内蒙古东部钓鱼台地区火山岩年代学、地球化学特征及地质意义

王利; 梁天意

doi:10.12401/j.nwg.2023036

内蒙古东部钓鱼台地区火山岩年代学、地球化学特征及地质意义

王利,
梁天意^,

辽宁省化工地质勘查院有限责任公司，辽宁锦州　121007

基金项目: 中国地质调查局项目“内蒙古1∶5万钓鱼台等四幅区域地质调查”（DD20160201-07）资助。

详细信息

作者简介: 王利（1987−），男，高级工程师，主要从事基础及矿产地质研究。E−mail：373519089@qq.com

通讯作者: 梁天意（1988−），男，博士，高级工程师，主要从事基础地质、矿产地质方面的研究。E−mail：327251026@qq.com。

中图分类号: P595；P588.12

收稿日期: 2022-09-20

修回日期: 2022-12-27

录用日期: 2023-01-26

刊出日期: 2025-02-20

Geochronology, Geochemistry and Geological Significance of Volcanic Rocks in the Diaoyutai Area, Eastern Inner Mongolia

WANG Li,
LIANG Tianyi^,

Chemical Geological Prospecting Institute of Liaoning Province Co.LTD, Jinzhou121007, Liaoning, China

More Information

Corresponding author: LIANG Tianyi, 327251026@qq.com

Received Date: 20 September 2022

Revised Date: 27 December 2022

Accepted Date: 26 January 2023

Publish Date: 20 February 2025

摘要

摘要:
笔者通过对内蒙古东部钓鱼台地区火山岩岩石学、年代学和地球化学等方面的研究，探讨该地区火山岩形成时代、岩浆来源及构造背景，为研究大兴安岭中段地区在中-晚侏罗世的岩浆活动和构造演化提供依据。笔者选取钓鱼台地区满克头鄂博组流纹质凝灰岩，系统地开展岩石学、LA-ICP-MS U-Pb测年和岩石地球化学等研究工作。根据研究结果显示，内蒙古东部钓鱼台地区的满克头鄂博组火山岩形成于中—晚侏罗世（160.3±2.2 ）Ma，火山岩SiO₂含量平均为74.98%，Al₂O₃含量平均为13.33%，CaO含量平均为0.82%，全碱（ALK）含量平均为6.96%，显示为高钾钙碱性系列岩石，稀土元素配分曲线为明显的右倾特征，轻稀土富集而重稀土亏损，轻重稀土分馏明显，Eu具有明显的负异常，岩石表现为富集Rb、Th、U、Nd等大离子亲石元素（LILE），亏损Nb、Sr、P、Ti等高场强元素（HFSE），与A型花岗岩的地球化学特征相似。结合区域地质资料和前人研究成果，研究区内满克头鄂博组火山岩岩浆主要来源于地壳的部分熔融，可能有地幔物质参与，产生于伸展构造背景下，推断与蒙古-鄂霍茨克洋闭合后板块俯冲后撤作用导致的岩石圈伸展作用有关。
- 大兴安岭中段 /
- U-Pb年代学 /
- 岩石地球化学 /
- 满克头鄂博组 /
- 构造背景
Abstract:
Through the study of the petrology, chronology and geochemistry of volcanic rocks in Diaoyutai area in Eastern Inner Mongolia, to discuss the formation age of volcanic rocks, the source of magma and the tectonic background in this area, and to provide a basis for studying the magmatic activity and tectonic evolution in the middle part of the Great Xing'an Range during the Mid-Late Jurassic. This paper selects rhyolite tuff from Manketouebo Formation in Diaoyutai area, Studies on petrology, LA-ICP-MS U-Pb dating and rock geochemistry have been carried out systematically. According to the research results, the volcanic rocks of the Manketouebo Formation in the Diaoyutai area of eastern Inner Mongolia were formed in the middle to Late Jurassic (160.3±2.2) Ma, The average SiO₂ content of medium coarse monzogranite is 74.98%, the average Al₂O₃ content is 13.33%, the average CaO content is 13.33%, the average total alkali (ALK) content is 6.96%, it shows high potassium calc-alkaline series rocks. The distribution curve of rare earth elements is right-leaning, with enrichment of light rare earth and deficit of heavy rare earth, significant fractionation of light and light rare earth, and Eu has obvious negative anomaly, the rocks are enriched in Rb、Th、U、Nd (LILE), and depleted in Nb、 Sr、P、Ti (HFS), and the geochemical characteristics are similar to those of A-type granite. Combined with regional geological data and previous research results, the volcanic magma of the Manketouebo Formation in the study area is mainly derived from the partial melting of the crust, which may involve mantle material, and it should be generated in the extensional tectonic background. It is inferred that it is related to the lithosphere extension caused by the plate subduction and retraction after the closure of the Mongolian-Okhotsk Ocean.
- The middle part of the Great Xing'an Range /
- U-Pb Chronology /
- geochemistry /
- Manketouebo Formation /
- tectonic background

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图 1 钓鱼台地区地质简图（a据刘晨等，2017改编）

Figure 1.

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图 2 钓鱼台地区火山岩野外（a）及镜下照片（b）

Figure 2.

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图 3 钓鱼台地区火山岩部分锆石阴极发光（CL）图

Figure 3.

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图 4 钓鱼台地区火山岩（TW11）锆石U-Pb年龄谐和图(a)及加权平均图(b)

Figure 4.

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图 5 钓鱼台地区火山岩TAS图解和SiO₂-K₂O图解（a据Irvine et al., 1971；b据Peccerillo et al., 1976）

Figure 5.

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图 6 钓鱼台地区火山岩微量元素原始地幔标准化蛛网图（a）和稀土元素球粒陨石标准化REE图解（b）（标准化数据源自Sun等, 1989）

Figure 6.

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图 7 钓鱼台地区火山岩类型判别图解（a据Whalen et al., 1987; b据Alther et al., 2000）

Figure 7.

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图 8 钓鱼台地区火山岩构造判别图解（a据Pearce et al., 1984; b据Eby, 1990）

Figure 8.

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表 1 钓鱼台地区火山岩（TW11）锆石U-Pb测试结果

Table 1. Zircon U-Pb test results of volcanic rocks（TW11）in the Diaoyutai area

编号	含量（10⁻⁶）			Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²³⁸U/²³²Th	²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U
编号	Pb	Th	U	Th/U	比值	1σ	比值	1σ	比值	1σ	比值	年龄（Ma）	1σ	年龄（Ma）	1σ	年龄（Ma）	1σ
TW11-01	37.5	162.9	690.3	0.24	0.0533	0.002	0.1878	0.0072	0.0256	0.0003	3.13	342.7	89.8	174.8	6.2	163	2.1
TW11-02	44.8	247.6	452.1	0.55	0.0561	0.0029	0.1964	0.0099	0.0255	0.0003	1.37	453.8	110.2	182.1	8.4	162.3	2.2
TW11-03	42.6	224.9	609.2	0.37	0.0523	0.0022	0.1761	0.0076	0.0245	0.0003	2.16	301.9	91.7	164.7	6.5	156	2
TW11-04	29.2	94.3	139.3	0.68	0.0606	0.0036	0.3916	0.0236	0.0467	0.0008	1.12	633.4	123.9	335.5	17.2	294.2	5
TW11-05	82.2	400.1	1221.7	0.33	0.0519	0.0016	0.1747	0.0053	0.0244	0.0002	2.4	279.7	70.4	163.5	4.6	155.6	1.4
TW11-06	36.9	155.2	665.8	0.23	0.0493	0.0021	0.1683	0.0069	0.0249	0.0003	3.26	164.9	100	157.9	6	158.7	1.9
TW11-07	41.7	148.4	126.9	1.17	0.0547	0.0047	0.3462	0.0275	0.0467	0.0008	0.67	466.7	195.3	301.8	20.7	294.3	4.6
TW11-08	29.7	128.9	558.8	0.23	0.0483	0.002	0.1685	0.0064	0.0255	0.0003	3.37	122.3	96.3	158.1	5.5	162.4	2
TW11-09	51	110.9	157.7	0.7	0.0605	0.0032	0.5803	0.0324	0.0694	0.0012	1.14	620.4	114.8	464.7	20.8	432.3	7
TW11-10	61.2	206.7	257.2	0.8	0.0532	0.0031	0.3368	0.0187	0.0464	0.0007	0.97	338.9	126.8	294.8	14.2	292.4	4.1
TW11-11	31.3	139.8	495.7	0.28	0.0505	0.0025	0.1764	0.0085	0.0255	0.0003	2.8	216.7	112.9	165	7.3	162.4	2
TW11-12	20.3	123.3	141.9	0.87	0.0546	0.0044	0.1938	0.0154	0.0259	0.0005	0.91	394.5	178.7	179.9	13.1	164.8	3
TW11-13	38	260	176.4	1.47	0.0476	0.0047	0.1582	0.014	0.0249	0.0005	0.54	79.7	218.5	149.1	12.3	158.6	3.5
TW11-14	27.4	92.3	147.4	0.63	0.0564	0.0032	0.3524	0.0217	0.0454	0.0009	1.23	477.8	121.3	306.5	16.3	286.2	5.8
TW11-15	65.2	465.6	237.5	1.96	0.0545	0.0037	0.1912	0.0125	0.0259	0.0004	0.43	390.8	186.1	177.6	10.7	165	2.5
TW11-16	25.3	150.5	258.4	0.58	0.048	0.0032	0.162	0.0102	0.025	0.0004	1.36	101.9	148.1	152.5	8.9	159.1	2.4
TW11-17	60.3	278.2	812.8	0.34	0.0514	0.002	0.1878	0.0076	0.0265	0.0004	2.2	257.5	90.7	174.8	6.5	168.5	2.5
TW11-18	23.7	124.8	289.3	0.43	0.051	0.0031	0.1833	0.0113	0.0264	0.0005	1.72	242.7	144.4	170.9	9.7	168	2.9
TW11-19	42.1	209.3	649.6	0.32	0.0505	0.0027	0.1731	0.0094	0.0248	0.0003	2.59	220.4	119.4	162.1	8.2	158.2	2.1
TW11-20	92.4	583	801.8	0.73	0.0538	0.0022	0.1833	0.0074	0.0248	0.0003	1.43	364.9	60.2	170.9	6.3	158	1.9

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表 2 钓鱼台地区火山岩主量元素（%）、微量和稀土元素（10⁻⁶）分析结果

Table 2. Major (%), trace and REE element (10⁻⁶) analytical results of volcanic rocks in the Diaoyutai area

样品编号	DP7H01	DP7H02	DP7H03	DP7H04	DP7H05	DP7H06
岩石名称	流纹质凝灰岩
SiO₂	75.32	74.92	73.14	75	76.64	74.88
TiO₂	0.06	0.06	0.14	0.23	0.19	0.29
Al₂O₃	14.41	13.64	14.04	12.51	12.6	12.79
Fe₂O₃	0.53	0.15	0.3	1.27	0.69	1.01
FeO	0.68	1.69	1.72	0.68	0.54	0.97
MnO	0.03	0.07	0.09	0.06	0.07	0.06
MgO	0.75	0.56	1.15	0.47	0.31	0.28
CaO	0.52	0.95	2.33	0.52	0.3	0.3
Na₂O	2.68	2.56	1.9	2.5	2.18	4.42
K₂O	3.56	4.4	3.89	4.87	4.2	4.62
P₂O₅	0.04	0.06	0.07	0.05	0.03	0.05
LOI	1.7	1.07	1.03	1.18	2.16	0.71
∑	100.27	100.14	99.81	99.34	99.91	100.4
ALK	6.24	6.96	5.79	7.37	6.38	9.04
N/K	0.75	0.58	0.49	0.51	0.52	0.96
A/CNK	1.57	1.28	1.21	1.21	1.45	1
Mg^#	53.61	35.36	50.74	31.49	32.25	20.99
SI	9.15	5.98	12.83	4.81	3.92	2.48
DI	5.4	11.99	8.49	18.91	16.04	26.17
Li	31.73	34.04	46.73	3.58	6.55	5.48
Be	3.44	2.25	3	3.48	3.48	2.41
V	6.96	4.04	9.63	12.02	14.15	8.81
Cr	2.14	1.69	1.57	2.27	14.67	2.52
Co	0.2	0.28	1.07	1.18	3.73	0.53
Ni	1.59	0.59	1.22	1.4	10.89	3.41
Cu	2.05	1.72	2.91	3.21	3.16	3.58
Zn	21.07	42.35	42.29	80.57	89.32	131.63
Ga	22.98	19.22	16.7	22.44	19.59	18.85
Rb	148.93	152.94	102.92	180.9	199.38	118.41
Zr	93.41	126.5	110.7	251.16	196.38	242.26
Nb	12.43	10.87	8.54	19.63	21.99	13.69
Mo	1.17	1.82	0.32	0.53	3.27	0.36
In	0.16	0.03	0.02	0.03	0.02	0.02
Ba	741.57	1207.12	595.11	152.26	103.65	387.61
Sr	51.9	205.21	154.72	73.08	43.53	54.27
Hf	3.57	3.1	3.63	8.43	8.04	6.74
Ta	0.98	0.7	0.6	1.38	1.68	0.88
W	0.45	0.25	0.26	1.04	1.56	2.11
Pb	21	19.88	11.48	20.89	37.09	16.91
Bi	0.13	0.12	0.01	0.5	0.63	0.07

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续表2
样品编号	DP7H01	DP7H02	DP7H03	DP7H04	DP7H05	DP7H06
Th	5.55	4.59	4.96	19.4	21.65	8.77
U	1.74	1.57	1.44	4.05	6.05	2.1
Au	0.81	0.85	1.38	0.74	0.42	1.22
Ag	0.06	0.04	0.03	0.04	0.05	0.06
B	21.83	13.29	11.18	4.46	8.01	4.33
F	1536.74	639.06	880.52	381.14	465.67	264.69
Y	14	14.1	12.1	23.6	25.1	27.1
La	19.3	14.9	20.5	29.8	40.1	35.9
Ce	39.2	42	37.1	70.6	64.1	63
Pr	3.96	3.25	4.2	6.52	8.64	8.84
Nd	13.9	11.6	14.6	22.7	27.1	34.8
Sm	2.77	2.48	2.54	4.07	4.62	6
Eu	0.46	0.53	0.66	0.36	0.31	0.79
Gd	2.51	2.14	2.22	3.82	4.26	5.13
Tb	0.41	0.36	0.35	0.61	0.69	0.78
Dy	2.36	2.16	1.98	3.88	4.4	4.47
Ho	0.43	0.39	0.38	0.8	0.85	0.84
Er	1.17	1.04	1.09	2.42	2.64	2.37
Tm	0.2	0.18	0.21	0.47	0.52	0.44
Yb	1.21	1.11	1.22	2.88	3.15	2.64
Lu	0.18	0.16	0.19	0.44	0.49	0.41
ΣREE	88.06	82.3	87.24	149.37	161.87	166.41
LREE	79.59	74.76	79.6	134.05	144.87	149.33
HREE	8.47	7.54	7.64	15.32	17	17.08
LREE/HREE	9.4	9.92	10.42	8.75	8.52	8.74
(La/Yb)_N	11.44	9.63	12.05	7.42	9.13	9.75
δEu	0.53	0.7	0.85	0.28	0.21	0.44
δCe	1.1	1.48	0.98	1.24	0.84	0.87

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