96-5_files/large2.pdf
[18]	Maclean W H. Mass change calculations in altered rock series[J]. MineraliumDeposita, 1990, 25(1):44-49.
[19]	Shannon R D. Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides[J]. Acta Crystallographica Section A, 1976, 32(5):751-767. doi: 10.1107/S0567739476001551
[20]	Niu Y, Batiza R. Trace element evidence from seamounts for recycled oceanic crust in the Eastern Pacific mantle[J]. Earth & Planetary Science Letters, 1998, 155(1/2):147-147. https://www.researchgate.net/publication/222314997_Trace_element_evidence_from_seamounts_for_recycled_oceanic_crust_in_the_Eastern_Pacific_mantle_vol_148_pg_471_1997
[21]	Niu Y, Hékinian R. Basaltic liquids and harzburgitic residues in the Garrett Transform: a case study at fast-spreading ridges[J]. Earth & Planetary Science Letters, 1997, 146(1/2):243-258. https://www.researchgate.net/publication/245580976_Basaltic_liquids_and_harzburgitic_residues_in_the_Garrett_Transform_A_case_study_at_fast-spreading_ridges
[22]	Niu Y. Bulk-rock Major and Trace Element Compositions of Abyssal Peridotites: Implications for Mantle Melting, Melt Extraction and, Post-melting Processes Beneath Mid-Ocean Ridges[J]. Journal of Petrology, 2004, 45(12):2423-2458. doi: 10.1093/petrology/egh068
[23]	Niu Y. ChemInform Abstract: Earth Processes Cause Zr-Hf and Nb-Ta Fractionations, but Why and How?[J]. ChemInform, 2012, 43(29):3587-3591. https://www.researchgate.net/publication/264214788_ChemInform_Abstract_Earth_Processes_Cause_Zr-Hf_and_Nb-Ta_Fractionations_but_Why_and_How
[24]	Alard O, Luguet A, Pearson N J, et al. In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle[J]. Nature, 2005, 436(7053):1005-8. doi: 10.1038/nature03902
[25]	Thompson R N, O'Hara M J. An Assessment of the Relative Roles of Crust and Mantle in Magma Genesis: An Elemental Approach[and Discussion][J]. Philosophical Transactions of the Royal Society A Mathematical Physical & Engineering Sciences, 1984, 310(1514):549-590.
[26]	Eiler J M, Crawford A, Elliott T, et al. Oxygen Isotope Geochemistry of Oceanic-Arc Lavas[J]. Journal of Petrology, 2000, 41(2):229-256. doi: 10.1093/petrology/41.2.229
[27]	Chung S L, Wang K L, Crawford A J, et al. High-Mg potassic rocks from Taiwan: implications for the genesis of orogenic potassiclavas[J]. Lithos, 2001, 59(4):153-170. doi: 10.1016/S0024-4937(01)00067-6
[28]	Taylor S R, Mclennan S M. The Continental Crust: Its Composition and Evolution, An Examination of the Geochemical Record Preserved in Sedimentary Rocks[J]. Journal of Geology, 1985, 94(4): 632-633. https://www.researchgate.net/publication/224929850_The_Continental_Crust_its_Composition_and_Evolution_An_Examination_of_the_Geochemical_Record_Preserved_in_Sedimentary_Rocks
[29]	Mahoney J J, Coffin M F. Plume/Lithosphere Interaction in the Generation of Continental and Oceanic Flood Basalts: Chemical and Isotopic Constraints[C]//Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism. American Geophysical Union, 2013:335-355.
[30]	Jochum K P, Mcdonough W F, Palme H, et al. Compositional constraints on the continental lithospheric mantle from trace elements in spinel peridotitexenoliths[J]. Nature, 1989, 340(6234):548-550. doi: 10.1038/340548a0
[31]	Pearce J A, Norry M J. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks[J]. Contributions to Mineralogy and Petrology, 1979, 69(1):33-47. doi: 10.1007/BF00375192
[32]	汪云亮, 张成江, 修淑芝. 玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别[J]. 岩石学报, 2001, 17(3):413-421. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200103008.htm
[33]	万渝生, 吴澄宇, 张炳熹, 稀土元素地球化学与玄武质岩石的成因-应用与问题. 岩石圈研究的现代方法.[M] 北京: 原子能出版社, 1997: 215-228.
[34]	Taylor S R, Mclennan S M. The chemical composition of the Archaeancrust[J]. Geological Society London Special Publications, 1986, 24:173-178. doi: 10.1144/GSL.SP.1986.024.01.16
[35]	Taylor S R, Mclennan S M. The geochemical evolution of the continental crust[J]. Reviews of Geophysics, 1995, 33(2):293-301.
[36]	高山, 骆庭川, 张本仁,等. 中国东部地壳的结构和组成[J]. 中国科学:地球科学, 1999, 29(3):204-213. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199903001.htm
[37]	洪大卫, 王式, 谢锡林,等. 兴蒙造山带正ε_Nd(t)值花岗岩的成因和大陆地壳生长[J]. 地学前缘, 2000(2):441-456.
[38]	Wu F Y, Jahn B M, Wilde S, et al. Phanerozoic crustal growth: UPb and Sr-Nd isotopic evidence from the granites in northeastern China[J]. Tectonophysics, 2000, 328(1):89-113. https://www.researchgate.net/publication/223576713_Phanerozoic_crustal_growth_U-Pb_and_Sr-Nd_isotopic_evidence_from_the_granites_in_northeastern_China
[39]	Jahn B M, Griffin W L, Windley B. Continental growth in the Phanerozoic: Evidence from Central Asia[J]. Tectonophysics, 2000, 328(328):vii-x. https://www.researchgate.net/publication/240379167_Continental_growth_in_the_Phanerozoic_Evidence_from_Central_Asia
[40]	吴福元, 孙德有. 东北地区显生宙花岗岩的成因与地壳增生[J]. 岩石学报, 1999, 15(2):181-189. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB902.003.htm
[41]	Martin H. Adakitic magmas: modern analogues of Archaeangranitoids[J]. Lithos, 1999, 46(3):411-429. doi: 10.1016/S0024-4937(98)00076-0
[42]	罗毅, 王正邦, 周德安. 额尔古纳超大型火山热液型铀成矿带地质特征及找矿前景[J]. 东华理工大学学报(自然科学版), 1997(1): 1-10. http://www.cnki.com.cn/Article/CJFDTOTAL-HDDZ701.000.htm
[43]	武广, 孙丰月, 赵财胜,等. 额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义[J]. 科学通报, 2005, 50(20):2278-2288. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200520016.htm
[44]	边红业, 吉峰, 表尚虎. 大兴安岭富西里地区赞岐岩-(石英)二长闪长岩LA-ICP-MS锆石U-Pb定年及其地质意义[J]. 世界地质, 2014, 33(4):768-779. http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ201404004.htm
[45]	Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1): 1-30. doi: 10.1016/j.jseaes.2010.11.014
[46]	Gou J, Sun D Y, Ren Y S, et al. Petrogenesis and geodynamic setting of Neoproterozoic and Late Paleozoic magmatism in the Manzhouli-Erguna area of Inner Mongolia, China: Geochronological, geochemical and Hf isotopic evidence[J]. Journal of Asian Earth Sciences, 2013, 67: 114-137. https://www.researchgate.net/publication/258794425_Petrogenesis_and_geodynamic_setting_of_Neoproterozoic_and_Late_Paleozoic_magmatism_in_the_Manzhouli-Erguna_area_of_Inner_Mongolia_China_Geochronological_geochemical_and_Hf_isotopic_evidence
[47]	张一涵. 内蒙古东北部额尔古纳河群和乌宾敖包组的形成时代与物源:碎屑锆石U-Pb年代学证据[D]. 吉林大学硕士学位论文, 2014.
[48]	李明. 中国东北现代河流碎屑锆石U-Pb年代学和Hf同位素研究及大陆生长与演化[D]. 中国地质大学博士学位论文, 2010.
[49]	陈岳龙, 李大鹏, 刘长征, 等. 大兴安岭的形成与演化历史: 来自河漫滩沉积物地球化学及其碎屑锆石U-Pb年龄, Hf同位素组成的证据[J]. 地质学报, 2014, 88(1): 1-14. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201401001.htm
[50]	Powell C M, Powell C M. Assembly and break-up of Rodinia: introduction to the special volume[J]. Precambrian Research, 2001, 110(1):1-8. https://www.researchgate.net/publication/263311146_Assembly_and_break-up_of_Rodinia_Introduction_to_the_special_volume
[51]	郭进京, 张国伟, 陆松年,等. 中国新元古代大陆拼合与Rodinia超大陆[J]. 高校地质学报, 1999(2):148-156. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX902.002.htm
[52]	周建波, 曾维顺, 曹嘉麟,等. 中国东北地区的构造格局与演化:从500Ma到180Ma[J]. 吉林大学学报(地), 2012, 42(5):1298-1316. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201205005.htm
[53]	Hoffman P F. Did the breakout of laurentia turn gondwanaland inside-out?[J]. Science, 1991, 252(5011):1409-12. doi: 10.1126/science.252.5011.1409