内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定

杜继宇; 陶楠; 郭建超; 江斌; 杜贯新

doi:10.3799/dqkx.2019.215

内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定

doi: 10.3799/dqkx.2019.215

杜继宇^1,2,,
陶楠^2, ,,
郭建超²,
江斌²,
杜贯新²

1.
吉林大学地球科学学院, 吉林长春 130061
2.
中国地质调查局沈阳地质调查中心, 辽宁沈阳 110034

基金项目:

中国地质调查局项目 DD20160048-02

中国地质调查局项目 DD20190039

中国地质调查局项目 DD20160048-01

中国地质调查局项目 DD20190042

中国地质调查局项目 DD20190039-06

中国地质调查局项目 DD20190360

中国地质调查局项目 12120115031101

详细信息

作者简介:
杜继宇(1988—), 男, 在职博士研究生, 工程师, 主要从事大兴安岭地区构造地质及岩石地球化学研究

通讯作者:
陶楠(1982—), 男, 高级工程师

中图分类号: P597
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出版历程
- 收稿日期: 2019-08-28
- 刊出日期: 2019-11-11

Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean

Du Jiyu^{1,2
,},
Tao Nan^{2
, ,},
Guo Jianchao²,
Jiang Bin²,
Du Guanxin²

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Shenyang Center of Geological Surey, China Geological Survey, Shenyang 110034, China

摘要

摘要: 古亚洲洋闭合时限一直存在争议.对巴林右旗巴彦查干岩体进行了地球化学、锆石U-Pb测年和Lu-Hf同位素研究，确定其时代和成因，探讨区域构造背景.巴彦查干岩体岩性为二云母二长花岗岩.测年显示，花岗岩侵位于232.0~241.7 Ma，为中晚三叠世.花岗岩富硅和铝，贫镁和铁，属强过铝系列（A/CNK=1.10~1.25），富集轻稀土和大离子亲石元素，亏损重稀土和Nb、Ta等高场强元素，具S型花岗岩特征.锆石的ε_Hf（t）值为-1.8~+4.01，二阶段模式年龄（t_DM2）在1 006~1 380 Ma之间.上述研究表明，原始岩浆起源于加厚陆壳的部分熔融.结合内蒙古东南部蛇绿混杂岩、晚古生代岩浆岩带和沉积环境、三叠纪碰撞相关花岗岩带等研究，推测古亚洲洋东段的闭合发生在晚二叠世；三叠纪进入陆陆碰撞阶段.
- 巴林右旗 /
- 中晚三叠世 /
- S型花岗岩 /
- 年代学 /
- 地球化学 /
- 古亚洲洋
Abstract: It is a highly controversial topic about the closure of the Paleo-Asian Ocean. Based on the geochemistry, zircon U-Pb dating and Lu-Hf isotope studies of Bayanchagan pluton in Balinyouqi, in this paper, it discusses its formation age, petrogenesis and the regional tectonic setting. Bayanchagan pluton is two-mica monzogranites. LA-ICP-MS zircon U-Pb dating indicates the two-mica monzogranite formed in the Middle-Late Triassic(232.0-241.7 Ma). The two-mica monzogranite is high in SiO₂, Al₂O₃ and low in MgO, Fe₂O₃, belonging to strongly peraluminous series(A/CNK=1.10-1.25), enriched in light rare earth elements and large ion lithophile elements, and depleted in heavy rare earth elements and high field strength elements(Nb, Ta), showing that it is S-type granite. Hf isotopic analysis results show ε_Hf(t) values of -1.8 to +4.01, two-stage model ages ranging from 1 006 Ma to 1 380 Ma, respectively, indicating that the primary magma was derived from the partial melting of a thickened crust. Combined with the studies of the ophiolitic melange, magmatic belt and sedimentary environment of Late Paleozoic, collision related granites, and so on, it is suggested that the eastern segment of the Paleo-Asian Ocean closed in the Late Permian-Early Triassic, and was at the period of continental collision during Triassic.
- Balinyouqi area /
- Middle-Late Triassic /
- S-type granite /
- geochronology /
- geochemistry /
- Paleo-Asian Ocean

HTML全文

图 1 研究区地质简图

Ⅰ.额尔古纳地块；Ⅱ.兴安地块；Ⅲ.松嫩地块；Ⅳ.佳木斯地块；Ⅴ.完达山地体；Ⅵ.华北北缘增生带；Ⅶ.华北板块；F1.蒙古-鄂霍茨克构造带；F2.塔源-喜贵图构造带；F3.贺根山-黑河构造带；F4.嫩江-八里罕构造带；F5.西拉木伦-长春构造带；F6.赤峰-开原断裂；F7.伊通-依兰断裂；F8.敦化-密山断裂；F9.牡丹江断裂.图b据Wu et al.(2011)修改

Fig. 1. Geological sketch map of the studied area

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图 2 巴彦查干二云母二长花岗岩的野外宏观（a）及镜下显微（b）照片

Qtz.石英；Pl.斜长石；Af.碱性长石；Bit.黑云母；Mus.白云母

Fig. 2. Photomicrographs of the two-mica monzogranites from Bayanchagan

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图 3 巴彦查干二云母二长花岗岩（D3172-1和1013-1）锆石阴极发光图像

红色及黄色圆圈分别表示了LA-ICP-MS U-Pb及Hf同位素测试点位置

Fig. 3. CL images of zircons for the two-mica monzogranites(D3172-1 and 1013-1)from Bayanchagan

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图 4 巴彦查干二云母二长花岗岩（D3172-1和1013-1）锆石U-Pb谐和图

Fig. 4. Zircon U-Pb concordia diagrams for the two-mica monzogranites(D3172-1 and 1013-1)from Bayanchagan

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图 5 巴彦查干三叠纪二云母二长花岗岩的锆石ε_Hf(t)-t图解

据Yang et al.(2006)

Fig. 5. Zircon Hf isotopic features for the Triassic two-mica monzogranites from Bayanchagan

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图 6 巴彦查干二云母二长花岗岩SiO₂-K₂O (a)和A/CNK-A/NK(b)图解

图a据Peccerillo and Taylor(1976)；图b据Maniar and Piccoli(1989)

Fig. 6. Plot of SiO₂ vs. K₂O (a) and A/CNK vs. A/NK (b) for the two-mica monzogranites from Bayanchagan

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图 7 巴彦查干二云母二长花岗岩的球粒陨石标准化稀土元素配分图（a）和原始地幔标准化微量元素蛛网图（b）

图a标准化值据文献Boynton(1984)；图b标准化值据Sun and McDonough(1989)

Fig. 7. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagrams (b) for the two-mica monzogranites from Bayanchagan

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图 8 巴彦查干二云母二长花岗岩成因类型判别图

据文献Whalen et al.(1987)

Fig. 8. Genetic type discrimination for the two-mica monzogranites from Bayanchagan

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图 9 巴彦查干二云母二长花岗岩源岩判别图解

A.泥质岩部分熔融；B.杂砂岩部分熔融；C.基性岩源岩部分熔融.据文献Altherr et al.(2000)

Fig. 9. Source rock discrimination diagram for the two-mica monzogranites from Bayanchagan

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图 10 巴彦查干二云母二长花岗岩Harker图解

Fig. 10. Harker diagrams for the two-mica monzogranites from Bayanchagan

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图 11 巴彦查干二云母二长花岗岩La-La/Sm图解

据文献Wang et al.(2011)

Fig. 11. La-La/Sm diagram for the two-mica monzogranites from Bayanchagan

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图 12 巴彦查干二云母二长花岗岩的R₁-R₂构造判别图解

R₁=4Si-11(Na+K)-2(Fe+Ti)；R₂=6Ca+2Mg+Al.①地幔斜长花岗岩；②破坏性活动陆缘（板块碰撞前）花岗岩；③板块碰撞后隆起期花岗岩；④晚造山期花岗岩；⑤非造山区A型花岗岩了；⑥同碰撞（S型）花岗岩；⑦造山期后A型花岗岩.据文献Batchelor (1985)

Fig. 12. R₁-R₂ tectonic discrimination diagram for the two-mica monzogranites from Bayanchagan

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图 13 西拉木伦缝合带蛇绿混杂岩及三叠纪花岗岩时空分布特征

据沈阳地质调查中心(2019)《大兴安岭地区区域地质调查片区总结与服务产品开发》项目成果图件修改.图中上标a表示中国地质大学(武汉)（2008）1:25万锡林浩特幅区域地质调查报告; 上标b表示中国地质大学(武汉)(2008)1:25万林西县幅区域地质调查报告; 上标c表示内蒙古自治区第十地质矿产勘查开发院(1997)1:5万双井幅地质图

Fig. 13. Spatio-temporal distribution features of ophiolitic melange and Triassic granites in Xar Moron suture

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表 1 巴林右旗巴彦查干二云母二长花岗岩主量、稀土元素、微量元素分析结果及特征参数

Table 1. Representative major and trace element data of two-mica monzogranites(D3172-1)from Bayanchagan in Balinyouqi

样品编号	D3172-1	D3172-2	D3172-3	DB18-1-1	DB18-1-4	1013-1
SiO₂	71.20	71.70	72.00	73.17	74.15	74.44
TiO₂	0.165	0.140	0.140	0.247	0.120	0.093
Al₂O₃	15.746	15.695	15.393	14.238	13.794	13.401
Fe₂O₃	0.771	0.672	0.796	1.572	0.922	0.675
FeO	0.490	0.580	0.450	0.476	0.373	0.810
MnO	0.012	0.014	0.015	0.050	0.054	0.025
MgO	0.372	0.333	0.311	0.172	0.062	0.333
CaO	1.008	0.915	0.800	0.329	0.494	0.422
Na₂O	3.435	3.619	3.611	3.950	3.145	2.927
K₂O	5.290	5.401	5.219	3.998	5.950	5.983
P₂O₅	0.115	0.097	0.103	0.078	0.013	0.068
LOI	0.914	0.794	0.905	1.263	0.966	0.625
Total	99.52	99.96	99.74	99.54	100.04	99.80
Na₂O+K₂O	8.725	9.020	8.830	7.948	9.095	8.910
K₂O/Na₂O	1.540	1.492	1.445	1.012	1.892	2.044
A/CNK	1.19	1.17	1.18	1.25	1.10	1.11
A/NK	1.38	1.33	1.33	1.32	1.19	1.19
Rb	122.62	119.23	118.63	126.21	171.93	184.72
Ba	1 700.00	1 700.00	1 700.00	709.56	509.85	390.00
Th	12.593	9.900	12.115	23.415	36.098	11.782
U	2.502	1.884	1.925	1.547	6.624	6.001
Ta	0.623	0.600	0.468	3.240	1.291	1.123
Nb	1.59	1.54	1.17	11.45	6.39	7.27
Sr	348.48	335.01	310.33	155.04	191.04	142.28
Zr	136.53	130.87	130.83	158.92	104.83	102.44
Hf	2.584	2.192	2.228	5.283	4.405	3.397
Y	5.864	4.898	5.018	9.844	10.348	7.108
Ni	2.182	1.691	1.362	1.730	3.750	1.515
Cr	8.710	6.890	6.790	10.380	8.280	6.845
Ga	17.05	17.30	16.60	20.44	17.35	17.66
La	41.560	34.574	39.532	31.644	23.743	14.110
Ce	74.770	61.225	70.689	58.710	42.145	31.540
Pr	7.732	6.473	7.504	6.406	5.370	3.825
Nd	25.17	20.88	23.69	21.65	19.55	14.92
Sm	3.191	2.846	2.945	3.639	4.130	3.587
Eu	2.300	2.114	2.129	0.599	0.498	0.502
Gd	3.310	2.757	3.114	2.893	2.995	2.500
Tb	0.264	0.254	0.265	0.459	0.462	0.384
Dy	1.039	0.890	0.965	2.011	1.948	1.344
Ho	0.176	0.148	0.145	0.314	0.313	0.286
Er	0.478	0.462	0.476	0.809	0.828	0.620
Tm	0.074	0.061	0.060	0.113	0.123	0.210
Yb	0.416	0.414	0.381	0.759	0.829	0.718
Lu	0.064	0.053	0.050	0.101	0.110	0.125
(La/Yb)_N	71.65	59.90	74.43	29.91	20.54	14.10
δEu	2.16	2.31	2.15	0.56	0.43	0.51
∑REE	160.55	133.15	151.95	130.11	103.04	74.67
LREE/HREE	26.58	25.42	26.85	16.44	12.54	11.07
10 000Ga/Al	2.05	2.08	2.04	2.71	2.38	2.49
Rb/Nd	4.87	5.71	5.01	5.83	8.79	12.38
Rb/Sr	0.35	0.36	0.38	0.81	0.90	1.30
C/MF	0.70	0.66	0.60	0.19	0.48	0.27
A/MF	6.01	6.22	6.30	4.57	7.40	4.70
La/Sm	13.02	12.15	13.42	8.70	5.75	3.93
锆石饱和温度	784	780	780	797	761	748
注：主量元素质量分数单位为%；稀土元素和微量元素质量分数单位为10^-6；锆石饱和温度单位为℃.

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表 2 西拉木伦缝合带蛇绿混杂岩化石及同位素统计

Table 2. Fossil and geochronologic data in Xar Moron suture

序号	位置	化石类型	同位素				资料来源
序号	位置	化石类型	岩性	方法	年龄（Ma）	年代	资料来源
1	柯单山	薄壳型介形虫				奥陶纪	邵济安等，2017
2	柯单山		超基性岩	Sm-Nd	665±46	新元古代	陈森煌等，1991
3	柯单山		辉长岩	U-Pb	281.1±6.4	早二叠世	叶栩松等，2011
4	柯单山		辉长岩	U-Pb	276	早二叠世	a
5	五道石门	有孔虫				志留纪-现代	邵济安等，2017
6	五道石门	小腕足类				寒武-奥陶纪	邵济安等，2017
7	杏树洼	放射虫				中二叠世	王玉净和樊志勇，1997
8	杏树洼		辉长岩	U-Pb	273.9±1.3	早二叠世	殷东方，2018
9	九井子		辉长岩	U-Pb	274.7±1.7	早二叠世	刘建峰等，2016
10	二八地	牙形石				奥陶-志留纪	邵济安等，2017
注：a为中国地质大学（武汉）（2008）1:25万林西县幅区域地质调查报告.

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表 3 西拉木伦缝合带三叠纪花岗岩同位素年龄统计

Table 3. Geochronologic data of Triassic granites in Xar Moron suture

序号	岩体名称	岩石类型	年龄（Ma）	资料来源
1	双井子	二云母花岗岩	229.2±4.1	李锦轶等，2007
2	双井子	二云母二长花岗岩	237.5±2.7	李锦轶等，2007
3	转山子	花岗岩	245.6±0.9	刘建峰等，2014
4	转山子	花岗岩	246±2	Wu et al.，2011
5	建设屯	花岗闪长岩	249±2	刘建峰等，2013
6	龙头山	花岗岩	241±3	刘伟等，2007
7	龙头山	花岗岩	226.2±3.9	Liu et al.，2005
8	新林	花岗闪长岩	241±2	Wu et al.，2011
9	锡林浩特水库南	花岗岩	233±12	a
10	白音锡勒牧场	二长花岗岩	246.4±4.7	b
11	兰家营子	花岗闪长岩	242.1±6.4	a
12	吴营子	正长花岗岩	249	b
13	巴彦查干	二云母二长花岗岩	241.7±0.58	本次
14	巴彦查干	二云母二长花岗岩	232.0±1.9	本次
注：a表示中国地质大学（武汉）（2008）1:25万锡林浩特市幅区域地质调查报告；b表示内蒙古自治区第十地质矿产勘查开发院（1997）1:5万双井幅地质图.

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