内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义

秦锦华; 刘翠; 石玉若; 罗照华; 邓晋福; 李玥霄

doi:10.3799/dqkx.2018.585

内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义

doi: 10.3799/dqkx.2018.585

1.
中国地质科学院矿产资源研究所, 北京 100037
2.
中国地质大学地球科学与资源学院, 北京 100083
3.
中国地质科学院地质研究所, 北京 100037

基金项目:

中国地质调查局项目 DD20160056

中国地质调查局项目 1212011121075

中国地质调查局项目 12120114020901

中国地质调查局项目 12120115069701

详细信息

作者简介:
秦锦华(1992-), 男, 博士研究生, 矿物学、岩石学、矿床学专业

通讯作者:
刘翠

中图分类号: P581
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- 被引次数: 0
出版历程
- 收稿日期: 2018-05-21
- 刊出日期: 2019-04-15

Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia

Qin Jinhua^{1,2
,},
Liu Cui^{2
, ,},
Shi Yuruo³,
Luo Zhaohua²,
Deng Jinfu²,
Li Yuexiao²

1.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

摘要

摘要: 晶洞花岗岩成因类型和大地构造背景等方面的研究，目前颇具争议.先前的研究认为晶洞碱长、正长花岗岩属于A型花岗岩，形成于伸展环境，近年来的研究发现其成因类型具多样性.报道了博克图晶洞花岗岩的岩石学、岩石地球化学、年代学等方面的特征.SHRIMP锆石U-Pb定年结果为140.8±2.2 Ma，指示其属于早白垩世的产物.且其具有高SiO₂，高ALK（Na₂O+K₂O）（7.99%~8.43%），K₂O/Na₂O=1.0~1.1，以及低的FeO^T（1.15%~1.30%）.微量元素富Th、U、Cs、Rb，贫Ba、Sr、P、Ti，10 000*Ga/Al、总稀土含量以及Zr+Nb+Y+Ce值均低于A型花岗岩最低平均值，由此指示其应属于Ⅰ型花岗岩，Hf同位素特征显示其成分为新生地壳来源.动力学机制上，博克图晶洞花岗岩主要受制于早白垩世时期蒙古-鄂霍次克洋闭合作用.在东北地区岩石圈由增厚到减薄转换事件中，早期的新生地壳在地幔物质的底侵作用下发生低程度的部分熔融作用.
- 晶洞花岗岩 /
- Ⅰ型花岗岩 /
- SHRIMP U-Pb年龄 /
- 部分熔融 /
- 岩石学
Abstract: Genetic types and tectonic backgrounds of miarolitic granite are still controversial. Previous studies have suggested that miarolitic alkali feldspar granites and miarolitic syenite granites belong to A-type granite formed in extensional environment. However, recent studies have found the diversity of the genetic types. In this paper, the petrology, geochemistry and geochronology of Boketu miarolite pluton are present. The zircon SHRIMP U-Pb dating results yield an age of 140.8±2.2 Ma, belonging to the Early Cretaceous. The pluton is characterized by high SiO₂ content, and full high alkali content (7.99%-8.43%), with high K₂O/Na₂O (1.0-1.1); low total Fe content (1.15%-1.30%). On the primitive mantle-normalized spider diagrams, the granite is characterized by positive Th, U, Cs, Rb anomalies and negative Ba, Sr, P, Ti anomalies. 10 000*Ga/Al ratio, the total rare earth content and Zr+Nb+Y+Ce values are lower than the minimum value of the A-type granites. It is indicated that it should belong to Ⅰ-type granite. Hf isotope compositions show the source of juvenile crust. It is mainly restricted by the closure of the Mongolian-Okhotsk ocean, during which the lithosphere transformation from thickening to thinning took place. The granites are formed by the low-degree partial melting of juvenile crust in the underplating of the mantle.
- miarolitic granite /
- Ⅰ-type granite /
- SHRIMP U-Pb dating /
- partial melting /
- petrology

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图 1 东北地区构造简图

①蒙古-鄂霍次克缝合带；②德尔布干断裂；③贺根山断裂；④西拉沐沦断裂；⑤嫩江-八里罕断裂；⑥牡丹江断裂；⑦佳木斯-伊通断裂；⑧敦化-密山断裂；⑨锡霍特-阿林中央带断裂；红色五角星为博克图晶洞花岗岩岩体位置.据张兴洲等(2006)修改

Fig. 1. Tectonic map of NE China

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图 2 博克图地区地质简图

据内蒙古区域地质调查院(2007, 内蒙古自治区1:25万扎兰屯幅地质图)改

Fig. 2. Geological map of Boketu area

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图 3 博克图晶洞花岗岩野外露头照片

a.野外露头照片；b.晶洞照片

Fig. 3. The field occurrence photos of Boketu miarolitic granite

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图 4 博克图晶洞花岗岩的岩相学照片

Q.石英；Kf.钾长石；Pl.斜长石；Bi.黑云母；Ms.白云母，Chl.绿泥石

Fig. 4. Petrographic photos of Boketu miarolitic granite

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图 5 锆石颗粒的阴极发光图像

Fig. 5. Cathodoluminescence images of zircon grains

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图 6 博克图花岗岩锆石SHRIMP U-Pb年龄谐和图

Fig. 6. SHRIMP U-Pb concordia diagram of zircon from Boketu miarolitic granite

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图 7 博克图花岗岩的K₂O-SiO₂图(a)和SiO₂-(Na₂O+K₂O-CaO)图(b)

A.碱性系列，AC.碱钙性系列，CA.钙碱性系列，A.钙质系列

Fig. 7. K₂O vs. SiO₂ diagram (a) and SiO₂ vs. (Na₂O+K₂O-CaO) diagram (b) of Boketu miarolitic granite

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图 8 博克图花岗岩的微量元素蛛网图(a)和稀土元素配分图(b)

标准化值据Sun and McDonough(1989)

Fig. 8. Primitive mantle-normalized spider diagram(a) and chondrite-normalized REE pattern(b) of Boketu miarolitic granite

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图 9 10 000×Ga/Al-(Zr+Nb+Y+Ce)图解

据Eby(1990)

Fig. 9. 10 000×Ga/Al-(Zr+Nb+Y+Ce) diagram of Boketu miarolitic granite

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图 10 高分异的Ⅰ型花岗岩、A型花岗岩判别图解

底图据Collins et al.(1982)

Fig. 10. High differentiation (high fractional) Ⅰ-type granite and A-type granite discrimination diagrams

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图 11 岩体SiO₂-P₂O₅图解(a)和Y-Rb图解(b)

据Chappell and White(2001)

Fig. 11. SiO₂-P₂O₅ diagram (a) and Y-Rb diagram (b) of Boketu miarolitic granite

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图 12 博克图晶洞花岗岩的锆石ε_Hf(t)-t图解

Fig. 12. The zircon ε_Hf(t)-t diagram of Boketu miarolitic granite

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图 13 岩石样品Nb-Y判别图解(a)、Rb-(Yb+Ta)判别图解(b)、Ta-Yb判别图解(c)和A/CNK-A/NK图解(d)

图a、b、c据Pearce et al.(1984)；图d据Maniar and Piccoli(1989).WPG.班内花岗岩，VAG.火山弧花岗岩，ORG.洋中脊花岗岩，syn-COLG.同碰撞花岗岩，IAGIAG.岛弧花岗岩类；CAG.大陆弧花岗岩类；CCG.大陆碰撞花岗岩类；POG.后造山花岗岩类；RRG.与裂谷有关的花岗岩类；OP.大洋斜长花岗岩；CEUG.与大陆的造陆抬升有关的花岗岩类

Fig. 13. Nb-Y diagram (a), Rb-(Yb+Ta) diagram (b), Ta-Yb diagram (c) and A/CNK-A/NK diagram(d) of granite samples

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表 1 博克图晶洞花岗岩SHRIMP锆石U-Pb年龄

Table 1. The SHRIMP zircon U-Pb ages of Boketu miarolitic granite

点号	含量(10^-6)			Th/U	同位素比值						年龄(Ma)
点号	U	Th	²⁰⁶Pb	Th/U	²⁰⁶Pb/²³⁸U	±%	²⁰⁷Pb^*/²³⁵U	±%	²⁰⁷Pb/²⁰⁶Pb	±%	²⁰⁶Pb/²³⁸U	²⁰⁷Pb/²³⁵U	²⁰⁷Pb/²⁰⁶Pb
BKT3-1	263	138	5.23	0.54	0.022 60	2.7	0.161 0	6.0	0.051 6	5.4	144.1±3.9	147.4±3.9	-947±950
BKT3-2	250	144	4.77	0.60	0.022 21	2.5	0.137 3	6.5	0.046 6	5.7	141.6±3.5	141.3±3.9	28±140
BKT3-3	148	96	2.67	0.67	0.020 32	4.1	0.119 0	10	0.055 8	7.0	129.7±5.3	131.4±5.6	-1 020±1 900
BKT3-4	699	446	12.9	0.66	0.021 40	2.2	0.152 3	4.6	0.051 5	4.1	136.5±3.0	137.4±3.3	-5±210
BKT3-5	590	404	11.5	0.71	0.022 77	2.3	0.152 6	4.9	0.053 7	3.9	145.1±3.4	144.3±3.8	359±88
BKT3-6	620	386	11.5	0.64	0.021 27	2.4	0.199 6	3.5	0.052 5	3.6	135.7±3.2	140.3±3.5	-462±680
BKT3-7	115	79	2.20	0.71	0.021 30	3.7	0.149 0	12	0.065 4	8.1	135.9±5.0	139.6±5.4	-1 450±1 800
BKT3-8	545	323	10.3	0.61	0.021 91	2.1	0.145 8	4.7	0.050 4	4.0	139.7±2.9	139.4±3.3	212±93
BKT3-9	646	655	12.1	1.05	0.021 78	2.0	0.145 3	4.3	0.050 6	3.6	138.9±2.8	138.5±3.4	225±83
BKT3-10	422	330	8.57	0.81	0.023 66	2.2	0.195 3	4.5	0.053 9	4.3	150.8±3.3	151.8±3.8	368±97
BKT3-11	554	337	10.60	0.63	0.021 97	2.4	0.174 2	4.4	0.054 3	3.9	140.1±3.3	142.6±3.7	-234±240
BKT3-12	345	168	6.62	0.50	0.022 33	2.3	0.146 4	6.0	0.054 5	4.8	142.3±3.3	141.2±3.6	390±110
BKT3-13	804	475	15.70	0.61	0.022 61	2.2	0.162 9	3.8	0.050 4	3.3	144.1±3.1	145.4±3.4	-52±190

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表 2 Hf同位素分析结果

Table 2. Hf isotopic analysis results of Boketu miarolitic granite

样品	¹⁷⁶Yb/¹⁷⁷Hf	2σ	¹⁷⁶Lu/¹⁷⁷Hf	2σ	¹⁷⁶Hf/¹⁷⁷Hf	2σ	ε_Hf(0)	ε_Hf(t)	f_(Lu/Hf)	T_DM1(Ma)	T_DM2(Ma)
BKT3-1	0.047 76	0.000 98	0.001 35	0.000 018	0.282 88	0.000 028	3.8	6.87	-0.96	534.09	1 013.46
BKT3-2	0.047 73	0.000 35	0.001 39	0.000 003	0.282 85	0.000 025	2.8	5.76	-0.96	575.28	1 110.83
BKT3-3	0.044 42	0.000 34	0.001 28	0.000 004	0.282 81	0.000 021	1.3	4.09	-0.96	632.68	1 254.96
BKT3-4	0.055 90	0.000 07	0.001 59	0.000 006	0.282 73	0.000 028	-1.6	1.27	-0.95	755.74	1 513.20
BKT3-5	0.071 01	0.001 78	0.001 96	0.000 042	0.282 75	0.000 031	-0.9	2.08	-0.94	734.64	1 444.60
BKT3-6	0.062 65	0.000 59	0.001 96	0.000 008	0.282 82	0.000 022	1.7	4.51	-0.94	629.08	1 220.43
BKT3-7	0.055 08	0.000 29	0.001 64	0.000 019	0.282 82	0.000 024	1.6	4.49	-0.95	627.18	1 223.48
BKT3-8	0.041 42	0.000 42	0.001 25	0.000 019	0.282 83	0.000 021	2.0	4.92	-0.96	605.04	1 184.99
BKT3-9	0.047 54	0.000 38	0.001 40	0.000 001	0.282 80	0.000 026	1.0	3.95	-0.96	645.13	1 271.74
BKT3-10	0.055 34	0.000 71	0.001 60	0.000 015	0.282 83	0.000 024	2.0	5.15	-0.95	608.4	1 170.60
注：T_DM1为单阶段模式年龄；T_DM2为两阶段模式年龄；f_(Lu/Hf)为分馏因子，Hf同位素数据具体处理参考Wu et al.(2006).

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