豫西小秦岭地区晚古元古代地壳深熔作用及构造意义：岩石学和锆石U-Pb年代学证据

朱越; 周汉文; 李少林; 谢瑜; 丁振举; 李建威; 姚书振

doi:10.3799/dqkx.2015.067

豫西小秦岭地区晚古元古代地壳深熔作用及构造意义：岩石学和锆石U-Pb年代学证据

doi: 10.3799/dqkx.2015.067

朱越^1,,
周汉文^{1, 2, ,},
李少林¹,
谢瑜¹,
丁振举³,
李建威³,
姚书振³

1.
中国地质大学地球科学学院，湖北武汉 430074
2.
中国地质大学地质过程与矿产资源国家重点实验室，湖北武汉 430074
3.
中国地质大学资源学院，湖北武汉 430074

基金项目:

国家自然科学基金重大研究计划重点项目 90814004

国土资源部全国危机矿山项目 20089939

详细信息

作者简介:
朱越(1989-)，女，硕士在读，主要从事矿物学、岩石学及矿床学方向研究.E-mail：zycug207@126.com

通讯作者:
周汉文，E-mail：hwzhou@cug.edu.cn

中图分类号: P586
计量
- 文章访问数: 4081
- HTML全文浏览量: 607
- PDF下载量: 672
- 被引次数: 0
出版历程
- 收稿日期: 2014-09-30
- 刊出日期: 2015-05-15

Late Paleoproterozoic Crustal Anatexis and Its Tectonic Significance: Evidence from Petrology and Zircon U-Pb Ages of Migmatite from Xiaoqinling Area, West Henan

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 太华群出露于华北中部造山带南段，是研究华北克拉通南缘演化的关键地区，对其研究不仅有助于深入了解华北克拉通古、中元古代构造演化特征，对于华北克拉通东西陆块碰撞时间的厘定也具有重要意义.通过对豫西小秦岭地区太华群深熔作用形成的3类混合岩开展岩相学研究，发现深熔作用对岩石的改造是不均匀的，明显受到了原岩的物质成分、岩石的结构构等性质的制约.通过对岩浆锆石及深熔锆石进行LA-ICP-MS定年，确定小秦岭地区太华群混合岩原岩年龄为早古元古代，深熔作用发生时间约为1.8 Ga.研究区混合岩形成于华北克拉通东、西陆块碰撞后的伸展阶段，与区域同时期形成的大量基性岩墙群及A型花岗岩共同记录了华北克拉通在1.8 Ga前后发生的大规模伸展拉张事件.
- 太华群 /
- 混合岩 /
- 深熔作用 /
- 地质年代学 /
- 华北克拉通南缘 /
- 岩石学 /
- 构造地质学
Abstract: The Taihua Group, exposed in the southernmost terminal Trans-North China Orogen (TNCO), is important for deciphering the mysterious evolution processes of the southern margin of the North China Craton during Proterozoic, and determination of the collision time of the eastern and western blocks of the North China Craton. Petrological study on three kinds of migmatites formed by anatexis from the Taihua Group in Xiaoqinling area, West Henan, indicates that the transformation of migmatites caused by anatexis is uneven, which is obviously limited by the composition of protolith, structure of rocks and other properties. LA-ICP-MS U-Pb dating of the anatexis zircons shows that the protolith crystallized in the Paleoproterozoic and the anatexis occurred at about 1.8 Ga. The migmatites and contemporaneous mafic dike swarms and A-type granite in the study area were generated in a post-orogenic, extensional environment following continent-continent collision at 1.85 Ga between the eastern and western blocks of the North China Craton.
- Taihua Group /
- migmatite /
- anatexis /
- geochronology /
- southern margin of North China Craton /
- petrology /
- tectonics

HTML全文

图 1 华北克拉通古元古代构造单元简图(a)及豫西小秦岭地区地质简图(b)

图a据赵国春等(2002)；图b据毕诗健等(2011)资料

Fig. 1. The sketch of Paleoproterozoic tectonic units for the North China Craton (a); geological sketch of Xiaoqinling area, showing representative sample locations (b)

下载: 全尺寸图片幻灯片

图 2 小秦岭地区太华群混合岩野外特征

a.混合岩化的细粒石榴石黑云矽线片麻岩(圈中为分散出现矿物粒度增大的斑块和团块)；b.粗粒石榴石黑云矽线条带状混合岩；c.条带状混合岩及深熔结晶花岗岩；d.中见粘性褶皱混合岩；e.混合岩化斜长角闪岩；f.雾迷状混合岩

Fig. 2. Photographs of migmatites from the Taihua Group in Xiaoqinling area

下载: 全尺寸图片幻灯片

图 3 小秦岭地区太华群混合岩镜下显微照片

a.石榴子石的分解(-)；b.石榴子石内部矿物共生组合(+)；c.黑云母的分解及向白云母的转变(+)；d.毛发状矽线石(-)；e.球状微斜长石包体与蠕虫结构(+)；f.长石增生净边结构(+)；g.长石的冠状体结构(+)；h.角闪石的部分熔融(+)

Fig. 3. Microphotographs of migmatites from the Taihua Group in Xiaoqinling area

下载: 全尺寸图片幻灯片

图 4 小秦岭地区太华群混合岩中代表性锆石阴极发光照片

Fig. 4. Representative cathodoluminescence(CL) images of zircons from migmatite in the Taihua Group

下载: 全尺寸图片幻灯片

图 5 豫西小秦岭地区太华群混合岩中锆石LA-ICP-MS U-Pb谐和图

Fig. 5. LA-ICP-MS zircon U-Pb concordia data of migmatite from the Taihua Group in Xiaoqinling area

下载: 全尺寸图片幻灯片

表 1 小秦岭太华群混合岩锆石LA-ICP-MS U-Pb测试结果

Table 1. LA-ICP-MS zircon U-Pb isotope data for migmatite samples in the Taihua Group

分析点		含量(10^-6)			Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U
分析点		Pb	Th	U	Th/U	比值	1σ	比值	1σ	比值	1σ	年龄(Ma)	1σ	年龄(Ma)	1σ	年龄(Ma)	1σ
	XQL2010-11
锆石核部	XQL2010-11-13	173.0	15.6	507.0	0.03	0.108 04	0.001 1	4.706 70	0.066 6	0.314 96	0.003 3	1 766	17	1 768	12	1 765	16
锆石核部	XQL2010-11-14	232.0	326.0	366.0	0.89	0.159 84	0.000 9	10.226 00	0.067 7	0.462 89	0.002 2	2 454	5	2 455	6	2 452	10
锆石边部及无核边锆石	XQL2010-11-01	298.0	14.7	843.0	0.02	0.108 90	0.001 7	4.785 69	0.094 9	0.317 95	0.004 0	1 781	28	1 782	17	1 780	20
	XQL2010-11-02	254.0	23.1	724.0	0.03	0.107 42	0.001 5	4.661 30	0.069 1	0.313 80	0.001 9	1 767	25	1 760	12	1 759	9
	XQL2010-11-03	260.0	13.6	735.0	0.02	0.108 80	0.001 2	4.787 96	0.062 4	0.318 24	0.002 7	1 789	19	1 783	11	1 781	13
	XQL2010-11-04	146.0	10.0	419.0	0.02	0.109 21	0.001 3	4.667 89	0.057 1	0.308 91	0.001 9	1 787	21	1 762	10	1 735	9
	XQL2010-11-05	31.1	88.8	156.0	0.57	0.069 19	0.002 5	1.504 09	0.050 6	0.157 78	0.001 4	906	74	932	21	944	8
	XQL2010-11-06	227.0	35.2	622.0	0.06	0.110 66	0.000 6	4.934 17	0.050 9	0.321 66	0.002 8	1 810	10	1 808	9	1 798	13
	XQL2010-11-07	202.0	19.4	583.0	0.03	0.108 53	0.000 6	4.667 72	0.037 1	0.310 50	0.001 9	1 776	11	1 761	7	1 743	10
	XQL2010-11-08	226.0	11.8	660.0	0.02	0.108 36	0.000 6	4.663 98	0.035 8	0.310 59	0.001 6	1 772	11	1 761	6	1 744	8
	XQL2010-11-09	177.0	12.1	542.0	0.02	0.107 87	0.001 5	4.422 88	0.056 3	0.296 37	0.001 9	1 765	26	1 717	11	1 673	10
	XQL2010-11-10	269.0	18.7	807.0	0.02	0.106 88	0.000 8	4.565 60	0.048 4	0.308 48	0.002 5	1 747	14	1 743	9	1 733	12
	XQL2010-11-11	142.0	13.0	405.0	0.03	0.109 20	0.001 1	4.856 42	0.060 6	0.321 24	0.002 1	1 787	19	1 795	11	1 796	10
	XQL2010-11-12	246.0	13.2	715.0	0.02	0.108 60	0.000 8	4.779 11	0.049 6	0.318 07	0.002 5	1 776	14	1 781	9	1 780	12
	XQL2010-11-15	34.5	44.0	55.6	0.79	0.158 87	0.002 2	10.194 25	0.158 4	0.465 15	0.005 2	2 444	23	2 453	14	2 462	23
	XQL2010-11-16	223.0	26.9	643.0	0.04	0.108 63	0.000 6	4.770 51	0.058 0	0.317 62	0.003 3	1 777	10	1 780	10	1 778	16
	XQL2010-11-17	250.0	24.4	709.0	0.03	0.108 69	0.000 6	4.774 41	0.037 5	0.317 49	0.001 6	1 777	10	1 780	7	1 777	8
	XQL2010-11-18	202.0	11.5	573.0	0.02	0.108 82	0.000 8	4.810 08	0.047 2	0.319 53	0.002 7	1 780	14	1 787	8	1 787	13
	XQL2010-11-19	402.0	12.4	1 160.0	0.01	0.108 43	0.000 5	4.726 75	0.043 1	0.314 70	0.002 7	1 773	8	1 772	8	1 764	13
	XQL2010-11-20	233.0	12.1	654.0	0.02	0.109 57	0.000 6	4.850 75	0.036 5	0.319 55	0.002 1	1 792	9	1 794	6	1 788	10
	XQL2010-11-21	153.0	14.5	435.0	0.03	0.108 06	0.000 8	4.708 59	0.037 7	0.314 67	0.001 6	1 769	14	1 769	7	1 764	8
	XQL2010-11-22	311.0	21.3	895.0	0.02	0.108 12	0.000 9	4.689 46	0.052 1	0.313 19	0.002 7	1 769	15	1 765	9	1 756	13
	XQL2010-11-23	179.0	14.8	514.0	0.03	0.109 87	0.000 8	4.797 63	0.054 3	0.315 74	0.003 2	1 798	14	1 784	10	1 769	16
	XQL2010-11-24	152.0	13.1	444.0	0.03	0.109 13	0.000 8	4.655 63	0.041 5	0.308 43	0.001 5	1 785	13	1 759	7	1 733	7
	XQL2010-11-25	207.0	25.1	582.0	0.04	0.108 79	0.000 8	4.800 40	0.049 8	0.319 76	0.002 8	1 789	13	1 785	9	1 789	14
	XQL2010-11-26	64.4	181.0	321.0	0.56	0.070 39	0.001 0	1.591 23	0.026 0	0.163 52	0.001 4	939	29	967	10	976	8
	XQL2010-11-27	152.0	15.2	423.0	0.04	0.111 27	0.001 6	4.993 89	0.073 8	0.324 92	0.003 4	1 820	31	1 818	12	1 814	17
	XQL2010-11-28	166.0	11.4	481.0	0.02	0.110 14	0.001 5	4.761 98	0.068 5	0.312 40	0.002 1	1 802	24	1 778	12	1 753	10
	XQL2010-10
锆石核部	XQL2010-10-06	238.0	144.0	490.0	0.29	0.132 60	0.002 2	7.270 90	0.123 2	0.395 30	0.002 6	2 132	29	2 145	15	2 148	12
锆石核部	XQL2010-10-12	260.0	168.0	577.0	0.29	0.120 90	0.001 7	6.045 80	0.085 0	0.360 50	0.002 1	1 970	25	1 982	12	1 985	10
锆石幔部	XQL2010-10-02	351.0	87.6	909.0	0.1	0.113 80	0.001 6	5.294 80	0.078 2	0.335 60	0.001 9	1 861	26	1 868	13	1 865	9
	XQL2010-10-07	747.0	16.5	2 001.0	0.01	0.114 10	0.001 5	5.219 50	0.069 4	0.330 20	0.002 4	1 866	29	1 856	11	1 840	12
	XQL2010-10-08	617.0	24.9	1 638.0	0.02	0.113 30	0.001 5	5.202 30	0.067 8	0.331 40	0.002 4	1 854	22	1 853	11	1 845	11
	XQL2010-10-09	388.0	79.5	969.0	0.08	0.115 20	0.001 6	5.436 50	0.081 8	0.340 10	0.002 4	1 883	26	1 891	13	1 887	12
	XQL2010-10-10	284.0	105.0	730.0	0.14	0.115 40	0.001 9	5.441 90	0.119 9	0.338 20	0.004 4	1 887	30	1 891	19	1 878	21
	XQL2010-10-11	348.0	118.0	883.0	0.13	0.113 90	0.001 8	5.272 20	0.097 8	0.333 00	0.003 2	1 862	32	1 864	16	1 853	16
	XQL2010-10-15	380.0	104.0	991.0	0.11	0.112 70	0.001 6	5.044 60	0.073 7	0.322 90	0.002 2	1 843	26	1 827	12	1 804	11
	XQL2010-10-18	720.0	13.3	1 962.0	0.01	0.112 80	0.001 4	5.081 30	0.059 4	0.325 30	0.002 2	1 856	50	1 833	10	1 815	11
	XQL2010-10-19	974.0	18.6	2 604.0	0.01	0.113 50	0.001 3	5.225 50	0.058 8	0.332 30	0.001 8	1 857	20	1 857	10	1 849	9
锆石边部及无核边锆石	XQL2010-10-01	497.0	26.4	1 386.0	0.02	0.110 70	0.001 5	4.927 00	0.067 5	0.321 50	0.002 3	1 810	24	1 807	12	1 797	11
	XQL2010-10-03	273.0	19.0	757.0	0.03	0.109 50	0.001 5	4.856 80	0.067 8	0.320 20	0.002 0	1 791	26	1 795	12	1 791	10
	XQL2010-10-04	397.0	15.7	1 098.0	0.01	0.109 00	0.001 5	4.889 00	0.075 7	0.323 60	0.002 7	1 783	21	1 800	13	1 807	13
	XQL2010-10-05	404.0	82.1	1 092.0	0.08	0.110 30	0.001 8	4.944 50	0.077 2	0.323 70	0.002 4	1 806	30	1 810	13	1 808	12
	XQL2010-10-13	434.0	19.0	1 182.0	0.02	0.109 60	0.001 3	4.865 90	0.061 9	0.320 30	0.002 2	1 792	22	1 796	11	1 791	11
	XQL2010-10-14	239.0	16.3	652.0	0.03	0.109 10	0.001 4	4.865 30	0.065 5	0.321 80	0.002 3	1 784	24	1 796	11	1 798	11
	XQL2010-10-16	236.0	17.8	661.0	0.03	0.107 20	0.001 6	4.643 70	0.068 4	0.312 60	0.001 9	1 754	28	1 757	12	1 753	9
	XQL2010-10-17	273.0	18.3	747.0	0.02	0.108 60	0.001 4	4.857 80	0.068 5	0.322 90	0.002 7	1 776	24	1 795	12	1 804	13
	XQL2010-10-20	336.0	71.1	905.0	0.08	0.112 20	0.001 4	5.024 40	0.062 9	0.323 10	0.001 8	1 836	23	1 823	11	1 805	9
	XQL2010-5
锆石核部	XQL2010-5-01	110.0	71.1	189.0	0.38	0.173 63	0.001 7	11.345 41	0.119 3	0.473 02	0.003 7	2 594	16	2 552	10	2 497	16
	XQL2010-5-02	77.7	76.2	117.0	0.65	0.184 01	0.001 9	13.181 85	0.172 9	0.518 38	0.005 3	2 700	17	2 693	12	2 692	23
	XQL2010-5-06	309.0	357.0	476.0	0.75	0.172 41	0.001 3	11.530 44	0.092 0	0.483 04	0.002 2	2 581	12	2 567	7	2 541	10
	XQL2010-5-07	68.7	34.1	122.0	0.28	0.173 08	0.002 2	11.144 70	0.139 9	0.466 13	0.003 8	2 588	21	2 535	12	2 467	17
	XQL2010-5-10	254.0	412.0	399.0	1.03	0.162 62	0.002 4	9.863 97	0.145 0	0.437 87	0.002 8	2 483	25	2 422	14	2 341	13
	XQL2010-5-11	103.0	113.0	169.0	0.67	0.167 04	0.002 4	10.381 47	0.158 0	0.448 65	0.003 8	2 528	24	2 469	14	2 389	17
	XQL2010-5-16	65.7	24.9	115.6	0.22	0.173 92	0.003 3	11.221 13	0.230 6	0.467 00	0.007 0	2 596	31	2 542	19	2 470	31
	XQL2010-5-17	89.1	60.0	158.0	0.38	0.163 74	0.002 5	10.125 85	0.163 7	0.447 15	0.003 6	2 495	26	2 446	15	2 383	16
	XQL2010-5-20	88.5	124.0	141.0	0.88	0.164 40	0.002 5	10.200 74	0.161 1	0.449 14	0.003 6	2 502	26	2 453	15	2 391	16
	XQL2010-5-23	71.8	54.6	117.0	0.47	0.174 83	0.003 1	11.661 81	0.229 7	0.481 58	0.005 3	2 606	29	2 578	18	2 534	23
	XQL2010-5-24	61.0	75.1	102.0	0.74	0.160 08	0.003 0	9.919 28	0.191 2	0.447 89	0.004 2	2 457	32	2 427	18	2 386	19
	XQL2010-5-28	129.0	121.0	224.0	0.54	0.163 49	0.002 5	9.990 44	0.154 5	0.441 54	0.003 2	2 492	26	2 434	14	2 358	15
锆石幔部	XQL2010-5-03	1.9	0.0	5.2	0.01	0.141 02	0.006 4	6.332 50	0.297 0	0.338 43	0.009 8	2 240	79	2 023	41	1 879	47
	XQL2010-5-04	4.1	0.5	9.3	0.05	0.145 25	0.006 4	7.427 11	0.293 8	0.384 02	0.007 8	2 291	76	2 164	35	2 095	36
	XQL2010-5-09	13.6	4.4	28.1	0.16	0.125 08	0.004 6	6.701 03	0.292 6	0.391 79	0.012 3	2 031	66	2 073	39	2 131	57
	XQL2010-5-14	7.8	0.2	21.5	0.01	0.118 34	0.004 0	5.250 38	0.169 1	0.324 93	0.004 5	1 931	61	1 861	27	1 814	22
	XQL2010-5-15	2.2	0.0	5.8	0.00	0.123 22	0.007 6	5.537 05	0.350 3	0.332 67	0.009 7	2 003	104	1 906	54	1 851	47
	XQL2010-5-18	66.6	20.5	168.0	0.12	0.120 91	0.004 7	5.67872	0.253 8	0.339 22	0.005 1	1 969	70	1 928	39	1 883	24
	XQL2010-5-19	5.3	0.2	13.6	0.01	0.12480	0.004 8	5.823 34	0.206 3	0.344 45	0.005 2	2 028	64	1 950	31	1 908	25
	XQL2010-5-21	23.0	25.1	39.4	0.64	0.149 47	0.004 0	8.163 82	0.252 5	0.394 40	0.006 6	2 340	46	2 249	28	2 143	31
	XQL2010-5-25	2.1	0.1	5.4	0.01	0.139 12	0.007 7	6.789 02	0.417 9	0.351 42	0.008 3	2 216	96	2 084	55	1 941	40
锆石边部及无核边锆石	XQL2010-5-05	1.2	0.5	2.4	0.21	0.218 89	0.014 2	11.210 81	0.689 2	0.412 01	0.017 7	2 973	104	2 541	57	2 224	81
	XQL2010-5-08	399.0	81.3	1 087.0	0.07	0.114 29	0.001 5	5.219 24	0.072 7	0.329 87	0.002 8	1 869	25	1 856	12	1 838	14
	XQL2010-5-12	415.0	211.0	1 149.0	0.18	0.109 39	0.001 5	4.703 52	0.065 5	0.310 25	0.001 8	1 791	25	1 768	12	1 742	9
	XQL2010-5-13	223.0	145.0	585.0	0.25	0.109 04	0.001 9	4.845 90	0.090 8	0.320 59	0.003 1	1 784	31	1 793	16	1 793	15
	XQL2010-5-22	250.0	169.0	657.0	0.26	0.112 24	0.001 7	5.022 35	0.077 1	0.323 27	0.002 3	1 836	27	1 823	13	1 806	11
	XQL2010-5-26	151.0	60.1	419.0	0.14	0.110 52	0.001 6	4.820 81	0.073 0	0.315 10	0.002 1	1 809	27	1 789	13	1 766	10
	XQL2010-5-27	246.0	7.9	713.0	0.01	0.112 15	0.001 5	4.905 80	0.067 8	0.315 81	0.001 8	1 835	24	1 803	12	1 769	9

下载: 导出CSV

表 2 前人的太华群岩石的定年结果

Table 2. Ages of rocks from Taihua Group

序号	岩性	采样位置	分析方法	年龄值(Ma)	文献出处
1	斜长角闪岩	洛宁	角闪石Ar-Ar坪年龄	2 373±47	倪志耀等(2003)
2	斜长角闪岩	洛宁	角闪石Ar-Ar等时线	2 349±47	倪志耀等(2003)
3	斜长角闪岩	洛宁	锆石Pb-Pb蒸发法	2 675±2	倪志耀等(2003)
4	石墨矽线片麻岩	外方山	锆石U-Pb LA-ICP-MS	2 730~2 500； 2 310~2 250	赵太平等(2004)
5	斜长角闪片麻岩	洛宁	锆石U-Pb LA-ICP-MS	2 340~2 300	蒋宗胜等(2011)
6	斜长角闪片麻岩	华山	锆石U-Pb LA-ICP-MS	2 293±7	王国栋等(2012)
7	斜长角闪岩	小秦岭	全岩Sm-Nd等时线	3 542±57	周汉文等(1998b)
8	斜长角闪岩	熊耳山	锆石U-Pb LA-ICP-MS	2 500~2 300	Xu et al.(2009)
9	黑云母片麻岩	小秦岭	锆石U-Pb LA-ICP-MS	2 500~2 300	Xu et al.(2009)
10	石英闪长岩	小秦岭	锆石SHRIMP	2 765±13	Huang et al.(2010)
11	石英闪长岩	小秦岭	锆石SHRIMP	2 723±9	Huang et al.(2010)
12	花岗闪长质片麻岩	小秦岭	CAMECA	2 305±23	Huang et al.(2012)
13	花岗质片麻岩	小秦岭	CAMECA	2 477±28	Huang et al.(2013)
14	石英闪长岩	小秦岭	锆石SHRIMP	2 477±8	Huang et al.(2013)
15	石英闪长岩	小秦岭	锆石SHRIMP	2 552±4	Huang et al.(2013)
16	花岗质片麻岩	小秦岭	锆石U-Pb LA-ICP-MS	2 346±28	Yu et al.(2013)
17	斜长角闪岩	鲁山	锆石U-Pb LA-ICP-MS	2 763±13	林慈銮(2006)
18	石墨石榴石矽线片麻岩	鲁山	锆石U-Pb LA-ICP-MS	2 260~2 140	Wan et al.(2006b)
19	TTG质片麻岩	鲁山	锆石U-Pb LA-ICP-MS	2 316±16	第五春荣等(2007)
20	TTG质片麻岩	鲁山	锆石U-Pb LA-ICP-MS	2 336±13	第五春荣等(2007)
21	TTG质片麻岩	鲁山	锆石Hf模式年龄	2 815	第五春荣等(2007)

下载: 导出CSV

表 3 华北克拉通及其南缘晚古元古代变质年龄

Table 3. Paleoproterozoic ages of North China Craton

序号	岩性	采样位置	分析方法	年龄值(Ma)	文献出处
1	角闪岩	河南熊耳山	锆石LA-ICP-MS	~2 100	Xu et al.(2009)
2	石墨矽线片麻岩	河南鲁山	锆石SHRIMP	1 840±70	赵太平等(2004)
3	石墨石榴石矽线片麻岩	河南鲁山	锆石SHRIMP	1 840±70	Wan et al.(2006b)
4	石英闪长质片麻岩	河南鲁山	锆石SHRIMP	1 917±37	Huang et al.(2010)
5	黑云母片麻岩	陕西小秦岭	锆石LA-ICP-MS	~2 100	Xu et al.(2009)
6	黑云斜长片麻岩	陕西小秦岭	锆石LA-ICP-MS	1 913±13	时毓等(2011)
7	石英闪长岩	陕西小秦岭	锆石SHRIMP	1 912±12	Huang et al.(2013)
8	花岗质片麻岩	陕西小秦岭	CAMECA	1 918±17	Huang et al.(2013)
9	石榴石-硅线石-黑云母片麻岩	内蒙古千里山	锆石LA-ICP-MS	1 920±17	Yin et al.(2009)
10	含石墨硅线石-黑云母片麻岩	山西大同	锆石SHRIMP	1 861±19	Wan et al.(2006a)
11	黑云母片麻岩	河北太行山	锆石SHRIMP	1 817±26	Guan et al.(2002)
12	高压麻粒岩	山西省桑干	锆石SHRIMP	1 817±12	Guo et al.(2005)
13	片麻岩	吉林省通化	锆石LA-ICP-MS	1 754±13	Lu et al.(2006)
14	含透辉石片麻岩	吉林省通化	锆石LA-ICP-MS	1 827±20	Lu et al.(2006)
15	含石墨片麻岩	吉林省通化	锆石LA-ICP-MS	1 838±35	Lu et al.(2006)
16	角闪岩	吉林省通化	锆石LA-ICP-MS	1 847±8	Lu et al.(2006)
17	磁铁矿二长花岗片麻岩	吉林省通化	锆石SHRIMP	1 914±13	Li and Zhao(2007)

下载: 导出CSV

参考文献(80)

Bi, S.J., Li, J.W., Li, Z.K., 2011. Geological Significance and Geochronology of Paleoproterozoic Mafic Dykes ofXiaoqinling Gold District, Southern Margin of the North China Craton. Earth Science—Journal of China University of Geosciences, 36(1): 17-32 (in Chinese with English abstract). http://www.researchgate.net/publication/279897754_Geological_significance_and_geochronology_of_Paleoproterozoic_mafic_dykes_of_Xiaoqinling_Gold_District_southern_margin_of_the_North_China_craton
Brown, M., 1994. The Generation, Segregation, Ascent and Emplacement of Granite Magma: The Migmatite-to-Crustally-Derived-Granite Connection in Thickened Orogens. Earth-Science Reviews, 36(1-2): 83-130. doi: 10.1016/0012-8252(94)90009-4
Brown, M., 2001. Crustal Melting and Granite Magmatism: Key Issues. Physics and Chemistry of the Earth (Part A), 26(4-5): 201-212. doi: 10.1016/S1464-1895(01)00047-3
Brown, M., 2007. Crustal Melting and Melt Extraction, Ascent and Emplacement in Orogens: Mechanisms and Consequences. Journal of the Geological Society, 164: 709-730. doi: 10.1144/0016-76492006-171
Brown, M., Averkin, Y., McLellan, E., et al., 1995. Melt Segregation in Migmatites. Journal of Geophysical Research-Solid Earth, 100(B8): 15655-15679. doi: 10.1029/95jb00517
Brown, M., Dallmeyer, R.D., 1996. Rapid Variscan Exhumation and the Role of Magma in Core Complex Formation: Southern Brittany Metamorphic Belt, France. Journal of Metamorphic Geology, 14(3): 361-379. doi: 10.1111/j.1525-1314.1996.00361.x
Brown, M., Pressley, R.A., 1999. Crustal Melting in Nature: Prosecuting Source Processes. Physics and Chemistry of the Earth(A), 24(3): 305-316. doi: 10.1016/s1464-1895(99)00034-4
Cheng, Y.Q., Yang, C.H., Wan, Y.S., et al., 2004. Early Precambrian Geological Characters and Anatectic Reconstruction of Crust in North Part of Middle Taihua Mountain. Geological Publishing House, Beijing, 191 (in Chinese).
Diwu, C.R., Sun, Y., Lin, C.L., et al., 2007. Zircon U-Pb Ages and Hf Isotopes and Their Geological Significance of Yiyang TTG Gneisses from Henan Province, China. Acta Petrologica Sinica, 23(2): 253-262 (in Chinese with English abstract).
Foster, D.A., Schafer, C., Fanning, C.M., et al., 2001. Relationships between Crustal Partial Melting, Plutonism, Orogeny, and Exhumation: Idaho-Bitterroot Batholiths. Tectonophysics, 342(3-4): 313-350. doi: 10.1016/S0040-1951(01)00169-X
Guan, H., Sun, M., Wilde, S.A., et al., 2002. SHRIMP U-Pb Zircon Geochronology of the Fuping Complex: Implications for Formation and Assembly of the North China Craton. Precambrian Research, 113(1-2): 1-18. doi: 10.1016/s0301-9268(01)00197-8
Guo, J.H., Sun, M., Chen, F.K., et al., 2005. Sm-Nd and SHRIMP U-Pb Zircon Geochronology of High-Pressure Granulites in the Sanggan Area, North China Craton: Timing of Paleoproterozoic Continental Collision. Journal of Asian Earth Sciences, 24(5): 629-642. doi: 10.1016/j.jseaes.2004.01.017
Hollister, L.S., 1993. The Role of Melt in the Uplift and Exhumation of Orogenic Belts. Chemical Geology, 108(1-4): 31-48. doi: 10.1016/0009-2541(93)90316-b
Hou, G.T., Liu, Y.L., Li, J.H., 2006. Evidence for ~1.8 Ga Extension of the Eastern Block of the North China Craton from SHRIMP U-Pb Dating of Mafic Dyke Swarms in Shandong Province. Journal of Asian Earth Sciences, 27(4): 392-401. doi: 10.1016/j.jseaes.2005.05.001
Hu, G.H., Hu, J.L., Chen, W., et al., 2010. Geochemistry and Tectonic Setting of the 1.78 Ga Mafic Dyke Swarms in the Mt. Zhongtiao and Mt. Song Areas, the Southern Margin of the North China Craton. Acta Petrologica Sinica, 26(5): 1563-1576(in Chinese with English abstract).
Hu, Z.C., Gao, S., Liu, Y.S., et al., 2008. Signal Enhancement in Laser Ablation ICP-MS by Addition of Nitrogen in the Central Channel Gas. Journal of Analytical Atomic Spectrometry, 23(8): 1093-1101. doi: 10.1039/b804760j
Huang, X.L., Niu, Y.L., Xu, Y.G., et al., 2010. Geochemistry of TTG and TTG-Like Gneisses from Lushan-Taihua Complex in the Southern North China Craton: Implications for Late Archean Crustal Accretion. Precambrian Research, 182(1-2): 43-56. doi: 10.1016/j.precamres.2010.06.020
Huang, X.L., Wilde, S.A., Yang, Q.J., et al., 2012. Geochronology and Petrogenesis of Gray Gneisses from the Taihua Complex at Xiong'er in the Southern Segment of the Trans-North China Orogen: Implications for Tectonic Transformation in the Early Paleoproterozoic. Lithos, 134-135: 236-252. doi: 10.1016/j.lithos.2012.01.004
Huang, X.L., Wilde, S.A., Zhong, J.W., 2013. Episodic Crustal Growth in the Southern Segment of the Trans-North China Orogen across the Archean-Proterozoic Boundary. Precambrian Research, 233: 337-357. doi: 10.1016/j.precamres.2013.05.016
Jiang, Z.S., Wang, G.D., Xiao, L.L., et al., 2011. Paleoproterozoic Metamorphic P-T-t Path and Tectonic Significance of the Luoning Metamorphic Complex at the Southern Terminal of the Trans-North China Orogen, Henan Province. Acta Petrologica Sinica, 27(12): 3701-3717 (in Chinese with English abstract).
Keay, S., Lister, G., Buick, I., 2001. The Timing of Partial Melting, Barrovian Metamorphism and Granite Intrusion in the Naxos Metamorphic Core Complex, Cyclades, Aegean Sea, Greece. Tectonophysics, 342(3-4): 275-312. doi: 10.1016/s0040-1951(01)00168-8
Kusky, T.M., Li, J.H., 2003. Paleoproterozoic Tectonic Evolution of the North China Craton. Journal of Asian Earth Sciences, 22(4): 383-397. doi: 10.1016/s1367-9120(03)00071-3
Li, H.M., Chen, Y.C., Wang, D.H., et al., 2007. SHRIMP U-Pb Zircon Ages of Metamorphic Rocks and Veins in the Xiaoqinling Area, Henan, and Their Geological Significance. Acta Petrologica Sinica, 23(10): 2504-2512(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200710019.htm
Li, J.H., He, W.Y., Qian, X.L., 1997. Genetic Mechanism and Tectonic Setting of Proterozoic Mafic Dyke Swarm: Its Implication for Paleoplate Reconstruction. Geological Journal of China Universities, 3(3): 272-281(in Chinese with English abstract). http://www.researchgate.net/publication/284503781_Genetic_mechanism_and_tectonic_setting_of_Proterozoic_mafic_dyke_swarm_Its_implication_for_paleoplate_reconstruction
Li, J.H., Kusky, T.M., Huang, X.N., 2002. Archean Podiform Chromitites and Mantle Tectonites in Ophiolitic Mélange, North China Craton: A Record of Early Oceanic Mantle Processes. GSA Today, 12: 4-11. http://www.researchgate.net/publication/250949175_Archean_Podiform_Chromitites_and_Mantle_Tectonites_in_Ophiolitic_Mlange_North_China_Craton_A_Record_of_Early_Oceanic_Mantle_Processes
Li, J.H., Qian, X.L., Huang, X.N., et al., 2000. Tectonic Framework of North China Block and Its Cratonization in the Early Precambrian. Acta Petrologica Sinica, 16(1): 1-10 (in Chinese with English abstract).
Li, S.Z., Zhao, G.C., 2007. SHRIMP U-Pb Zircon Geochronology of the Liaoji Granitoids: Constraints on the Evolution of the Paleoproterozoic Jiao-Liao-Ji Belt in the Eastern Block of the North China Craton. Precambrian Research, 158(1-2): 1-16. doi: 10.1016/j.precamres.2007.04.001
Lin, B.Q., Tao, T.Y., 1989. Study of the Main Gold-Bearing Strata of Archean in Xiaoqinling Area, Henan and Shaanxi. In: Lin, B.Q., ed., The Regional Metallogenic Conditions of Gold Deposits in Xiaoqinling Area, China (No. 3). Geological Publishing House, Beijing (in Chinese).
Lin, C.L., 2006. Geochemistry, Geochronology and Tectonic Settings of Archean Gneisses in Lushan, Henan Province(Dissertation). Northwest University, Xi'an (in Chinese with English abstract).
Liu, D.Y., Wilde, S.A., Wan, Y.S., et al., 2009. Combined U-Pb, Hafnium and Oxygen Isotope Analysis of Zircons from Meta-Igneous Rocks in the Southern North China Craton Reveal Multiple Events in the Late Mesoarchean-Early Neoarchean. Chemical Geology, 261(1-2): 140-154. doi: 10.1016/j.chemgeo.2008.10.041
Liu, F.L., Robinson, P.T., Gerdes, A., et al., 2010a. Zircon U-Pb Ages, REE Concentrations and Hf Isotope Compositions of Granitic Leucosome and Pegmatite from the North Sulu UHP Terrane in China: Constraints on the Timing and Nature of Partial Melting. Lithos, 117(1-4): 247-268. doi: 10.1016/j.lithos.2010.03.002
Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010b. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths. Journal of Petrology, 51(1-2): 537-571. doi: 10.1093/petrology/egp082
Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010c. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS. Chinese Science Bulletin, 55(15): 1535-1546. doi: 10.1007/s11434-010-3052-4
Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1-2): 34-43. doi: 10.1016/j.chemgeo.2008.08.004
Lu, J.S., Wang. G.D., Wang. H., et al., 2013. Metamorphic P-T-t Paths Retrieved from the Amphibolites, Lushan Terrane, Henan Province and Reappraisal of the Paleoproterozoic Tectonic Evolution of the Trans-North China Orogen. Precambrian Research, 238: 61-77. doi: 10.1016/j.precamres.2013.09.019
Lu, X.P., Wu, F.Y., Guo, J.H., et al., 2006. Zircon U-Pb Geochronological Constraints on the Paleoproterozoic Crustal Evolution of the Eastern Block in the North China Craton. Precambrian Research, 146(3-4): 138-164. doi: 10.1016/j.precamres.2006.01.009
Ni, Z.Y., Wang, R.M., Tong, Y., et al., 2003. ²⁰⁷Pb/²⁰⁶Pb Age of Zircon and ⁴⁰Ar/³⁹Ar of Amphibole from Plagioclase Amphibolite in the Taihua Group, Luoning, Henan, China. Geological Review, 49(4): 361-366 (in Chinese with English abstract). http://www.researchgate.net/publication/285499277_207Pb206Pb_age_of_zircon_and_Ar_Ar_of_amphibole_from_plagioclase_amphibolite_in_the_Taihua_Group_Luoning_Henan_China
Peng, P., Zhai, M.G., Ernst, R.E., et al., 2008. A 1.78 Ga Large Igneous Province in the North China Craton: The Xiong'er Volcanic Province and the North China Dyke Swarm. Lithos, 101(3-4): 260-280. doi: 10.1016/j.lithos.2007.07.006
Sawyer, E.W., 1999. Criteria for the Recognition of Partial Melting. Physics Chemistry of the Earth(Part A), 24(3): 269-279. doi: 10.1016/S1464-1895(99)00029-0
Sawyer, E.W., 2001. Melt Segregation in the Continental Crust: Distribution and Movement of Melt in Anatectic Rocks. Journal of Metamorphic Geology, 19(3): 291-309. doi: 10.1046/j.0263-4929.2000.00312.x
Schaltegger, U., Fanning, C.M., Gunther, D., et al., 1999. Growth, Annealing and Recrystallization of Zircon and Preservation of Monazite in High-Grade Metamorphism: Conventional and In-Situ U-Pb Isotope, Cathodoluminescence and Microchemical Evidence. Contributions to Mineralogy and Petrology, 134(2-3): 186-201. doi: 10.1007/s004100050478
Shi, Y., Yu, J.H., Xu, X.S., et al., 2011. U-Pb Ages and Hf Isotope Compositions of Zircons of Taihua Group in Xiaoqinling Area, Shanxi Province. Acta Petrologica Sinica, 27(10): 3095-3108(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_acta-petrologica-sinica_thesis/0201252023051.html
Solar, G.S., Brown, M., 2001. Petrogenesis of Migmatites in Maine, USA: Possible Source of Peraluminous Leucogranite in Plutons? Journal of Petrology, 42(4): 789-823. doi: 10.1093/petrology/42.4.789
Vanderhaeghe, O., 2009. Migmatites, Granites and Orogeny: Flow Modes of Partially-Molten Rocks and Magmas Associated with Melt/Solid Segregation in Orogenic Belts. Tectonophysics, 477(3-4): 119-134. doi: 10.1016/j.tecto.2009.06.021
Vanderhaeghe, O., Teyssier, C., 2001. Crustal-Scale Rheological Transitions during Late-Orogenic Collapse. Tectonophysics, 335(1-2): 211-228. doi: 10.1016/s0040-1951(01)00053-1
Wan, Y.S., Song, B., Liu, D.Y., et al., 2006a. SHRIMP U-Pb Zircon Geochronology of Palaeoproterozoic Metasedimentary Rocks in the North China Craton: Evidence for a Major Late Palaeoproterozoic Tectonothermal Event. Precambrian Research, 149(3-4): 249-271. doi: 10.1016/j.precamres.2006.06.006
Wan, Y.S., Wilde, S.A., Liu, D.Y., et al., 2006b. Further Evidence for ~1.85 Ga Metamorphism in the Central Zone of the North China Craton: SHRIMP U-Pb Dating of Zircon from Metamorphic Rocks in the Lushan Area, Henan Province. Gondwana Research, 9(1-2): 189-197. doi: 10.1016/j.gr.2005.06.010
Wang, G.D., Lu, J.S., Wang, H., et al., 2013. LA-ICP-MS U-Pb Dating of Zircons and ⁴⁰Ar/³⁹Ar Dating of Amphiboles of the Taihua Metamorphic Complex, Mt. Huashan, Southern Terminal of the Palaeoproterozoic Trans-North China Orogen. Acta Petrologica Sinica, 29(9): 3099-3114 (in Chinese with English abstract). http://www.researchgate.net/publication/295605442_LA-ICP-MS_U-Pb_dating_of_zircons_and_Ar-4039_Ar_dating_of_amphiboles_of_the_Taihua_Metamorphic_Complex
Wang, R.M., Ni, Z.Y., Tong, Y., 2002. Stratigraphic Unit or Tectonic Unit? Geology in China, 29(3): 281-285(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200203007.htm
Wang, Y.J., Peng, T.P., Fan, W.M., et al., 2007. Early Proterozoic Mafic Dikes in the North China Craton and Their Tectonic Implications. Bulletin of Mineralogy, Petrology and Geochemistry, 26(1): 1-9(in Chinese with English abstract).
Wu, Y.B., Zheng, Y.F., 2004. Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age. Chinese Science Bulletin. , 49(16): 1589-1604(in Chinese). doi: 10.1360/csb2004-49-16-1589
Xu, X.S., Griffin, W.L., Ma, X., et al., 2009. The Taihua Group on the Southern Margin of the North China Craton: Further Insights from U-Pb Ages and Hf Isotope Compositions of Zircons. Mineralogy and Petrology, 97(1-2): 43-59. doi: 10.1007/s00710-009-0062-5
Xue, L.W., Yu, X.D., Zhao, T.P., 1996. The Geochemical Characteristics of A-Type Granite in Songshan Area and Its Structural Environment. Acta Petrologica Sinica, 12(1): 137-144(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB601.011.htm
Yin, C.Q., Zhao, G.C., Sun, M., et al., 2009. LA-ICP-MS U-Pb Zircon Ages of the Qianlishan Complex: Constrains on the Evolution of the Khondalite Belt in the Western Block of the North China Craton. Precambrian Research, 174(1-2): 78-94. doi: 10.1016/j.precamres.2009.06.008
Yu, X.Q., Liu, J.L., Li, C.L., et al., 2013. Zircon U-Pb Dating and Hf Isotope Analysis on the Taihua Complex: Constraints on the Formation and Evolution of the Trans-North China Orogen. Precambrian Research, 230: 31-44. doi: 10.1016/j.precamres.2012.12.008
Zhao, G.C., Cawood, P.A., Wilde, S.A., et al., 2000. Metamorphism of Basement Rocks in the Central Zone of the North China Craton: Implications for Paleoproterozoic Tectonic Evolution. Precambrian Research, 103(1): 55-88. doi: 10.1016/S0301-9268(00)00076-0
Zhao, G.C., Sun, M., Wilde, S.A., 2002. Major Tectonic Units of the North China Craton and Their Paleoproterozoic Assembly. Science in China(Ser. D), 32(7): 538-549(in Chinese). http://qikan.cqvip.com/Qikan/Article/Detail?id=1001317729
Zhao, T.P., Zhai, M.G., Xia, B., et al., 2004. Zircon U-Pb SHRIMP Dating for the Volcanic Rocks of the Xiong'er Group: Constraints on the Initial Formation Age of the Cover of the North China Craton. Chinese Science Bulletin, 49(22): 2342-2349(in Chinese). doi: 10.1360/csb2004-49-22-2342
Zhao, T.P., Zhou, M.F., 2009. Geochemical Constraints on the Tectonic Setting of Paleoproterozoic A-Type Granites in the Southern Margin of the North China Craton. Journal of Asian Earth Sciences, 36(2-3): 183-195. doi: 10.1016/j.jseaes.2009.05.005
Zhou, H.W., Zhong, Z.Q., Ling, W.L., et al., 1998. Sm-Nd Isochron for the Amphibolites within Taihua Complex from Xiao Qinling Area, Western Henan and Its Geological Implications. Geochimica, 27(4): 367-372 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX199804007.htm
毕诗健, 李建威, 李占轲, 2011. 华北克拉通南缘小秦岭金矿区基性脉岩时代及地质意义. 地球科学——中国地质大学学报, 36(1): 17-32. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201101004.htm
程裕淇, 杨崇辉, 万渝生, 等, 2004. 太行山中北段早前寒武纪地质和深熔作用对地壳岩石的改造. 北京: 地质出版社, 191.
第五春荣, 孙勇, 林慈銮, 等, 2007. 豫西宜阳地区TTG质片麻岩锆石U-Pb定年和Hf同位素地质学. 岩石学报, 23(2): 253-262. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702007.htm
胡国辉, 胡俊良, 陈伟, 等, 2010. 华北克拉通南缘中条山-嵩山地区1.78 Ga基性岩墙群的地球化学特征及构造环境. 岩石学报, 26(5): 1563-1576. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201005021.htm
蒋宗胜, 王国栋, 肖玲玲, 等, 2011. 河南洛宁太华变质杂岩区早元古代变质作用P-T-t轨迹及其大地构造意义. 岩石学报, 27(12): 3701-3717. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201112017.htm
李厚民, 陈毓川, 王登红, 等, 2007. 小秦岭变质岩及脉体锆石SHRIMP U-Pb年龄及其地质意义. 岩石学报, 23(10): 2504-2512. doi: 10.3969/j.issn.1000-0569.2007.10.018
李江海, 何文渊, 钱祥麟, 1997. 元古代基性岩墙群的成因机制、构造背景及其古板块再造意义. 高校地质学报, 3(3): 272-281. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX703.003.htm
李江海, 钱祥麟, 黄雄南, 等, 2000. 华北陆块基底构造格局及早期大陆克拉通化过程. 岩石学报, 16(1): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200001000.htm
林宝钦, 陶铁镛, 1989. 豫陕小秦岭地区太古代主要含金地层特征研究, 见: 林宝钦主编. 中国金矿类型区域成矿条件文集(3)——小秦岭地区, 北京: 地质出版社.
林慈銮, 2006. 河南鲁山地区太古代片麻岩系的地球化学、锆石年代学及其构造环境(硕士学位论文), 西安: 西北大学.
倪志耀, 王仁民, 童英, 等, 2003. 河南洛宁太华岩群斜长角闪岩的锆石²⁰⁷Pb/²⁰⁶Pb和角闪石⁴⁰Ar/³⁹Ar年龄. 地质论评, 49(4): 361-366. doi: 10.3321/j.issn:0371-5736.2003.04.004
时毓, 于津海, 徐夕生, 等, 2011. 陕西小秦岭地区太华群的锆石U-Pb年龄和Hf同位素组成. 岩石学报, 27(10): 3095-3108. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201110025.htm
王国栋, 卢俊生, 王浩, 等, 2013. 华山太华变质杂岩中LA-ICP-MS锆石U-Pb定年及角闪石⁴⁰Ar/³⁹Ar定年. 岩石学报, 29(9): 3099-3114. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201309012.htm
王仁民, 倪志耀, 童英, 2002. 是地层单元还是构造单元?中国地质, 29(3): 281-285. doi: 10.3969/j.issn.1000-3657.2002.03.008
王岳军, 彭头平, 范蔚茗, 等, 2007. 华北陆块早元古代基性岩墙群及其构造意义. 矿物岩石地球化学通报, 26(1): 1-9. doi: 10.3969/j.issn.1007-2802.2007.01.001
吴元保, 郑永飞, 2004. 锆石成因矿物学研究及其对U-Pb年龄解释的制约. 科学通报, 49(16): 1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002
薛良伟, 尉向东, 赵太平, 1996. 嵩山A型花岗岩的地质地球化学特征和构造环境. 岩石学报, 12(1): 137-144. doi: 10.3321/j.issn:1000-0569.1996.01.012
赵国春, 孙敏, Wilde, S.A., 2002. 华北克拉通基底构造单元特征及早元古代拼合. 中国科学(D辑), 32(7): 538-549. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200207001.htm
赵太平, 翟明国, 夏斌, 等, 2004. 熊耳群火山岩锆石SHRIMP年代学研究: 对华北克拉通盖层发育初始时间的制约. 科学通报, 49(22): 2342-2349. doi: 10.3321/j.issn:0023-074X.2004.22.015
周汉文, 钟增球, 凌文黎, 等, 1998. 豫西小秦岭地区太华杂岩斜长角闪岩Sm-Nd等时线年龄及其地质意义. 地球化学, 27(4): 367-372. doi: 10.3321/j.issn:0379-1726.1998.04.011