多龙矿集区色那东岩体年龄、成因与动力学背景

王勤; 林彬; 唐菊兴; 宋扬; 李彦波; 侯俊富; 李玉彬; 卫鲁杰

doi:10.3799/dqkx.2017.613

多龙矿集区色那东岩体年龄、成因与动力学背景

doi: 10.3799/dqkx.2017.613

王勤^1,2,,
林彬²,
唐菊兴^2, ,,
宋扬²,
李彦波³,
侯俊富⁴,
李玉彬¹,
卫鲁杰³

1.
成都理工大学地球科学学院, 四川成都 610059
2.
中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室, 北京 100037
3.
西藏自治区地质矿产勘查开发局第五地质大队, 青海格尔木 816000
4.
中铝西藏矿业有限公司, 西藏拉萨 850000

基金项目:

国土资源部公益性行业科研专项经费项目 201511017

详细信息

作者简介:
王勤(1983-), 男, 博士研究生, 工程师, 从事固体矿产勘查与评价相关工作, 主要从事区域成矿学研究

通讯作者:
唐菊兴

中图分类号: P597
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- 被引次数: 0
出版历程
- 收稿日期: 2017-12-18
- 刊出日期: 2018-04-15

Diagenesis, Lithogenesis and Geodynamic Setting of Intrusions in Senadong Area, Duolong District, Tibet

Wang Qin^{1,2
,},
Lin Bin²,
Tang Juxing^{2
, ,},
Song Yang²,
Li Yanbo³,
Hou Junfu⁴,
Li Yubin¹,
Wei Lujie³

1.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Key Laboratory of Metallogeny and Mineral Resources Assessment of Ministry of Land and Resources, Beijing 100037, China
3.
No.5 Geological Party, Tibet Bureau of Geology and Exploration, Golmud 816000, China
4.
Chinalco Tibet Mining Co., Ltd., Lhasa 850000, China

摘要

摘要: 多龙矿集区是我国首个铜金属资源量达到2 000万t以上的世界级铜金矿集区，外围找矿潜力依然十分巨大.首次报道矿集区东部色那东地区花岗斑岩体和闪长玢岩体的地质年代学及地球化学测试结果，为总结区域成矿规律提供基础数据.通过精确的锆石测年，全岩主、微量元素和锆石Hf同位素测试发现，上述岩体的成岩年龄均为123±2 Ma，岩石的形成与俯冲洋壳板片部分熔融有关，源区有明显幔源组分加入.色那东地区侵入岩与矿集区含矿斑岩空间上集中侵入，且同属早白垩世岩浆活动产物，暗示其具有相同动力学背景，是班公湖-怒江洋俯冲末期-碰撞初期弧-弧"软"碰撞的产物，其侵入过程为成矿提供了热量和流体来源，显示该地区仍有较好的成矿潜力.
- 锆石U-Pb年龄 /
- 岩石学 /
- 地球化学 /
- Hf同位素组成 /
- 色那东 /
- 西藏
Abstract: Duolong district has more than 20 million tons of copper resources, which is the top large-scale Cu-Au mineral district in China. However, the prospecting potential in its peripheral region is still huge. This paper reports the geochronology and geochemical test results of the granite porphyry and diorite porphyry in the Senadong area for the first time, providing data for regional metallogenic regularity. In this study, the accurate zircon isotopic dating, Hf isotopic and whole rock major and trace elements reveal that emplacement ages of granitic and dioritic porphyries 123±2 Ma, respectively; the formation of rocks is related to partial melting of subducted oceanic plate, and the magma contains significant mantle source component. Based on these results, it is proposed that the intrusions of the Senadong area adjacent to ore-bearing porphyry in Duolong district formed during the period of the Early Cretaceous magmatic activity, suggesting that they possibly have the same geodynamic background. All these intrusions are the products of Bangongco-Nujiang ocean arc-arc "soft" collision, which occurred in the end of subduction transform to the beginning of the collision. These magmas provide heat and fluid for mineralization, which suggests that the Senadong area could be a potential district to find the new porphyry deposits.
- U-Pb dating of zircon /
- petrology /
- geochemistry /
- Hf isotope /
- Senadong /
- Tibet

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图 1 西藏多龙矿集区地质略图

SJMB.三江成矿带; BNMB.班公湖-怒江成矿带; GDMB.冈底斯成矿带; NHMB.北喜马拉雅成矿带; BNS.班公湖-怒江缝合带; IYS.雅鲁藏布江缝合带; JS.金沙江缝合带; Q.第四系; K₂a.上白垩统阿布山组; K₁m.下白垩统美日切错组; J₁q.下侏罗统曲色组; J_1-2s.下-中侏罗统色洼组; T₃r.上三叠统日干配错组; ba.枕状玄武岩; ν.辉长岩; γπ.花岗斑岩; λοπ.石英闪长玢岩; λδπ.花岗闪长斑岩; DP.闪长玢岩.据林彬等(2016)

Fig. 1. Geological sketch map of the Duolong ore cluster, Tibet

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图 2 色那东地区侵入岩野外露头及手标本、显微镜下(正交偏光)照片

a.探槽揭露的花岗斑岩露头; b.花岗斑岩手标本; c.地表出露闪长玢岩岩脉; d.闪长玢岩手标本; e.闪长玢岩镜下特征(正交).Q.石英; Pl.斜长石; Hb.角闪石

Fig. 2. Field photographs, specimens and microscope picture (cross) of intrusions in Senadong area

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图 3 色那东地区侵入岩部分锆石CL图及测点位置

Fig. 3. Cathodoluminescence (CL) images with locations of analyses and ages of selected zircons from the intrusions, Senadong area

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图 4 色那东地区侵入岩锆石LA-ICP-MS U-Pb谐和图和²⁰⁶Pb/²³⁸U加权平均值图

Fig. 4. U-Pb concordia diagram and ²⁰⁶Pb/²³⁸U weighted average age of zircon from intrusions of Senadong area

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图 5 色那东地区侵入岩锆石Hf同位素组成与U-Pb年龄相关图解

底图据刘勇等(2012)

Fig. 5. Hf isotopic composition and U-Pb ages of zircons of intrusions in Senadong area

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图 6 色那东地区闪长玢岩TAS判别图(a)和A/NK-A/CNK图解(b)

Fig. 6. TAS (a) and A/NK-A/CNK (b) classification diagrams of diorite porphyry in Senadong area

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图 7 色那东地区闪长玢岩稀土元素配分曲线(a)和微量元素蛛网图(b)

球粒陨石数据和原始地幔数据据Sun and McDonough(1989)

Fig. 7. Chondrite-normalized rare earth element patterns (a) and primitive mantle-normalized trace element patterns (b) in the Senadong area

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图 8 多龙矿集区岩浆岩时空格架

Fig. 8. Temporal and spatial framework of igneous rocks in Duolong ore cluster

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图 9 色那东闪长玢岩微量元素构造环境判别图解

Fig. 9. Tectonic diagram of trace elements of diorite porphyry in Senadong area

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表 1 色那东地区侵入岩LA-ICP-MS锆石测年结果

Table 1. 1Zircon LA-ICP-MS data of intrusions in Senadong area

测点	Th(10^-6)	U(10^-6)	Th/U	²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		年龄(Ma)
测点	Th(10^-6)	U(10^-6)	Th/U	测值	1σ	测值	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
花岗斑岩
SND-1	145.0	219.0	0.7	0.124 9	0.012 6	0.018 9	0.000 9	120	11	121	6
SND-2	86.3	276.0	0.3	0.123 5	0.013 3	0.018 7	0.000 5	118	12	120	3
SND-3	27.1	76.0	0.4	0.132 2	0.038 7	0.019 7	0.001 0	126	35	126	6
SND-4	15.9	55.8	0.3	0.114 4	0.036 4	0.016 9	0.001 2	110	33	108	7
SND-5	25.7	83.0	0.3	0.131 5	0.040 4	0.019 7	0.000 9	125	36	126	6
SND-6	50.1	123.0	0.4	0.133 8	0.027 0	0.021 0	0.001 0	128	24	134	6
SND-7	103.0	173.0	0.6	0.121 6	0.021 4	0.019 4	0.000 7	117	19	124	5
SND-8	37.2	106.0	0.4	0.125 3	0.016 9	0.018 9	0.000 8	120	15	121	5
SND-9	48.9	117.0	0.4	0.129 9	0.023 6	0.019 3	0.000 8	124	21	123	5
SND-10	31.2	79.6	0.4	0.130 7	0.032 4	0.019 2	0.000 9	125	29	123	6
SND-11	29.8	92.9	0.3	0.123 4	0.059 3	0.017 0	0.001 0	118	54	109	6
SND-12	79.4	151.0	0.5	0.132 1	0.015 6	0.019 5	0.000 7	126	14	125	4
SND-13	17.6	59.1	0.3	0.126 4	0.024 0	0.019 1	0.001 0	121	22	122	6
SND-14	21.3	55.1	0.4	0.143 8	0.031 5	0.019 9	0.001 0	136	28	127	7
SND-15	73.7	152.0	0.5	0.132 2	0.011 9	0.019 3	0.000 7	126	11	123	4
SND-16	304.0	398.0	0.8	0.141 3	0.016 4	0.019 5	0.000 6	134	15	124	4
SND-17	41.5	97.8	0.4	0.117 2	0.049 7	0.018 9	0.000 8	113	45	121	5
SND-18	6.1	19.0	0.3	0.178 9	0.110 9	0.024 1	0.002 3	167	96	154	14
SND-19	198.0	257.0	0.8	0.139 6	0.018 3	0.017 8	0.000 8	133	16	114	5
SND-20	26.6	79.9	0.3	0.127 7	0.017 9	0.017 7	0.001 2	122	16	113	8
SND-21	27.2	94.7	0.3	0.122 0	0.016 4	0.018 7	0.001 1	117	15	119	7
SND-22	47.8	126.0	0.4	0.131 9	0.020 7	0.019 4	0.000 9	126	19	124	6
SND-23	14.2	53.4	0.3	0.150 3	0.041 5	0.021 9	0.001 9	142	37	140	12
SND-24	22.2	49.3	0.5	0.126 7	0.019 1	0.020 1	0.001 2	121	17	128	8
SND-25	29.4	83.8	0.4	0.140 0	0.026 0	0.020 0	0.001 0	133	23	128	6
闪长玢岩
SC-1	43.6	110.0	0.4	0.128 8	0.017 4	0.019 3	0.000 8	123	16	123	5
SC-2	55.1	130.0	0.4	0.124 5	0.021 3	0.018 8	0.000 7	119	19	120	4
SC-3	74.1	124.0	0.6	0.117 0	0.016 7	0.017 4	0.000 6	112	15	111	4
SC-4	76.3	132.0	0.6	0.130 4	0.015 0	0.019 6	0.000 7	125	14	125	5
SC-5	36.2	93.4	0.4	0.125 6	0.021 5	0.018 9	0.001 2	120	19	121	7
SC-6	67.0	117.0	0.6	0.142 3	0.021 5	0.021 1	0.001 1	135	19	134	7
SC-7	72.1	142.0	0.5	0.134 6	0.017 3	0.020 0	0.000 8	128	15	127	5
SC-8	45.2	99.5	0.5	0.123 9	0.015 1	0.018 5	0.000 9	119	14	118	6
SC-9	268.0	201.0	1.3	0.138 3	0.020 1	0.019 0	0.000 6	132	18	122	4
SC-10	69.8	258.0	0.3	0.327 3	0.047 8	0.040 4	0.002 4	287	37	255	15
SC-11	104.0	168.0	0.6	0.135 3	0.016 7	0.018 8	0.000 6	129	15	120	4
SC-12	90.3	156.0	0.6	0.128 9	0.020 6	0.018 8	0.000 8	123	19	120	5
SC-13	59.5	123.0	0.5	0.167 3	0.016 0	0.020 2	0.001 0	157	14	129	7
SC-14	228.0	262.0	0.9	0.146 2	0.016 1	0.019 7	0.000 7	139	14	126	4
SC-15	16.7	47.5	0.4	0.136 3	0.036 8	0.019 9	0.001 1	130	33	127	7
SC-16	16.9	39.2	0.4	0.142 9	0.055 8	0.019 7	0.001 2	136	50	126	8
SC-17	90.1	160.0	0.6	0.125 4	0.010 9	0.018 9	0.000 6	120	10	121	4
SC-18	54.0	112.0	0.5	0.126 9	0.031 6	0.018 9	0.001 0	121	28	120	7
SC-19	92.8	184.0	0.5	0.127 2	0.016 3	0.019 1	0.000 7	122	15	122	4
SC-20	69.1	145.0	0.5	0.131 6	0.017 9	0.019 7	0.000 7	126	16	126	4
SC-21	25.8	70.2	0.4	0.134 2	0.027 2	0.020 1	0.001 0	128	24	128	6
SC-22	32.4	81.7	0.4	0.130 4	0.018 9	0.019 8	0.001 0	125	17	127	6
SC-23	48.0	99.0	0.5	0.131 8	0.022 1	0.019 8	0.000 8	126	20	126	5
SC-24	54.9	116.0	0.5	0.148 1	0.024 0	0.021 6	0.001 2	140	21	138	7
SC-25	142.0	210.0	0.7	0.129 6	0.012 8	0.019 4	0.000 6	124	12	124	4

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表 2 色那东地区侵入岩锆石Hf同位素分析结果

Table 2. Results of Hf isotope analysis for zircons of intrusions in Senadong area

编号	年龄(Ma)	¹⁷⁶Yb/¹⁷⁷Hf	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Hf/¹⁷⁷Hf	2σ	¹⁷⁶Hf/¹⁷⁷Hf(t)	ε_Hf(0)	ε_Hf(t)	T_DM(Ma)	f_Lu-Hf	T_DM2(Ma)
SND-1	121	0.056 908	0.001 699	0.283 044	0.000 019	0.283 040	9.6	12.1	300	-0.95	401
SND-3	126	0.053 742	0.001 578	0.283 065	0.000 021	0.283 061	10.4	13.0	269	-0.95	350
SND-5	126	0.032 741	0.000 981	0.283 033	0.000 021	0.283 031	9.2	11.9	310	-0.97	419
SND-6	134	0.061 201	0.001 820	0.283 013	0.000 022	0.283 009	8.5	11.0	346	-0.95	472
SND-9	123	0.033 276	0.000 995	0.283 078	0.000 017	0.283 076	10.8	13.4	246	-0.97	318
SND-10	123	0.051 973	0.001 576	0.283 114	0.000 022	0.283 110	12.1	14.6	198	-0.95	241
SND-13	122	0.035 579	0.001 071	0.282 985	0.000 020	0.282 983	7.5	10.1	378	-0.97	529
SND-14	127	0.044 503	0.001 346	0.283 032	0.000 020	0.283 028	9.2	11.9	315	-0.96	423
SND-17	121	0.047 193	0.001 346	0.282 977	0.000 021	0.282 974	7.3	9.8	393	-0.96	549
SC-1	123	0.063 599	0.001 881	0.283 011	0.000 021	0.283 007	8.5	11.0	349	-0.94	474
SC-2	120	0.067 863	0.001 988	0.282 973	0.000 020	0.282 969	7.1	9.6	406	-0.94	563
SC-4	125	0.064 130	0.001 868	0.282 968	0.000 017	0.282 963	6.9	9.5	412	-0.94	572
SC-5	121	0.037 756	0.001 128	0.282 993	0.000 018	0.282 990	7.8	10.5	368	-0.97	511
SC-7	127	0.039 979	0.001 194	0.282 938	0.000 017	0.282 935	5.9	8.4	447	-0.96	638
SC-8	118	0.050 002	0.001 436	0.282 953	0.000 021	0.282 949	6.4	9.1	429	-0.96	602
SC-11	120	0.041 737	0.001 230	0.282 917	0.000 020	0.282 914	5.1	7.7	478	-0.96	686
SC-12	120	0.043 266	0.001 288	0.282 967	0.000 019	0.282 964	6.9	9.4	407	-0.96	573
SC-15	127	0.026 162	0.000 796	0.282 927	0.000 018	0.282 925	5.5	8.2	459	-0.98	658
SC-16	126	0.021 010	0.000 632	0.282 927	0.000 016	0.282 926	5.5	8.2	456	-0.98	657
SC-17	121	0.059 385	0.001 712	0.282 958	0.000 021	0.282 954	6.6	9.1	425	-0.95	596
SC-18	120	0.036 961	0.001 062	0.282 861	0.000 019	0.282 859	3.2	5.7	555	-0.97	811
SC-19	122	0.054 009	0.001 565	0.282 939	0.000 020	0.282 936	5.9	8.5	450	-0.95	636
SC-21	128	0.029 887	0.000 737	0.282 555	0.000 023	0.282 553	-7.7	-4.9	979	-0.98	1 492
SC-22	127	0.054 231	0.001 615	0.282 984	0.000 019	0.282 980	7.5	10.1	386	-0.95	533
注: ε_Hf(0)=((¹⁷⁶Hf/¹⁷⁷Hf)_S/(¹⁷⁶Hf/¹⁷⁷Hf)_{CHUR, 0}-1)×10 000; ε_Hf(t)=((¹⁷⁶Hf/¹⁷⁷Hf)_S-(¹⁷⁶Lu/¹⁷⁷Hf)_S×(e^λt-1))/((¹⁷⁶Hf/¹⁷⁷Hf)_{CHUR, 0}-(¹⁷⁶Lu/¹⁷⁷Hf)_CHUR×(e^λt-1))-1)×10 000; (¹⁷⁶Hf/¹⁷⁷Hf)_i=(¹⁷⁶Hf/¹⁷⁷Hf)_S-(¹⁷⁶Lu/¹⁷⁷Hf)_S×(e^λt-1))-1; T_Hf1=10/λ×ln[1+((¹⁷⁶Hf/¹⁷⁷Hf)_S-(¹⁷⁶Hf/¹⁷⁷Hf)_DM)/((¹⁷⁶Lu/¹⁷⁷Hf)_S-(¹⁷⁶Lu/¹⁷⁷Hf)_DM)]; T_Hf2=T_Hf1-(T_Hf1-t)(f_CC-f_S)/(f_CC-f_DM); f_Lu/Hf=(¹⁷⁶Lu/¹⁷⁷Hf)_S/(¹⁷⁶Lu/¹⁷⁷Hf)_CHUR-1.其中，(¹⁷⁶Lu/¹⁷⁷Hf)_S和(¹⁷⁶Hf/¹⁷⁷Hf)_S为样品测定值; (¹⁷⁶Lu/¹⁷⁷Hf)_CHUR和(¹⁷⁶Hf/¹⁷⁷Hf)_CHUR，0值分别为0.033 2和0.282 772(Blichert-Toft and Albarède, 2008); (¹⁷⁶Lu/¹⁷⁷Hf)_DM和(¹⁷⁶Hf/¹⁷⁷Hf)_DM值分别为0.038 4和0.283 25(Griffin et al., 2000); f_CC为大陆地壳的f_Lu/Hf(-0.55, Griffin et al., 2000)，f_DM为亏损地幔的f_Lu/Hf(0.16, Griffin et al., 2000)和f_S为样品的f_Lu/Hf; λ=1.867×10^-11·a^-1(Schärer et al., 1984)，t为锆石的形成时间.

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表 3 色那东地区闪长玢岩主量、微量和稀土元素分析结果

Table 3. Results of major elements, trace elements and rare earth elements of diorite porphyry in Senadong area

Sample No.	SC-B2	SC-B3	SC-B4	SC-B5	SC-B6
SiO₂	58.4	59.2	59.1	58.5	59.2
Al₂O₃	16.6	16.7	16.7	16.3	16.6
Fe₂O₃^T	6.48	6.28	6.54	6.2	6.14
FeO	2.67	2.83	2.59	3.18	2.62
MgO	2.5	2.56	2.6	2.48	2.46
CaO	5.08	4.73	4.09	5.09	4.99
Na₂O	3.6	4.29	4.97	4.52	4.1
K₂O	1.74	1.08	0.8	1.09	1.16
MnO	0.2	0.18	0.18	0.17	0.17
TiO₂	0.59	0.58	0.6	0.58	0.58
P₂O₅	0.14	0.14	0.14	0.14	0.14
LOI	4.7	4.33	3.73	4.85	4.47
Rb	59.6	45.1	33.6	40.1	43.7
Ba	563	451	468	319	326
Th	2.87	3.02	2.78	2.89	2.85
U	0.738	0.836	0.812	0.782	0.762
Cu	15.9	63.2	22.7	27.3	32.7
Zn	200	139	127	124	134
Ta	0.47	0.5	0.49	0.47	0.5
Nb	6.04	6.21	6.22	5.97	5.9
Sr	463	531	581	564	529
Bi	0.074	0.058	0.024	0.053	0.063
Zr	71.9	70.3	72.4	70.1	64.2
Hf	2.2	2.47	2.41	2.26	2.25
Ti	3 549	3 477	3 615	3 459	3 453
K	14 444	8 965	6 633	9 048	9 630
P	607	624	629	611	611
La	12.9	14.2	13.4	12.6	12.5
Ce	24.3	25.9	24.4	23.8	24.3
Pr	3.19	3.21	3.33	3.2	3.05
Nd	13	13.9	13.7	13.5	13.2
Sm	2.98	3.29	3.12	3.19	3.06
Eu	0.98	0.89	0.87	0.77	0.87
Gd	3	3.08	2.98	2.8	2.91
Tb	0.53	0.56	0.54	0.54	0.52
Dy	3.18	3.26	3.34	3.23	3.14
Ho	0.64	0.63	0.66	0.63	0.62
Er	2.11	2.05	1.91	1.92	1.98
Tm	0.32	0.35	0.33	0.33	0.31
Yb	2.1	2.19	2.04	2.2	2.1
Lu	0.34	0.31	0.33	0.33	0.32
Y	18.1	19	18.5	18.1	17.7
∑REE	69.6	73.8	71	69	68.9
LREE/HREE	4.7	4.94	4.85	4.76	4.79
LaN/YbN	4.17	4.4	4.46	3.89	4.04
δEu	0.99	0.84	0.85	0.77	0.88
δCe	0.89	0.89	0.86	0.89	0.93
注: K=K₂O×10 000×0.830 13; Ti=TiO₂×10 000×0.599 5; P=P₂O₅×10 000×0.436 46.

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