大兴安岭多宝山晚三叠世双峰式侵入岩年代学及地球动力学背景

刘宝山; 程招勋; 钱程; 张春鹏; 钟辉; 韩仁萍

doi:10.3799/dqkx.2020.214

大兴安岭多宝山晚三叠世双峰式侵入岩年代学及地球动力学背景

doi: 10.3799/dqkx.2020.214

1.
中国地质调查局沈阳地质调查中心, 辽宁沈阳 110034
2.
黑龙江省自然资源调查院, 黑龙江哈尔滨 150036

基金项目:

国家重点研发计划项目“典型矿集区三维地质结构与矿体定位” 2017YFC0601305

中国地质调查局地质调查项目 DD20190156

黑龙江省1∶5万矿调成果综合研究及找矿靶区优选项目 GY[2018]003

详细信息

作者简介:
刘宝山(1970-), 男, 高级工程师, 主要从事地质矿产调查.ORCID: 0000-0002-0841-6997.E-mail: liubaoshan1111@163.com

中图分类号: P588.12
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出版历程
- 收稿日期: 2020-07-20
- 刊出日期: 2021-07-15

Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area

1.
Shenyang Geological Survey Center, China Geological Survey, Shenyang 110034, China
2.
Heilongjiang Institute of Natural Resources, Harbin 150036, China

摘要

摘要: 多宝山矿区发现有侵位于晚奥陶世花岗闪长岩的角闪辉长岩和英云闪长岩，二者具有双峰式侵入岩的特征，在详细的野外地质调查基础上，对多宝山双峰式侵入岩进行了岩石学、年代学、地球化学方面的研究，并初步探讨其构造意义.角闪辉长岩的LA-ICP-MS锆石U-Pb年龄为224.3±1.7 Ma，英云闪长岩为226.3±2.3 Ma，两者形成于同一构造岩浆作用事件；侵入岩的SiO₂含量呈双峰式，稀土、微量元素特征表明它们具有岛弧岩浆特征，二者具有相同的岩石圈地幔源区，其源区可能受到了俯冲流体交代作用的影响.结合区域构造背景，认为其形成与鄂霍茨克洋壳俯冲有关，产于活动大陆边缘环境，它们可能是受地壳混染的OIB型玄武质岩浆在地壳中部的一个“双扩散”岩浆房通过结晶分异形成的.
- 双峰式侵入岩 /
- 晚三叠世 /
- 岛弧 /
- 大兴安岭 /
- 多宝山 /
- 构造地质
Abstract: Hornblende gabbro and tonalite which emplaced in Late Ordovician granodiorite were found in Duobaoshan mining area, possessed the characteristics of bimodal pattern intrusive rock.On the basis of detailed field geological survey, we reaserched the petrology, geochronology and geochemistry characteristics of bimodal pattern intrusive rock, and discuss their tectonic significance. The LA-ICP-MS zircon U-Pb ages of hornblende gabbro is 224.3±1.7 Ma, the LA-ICP-MS zircon U-Pb ages of tonalite is 226.3±2.3 Ma, they were both formed by the same tectonic magmatism.The SiO₂ content of intrusive rock is bimodal, their rare earth elements and microelements indicates the characteristics of island arc magma.They have the same mantle source, which influenced by the subduction metasomatic alteration of fluids. Based on analysis of the regional tectonic background, its formation is related to the Okhotsk subduction. The gabbro and tonalite which formed in the active continental margin environment, were interpreted to be formed through assimilation of OIB-type basaltic magma followed by fractional crystallization in a.double diffusive'magma chamber at the middle crust level.
- bimodal invasion rock /
- Late Triassic /
- island arc /
- Da Hinggan /
- Duobaoshan /
- tectonics

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图 1 多宝山地区地质简图

1. 第四系；2. 白垩系；3. 三叠系；4. 泥盆系；5. 志留系；6. 奥陶系；7. 早侏罗世花岗闪长岩；8. 早侏罗世花岗闪长斑岩；9. 晚三叠世花岗闪长岩/闪长岩；10. 中奥陶世花岗闪长斑岩；11. 早奥陶世花岗闪长岩；12. 闪长岩脉；13. 铜矿体；14. 韧性剪切带；15. 火山岩；16. 古生界/新生界；17. 花岗岩；18. 二长花岗岩；19. 断层；20. 地质界线；21. 铜/金/银矿床；22. 矿区；改绘引自文献石国明等（2018）；角图 1据张兴洲等（2006）；角据图 2杜琦等（1988）

Fig. 1. Geological map of Duobaoshan deposit

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图 2 多宝山矿区Ⅲ号采坑NW-SE壁地质单元岩性断面图

Fig. 2. Cross-section map of the No.Ⅲ ore zone in the Duobaoshan deposit

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图 3 角闪辉长岩与英云闪长岩接触关系特征

a. 角闪辉长岩；b. 英云闪长岩；c. 角闪石穿过角闪辉长岩与英云闪长岩接触界线；d. 角闪辉长岩与英云闪长岩成分互相溶通混合

Fig. 3. Contact characteristics of hornblende gabbro and tonalite

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图 4 多宝山双峰侵入岩显微照片

a. 英云闪长岩；b. 角闪辉长岩；c. 混染角闪辉长岩；d. 混染角闪辉长岩绿泥石交代角闪石；Qtz. 石英；Pl. 斜长石；Mus. 白云母；Kfs. 钾长石；Hb. 角闪石；Chl. 绿泥石

Fig. 4. Photomicrographs of Duobaoshan bimodal invasion rock

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图 5 角闪辉长岩及英云闪长岩锆石阴极发光图像及其测试位置及年龄值、Hf同位素值

Fig. 5. CL images of zircon crystals from hornblende gabbro and tonalite

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图 6 多宝山双峰式侵入岩锆石年龄谐和图

Fig. 6. Zircon U-Pb concordia diagrams of Duobaoshan bimodal invasion rock

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图 7 角闪辉长岩和英云闪长岩的锆石Hf同位素ε_Hf(t)-t图和¹⁷⁶Hf/¹⁷⁷Hf-t图

Fig. 7. Zircon Hf isotopic ε_Hf(t) vs. t plot and histogram of ¹⁷⁶Hf/¹⁷⁷Hf-t form hornblende gabbro and tonalite

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图 8 Zr/TiO₂×10^-4-Nb/Y图解(a)和SiO₂-K₂O(b)图解

Fig. 8. Zr/TiO₂×10^-4-Nb/Y (a) and SiO₂-K₂O (b) diagrams of gabbro and tonalite

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图 9 多宝山双峰侵入岩稀土元素球粒陨石标准化图解(a)和微量元素原始地幔标准化图解(b)

Fig. 9. Chondrite-normalized REE-patterns(a) and primitive mantle normalized spider diararm(b) for Duobaoshan bimodal invasion rock

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图 10 角闪辉长岩和英云闪长岩的Ba/Th-Th/Nb(a)和Ba/Zr-Th/Zr(b)图解

Fig. 10. Ba/Th-Th/Nb (a) and Ba/Zr-Th/Zr (b) diagrams for the hornblende gabbro and tonalite

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图 11 英云闪长岩Sr/Y-w(Y)(a)和(La/Yb)_N-Yb_N(b)图解

Fig. 11. Sr/Y-w(Y) (a) and (La/Yb)_N-Yb_N (b) diagrams for the Tonalite

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图 12 角闪辉长岩La/Nb-La(a)和Th/Yb-Ta/Yb(b)图解

Fig. 12. La/Nb-La (a) and Th/Yb-Ta/Yb (b) diagrams for the hornblende gabbro

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表 1 角闪辉长岩及英云闪长岩LA-ICP-MS锆石U-Pb测年结果

Table 1. LA-ICP-MS zircon U-Pb dating results of hornblende gabbro and tonalite

测点号	含量（10^-6）		Th/U	同位素比值						年龄(Ma)
测点号	Th	U	Th/U	²⁰⁷Pb/ ²⁰⁶Pb	误差（%）	²⁰⁷Pb/ ²³⁵U	误差（%）	²⁰⁶Pb/ ²³⁸U	误差（%）	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ
DBS01-01	67.7	98.5	0.7	0.06	0.35	0.26	1.57	0.03	0.05	217.1	2.9	431.5	140.7
DBS01-02	112.0	142	0.8	0.05	0.28	0.25	1.32	0.04	0.05	224.7	2.8	309.3	122.2
DBS01-03	55.4	78.5	0.7	0.05	0.34	0.27	1.61	0.04	0.06	235.0	3.6	309.3	148.1
DBS01-04	65.6	110	0.6	0.06	0.27	0.27	1.30	0.03	0.04	221.1	2.8	442.6	109.2
DBS01-05	118.0	145	0.8	0.06	0.28	0.27	1.30	0.04	0.04	223.4	2.4	450.0	111.1
DBS01-06	125.0	152	0.8	0.05	0.25	0.26	1.28	0.04	0.05	229.1	2.9	342.7	112.0
DBS01-07	109.0	156	0.7	0.05	0.26	0.25	1.20	0.04	0.05	229.4	3.0	213.0	120.4
DBS01-08	94.2	136	0.7	0.06	0.27	0.27	1.35	0.04	0.05	225.4	2.9	453.8	113.9
DBS01-09	75.0	122	0.6	0.05	0.25	0.26	1.18	0.04	0.04	227.1	2.7	322.3	102.8
DBS01-10	77.5	122	0.6	0.05	0.28	0.24	1.24	0.04	0.04	222.0	2.4	235.3	134.2
DBS01-11	239.0	248	1.0	0.05	0.19	0.26	0.98	0.04	0.04	232.2	2.5	250.1	83.3
DBS01-12	80.6	117	0.7	0.06	0.35	0.26	1.68	0.03	0.05	218.0	2.9	450.0	138.9
DBS01-13	107.0	139	0.8	0.05	0.25	0.25	1.21	0.04	0.04	225.6	2.7	209.3	110.2
DBS01-14	93.2	121	0.8	0.05	0.26	0.25	1.34	0.03	0.04	221.1	2.5	264.9	116.7
DBS01-15	100.0	147	0.7	0.05	0.24	0.26	1.19	0.04	0.04	228.4	2.8	301.9	137.9
DBS01-16	64.5	106	0.6	0.05	0.26	0.27	1.28	0.04	0.05	235.0	3.1	350.1	109.2
DBS01-17	80.0	119	0.7	0.05	0.28	0.26	1.25	0.04	0.05	230.0	2.9	344.5	118.5
DBS01-18	96.6	135	0.7	0.05	0.26	0.27	1.21	0.04	0.04	228.7	2.7	394.5	105.5
DBS01-19	89.6	116	0.8	0.05	0.34	0.24	1.62	0.04	0.04	223.7	2.8	209.3	155.5
DBS01-20	88.3	145	0.6	0.05	0.26	0.26	1.31	0.04	0.04	235.8	2.5	235.3	113.9
DBS01-21	107.0	153	0.7	0.06	0.23	0.28	1.13	0.04	0.04	236.2	2.7	427.8	94.4
DBS01-22	266.0	242	1.1	0.05	0.22	0.25	1.00	0.03	0.03	220.9	2.1	287.1	99.1
DBS01-23	128.0	149	0.9	0.06	0.24	0.26	1.18	0.03	0.04	221.2	2.6	409.3	98.1
DBS01-24	50.1	89.3	0.6	0.05	0.33	0.25	1.55	0.04	0.05	226.1	3.0	253.8	151.8
DBS01-25	74.5	139	0.5	0.05	0.26	0.25	1.25	0.04	0.05	230.5	3.1	209.3	122.2
DBS04-01	311.0	259	1.2	0.05	0.20	0.25	0.92	0.03	0.03	218.4	2.1	324.1	85.2
DBS04-02	143.0	185	0.8	0.05	0.22	0.26	1.07	0.04	0.04	224.4	2.8	361.2	94.4
DBS04-03	355.0	357	1.0	0.06	0.20	0.27	0.88	0.04	0.04	225.5	2.4	433.4	79.6
DBS04-04	407.0	336	1.2	0.05	0.19	0.26	0.91	0.03	0.03	220.4	1.9	346.4	84.3
DBS04-05	600.0	372	1.6	0.05	0.18	0.25	0.83	0.04	0.04	222.7	2.4	287.1	79.6
DBS04-06	227.0	235	1.0	0.05	0.21	0.25	1.07	0.04	0.04	224.7	2.4	227.8	96.3
DBS04-07	558.0	484	1.2	0.05	0.14	0.25	0.67	0.04	0.03	228.6	1.9	172.3	68.5
DBS04-08	341.0	293	1.2	0.05	0.17	0.25	0.81	0.04	0.04	223.5	2.2	239.0	77.8
DBS04-09	213.0	230	0.9	0.05	0.20	0.25	0.92	0.03	0.04	218.7	2.4	331.5	87.0
DBS04-10	401.0	265	1.5	0.05	0.18	0.25	0.81	0.04	0.04	226.5	2.3	194.5	81.5
DBS04-11	469.0	431	1.1	0.05	0.15	0.25	0.71	0.04	0.03	227.6	1.9	205.6	36.1
DBS04-12	314.0	252	1.2	0.05	0.18	0.26	0.85	0.04	0.03	223.8	2.0	305.6	75.0
DBS04-13	468.0	302	1.6	0.05	0.18	0.24	0.85	0.04	0.03	221.8	1.8	198.2	78.7
DBS04-14	829.0	650	1.3	0.05	0.14	0.24	0.69	0.04	0.03	225.0	1.8	172.3	64.8
DBS04-15	1 014.0	647	1.6	0.05	0.13	0.24	0.60	0.03	0.03	220.0	1.7	211.2	61.1
DBS04-16	499.0	455	1.1	0.05	0.17	0.25	0.76	0.03	0.03	217.9	1.9	366.7	73.1
DBS04-17	312.0	305	1.0	0.05	0.17	0.24	0.78	0.03	0.04	218.1	2.3	213.0	43.5
DBS04-18	184.0	243	0.8	0.05	0.21	0.26	0.97	0.04	0.04	227.6	2.3	327.8	88.9
DBS04-19	425.0	358	1.2	0.05	0.16	0.25	0.79	0.04	0.03	227.0	2.0	239.0	72.2
DBS04-20	159.0	192	0.8	0.05	0.21	0.25	1.06	0.04	0.04	231.7	2.5	209.3	98.1
DBS04-21	336.0	289	1.2	0.05	0.17	0.23	0.81	0.04	0.04	223.1	2.5	79.7	85.2
DBS04-22	222.0	268	0.8	0.05	0.15	0.23	0.73	0.04	0.03	226.6	2.1	400.1	-320
DBS04-23	425.0	342	1.2	0.05	0.15	0.25	0.77	0.04	0.03	231.0	2.1	189.0	70.4
DBS04-24	178.0	194	0.9	0.05	0.20	0.24	1.01	0.04	0.04	224.9	2.7	105.6	-94.4
DBS04-25	307.0	263	1.2	0.05	0.19	0.25	0.88	0.04	0.03	231.6	2.2	168.6	87.0

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表 2 角闪辉长岩和英云闪长岩锆石的LA-ICP-MS Hf同位素分析结果

Table 2. LA-ICP-MS zircon Hf isotopic compositions of hornblende gabbro and tonalite

样品编号	年龄(Ma)	¹⁷⁶Hf/¹⁷⁷Hf	1σ	¹⁷⁶Lu/¹⁷⁷Hf	1σ	¹⁷⁶Yb/¹⁷⁷Hf	1σ	ε_Hf(t)	t_DM1 (Ma)	t_DM2 (Ma)
DBS01-10	222.0	0.282 945	0.000 010	0.001 987	0.000 020	0.060 258	0.000 744	10.7	447	571
DBS01-19	223.7	0.282 973	0.000 011	0.002 174	0.000 024	0.062 486	0.000 770	11.7	408	508
DBS01-08	225.4	0.282 935	0.000 011	0.002 363	0.000 019	0.070 283	0.000 668	10.4	467	597
DBS01-02	224.7	0.282 919	0.000 010	0.002 335	0.000 012	0.071 291	0.000 421	9.8	489	631
DBS01-13	225.6	0.282 936	0.000 011	0.002 469	0.000 017	0.072 792	0.000 464	10.4	467	595
DBS01-15	228.4	0.282 942	0.000 010	0.002 515	0.000 013	0.074 225	0.000 358	10.6	458	581
DBS01-09	227.1	0.282 926	0.000 010	0.002 579	0.000 026	0.078 397	0.000 860	10.0	483	618
DBS01-06	229.1	0.282 903	0.000 010	0.002 957	0.000 055	0.092 137	0.001 832	9.2	521	671
DBS04-02	224.4	0.282 946	0.000 010	0.003 919	0.000 045	0.115 580	0.001 173	10.5	470	586
DBS04-03	225.5	0.282 969	0.000 010	0.004 008	0.000 057	0.112 198	0.001 705	11.3	436	535
DBS04-06	224.7	0.282 947	0.000 009	0.003 387	0.000 032	0.099 689	0.001 004	10.6	461	578
DBS04-10	226.5	0.282 922	0.000 010	0.003 982	0.000 064	0.117 898	0.002 292	9.7	508	640
DBS04-19	227.0	0.282 979	0.000 010	0.004 216	0.000 083	0.126 598	0.002 490	11.7	423	513

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表 3 角闪辉长岩和英云闪长岩主量元素（%）和微量元素(10^-6)分析结果

Table 3. Maior elements (%) and rare earth elements (10^-6) of hornblende gabbro and tonalite

样号	DBS04-1	DBS04-2	DBS04-3	DBS04-4	DBS01-1	DBS01-2	DBS01-3	DBS01-4
岩性	角闪辉长岩	角闪辉长岩	角闪辉长岩	角闪辉长岩	英云闪长岩	英云闪长岩	英云闪长岩	英云闪长岩
SiO₂	44.16	43.81	43.73	43.89	64.29	64.51	66.44	64.25
Al₂O₃	16.47	18.70	17.11	19.30	17.03	17.21	16.54	16.74
Fe₂O₃	2.31	4.78	2.69	4.23	1.54	1.86	1.29	1.56
FeO	4.95	6.14	6.30	5.89	1.39	1.00	1.16	1.32
MgO	14.77	6.48	12.40	6.07	0.99	1.14	1.03	1.16
CaO	8.10	9.31	8.43	9.61	2.95	2.75	2.27	2.73
Na₂O	3.65	2.91	3.15	3.15	5.61	5.53	5.54	5.42
K₂O	0.66	1.44	0.70	1.13	2.88	2.96	2.62	2.84
MnO	0.096	0.13	0.11	0.12	0.10	0.099	0.085	0.097
P₂O₅	0.20	0.44	0.28	0.65	0.17	0.17	0.16	0.17
TiO₂	1.07	1.51	1.37	1.38	0.36	0.33	0.31	0.33
LOI	3.66	4.19	3.73	4.57	2.18	2.38	2.44	2.76
Total	100.09	99.84	100.00	100.00	99.48	99.95	99.86	99.37
Li	13.0	12.2	14.7	15.1	8.13	3.99	8.26	3.71
Sc	19.2	21.4	24.8	20.8	2.99	2.35	2.22	2.26
V	152	198	192	184	23.7	23.8	20.7	20.8
Cr	8.73	11.2	8.64	6.55	19.8	13.7	11.7	4.81
Co	35.0	43.5	43.3	38.7	5.12	4.87	3.42	4.13
Cu	107	87.5	75.3	87.1	19.8	53.3	14.7	34.1
Zn	74.4	80.1	78.7	78.8	99.9	72.9	73.5	71.2
Ga	22.2	23.2	21.4	22.4	21.1	19.6	20.1	19.3
Rb	9.96	20.2	9.70	15.0	34.9	37.0	32.3	37.7
Sr	1 200	1 200	1 200	1 400	964	726	798	744
Y	19.1	24.4	23.5	22.3	11.5	10.2	9.91	10.7
Zr	108	69.3	100	75.0	216	210	205	223
Nb	4.02	4.51	4.56	2.80	7.52	6.94	6.36	6.71
Ni	0.45	1.05	1.33	0.92	6.29	4.76	3.26	2.44
Be	1.21	0.97	1.13	1.03	2.20	2.12	1.93	2.17
Cd	0.095	0.17	0.086	0.14	0.28	0.29	0.25	0.27
Sn	1.70	1.37	2.29	1.41	1.58	1.70	1.65	2.29
Cs	0.73	1.27	0.71	1.06	1.09	1.39	1.19	1.32
Ba	248	430	233	335	934	1000	767	905
La	19.0	18.3	20.2	18.8	35.7	31.8	28.5	33.2
Ce	43.9	44.9	48.3	46.8	73.0	65.3	62.6	67.3
Pr	6.49	6.88	7.36	7.22	8.97	8.00	7.57	8.16
Nd	29.6	34.9	34.3	34.1	33.0	29.2	26.5	29.8
Sm	6.00	7.06	7.36	7.13	4.72	4.23	4.12	4.37
Eu	1.77	2.32	2.10	2.16	1.90	2.02	1.49	1.87
Gd	4.61	5.37	5.56	5.38	3.90	3.44	3.19	3.61
Tb	0.70	0.84	0.86	0.83	0.47	0.41	0.38	0.44
Dy	3.78	4.54	4.63	4.40	2.17	1.95	1.90	1.99
Ho	0.69	0.91	0.85	0.81	0.39	0.34	0.32	0.35
Er	1.72	2.12	2.16	2.06	1.05	0.95	0.91	0.97
Tm	0.29	0.38	0.36	0.33	0.18	0.17	0.15	0.17
Yb	1.66	2.04	2.07	1.89	1.13	1.00	0.94	1.00
Lu	0.21	0.28	0.26	0.26	0.15	0.13	0.12	0.13
Hf	3.41	3.79	4.41	3.44	3.14	3.02	2.77	3.06
Ta	0.40	0.46	0.66	0.51	0.58	0.55	0.60	0.95
Pb	10.8	10.8	13.1	9.93	60.3	35.0	40.3	29.1
Th	2.14	1.76	1.85	1.47	4.68	4.77	4.68	5.38
U	0.44	0.43	0.52	0.39	1.44	1.33	1.06	1.31
∑REE	120.38	130.83	136.27	132.13	166.80	148.86	138.66	153.33
LREE	106.71	114.35	119.53	116.17	157.36	140.46	130.76	144.69
HREE	13.67	16.48	16.74	15.96	9.44	8.40	7.90	8.65
L/H	7.81	6.94	7.14	7.28	16.67	16.73	16.55	16.73
δCe	0.60	0.47	0.72	0.50	0.13	0.10	0.13	0.13
δEu	0.99	1.11	0.96	1.03	1.31	1.57	1.21	1.40

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大兴安岭多宝山晚三叠世双峰式侵入岩年代学及地球动力学背景

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刘宝山(1970-), 男, 高级工程师, 主要从事地质矿产调查.ORCID: 0000-0002-0841-6997.E-mail: liubaoshan1111@163.com

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Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area

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大兴安岭多宝山晚三叠世双峰式侵入岩年代学及地球动力学背景

doi: 10.3799/dqkx.2020.214

作者简介: 刘宝山(1970-), 男, 高级工程师, 主要从事地质矿产调查.ORCID: 0000-0002-0841-6997.E-mail: liubaoshan1111@163.com

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Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area

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作者简介:
刘宝山(1970-), 男, 高级工程师, 主要从事地质矿产调查.ORCID: 0000-0002-0841-6997.E-mail: liubaoshan1111@163.com