内蒙古高尧乌拉白音高老组地质及年代学特征

董培培; 李英杰; 王根厚; 辛后田; 王金芳; 李红阳

doi:10.12090/j.issn.1006-6616.2021.27.01.014

内蒙古高尧乌拉白音高老组地质及年代学特征

1.
河北地质大学, 河北石家庄 050031

2.
中国地质大学地球科学与资源学院, 北京 100083

3.
天津地质矿产研究所, 天津 300170

基金项目:
国家自然科学基金项目(41502211, 41972061);中国地质调查局地质调查项目(1212011120711, 12120114064201, DD20190004, DD20160039, DD20160041)

详细信息

作者简介: 董培培(1985-), 女, 硕士, 讲师, 从事岩石学和地球化学研究。E-mail: 120650334@qq.com

通讯作者: 李英杰(1976-), 女, 博士, 教授, 主要从事岩浆岩与大地构造研究。E-mail: liyingjie820@126.com

中图分类号: P597

收稿日期: 2019-10-15

修回日期: 2020-03-25

刊出日期: 2021-02-28

Geological and chronological characteristics of the Baiyin'gaolao Formation in Gaoyaowula, Inner Mongolia

1.
Heibei GEO University, Shijiazhuang 050031, Hebei, China

2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

3.
Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

More Information

Corresponding author: LI Yingjie, liyingjie820@126.com

Received Date: 15 October 2019

Revised Date: 25 March 2020

Publish Date: 28 February 2021

摘要

摘要:
通过1：50000区域地质调查，运用"火山构造-岩性岩相-火山地层"三重填图方法，将内蒙古东乌旗高尧乌拉白音高老组划分为3个岩性段，一段为火山碎屑沉积岩，二段为中性火山岩，三段为酸性火山岩，构成一个完整的沉积-喷发旋回。早期至晚期岩浆具有由中性向酸性演化的特征。划分出爆发相、侵出相、溢流相、火山通道相、喷发-沉积相及潜火山相等火山岩相；圈出12个Ⅴ级火山机构。获得高尧乌拉白音高老组二段粗安岩和三段流纹岩的LA-ICP-MS锆石U-Pb年龄分别为128.2±0.9 Ma和125.5±0.5 Ma，表明其形成时代为早白垩世。
- 白音高老组 /
- 火山作用 /
- LA-ICP-MS锆石U-Pb定年 /
- 高尧乌拉 /
- 内蒙古
Abstract:
Based on a regional geological survey at a scale of 1:50000, it reveals that the volcanic rocks from the Baiyin'gaolao Formation of Gaoyaowula in Inner Mongolia could be divided into three lithologic segments by the triple mapping method of "volcanic structure-lithology and lithofacies-volcanic formation". The first lithologic segment is composed of pyroclastic sedimentary rocks, the second intermediate volcanic rocks and the third acidic volcanic rocks. The three lithologic segments constitute a complete depositonal-eruptive cycle, and the early to late magma is characterized by a transition from neutral to acid. The Baiyin'gaolao Formation can be classified into eruptive facies, intrusive facies, overflow facies, volcanic vent facies, eruption-deposition facies and subvolcanic facies, etc. Twelve V-grade volcanic apparatuses are delineated. The Zircon U-Pb LA-ICP-MS dating of the trachyandesite from the second lithologic segment of the Baiyin'gaolao Formation of Gaoyaowula and the rhyolite from the third are 128.2±0.9 Ma and 125.5±0.5 Ma respectively, indicating that the formation age is early-Cretaceous.
- Baiyin'gaolao Formation /
- volcanism /
- LA-ICP-MS zircon U-Pb dating /
- Gaoyaowula /
- Inner Mongolia

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图 1 研究区地质图

Figure 1.

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图 2 高尧乌拉白音高老组火山岩剖面图

Figure 2.

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图 3 高尧乌拉白音高老组火山岩野外及显微镜下照片

Figure 3.

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图 4 内蒙古东乌旗高尧乌拉白音高老组二段粗安岩和三段流纹岩锆石阴极发光代表图像

Figure 4.

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图 5 锆石U-Pb年龄谐和图和直方图

Figure 5.

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图 6 高尧乌拉白音高老组火山岩TAS分类图

Figure 6.

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图 7 高尧乌拉白音高老组火山岩SiO₂-K₂O分类图解

Figure 7.

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图 8 高尧乌拉白音高老组火山岩A/CNK-A/NK图

Figure 8.

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图 9 高尧乌拉白音高老组火山岩稀土元素及微量元素特征

Figure 9.

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图 10 高尧乌拉白音高老组流纹岩构造环境判别图解

Figure 10.

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图 11 A₁和A₂型花岗岩类三角形判别图解(Eby，1992)

Figure 11.

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表 1 内蒙古高尧乌拉白音高老组火山岩实测剖面地层层序及韵律划分

Table 1. Stratigraphic sequence and rhythm classification of the measured section of the volcanic rocks from the Baiyin'gaolao Formation, Gaoyaowula

岩石地层单位		层号	岩性	分层厚度/m	组段厚度/m	形成方式	韵律划分
组	段	层号	岩性	分层厚度/m	组段厚度/m	形成方式	韵律划分
白音高老组	三段	17	紫色流纹质火山角砾岩	26.3	157.7	火山通道相	⑥
		16	灰紫色条带状球粒流纹岩	21.5		溢流相
		15	黑色黑曜岩	20.8		溢流相
		14	灰紫色条带状球粒流纹岩	18.6		溢流相
		13	灰紫色流纹岩	17.2		溢流相
		12	灰紫色流纹质晶屑凝灰岩	11.6		空落堆积相
		11	灰紫色流纹岩	21.7		溢流相	⑤
		10	紫红色流纹质晶屑凝灰岩	10.3		空落堆积相	⑤
		9	凝灰质砾岩	9.7		喷发-沉积相	④
	二段	8	灰紫色安山质火山角砾岩	23.6	207	火山通道相	③
		7	浅灰色含角砾粗安岩	57.4		溢流相
		6	浅灰色安山质含角砾熔结凝灰岩	14.3		碎屑流堆积相
		5	浅灰色安山质岩屑晶屑凝灰岩	32.9		空落堆积相
		4	灰紫色粗安岩	52.1		溢流相	②
		3	浅灰色安山质晶屑凝灰岩	26.7		空落堆积相	②
	一段	2	灰绿色凝灰质砂岩	11.9	30.1	火山沉积相	①
	一段	1	浅灰色凝灰质砾岩	18.2	30.1	火山沉积相	①
玛尼吐组		0	安山岩			溢流相

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表 2 高尧乌拉白音高老组二段粗安岩和三段流纹岩LA-ICP-MS锆石U-Pb同位素分析结果

Table 2. LA-ICP-MS zircon U-Pb isotopic analysis of the trachyandesites and rhyolites from the Baiyin'gaolao Formation, Gaoyaowula

点号	元素含量/×10^-6		Th/U	²⁰⁶Pb/²³⁸U		²⁰⁷Pb/²³⁵U		²⁰⁷Pb/²⁰⁶Pb		²⁰⁸Pb/²³²Th		²⁰⁶Pb/²³⁸U		²⁰⁷Pb/²³⁵U
点号	Th	U	Th/U	比值	1σ	比值	1σ	比值	1σ	比值	1σ	年龄/Ma	±1σ	年龄/Ma	±1σ
粗安岩(TW9846)
1	117	438	0.27	0.0200	0.0002	0.1339	0.0056	0.0486	0.0019	0.0080	0.0004	127	1	128	5
2	168	677	0.25	0.0201	0.0002	0.1354	0.0049	0.0489	0.0018	0.0094	0.0003	128	1	129	5
3	143	522	0.27	0.0197	0.0002	0.1472	0.0051	0.0542	0.0018	0.0070	0.0002	126	1	139	5
4	78	337	0.23	0.0197	0.0002	0.1288	0.0072	0.0473	0.0026	0.0088	0.0003	126	1	123	7
5	91	446	0.21	0.0200	0.0002	0.1436	0.0052	0.0521	0.0019	0.0080	0.0003	128	1	136	5
6	204	769	0.27	0.0201	0.0002	0.1382	0.0040	0.0498	0.0014	0.0077	0.0002	128	1	131	4
7	130	529	0.25	0.0199	0.0002	0.1472	0.0056	0.0535	0.0019	0.0075	0.0003	127	1	139	5
8	155	545	0.29	0.0199	0.0002	0.1279	0.0053	0.0466	0.0019	0.0078	0.0003	127	1	122	5
9	144	576	0.25	0.0202	0.0002	0.1471	0.0052	0.0528	0.0018	0.0088	0.0003	129	1	139	5
10	119	495	0.24	0.0206	0.0002	0.1528	0.0072	0.0539	0.0024	0.0100	0.0004	131	1	144	7
11	270	864	0.31	0.0200	0.0002	0.1395	0.0035	0.0505	0.0012	0.0081	0.0002	128	1	133	3
12	142	613	0.23	0.0206	0.0002	0.1561	0.0053	0.0549	0.0018	0.0098	0.0003	132	1	147	5
13	147	520	0.28	0.0203	0.0002	0.1361	0.0053	0.0486	0.0018	0.0078	0.0002	130	1	130	5
14	93	386	0.24	0.0204	0.0002	0.1461	0.0070	0.0520	0.0024	0.0090	0.0004	130	1	138	7
15	218	699	0.31	0.0203	0.0002	0.1432	0.0078	0.0512	0.0024	0.0085	0.0004	129	1	136	7
16	139	487	0.29	0.0205	0.0002	0.1521	0.0056	0.0539	0.0019	0.0090	0.0003	131	1	144	5
17	261	808	0.32	0.0202	0.0002	0.1465	0.0039	0.0525	0.0013	0.0082	0.0003	129	1	139	4
18	122	416	0.29	0.0210	0.0002	0.1517	0.0070	0.0524	0.0024	0.0095	0.0003	134	2	143	7
19	135	418	0.32	0.0198	0.0002	0.1329	0.0067	0.0487	0.0024	0.0074	0.0002	126	1	127	6
20	146	578	0.25	0.0198	0.0002	0.1350	0.0053	0.0495	0.0019	0.0072	0.0002	126	1	129	5
21	163	452	0.36	0.0197	0.0002	0.1389	0.0061	0.0512	0.0022	0.0065	0.0002	125	1	132	6
流纹岩(TW9850)
1	281	646	0.43	0.0193	0.0002	0.1325	0.0045	0.0499	0.0016	0.0050	0.0001	123	1	126	4
2	99	343	0.29	0.0197	0.0002	0.1452	0.0098	0.0533	0.0034	0.0070	0.0003	126	1	138	9
3	162	422	0.38	0.0196	0.0002	0.1435	0.0054	0.0530	0.0019	0.0040	0.0002	125	1	136	5
4	141	422	0.33	0.0195	0.0002	0.1314	0.0071	0.0488	0.0026	0.0067	0.0003	125	1	125	7
5	182	508	0.36	0.0198	0.0002	0.1520	0.0055	0.0557	0.0020	0.0070	0.0003	126	1	144	5
6	203	646	0.31	0.0197	0.0002	0.1617	0.0051	0.0595	0.0018	0.0080	0.0003	126	1	152	5
7	140	564	0.25	0.0196	0.0002	0.1343	0.0054	0.0497	0.0019	0.0073	0.0003	125	1	128	5
8	137	500	0.27	0.0197	0.0002	0.1357	0.0052	0.0500	0.0019	0.0075	0.0003	126	1	129	5
9	100	461	0.22	0.0197	0.0002	0.1347	0.0061	0.0495	0.0022	0.0076	0.0004	126	1	128	6
10	193	750	0.26	0.0195	0.0002	0.1395	0.0038	0.0518	0.0014	0.0082	0.0003	125	1	133	4
11	112	450	0.25	0.0200	0.0002	0.1463	0.0065	0.0531	0.0024	0.0090	0.0004	128	1	139	6
12	219	776	0.28	0.0196	0.0002	0.1316	0.0041	0.0486	0.0015	0.0088	0.0004	125	1	126	4
13	193	679	0.28	0.0197	0.0002	0.1521	0.0042	0.0560	0.0015	0.0090	0.0004	126	1	144	4
14	142	585	0.24	0.0195	0.0002	0.1371	0.0044	0.0510	0.0016	0.0084	0.0003	125	1	130	4
15	242	854	0.28	0.0198	0.0002	0.1339	0.0035	0.0491	0.0012	0.0077	0.0002	126	1	128	3
16	192	598	0.32	0.0195	0.0002	0.1323	0.0047	0.0491	0.0017	0.0078	0.0002	125	1	126	5
17	208	675	0.31	0.0196	0.0002	0.1364	0.0040	0.0504	0.0015	0.0079	0.0003	125	1	130	4

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表 3 高尧乌拉白音高老组二段粗安岩和三段流纹岩主量元素(%)和微量元素(×10^-6)分析结果

Table 3. Major (wt%) and trace (×10^-6) element analysis results of the trachyandesites and rhyolites from the Baiyin'gaolao Formation, Gaoyaowula

主量及微量元素	XT109 粗安岩	XT109-2 粗安岩	XT4524 粗安岩	XT4525-2 粗安岩	XT4503-1 粗安岩	P35XT32 流纹岩	P34XT09 流纹岩	P43XT03 流纹岩	XT4404 流纹岩	P21XT17 流纹岩
SiO₂	57.45	59.02	62.40	64.11	63.89	76.02	76.60	76.37	77.87	76.51
TiO₂	1.63	1.54	0.80	0.55	0.48	0.06	0.06	0.05	0.06	0.06
Al₂O₃	24.32	22.86	17.31	15.80	16.61	12.59	12.71	12.40	11.55	12.43
Fe₂O₃	1.43	0.80	4.37	4.46	3.48	0.79	0.76	0.32	1.04	0.93
FeO	1.81	2.52	0.55	0.52	0.62	0.25	0.07	0.18	0.08	0.22
MnO	0.130	0.130	0.160	0.089	0.095	0.04	0.04	0.02	0.02	0.02
MgO	0.75	0.71	0.68	1.03	0.99	0.15	0.08	0.13	0.07	0.08
CaO	1.15	1.60	4.53	2.85	1.45	0.50	0.43	0.96	0.47	0.44
Na₂O	2.57	3.21	3.97	3.97	3.41	3.57	3.63	3.85	3.56	3.60
K₂O	5.35	4.51	3.50	4.47	5.41	4.75	4.81	4.61	4.46	4.60
P₂O₅	0.28	0.35	0.29	0.19	0.20	0.03	0.02	0.02	0.02	0.02
LOI	2.90	2.61	1.29	1.82	3.21	1.22	0.74	1.05	0.76	1.01
TOTAL	99.80	99.85	99.84	99.84	99.82	99.96	99.95	99.95	99.97	99.93
Na₂O+K₂O	7.92	7.72	7.47	8.44	8.82	8.32	8.44	8.46	8.02	8.20
Mg^#	30.67	28.66	21.94	29.58	32.43	22.33	16.68	32.29	10.31	12.55
La	31.9	39.3	18.4	21.1	20.7	25.21	31.53	20.41	29.87	36.63
Ce	34.1	29.9	27.1	30.6	26.1	45.68	57.33	36.71	51.33	62.91
Pr	58.6	57.1	53.5	54.3	57.2	5.99	7.71	5.28	6.82	9.48
Nd	9.07	8.90	6.77	7.10	6.06	22.14	28.63	20.36	25.77	35.90
Sm	7.72	7.88	5.14	5.09	4.34	3.82	5.50	4.07	4.87	6.85
Eu	1.49	1.65	1.39	1.38	1.27	0.28	0.36	0.27	0.44	0.41
Gd	6.27	6.77	4.37	4.35	3.88	3.04	4.39	3.48	4.26	5.34
Tb	1.03	1.14	0.69	0.71	0.65	0.47	0.74	0.60	0.73	0.85
Dy	6.03	6.82	3.6	3.97	3.57	2.50	4.10	3.34	4.17	4.42
Ho	1.14	1.30	0.70	0.77	0.72	0.49	0.81	0.66	0.86	0.83
Er	3.22	3.73	2.01	2.36	2.23	1.57	2.48	1.99	2.65	2.49
Tm	0.48	0.59	0.35	0.46	0.44	0.31	0.49	0.38	0.50	0.46
Yb	2.90	3.71	2.03	2.91	2.70	2.02	3.07	2.40	3.19	2.87
Lu	0.43	0.58	0.5	0.71	0.67	0.44	0.62	0.50	0.63	0.60
Y	31.9	39.3	18.4	21.1	20.7	14.21	23.55	18.61	27.19	23.49
Sc	16.7	18.2	13.0	9.9	5.5	2.80	2.62	2.15	2.72	2.14
Ni	9.10	10.4	3.08	2.03	2.35	1.99	0.30	0.91	0.41	1.52
Rb	78.0	79.8	96.1	146.0	187.0	160.66	151.57	139.15	155.83	132.60
Cr	12.5	19.1	25.8	19.3	7.2	2.83	1.23	2.84	3.27	4.30
Co	17.60	21.80	10.40	7.86	4.66	0.61	0.08	0.42	0.32	0.47
V	212.0	206.0	112.0	62.3	46.3	5.27	2.34	4.90	6.17	4.94
Zr	294	295	151	179	182	86.36	77.91	78.18	67.82	83.68
Hf	8.69	8.64	3.91	4.42	4.21	3.87	3.65	3.40	2.74	3.59
Ta	0.71	0.69	0.67	0.51	0.41	0.87	0.67	1.00	1.24	1.05
Sr	178	213	590	394	331	18.89	9.48	21.82	24.85	15.70
Ba	682	494	624	885	721	280.84	242.34	135.80	273	205.24
Nb	11.60	11.00	8.44	7.96	6.14	10.94	10.32	10.46	11.17	9.90
Cs	11.30	17.50	4.84	5.11	7.81	5.02	4.61	4.89	6.44	5.51
Ga	29.9	29.7	22.0	19.6	17.1	16.51	15.55	14.76	16.29	14.95
Pb	4.2	5.7	14.4	18.2	14.7	22.67	20.60	23.23	25.47	20.50
Th	8.87	8.41	7.35	8.61	6.96	11.69	9.95	13.16	15.00	12.87
U	2.17	2.35	1.92	2.19	2.78	4.58	3.16	3.00	3.28	3.06
∑REE	164.38	169.37	126.55	135.81	130.53	113.96	147.76	100.45	136.09	170.04
LREE/HREE	6.65	5.87	7.88	7.36	7.78	9.51	7.85	6.52	7.01	8.52
(La/Yb)_N	7.89	7.60	6.50	5.20	5.50	8.95	7.37	6.10	6.72	9.15
δEu	0.63	0.67	0.87	0.87	0.93	0.24	0.22	0.21	0.29	0.20

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内蒙古高尧乌拉白音高老组地质及年代学特征

1. 河北地质大学, 河北 石家庄 050031 2. 中国地质大学地球科学与资源学院, 北京 100083 3. 天津地质矿产研究所, 天津 300170

作者简介: 董培培(1985-), 女, 硕士, 讲师, 从事岩石学和地球化学研究。E-mail: 120650334@qq.com

通讯作者: 李英杰(1976-), 女, 博士, 教授, 主要从事岩浆岩与大地构造研究。E-mail: liyingjie820@126.com

Geological and chronological characteristics of the Baiyin'gaolao Formation in Gaoyaowula, Inner Mongolia

1. Heibei GEO University, Shijiazhuang 050031, Hebei, China 2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China 3. Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

Corresponding author: LI Yingjie, liyingjie820@126.com

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1.
河北地质大学, 河北石家庄 050031

2.
中国地质大学地球科学与资源学院, 北京 100083

3.
天津地质矿产研究所, 天津 300170

1.
Heibei GEO University, Shijiazhuang 050031, Hebei, China

2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

3.
Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China