大兴安岭中段早三叠世O型埃达克岩的发现及其大地构造意义

李世超; 张凌宇; 李鹏川; 施璐; 郑常青

doi:10.3799/dqkx.2017.136

大兴安岭中段早三叠世O型埃达克岩的发现及其大地构造意义

doi: 10.3799/dqkx.2017.136

1.
吉林大学地球科学学院, 吉林长春 130061
2.
沈阳地质矿产研究所, 辽宁沈阳 110034

基金项目:

国家自然科学基金项目 41272223

国家自然科学基金项目 41602209

国家自然科学基金项目 41472164

科技部“973”项目 2013CB429802

国家自然科学基金项目 41340024

详细信息

作者简介:
李世超(1980-), 男, 博士, 副教授, 主要从事构造地质学教学与研究工作

通讯作者:
郑常青

中图分类号: P541;P588.14
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出版历程
- 收稿日期: 2017-03-18
- 刊出日期: 2017-12-15

Discovery and Tectonic Implications of Early Triassic O-Type Adakite in Middle of Great Xing'an Range

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Shenyang Institute of Geology and Mineral Resources, Shenyang 110034, China

摘要

摘要: 为了研究大兴安岭中段地区早三叠世的构造背景问题，以下三叠统哈达陶勒盖组火山岩为研究对象，通过野外观测和X射线荧光光谱分析法、等离子质谱法分别对样品的主量、微量元素进行了测试.结果显示哈达陶勒盖组火山岩是一套中酸性钙碱系列岩石组合，具有高Sr、低Yb与Y和高Sr/Y的特点，为钠质（O型）埃达克岩.结合区域资料认为，古亚洲洋于早三叠世时期闭合的碰撞应力使贺根山-嫩江-黑河构造带活化，推动构造带内年轻地壳由南向北俯冲，进而推动古生代残留洋壳向更深的地幔插入，在此过程中加热并熔融、喷出地表形成哈达陶勒盖组埃达克岩，并在山间盆地沉积了湖相碎屑堆积-老龙头组.
- 早三叠世 /
- O型埃达克岩 /
- 哈达陶勒盖组 /
- 大兴安岭中段 /
- 地球动力学 /
- 岩石学
Abstract: In order to study the tectonic setting of the Early Triassic of the middle of the Greater Xing'an Range, the volcanic rocks of Lower Triassic Hadataolegai Formation was studied by field observation. Respectively, the main elements and trace elements were analyzed by XRF and ICP-MS. The results show that the volcanic rocks are a series of calcareous series rocks with high Sr, low Yb, Y and high Sr/Y ratios, showing geochemical features of O-type adakites are related to subduction of oceanic slab. we suggests Paleo-Asian Ocean collision along the line of Silumulon River-Changchun-Yanji which activated Hegenshan-Nenjiang-Heihe structural belt in Early Triassic. The collision pushed the young crust to subduct northward along Hegenshan-Nenjiang-Heihe line. The residual Paleozoic oceanic crust are advanced to the deeper mantle melting and then the Hadataolegai Formation adakites were formed. At the same time, the Laolongtou Formation that is lacustrine clastic sediments was deposited in the intermountain basin.
- Early Triassic /
- O-type adakite /
- Hadataolegai Formation /
- middle of Greater Xing'an Range /
- geodynamics /
- petrology

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图 1 大兴安岭中段下三叠统地层分布图

Fig. 1. Distribution map of Lower Triassic stratain in the middle of the Greater Xing'an Mountains

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图 2 哈达陶勒盖组火山岩的显微照片

a.单偏光；b.正交偏光；Pl.斜长石；Bi.黑云母；Aug.普通辉石；Am.角闪石

Fig. 2. Micrograph of volcanic rock from Hadataolegai Formation

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图 3 大兴安岭中段地区早三叠世哈达陶勒盖组火山岩Nb/Y-Zr/Ti图解

底图据Pearce(1996)

Fig. 3. Nb/Y-Zr/Ti Diagram of volcanic rock from Hadataolegai Formation in Early Triassic in the middle of the Greater Xing'an Mountains

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图 4 大兴安岭中段地区哈达陶勒盖组图解

a.AFM图解；b.Th-Hf/3-Ta图解；c.Th-Hf/3-Nb/16图解；d.Th-Zr/117-Nb/16图解；AFM图解据Irvine and Baragar(1971)；b、c、d图解据Wood(1980)；WPA.板内碱性玄武岩；WPT.板内拉斑玄武岩；IAT.岛弧拉斑玄武岩；E-MORB.富集型洋中脊玄武岩；N-MORB.正常洋中脊玄武岩；IAB.岛弧玄武岩；CAB.钙碱性玄武岩

Fig. 4. Diagrams of rock from Hadataolegai Formation in the middle of the Greater Xing'an Mountains

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图 5 大兴安岭中段地区哈达陶勒盖组火山岩Harker图解

空心数据引用自内蒙古自治区第二区域地质调查队

Fig. 5. Harker Diagram of volcanic rock from Hadataolegai Formation in the middle of the Greater Xing'an Mountains

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图 6 大兴安岭中段地区哈达陶勒盖组火山岩图解

a.稀土元素配分模式图，球粒陨石标准化值据Boynton(1984)；b.微量元素蛛网图，原始地幔标准化值据Sun and McDonough(1989)

Fig. 6. REE partition pattern graphs

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图 7 大兴安岭中段哈达陶勒盖组火山岩图解

a.Yb_N-(La/Yb)_N判别图解，底图据Drummond(1990)；b.Y-Sr/Y判别图解，底图据Defant et al.(2002)；c.Yb-Sr/Yb判别图解，底图据张旗(2008)

Fig. 7. Yb_N-(La/Yb)_N discrimination diagrams

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图 8 大兴安岭中段哈达陶勒盖组火山岩的两类埃达克岩的成分对比图

a.SiO₂-MgO成分图解(Wang et al., 2007)；b.SiO₂-Mg^#成分图解(Sheppard et al., 2001)

Fig. 8. Components comparison picture of two kinds of adakites of volcanic rock of volcanic rock in Hadataolegai Fomation in the middle of the Greater Xing'an Mountains

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图 9 研究区晚二叠世-早三叠沉积地层分布图

Fig. 9. Distribution map of sedimentary strata in Late Permian-Early Triassic in the study area

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图 10 林甸-扎兰屯大地电磁测深(MT)二维反演

据张兴洲，内部资料

Fig. 10. 2D inversion on tellaric electromagnetic sounding (MT) at Lindain-Zhalantun

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图 11 晚二叠世及三叠纪构造演化模式图

P₃z.哲斯组；P₃l.林西组；T₁l.老龙头组；T₁hd.哈达陶勒盖

Fig. 11. Triassic tectonic evolution model in the study area

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表 1 哈达陶勒盖组的地球化学分析结果(单位：10^-6)

Table 1. Geochemical data of Hadataolegai Formation volcanic rocks

样号	B1096-1	B1101-1	B1102-1	B2018-2	B2068-1	B2073-5	B3079-1	B6002-2
岩性	气孔杏仁状安山岩	玄武安山岩	玄武安山岩	绿帘石化英安岩	安山岩	辉石安山岩	辉石安山岩	角闪辉石安山岩
SiO₂	60.20	63.10	62.90	64.50	63.0	58.60	56.15	59.90
Al₂O₃	17.00	16.10	15.75	16.60	15.90	16.20	18.00	15.70
Fe₂O₃	5.20	2.75	3.04	3.74	3.76	4.54	6.34	3.50
FeO	1.30	1.95	2.05	0.65	1.15	1.65	0.34	2.04
CaO	1.46	3.95	2.67	2.70	3.22	5.42	3.52	3.79
MgO	2.52	2.13	2.04	0.76	2.46	3.60	3.64	2.84
K₂O	1.78	3.24	4.22	2.93	4.40	2.94	2.38	3.98
Na₂O	6.91	3.96	4.22	5.32	3.35	4.29	6.19	4.98
TiO₂	1.05	0.78	0.76	0.56	0.66	0.83	0.98	0.86
P₂O₅	0.34	0.28	0.28	0.22	0.21	0.29	0.39	0.33
MnO	0.08	0.065	0.076	0.089	0.062	0.100	0.085	0.082
LOI	1.82	1.24	1.46	1.69	1.32	1.14	1.72	1.42
Cu	89.80	24.10	25.60	9.08	67.20	59.30	15.00	42.70
Pb	18.3	16.2	17.4	14.9	23.3	19.8	11.2	26.4
Zn	84.6	75.0	73.7	78.8	66.7	74.6	59.0	67.8
Cr	128.0	61.5	63.9	14.5	49.9	112.0	75.6	92.8
Rb	13.6	61.9	90.5	51.6	91.1	42.7	16.2	48.2
Mo	0.57	0.70	1.29	0.17	0.39	0.42	0.15	0.64
Sr	459	875	1 000	684	916	1 410	1 960	604
Ba	619	1 020	1 260	1 620	946	1 010	1 240	1 460
Nb	4.66	6.51	6.28	6.64	7.19	4.36	2.62	7.90
Ta	0.40	0.43	0.45	0.40	0.49	0.36	0.18	0.56
Zr	168	214	209	238	283	159	112	310
Hf	4.48	5.46	5.41	6.16	7.79	4.32	3.26	8.61
U	1.40	1.37	1.39	1.39	3.74	1.92	0.30	3.84
Th	2.55	4.96	4.80	4.43	16.10	7.10	4.08	14.00
La	25.6	31.9	33.5	26.2	40.2	34.1	38.0	44.6
Ce	60.9	61.3	62.3	55.4	83.3	72.8	71.2	82.4
Pr	7.48	7.61	7.76	6.86	10.10	8.93	12.00	12.80
Nd	30.6	29.5	29.5	27.3	38.0	35.9	50.4	51.0
Sm	5.59	5.06	4.87	4.98	6.22	6.11	8.52	8.63
Eu	1.59	1.49	1.54	1.79	1.46	1.77	2.52	2.20
Gd	4.41	3.96	4.02	4.21	4.73	4.71	5.64	6.08
Tb	0.58	0.54	0.54	0.65	0.68	0.64	0.70	0.82
Dy	2.93	2.32	2.39	3.51	3.04	2.68	2.66	3.62
Ho	0.54	0.44	0.42	0.68	0.57	0.48	0.42	0.64
Er	1.50	1.13	1.09	1.92	1.60	1.38	1.11	1.82
Tm	0.20	0.16	0.15	0.30	0.24	0.19	0.14	0.26
Yb	1.30	0.92	0.99	2.07	1.56	1.18	0.88	1.69
Lu	0.20	0.15	0.16	0.34	0.23	0.19	0.13	0.26
Y	13.6	11.4	11.6	18.4	16.0	12.9	11.4	17.2
Mg^#	54.68	50.31	62.49	61.39	64.83	43.15	52.58	55.77
σ	4.39	2.58	3.58	3.17	3.00	3.35	5.59	4.75
A/CNK	1.07	0.94	0.96	0.99	0.99	0.81	0.94	0.81
∑REE	157.02	157.88	160.83	154.61	207.93	183.96	205.72	234.02
δEu	1.20	0.82	0.98	0.93	1.01	1.06	1.02	1.11

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表 2 哈达陶勒盖组火山岩与埃达克岩特征比较

Table 2. Comparison table of characteristics of adakites and volcanic rock from Hadataolegai Formation

	埃达克岩特征(值)	哈达陶勒盖组火山岩
岩石组合	安山岩、英安岩、流纹岩	安山岩、英安岩、流纹岩
矿物组合	斜长石+角闪石+黑云母+辉石	斜长石+角闪石+黑云母+辉石
SiO₂含量(10^-2)	≥56.00	61.04
Al₂O₃含量(10^-2)	≥15.00	16.41
MgO含量(10^-2)	＜3.00(很少超过6.00)	2.50
Mg^#	≈50.00	45.08(剔除一件绿帘石化样品后47.91)
Na₂O与K₂O关系	Na₂O＞K₂O	Na₂O＞K₂O
Na₂O含量(10^-2)	4.0±	4.9
K₂O含量(10^-2)	1.00~2.00±	3.23
Sr含量(10^-6)	＞400.0	988.5
Yb含量(10^-6)	≤1.90	1.32
Y含量(10^-6)	≤18.00	14.06
Sr/Y	＞20.00~40.00	75.94
La/Yb	＞20.00	28.14
Zr/Sm	＞50.00	35.46
高场强元素	Nb、Ta、Zr、Hf、Ti、P亏损	Nb、Ta、Zr、Ti、P亏损，Hf无数据
Eu异常	无异常	1.016
Sr异常	正异常	正异常
注：特征(值)由Gill(1981)、Drummond(1990)和Defant and Drummond(1990).

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