东昆中构造混杂岩带清泉沟弧前玄武岩地质、地球化学特征及构造环境

李瑞保; 裴先治; 李佐臣; 裴磊; 陈国超; 李小兵; 陈有炘; 刘成军; 魏博

doi:10.3799/dqkx.2018.540

东昆中构造混杂岩带清泉沟弧前玄武岩地质、地球化学特征及构造环境

doi: 10.3799/dqkx.2018.540

李瑞保^1,2,,
裴先治^1,2, ,,
李佐臣^1,2,
裴磊¹,
陈国超¹,
李小兵¹,
陈有炘¹,
刘成军¹,
魏博¹

1.
长安大学地球科学与资源学院, 陕西西安 710054
2.
长安大学西部矿产资源与地质工程教育部重点实验室, 自然资源部岩浆作用成矿与找矿重点实验室, 陕西西安 710054

基金项目:

青海省国土资源厅-中国铝业公司公益性区域地质矿产调查基金项目 200801

中央高校基本科研业务费专项资金项目 310827161006

国家自然科学基金项目 41502191

国家自然科学基金项目 41472191

中央高校基本科研业务费专项资金项目 310827173702

中央高校基本科研业务费专项资金项目 2013G1271092

中央高校基本科研业务费专项资金项目 2013G1271091

中央高校基本科研业务费专项资金项目 310827161002

国家自然科学基金项目 41172186

中央高校基本科研业务费专项资金项目 CHD2011TD020

详细信息

作者简介:
李瑞保(1982-), 男, 副教授, 博士, 主要从事构造地质学和区域地质学研究

通讯作者:
裴先治

中图分类号: P548
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出版历程
- 收稿日期: 2018-02-10
- 刊出日期: 2018-12-15

Geochemistry and Tectonic Setting of Qingquangou Forearc Basalts in Central Tectonic Mélange of East Kunlun Orogen

1.
School of Earth Science and Resources, Chang'an University, Xi'an 710054, China
2.
Key Laboratory of Western Mineral Resources and Geological Engineering, Ministry of Education, Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Natural Resources, Chang'an University, Xi'an 710054, China

摘要

摘要: 东昆中构造混杂岩带东段清泉沟玄武岩岩石源区及构造环境研究具有重要意义.通过对清泉沟玄武岩进行详细的地质、地球化学和构造环境研究，结果表明，该套玄武岩属于亚碱性拉斑玄武岩系列，球粒陨石标准化稀土元素配分图呈现轻稀土元素弱亏损-弱富集的特征，与正常大洋中脊玄武岩（NMORB）和西太平洋IBM弧前玄武岩（FAB）配分特征相似.岩石成因研究表明其源区具亏损地幔特征，且地幔熔融程度比NMORB源区熔融程度较高.构造环境研究表明该套玄武岩形成于大洋初始俯冲阶段的弧前环境.综合区域地质资料，认为东昆中古洋盆至少于中寒武世（510 Ma）之前开始向北俯冲，在俯冲初期形成了清泉沟弧前玄武岩，构成了俯冲带初始弧壳或不成熟洋内岛弧.
- 东昆仑 /
- 蛇绿岩 /
- 清泉沟 /
- 弧前玄武岩 /
- 地球化学
Abstract: The research on magmatic source and tectonic setting of Qingquangou basalts in eastern section of East Kunlun is important for discussion of the tectonic evolution of East Kunlun ocean. This paper presents a systematic field geology, geochemistry, and tectonic setting research. The results show that the SiO₂ contents of Qingquangou basalts range from 48.60% to 49.28%, MgO contents range from 7.72%-8.00%, TiO₂ contents range from 1.07%-1.10% (average values, 1.09%), which are similar to the values of Izu-Bonin-Mariana forearc basalt, West Pacific. The basalts are classified into the tholeiitic basalt of subalkaline series based on the major elements feature. Qingquangou basalts are characterized by the ∑LREEs range from 22.64×10^-6-33.31×10^-6, ∑HREEs range from 13.13×10^-6-18.37×10^-6, ∑REEs range from 36.02×10^-6-51.68×10^-6, and (La/Yb)_N range from 0.88-1.10. The chondrite normalized REE patterns show the widely enriched-depleted feature of LREE, resembling the feature of NMORB basalts and IBM forearc basalts, West Pacific. Moreover, the samples have low ratios of Ti/Y (312) and Ti/V (< 20), also indicative of the forearc basalt feature. The primitive mantle normalized trace element spider diagram shows enriched LILEs and undifferentiated HFSEs (e.g., Nb, Ta, Zr, Hf, etc.) features. Petrogenesis research shows that its source was derived from the depleted mantle, and further proves that its partial melting degree is higher than that of NMORB-type basalts. Additionally, the tectonic discrimination diagram suggests that the basalts formed in forearc tectonic setting. Combined with the previous data, it is concluded that East Kunlun ocean began to subduct northward at Middle Cambrian (ca.510 Ma), and that Qingquangou forearc basalts were generated meanwhile, forming the nascent island arc crust.
- East Kunlun /
- ophiolite /
- Qingquangou /
- forearc basalt /
- geochemistry

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图 1 东昆仑造山带及邻区构造简图(a)和研究区及邻区地质简图(b)

Fig. 1. Simplified tectonic map of East Kunlun orogen and neighboring area (a) and geological map of studying area and neighboring area (b)

下载: 全尺寸图片幻灯片

图 2 清泉沟玄武岩实测地质剖面

1.石英岩；2.黑云石英片岩；3.黑云斜长片麻岩；4.花岗质片麻岩；5.变安山岩；6.变玄武岩；7.长英质糜棱岩；8.印支期花岗岩；9.断裂构造

Fig. 2. Measured geological section of Qingquangou basalts

下载: 全尺寸图片幻灯片

图 3 清泉沟玄武岩及其围岩野外及镜下特征

a.花岗质片麻岩；b.花岗质片麻岩与纳赤台岩群黑云石英片岩呈断层接触；c，d.强片理化变玄武岩；e.变玄武岩镜下特征(单偏光)；f.变玄武岩镜下特征(正交偏光)；Hb.角闪石

Fig. 3. Field photos and micrograph features of Qingquangou basalts and wall rocks

下载: 全尺寸图片幻灯片

图 4 清泉沟玄武岩岩石类型判别图解

Fig. 4. Discrimination diagrams of rock types of Qingquangou basalts

下载: 全尺寸图片幻灯片

图 5 清泉沟玄武岩稀土元素球粒陨石标准化配分图解

球粒陨石数据据Boynton(1984)；IBM弧前玄武岩数据据Falloon et al.(2014)

Fig. 5. Chondrite-normalized REE patterns of Qingquangou basalts

下载: 全尺寸图片幻灯片

图 6 清泉沟玄武岩微量元素NMORB标准化蛛网图解

原始地幔标准化数据据Sun and McDonough(1989)

Fig. 6. NMORB-normalized spidergram of Qingquangou basalts

下载: 全尺寸图片幻灯片

图 7 清泉沟玄武岩Ti/Y-Zr/Y图解(a)和Ti-V图解(b)

a.据Meschede(1986); b.据Shervais(1982)

Fig. 7. Ti/Y-Zr/Y (a) and Ti-V (b) diagrams of Qingquangou basalts

下载: 全尺寸图片幻灯片

图 8 清泉沟玄武岩Nb/Yb-Th/Yb图解(a)和La/Yb-Yb图解(b)

MORB，OIB数据据Baker et al.(1997); Pearce(2008); El-Rahman et al.(2009)

Fig. 8. Nb/Yb-Th/Yb (a) and La/Yb-Yb (b) diagrams of Qingquangou basalts

下载: 全尺寸图片幻灯片

图 9 清泉沟弧前玄武岩形成模式

Fig. 9. Formation mechanism of Qingquangou forearc basalts (FABs)

下载: 全尺寸图片幻灯片

表 1 清泉沟玄武岩主量元素(%)和微量元素(10^-6)分析结果

Table 1. Results of major elements(%) and trace elements (10^-6) from Qingquangou basalts

样品	XRD380-1	XRD380-2	XRD380-3	XRD380-4	XRD380-6	XRD380-7	XRD380-8
SiO₂	48.78	49.05	49.23	49.28	48.94	48.60	48.94
TiO₂	1.10	1.08	1.07	1.07	1.09	1.10	1.09
Al₂O₃	14.14	13.97	13.69	13.85	13.57	13.97	13.86
Fe₂O₃^T	13.45	12.80	12.83	12.77	13.01	12.23	12.31
MnO	0.20	0.18	0.19	0.19	0.20	0.19	0.21
MgO	7.65	7.75	7.63	7.62	7.81	8.00	7.92
CaO	10.67	11.16	11.10	11.35	11.42	11.40	11.14
Na₂O	2.30	2.24	2.46	2.05	2.34	2.32	2.56
K₂O	0.26	0.14	0.12	0.16	0.23	0.17	0.15
P₂O₅	0.08	0.09	0.08	0.09	0.09	0.09	0.08
LOI	0.69	1.07	0.82	0.84	0.69	0.90	0.68
Total	99.32	99.53	99.22	99.27	99.39	98.97	98.94
La	2.86	4.78	2.95	3.16	3.13	3.74	3.26
Ce	8.04	11.83	8.03	9.45	8.59	9.26	8.32
Pr	1.24	1.95	1.27	1.33	1.31	1.56	1.41
Nd	7.34	10.53	7.23	7.55	7.60	7.82	7.21
Sm	2.34	3.26	2.30	2.42	2.43	2.48	2.38
Eu	0.88	0.97	0.85	0.91	0.89	0.90	0.84
Gd	3.14	4.18	3.12	3.20	3.20	3.15	2.99
Tb	0.56	0.75	0.55	0.56	0.56	0.56	0.54
Dy	3.72	5.10	3.69	3.74	3.74	3.79	3.70
Ho	0.80	1.11	0.80	0.81	0.82	0.80	0.80
Er	2.38	3.34	2.36	2.37	2.39	2.26	2.32
Tm	0.35	0.50	0.34	0.35	0.35	0.36	0.37
Yb	2.03	2.92	1.95	1.99	2.00	2.38	2.49
Lu	0.33	0.47	0.33	0.33	0.33	0.37	0.37
∑REE	36.02	51.68	35.77	38.16	37.35	39.43	37.00
∑LREE	22.70	33.31	22.64	24.82	23.95	25.76	23.42
∑HREE	13.32	18.37	13.13	13.34	13.40	13.67	13.58
∑LREE/∑HREE	1.70	1.81	1.72	1.86	1.79	1.88	1.72
δEu	0.99	0.80	0.98	1.00	0.98	0.98	0.96
(La/Yb)_N	0.95	1.10	1.02	1.07	1.06	1.06	0.88
(La/Sm)_N	0.77	0.92	0.81	0.82	0.81	0.95	0.86
(Gd/Yb)_N	1.25	1.16	1.29	1.30	1.29	1.07	0.97
V	373.26	363.51	374.17	378.38	367.85	313.00	323.00
Cr	211.38	197.93	198.17	197.87	263.13	166.00	164.00
Co	47.58	52.37	46.12	47.23	47.88	50.80	47.60
Ni	106.75	91.93	100.33	101.50	96.89	90.20	97.80
Rb	19.43	13.72	6.30	5.86	7.94	13.70	6.50
Sr	192.84	213.65	218.43	213.00	228.93	159.00	155.00
Y	19.42	27.59	19.02	19.11	18.12	22.80	22.90
Zr	53.70	54.17	54.55	53.39	56.19	56.60	53.70
Nb	2.48	2.82	2.50	2.51	2.68	2.83	2.53
Cs	0.92	2.09	0.67	0.64	0.25	2.88	0.93
Ba	51.52	33.70	41.35	56.75	237.76	33.60	40.10
Hf	1.46	1.50	1.53	1.46	1.56	1.86	1.78
Ta	0.16	0.19	0.16	0.16	0.18	0.19	0.17
Pb	4.85	3.12	1.22	1.39	4.32	3.07	1.36
Th	0.31	1.18	0.30	0.40	0.29	0.41	0.34
U	0.17	0.13	0.16	0.13	0.15	0.12	0.16
Nb/U	14.64	21.89	15.17	19.53	17.53	23.58	15.81
Nb/Ta	15.18	15.08	15.31	15.49	15.25	14.89	14.88
Nb/La	0.87	0.59	0.85	0.79	0.86	0.76	0.78
Ti/Y	339.55	234.66	337.28	335.62	360.63	289.23	285.35
Nb/Yb	1.22	0.96	1.28	1.26	1.34	1.19	1.02
Ta/Yb	0.08	0.06	0.08	0.08	0.09	0.08	0.07
Zr/Y	2.76	1.96	2.87	2.79	3.10	2.48	2.34
注：Mg^#=Mg/(Fe+Mg).

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