Zircon U-Pb Geochronology and Significance of Granites from Zhuozishan Region, Wuhai, Inner Mongolia

doi:10.19657/j.geoscience.1000-8527.2020.050

Abstract

Abstract:

The Zhuozishan granites in Wuhai (Inner Mongolia)are located at the intersection of the western margin of Ordos basin and the eastern margin of Alxa block, and comprise mainly syenogranite and monzogranite.LA-ICP-MS zircon U-Pb dating indicates that the syenogranite and monzogranite were emplaced in (2,039±79) Ma and (1,866±120) Ma, respectively, which are the products of Paleoproterozoic magmatsm.According to geochemical characteristics, the syenogranite and monzogranite are calc-alkaline, and both are rich in Si, Al and Ka, but relatively poor in Ti, Na and Ca. In addition, the granites are peraluminous (A/CNK=1.19-1.32).There is significant total REE difference between the monzogranite (17.36×10^-6-11.70×10^-6) and syenogranite(241.05×10^-6).Meanwhile, our data show that LREEs are obviously enriched and HREEs are relatively depleted. The former shows obvious negative Eu anomaly (Eu/Eu^*=0.36), and the latter shows obvious positive Eu anomaly (Eu/Eu^*=3.39-4.89), indicating that the fractionation degree of syenogranite is higher.In terms of trace elements, syenogranite is characterized by enrichments in Th, U, Pb, and large ion lithophile elements (LILEs, e.g., Rb, K),but depleted in Ba, Nb, and Ti. Monzogranite is characterized by enrichments in LILEs and depletions in high field strength elements (HFSEs, e.g., Th, Nb, Ta, and Ti).Considering the regional geological background, these rocks were likely formed by partial melting of argillaceous rocks in different stages of the same magmatic phase, representing the products of the same collision stage. This indicates that there were two magmatic events in the Late Paleoproterozoic Zhuozishan.Considering the contact characteristics of strata and the mineralization distribution characteristics, we infered that the final orogenic event between the Alxa and Ordos blocks was completed by the end Paleoproterozoic.

Key words: Alxa block, North China Craton, disconformity, zircon U-Pb dating, amalgamation, Paleoproterozoic

CLC Number:

P618
P597

HE Zeyu, SHEN Junfeng, ZHANG Shanming, LIU Jun, DU Baisong. Zircon U-Pb Geochronology and Significance of Granites from Zhuozishan Region, Wuhai, Inner Mongolia[J]. Geoscience, 2021, 35(02): 523-534.

Figures/Tables 13

Fig.1 Geologic map of Zhuozishan region, Wuhai, Inner Mongolia(modified from reference [15])

Fig.2 Field photos showing the characteristics of the Zhuozishan granites

Fig.3 Thin-section microphotographs of the Zhuozishan granites

Fig.4 Zircon CL images and representative ages for the Zhuozishan granites

Table 1 LA-ICP-MS zircon U-Pb dating results of the Zhuozishan granite sample Zr01

点号	元素含量/10^-6			Th/U	同位素比值						年龄/Ma
点号	Pb	Th	U	Th/U	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ
1	2 498	2 735	2 373	1.15	0.115 0	0.002 5	2.240 2	0.040 9	0.140 5	0.001 1	1 880	38	1 194	15	848	6
2	1 683	1 027	1 155	0.89	0.115 5	0.002 4	4.889 2	0.114 5	0.305 2	0.003 5	1 889	38	1 800	20	1 717	18
3	2 618	184	8 895	0.02	0.230 7	0.004 2	1.157 2	0.025 1	0.036 3	0.000 6	3 057	29	781	12	230	4
4	807	360	827	0.44	0.115 3	0.002 3	4.405 0	0.114 8	0.274 7	0.004 6	1 884	35	1 713	22	1 565	23
5	4 202	3 077	3 948	0.78	0.105 3	0.002 0	3.039 5	0.069 5	0.208 5	0.002 9	1 720	35	1 418	17	1 221	16
6	958	529	1 562	0.34	0.110 7	0.002 1	3.180 0	0.075 2	0.207 4	0.003 2	1 813	35	1 452	18	1 215	17
7	1 099	579	1 660	0.35	0.122 8	0.002 4	3.474 9	0.069 1	0.204 0	0.001 6	1 998	34	1 522	16	1 197	9
8	1 108	940	2 991	0.31	0.098 7	0.002 1	1.573 4	0.033 0	0.115 2	0.000 9	1 599	40	960	13	703	5
9	800	186	1 678	0.11	0.121 6	0.002 5	2.816 6	0.057 1	0.167 2	0.001 3	1 989	37	1 360	15	996	7
10	910	647	1 738	0.37	0.107 0	0.002 0	2.622 5	0.049 2	0.176 8	0.001 4	1 750	35	1 307	14	1 050	8
11	648	168	1 150	0.15	0.126 4	0.002 3	4.547 4	0.080 3	0.259 3	0.001 8	2 048	31	1 740	15	1 486	9
12	1 764	1 443	2 276	0.63	0.107 8	0.001 8	2.533 5	0.041 9	0.169 3	0.001 1	1 763	32	1 282	12	1 009	6
13	2 143	2 839	3 372	0.84	0.127 9	0.002 4	1.669 4	0.035 2	0.094 3	0.001 2	2 069	34	997	13	581	7
14	2 334	2 345	2 520	0.93	0.109 5	0.002 0	2.282 4	0.046 4	0.150 2	0.001 8	1 791	29	1 207	14	902	10
15	787	398	1 523	0.26	0.116 5	0.002 3	3.403 6	0.082 8	0.210 9	0.003 6	1 903	3	1 505	19	1 233	19
16	2 130	1 890	2 576	0.73	0.131 7	0.002 8	2.487 1	0.057 0	0.137 1	0.002 3	2 120	37	1 268	17	828	13
17	1 122	754	1 628	0.46	0.113 3	0.002 3	3.069 2	0.072 6	0.194 4	0.002 3	1 854	42	1 425	18	1 145	12
18	4 455	5 437	5 660	0.96	0.201 3	0.006 4	2.010 9	0.044 8	0.074 3	0.001 1	2 837	52	1 119	15	462	7
19	1 491	1 592	2 589	0.62	0.110 3	0.002 0	2.095 0	0.048 2	0.136 2	0.002 0	1 806	32	1 147	16	823	11

Table 1 LA-ICP-MS zircon U-Pb dating results of the Zhuozishan granite sample Zr01

点号	元素含量/10^-6			Th/U	同位素比值						年龄/Ma
点号	Pb	Th	U	Th/U	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ
1	2 498	2 735	2 373	1.15	0.115 0	0.002 5	2.240 2	0.040 9	0.140 5	0.001 1	1 880	38	1 194	15	848	6
2	1 683	1 027	1 155	0.89	0.115 5	0.002 4	4.889 2	0.114 5	0.305 2	0.003 5	1 889	38	1 800	20	1 717	18
3	2 618	184	8 895	0.02	0.230 7	0.004 2	1.157 2	0.025 1	0.036 3	0.000 6	3 057	29	781	12	230	4
4	807	360	827	0.44	0.115 3	0.002 3	4.405 0	0.114 8	0.274 7	0.004 6	1 884	35	1 713	22	1 565	23
5	4 202	3 077	3 948	0.78	0.105 3	0.002 0	3.039 5	0.069 5	0.208 5	0.002 9	1 720	35	1 418	17	1 221	16
6	958	529	1 562	0.34	0.110 7	0.002 1	3.180 0	0.075 2	0.207 4	0.003 2	1 813	35	1 452	18	1 215	17
7	1 099	579	1 660	0.35	0.122 8	0.002 4	3.474 9	0.069 1	0.204 0	0.001 6	1 998	34	1 522	16	1 197	9
8	1 108	940	2 991	0.31	0.098 7	0.002 1	1.573 4	0.033 0	0.115 2	0.000 9	1 599	40	960	13	703	5
9	800	186	1 678	0.11	0.121 6	0.002 5	2.816 6	0.057 1	0.167 2	0.001 3	1 989	37	1 360	15	996	7
10	910	647	1 738	0.37	0.107 0	0.002 0	2.622 5	0.049 2	0.176 8	0.001 4	1 750	35	1 307	14	1 050	8
11	648	168	1 150	0.15	0.126 4	0.002 3	4.547 4	0.080 3	0.259 3	0.001 8	2 048	31	1 740	15	1 486	9
12	1 764	1 443	2 276	0.63	0.107 8	0.001 8	2.533 5	0.041 9	0.169 3	0.001 1	1 763	32	1 282	12	1 009	6
13	2 143	2 839	3 372	0.84	0.127 9	0.002 4	1.669 4	0.035 2	0.094 3	0.001 2	2 069	34	997	13	581	7
14	2 334	2 345	2 520	0.93	0.109 5	0.002 0	2.282 4	0.046 4	0.150 2	0.001 8	1 791	29	1 207	14	902	10
15	787	398	1 523	0.26	0.116 5	0.002 3	3.403 6	0.082 8	0.210 9	0.003 6	1 903	3	1 505	19	1 233	19
16	2 130	1 890	2 576	0.73	0.131 7	0.002 8	2.487 1	0.057 0	0.137 1	0.002 3	2 120	37	1 268	17	828	13
17	1 122	754	1 628	0.46	0.113 3	0.002 3	3.069 2	0.072 6	0.194 4	0.002 3	1 854	42	1 425	18	1 145	12
18	4 455	5 437	5 660	0.96	0.201 3	0.006 4	2.010 9	0.044 8	0.074 3	0.001 1	2 837	52	1 119	15	462	7
19	1 491	1 592	2 589	0.62	0.110 3	0.002 0	2.095 0	0.048 2	0.136 2	0.002 0	1 806	32	1 147	16	823	11

Fig.5 Zircon concordia U-Pb diagrams for the Zhuozishan granites

Table 2 LA-ICP-MS zircon U-Pb dating results of the Zhuozishan granite sample Zr02

点号	元素含量/10^-6			Th/U	同位素比值						年龄/Ma
点号	Pb	Th	U	Th/U	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ
1	202	66	316	0.21	0.131 2	0.002 8	4.880 8	0.115 9	0.268 3	0.003 7	2 114	37	1 799	20	1 532	19
2	56	209	389	0.54	0.050 9	0.002 4	0.285 0	0.013 4	0.040 7	0.000 4	235	109	255	11	257	3
3	165	67	168	0.40	0.124 4	0.002 5	6.378 2	0.133 1	0.369 9	0.003 8	2 021	35	2 029	18	2 029	18
4	286	108	334	0.32	0.122 4	0.002 4	5.780 5	0.112 6	0.340 7	0.002 5	1 992	31	1 943	17	1 890	12
5	149	44	194	0.23	0.125 3	0.002 9	5.371 3	0.126 7	0.309 6	0.003 0	2 032	42	1 880	20	1 738	15
6	46	17	42	0.40	0.128 1	0.004 3	6.663 5	0.215 7	0.378 3	0.004 7	2 072	59	2 068	29	2 068	22
7	130	53	150	0.36	0.124 2	0.002 9	5.866 3	0.146 6	0.342 1	0.005 2	2 017	41	1 956	22	1 897	25
8	240	37	617	0.06	0.126 7	0.002 4	2.914 5	0.058 3	0.166 0	0.001 6	2 054	33	1 386	15	990	9
9	399	41	776	0.05	0.134 4	0.002 4	3.198 3	0.058 3	0.171 7	0.001 2	2 167	31	1 457	14	1 022	6
10	174	59	208	0.28	0.124 1	0.002 4	6.327 8	0.119 9	0.368 5	0.002 6	2 016	33	2 022	17	2 022	12
11	154	30	266	0.11	0.127 1	0.002 6	5.049 4	0.104 5	0.287 3	0.002 7	2 059	36	1 828	18	1 628	14
12	359	168	480	0.35	0.120 6	0.002 4	4.494 3	0.090 3	0.269 3	0.002 1	1 965	35	1 730	17	1 537	10
13	371	280	997	0.28	0.105 7	0.002 4	1.887 3	0.049 1	0.129 0	0.002 0	1 728	41	1 077	17	782	11
14	407	133	590	0.22	0.154 3	0.003 7	3.696 5	0.108 0	0.178 7	0.005 2	2 394	40	1 571	23	1 060	29
15	2 905	359	4 461	0.08	0.303 1	0.006 4	2.552 9	0.049 0	0.061 2	0.000 7	3 486	33	1 287	14	383	4
16	166	44	289	0.15	0.140 4	0.003 0	4.254 4	0.118 9	0.222 5	0.005 8	2 232	37	1 685	23	1 295	31
17	447	165	745	0.22	0.159 0	0.003 6	3.290 1	0.083 7	0.148 5	0.001 7	2 456	39	1 479	20	892	9
18	391	223	800	0.28	0.130 9	0.002 5	2.602 2	0.067 9	0.143 7	0.002 9	2 110	33	1 301	19	865	16
19	132	50	165	0.30	0.126 9	0.002 6	6.104 3	0.138 8	0.347 1	0.004 2	2 055	37	1 991	20	1 921	20
20	202	76	286	0.27	0.121 4	0.002 4	5.365 0	0.132 4	0.316 8	0.004 4	1 977	35	1 879	21	1 774	22

Table 2 LA-ICP-MS zircon U-Pb dating results of the Zhuozishan granite sample Zr02

点号	元素含量/10^-6			Th/U	同位素比值						年龄/Ma
点号	Pb	Th	U	Th/U	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ
1	202	66	316	0.21	0.131 2	0.002 8	4.880 8	0.115 9	0.268 3	0.003 7	2 114	37	1 799	20	1 532	19
2	56	209	389	0.54	0.050 9	0.002 4	0.285 0	0.013 4	0.040 7	0.000 4	235	109	255	11	257	3
3	165	67	168	0.40	0.124 4	0.002 5	6.378 2	0.133 1	0.369 9	0.003 8	2 021	35	2 029	18	2 029	18
4	286	108	334	0.32	0.122 4	0.002 4	5.780 5	0.112 6	0.340 7	0.002 5	1 992	31	1 943	17	1 890	12
5	149	44	194	0.23	0.125 3	0.002 9	5.371 3	0.126 7	0.309 6	0.003 0	2 032	42	1 880	20	1 738	15
6	46	17	42	0.40	0.128 1	0.004 3	6.663 5	0.215 7	0.378 3	0.004 7	2 072	59	2 068	29	2 068	22
7	130	53	150	0.36	0.124 2	0.002 9	5.866 3	0.146 6	0.342 1	0.005 2	2 017	41	1 956	22	1 897	25
8	240	37	617	0.06	0.126 7	0.002 4	2.914 5	0.058 3	0.166 0	0.001 6	2 054	33	1 386	15	990	9
9	399	41	776	0.05	0.134 4	0.002 4	3.198 3	0.058 3	0.171 7	0.001 2	2 167	31	1 457	14	1 022	6
10	174	59	208	0.28	0.124 1	0.002 4	6.327 8	0.119 9	0.368 5	0.002 6	2 016	33	2 022	17	2 022	12
11	154	30	266	0.11	0.127 1	0.002 6	5.049 4	0.104 5	0.287 3	0.002 7	2 059	36	1 828	18	1 628	14
12	359	168	480	0.35	0.120 6	0.002 4	4.494 3	0.090 3	0.269 3	0.002 1	1 965	35	1 730	17	1 537	10
13	371	280	997	0.28	0.105 7	0.002 4	1.887 3	0.049 1	0.129 0	0.002 0	1 728	41	1 077	17	782	11
14	407	133	590	0.22	0.154 3	0.003 7	3.696 5	0.108 0	0.178 7	0.005 2	2 394	40	1 571	23	1 060	29
15	2 905	359	4 461	0.08	0.303 1	0.006 4	2.552 9	0.049 0	0.061 2	0.000 7	3 486	33	1 287	14	383	4
16	166	44	289	0.15	0.140 4	0.003 0	4.254 4	0.118 9	0.222 5	0.005 8	2 232	37	1 685	23	1 295	31
17	447	165	745	0.22	0.159 0	0.003 6	3.290 1	0.083 7	0.148 5	0.001 7	2 456	39	1 479	20	892	9
18	391	223	800	0.28	0.130 9	0.002 5	2.602 2	0.067 9	0.143 7	0.002 9	2 110	33	1 301	19	865	16
19	132	50	165	0.30	0.126 9	0.002 6	6.104 3	0.138 8	0.347 1	0.004 2	2 055	37	1 991	20	1 921	20
20	202	76	286	0.27	0.121 4	0.002 4	5.365 0	0.132 4	0.316 8	0.004 4	1 977	35	1 879	21	1 774	22

Table 3 Major(%),rare earth (10-6) and trace element (10-6) contents of the Zhuozishan granites

样品号	SiO₂	TiO₂	Al₂O₃	Fe₂ $O 3 T$	CaO	MgO	K₂O	Na₂O	MnO	P₂O₅	烧失量	总量	Mg^#	Li
Zr01	74.54	0.12	13.44	0.88	1.12	0.23	5.85	2.66	0.02	0.11	0.91	99.88	32.12	4.87
Zr02	75.47	0.06	13.85	0.60	1.24	0.23	3.81	3.70	0.02	0.11	0.86	99.93	40.99	10.80
Zr03	74.06	0.02	14.81	0.14	0.62	0.09	6.04	3.54	0.01	0.14	0.46	99.91	54.36	6.00
样品号	Be	Sc	V	Cr	Co	Ni	Cu	Zn	Ga	Rb	Sr	Y	Zr	Nb
Zr01	0.31	2.00	3.55	3.50	0.85	1.00	1.97	10.80	15.1	155.00	102.00	3.30	11.79	4.88
Zr02	1.67	2.41	8.42	5.95	0.44	0.93	1.94	16.40	12.9	137.00	84.90	1.56	3.29	3.11
Zr03	0.59	0.81	7.52	4.67	0.10	0.56	0.45	3.35	10.4	181.00	95.80	0.59	1.30	0.89
样品号	Cs	Ba	Hf	Ta	Pb	Th	U	La	Ce	Pr	Nd	Sm	Eu	Gd
Zr01	1.76	59.09	15.47	11.46	477.46	429.41	216.67	55.40	110.00	12.20	41.30	6.83	0.80	6.39
Zr02	3.47	26.61	4.50	10.73	378.87	12.00	25.71	3.41	6.08	0.70	2.43	0.53	0.57	0.48
Zr03	3.11	53.8	1.59	6.34	505.63	7.29	12.38	2.55	4.28	0.51	1.81	0.34	0.55	0.34
样品号	Tb	Dy	Ho	Er	Tm	Yb	Lu	ΣREE	(La/Yb)_N	Eu/Eu^*	Sr/Y	Nb/Ta	σ	A/CNK
Zr01	0.84	3.68	0.56	1.40	0.18	1.14	0.33	241.05	34.86	0.36	6.80	10.38	2.30	1.19
Zr02	0.11	1.02	0.23	0.65	0.13	0.87	0.15	17.36	2.81	3.39	11.92	7.07	1.74	1.32
Zr03	0.07	0.44	0.09	0.28	0.05	0.34	0.06	11.70	5.38	4.89	35.61	3.42	2.95	1.28

Table 3 Major(%),rare earth (10-6) and trace element (10-6) contents of the Zhuozishan granites

样品号	SiO₂	TiO₂	Al₂O₃	Fe₂ $O 3 T$	CaO	MgO	K₂O	Na₂O	MnO	P₂O₅	烧失量	总量	Mg^#	Li
Zr01	74.54	0.12	13.44	0.88	1.12	0.23	5.85	2.66	0.02	0.11	0.91	99.88	32.12	4.87
Zr02	75.47	0.06	13.85	0.60	1.24	0.23	3.81	3.70	0.02	0.11	0.86	99.93	40.99	10.80
Zr03	74.06	0.02	14.81	0.14	0.62	0.09	6.04	3.54	0.01	0.14	0.46	99.91	54.36	6.00
样品号	Be	Sc	V	Cr	Co	Ni	Cu	Zn	Ga	Rb	Sr	Y	Zr	Nb
Zr01	0.31	2.00	3.55	3.50	0.85	1.00	1.97	10.80	15.1	155.00	102.00	3.30	11.79	4.88
Zr02	1.67	2.41	8.42	5.95	0.44	0.93	1.94	16.40	12.9	137.00	84.90	1.56	3.29	3.11
Zr03	0.59	0.81	7.52	4.67	0.10	0.56	0.45	3.35	10.4	181.00	95.80	0.59	1.30	0.89
样品号	Cs	Ba	Hf	Ta	Pb	Th	U	La	Ce	Pr	Nd	Sm	Eu	Gd
Zr01	1.76	59.09	15.47	11.46	477.46	429.41	216.67	55.40	110.00	12.20	41.30	6.83	0.80	6.39
Zr02	3.47	26.61	4.50	10.73	378.87	12.00	25.71	3.41	6.08	0.70	2.43	0.53	0.57	0.48
Zr03	3.11	53.8	1.59	6.34	505.63	7.29	12.38	2.55	4.28	0.51	1.81	0.34	0.55	0.34
样品号	Tb	Dy	Ho	Er	Tm	Yb	Lu	ΣREE	(La/Yb)_N	Eu/Eu^*	Sr/Y	Nb/Ta	σ	A/CNK
Zr01	0.84	3.68	0.56	1.40	0.18	1.14	0.33	241.05	34.86	0.36	6.80	10.38	2.30	1.19
Zr02	0.11	1.02	0.23	0.65	0.13	0.87	0.15	17.36	2.81	3.39	11.92	7.07	1.74	1.32
Zr03	0.07	0.44	0.09	0.28	0.05	0.34	0.06	11.70	5.38	4.89	35.61	3.42	2.95	1.28

Fig.6 Geochemical classification diagrams for the Zhuozishan granites

Fig.7 Chondrite-normalized REE patterns(a) and primitive mantle-normalized trace element spidergrams(b) for the Zhuozishan granites

Fig.8 Petrogenesis and tectonic discrimination diagrams for the Zhuozishan granites

Fig.9 Sedimentary characteristics and contact relations of Proterozoic sequences

Fig.10 Contact relationship between the Ordovician and Permian sequences

References 52

[1]	ZHAI M G, SANTOSH M. The Early Precambrian odyssey of the North China Craton:A synoptic overview[J]. Gondwana Research, 2011,20(1):6-25. DOI URL
[2]	LIU D Y, NUTMAN A P, COMPSTON W, et al. Remnants of ≥3800 Ma crust in the Chinese part of the Sino-Korean craton[J]. Geology, 1992,20(4):339-342. DOI URL
[3]	DIWU C R, SUN Y, WILDE S A, et al. New evidence for ~4.45 Ga terrestrial crust from zircon xenocrysts in Ordovician ignimbrite in the North Qinling Orogenic Belt,China[J]. Gondwana Research, 2013,23(4):1484-1490. DOI URL
[4]	李正辉, 柳小明, 董云鹏, 等. 贺兰山古元古代同碰撞花岗岩地球化学、锆石 U-Pb年代及其地质意义[J]. 岩石学报, 2013,29(7):2405-2415.
[5]	翟明国. 华北克拉通构造演化[J]. 地质力学学报, 2019,25(5):722-745.
[6]	翟明国. 华北克拉通的形成演化与成矿作用[J]. 矿床地质, 2010,29(1):24-36.
[7]	ZHAI M G, BIAN A G, ZHAO T P. The amalgamation of the supercontinent of North China Craton at the end of Neo-Archaean and its breakup during late Palaeoproterozoic and Meso-Proterozoic[J]. Science in China Series D: Earth Sciences, 2000,43(S1):219-232.
[8]	KUSKY T M, LI J H, GLASS A, et al. Origin and emplacement of Archean ophiolites of the central orogenic belt,North China Craton[J]. Developments in Precambrian Geology, 2004,13:223-274.
[9]	KUSKY T M, WINDLEY B F, POLAT A. Geological evidence for the operation of plate tectonics throughout the Archean: records from Archean paleo-plate boundaries[J]. Journal of Earth Science, 2018,29(6):1291-1303. DOI URL
[10]	黄雄南, 张家声, 彭澎, 等. 贺兰山北段古元古代结晶基底变形特征及其区域构造意义[J]. 岩石学报, 2013,29(7):2353-2370.
[11]	ZHU R X, ZHENG T Y. Destruction geodynamics of the North China Craton and its Paleoproterozoic plate tectonics[J]. Chinese Science Bulletin, 2009,54(19):3354-3366.
[12]	翟明国, 彭澎. 华北克拉通古元古代构造事件[J]. 岩石学报, 2007,23(11):2665-2682.
[13]	SANTOSH M. Assembling North China Craton within the Columbia supercontinent: the role of double-sided subduction[J]. Precambrian Research, 2010,178(1/2/3/4):149-167. DOI URL
[14]	李江海, 钱祥麟. 鄂尔多斯陆块周边孔兹岩系地层对比及其克拉通化意义[J]. 现代地质, 1999,13(2):209-210.
[15]	李锦轶, 张进, 曲军峰. 华北与阿拉善两个古陆在早古生代晚期拼合: 来自宁夏牛首山沉积岩系的证据[J]. 地质论评, 2012,58(2):208-214.
[16]	LIU Y S, GAO S, HU Z C, et al. 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[J]. Journal of Petrology, 2010,51:537-571. DOI URL
[17]	LUDWIG K R. User’s Manual for Isoplot/Ex (ver.3.00):A Geochronological Toolkit for Microsoft Excel[M]. Berkeley:Berkeley Geochronology Center , 2003: 1-55.
[18]	王岚, 杨理勤, 王亚平, 等. 锆石LA-ICP-MS原位微区U-Pb定年及微量元素的同时测定[J]. 地球学报, 2012,33(5):764-765.
[19]	何朝鑫, 陈翠华, 李佑国, 等. 青海省都兰县双庆铁矿床磁铁矿地球化学特征及成因意义[J]. 矿物学报, 2015,35(3):359-364.
[20]	戴朝成, 黄成, 焦正, 等. 内蒙古中部乌拉山地区西沙德盖岩体地球化学-年代学特征及其地质意义[J]. 现代地质, 2017,31(4):662-671.
[21]	董春艳, 刘敦一, 李俊建, 等. 华北克拉通西部孔兹岩带形成时代新证据:巴彦乌拉—贺兰山地区锆石SHRIMP定年和Hf同位素组成[J]. 科学通报, 2007,52(16):1913-1922.
[22]	钟长汀, 邓晋福, 万渝生, 等. 华北克拉通北缘中段古元古代造山作用的岩浆记录:S型花岗岩地球化学特征及锆石SHRIMP年龄[J]. 地球化学, 2007,36(6):585-600.
[23]	MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994,37(3/4):215-224. DOI URL
[24]	肖娥, 胡建, 张遵忠, 等. 东秦岭花山复式岩基中蒿坪与金山庙花岗岩体岩石地球化学、锆石U-Pb年代学和Lu-Hf同位素组成[J]. 岩石学报, 2012,28(12):4031-4046.
[25]	李琦, 王疆涛, 曾忠诚, 等. 阿尔金造山带南缘蛇绿构造混杂岩带中晚奥陶世—早志留世二长花岗岩年代学、地球化学特征及地质意义[J]. 现代地质, 2020,34(1):51-63.
[26]	SYLVESTER P J. Post-collisional strongly peraluminous granites[J]. Lithos, 1998,45(1/2/3/4):29-44. DOI URL
[27]	庞岚尹, 高昕宇, 孙乾迎, 等. 贺兰山中段古元古代黄旗口花岗质岩石的成因及其构造意义[J]. 岩石学报, 2019,35(8):2344-2362.
[28]	PATINO D A E, BEARD J S. Dehydration-melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar[J]. Journal of Petrology, 1995,36(3):707-738. DOI URL
[29]	SKJERLIE K P, JOHNSTON A D. Vapour-absent melting from 10 to 20 kbar of crustal rocks that contain multiple hydrous phases: Implications for anatexis in the deep to very deep continental crust and active continental margins[J]. Journal of Petrology, 1996,37(3):661-691. DOI URL
[30]	VAVRA G, SCHMID R, GEBAUER D. Internal morphology, habit and U-Th-Pb microanalysis of amphibolite togranulite facies zircons: Geochronology of the Ivrea Zone (Southern Alps)[J]. Contributions to Mineralogy and Petrology, 1999,134:380-404. DOI URL
[31]	PEARCE J A, HARRIS N B M, TINDLE A G . Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984,25(4):956-983. DOI URL
[32]	HARRIS N B W, PEARCE J A, TINDLE A G. Geochemical characteristics of collision-zone magmatism[J]. Geological Society,London, Special Publications, 1986,19(1):67-81. DOI URL
[33]	耿元生, 周喜文, 王新社, 等. 内蒙古贺兰山地区古元古代晚期的花岗岩浆事件及其地质意义: 同位素年代学的证据[J]. 岩石学报, 2009,25(8):1830-1842.
[34]	甘保平, 第五春荣, 王伯隆, 等. 贺兰山古元古代花岗岩年代学及地球化学特征:对华北克拉通西部孔兹岩带形成和演化的制约[J]. 岩石学报, 2019,35(8):2325-2343.
[35]	WHALEN J B, CURRIE K L, CHAPPELL B W. A-type granites: geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987,95(4):407-419. DOI URL
[36]	BATCHELOR R A, BOWDEN P. Petrogenetic interpretation of granitoid rock series using multicationic parameters[J]. Chemical Geology, 1985,48(1/2/3/4):43-55. DOI URL
[37]	任纪舜, 姜春发, 张正坤, 等. 中国大地构造及其演化: 1∶400万中国大地构造图简要说明[M]. 北京: 科学出版社, 1980: 1-124.
[38]	伍家善, 耿元生, 沈其韩, 等. 中朝古大陆太古宙地质特征及构造演化[M]. 北京: 地质出版社, 1998: 192-211.
[39]	张振法, 李超英, 牛颖智. 阿拉善—敦煌陆块的性质、范围及其构造作用和意义[J]. 内蒙古地质, 1997(2):1-14.
[40]	万渝生, 许志琴, 杨经绥, 等. 祁连造山带及邻区前寒武纪深变质基底的时代和组成[J]. 地球学报, 2003,24(4):319-324.
[41]	ZHAI M G, GUO J H, LIU W J. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton: A review[J] . Journal of Asian Earth Sciences, 2005,24(5):547-561. DOI URL
[42]	ZHAO G C, SUN M, WILDE S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton: Key issues revisited[J]. Precambrian Research, 2005,136(2):177-202. DOI URL
[43]	耿元生, 王新社, 吴春明, 等. 阿拉善变质基底古元古代晚期的构造热事件[J]. 岩石学报, 2010,26(4):1159-1170.
[44]	张进, 李锦轶, 刘建峰, 等. 内蒙古狼山西南地区枕状玄武岩LA-ICP-MS锆石U-Pb年龄及意义[J]. 地质通报, 2013,32(增):287-296.
[45]	张建新, 宫江华. 阿拉善地块性质和归属的再认识[J]. 岩石学报, 2018,34(4):940-962.
[46]	黄宝春, 杨振宇, 朱日祥, 等. 河西走廊和阿拉善东缘地区中寒武世古地磁研究的初步结果[J]. 地球物理学报, 2000,43(3):393-401.
[47]	张进, 李锦轶, 刘建峰, 等. 早古生代阿拉善地块与华北地块之间的关系:来自阿拉善东缘中奥陶统碎屑锆石的信息[J]. 岩石学报, 2012,28(9):2912-2934.
[48]	YUAN W, YANG Z Y. The Alashan Terrane was not part of North China by the Late Devonian: Evidence from detrital zircon U-Pb geochronology and Hf isotopes[J]. Gondwana Research, 2015,27(3):1270-1282. DOI URL
[49]	ZHANG B H, ZHANG J, ZHANG Y P, et al. Tectonic affinity of the Alxa Block,Northwest China: Constrained by detrital zircon U-Pb ages from the Early Paleozoic strata on its southern and eastern margins[J]. Sedimentary Geology, 2016,339:289-303. DOI URL
[50]	ZHANG J, ZHANG B H, ZHAO H . Timing of amalgamation of the Alxa Block and the North China Block: Constraints based on detrital zircon U-Pb ages and sedimentologic and structural evidence[J]. Tectonophysics, 2016,668/669:65-81. DOI URL
[51]	蒋苏扬, 黄文辉, 张永生. 鄂尔多斯盆地西缘中奥陶统地球化学特征及古环境意义[J]. 现代地质, 2020,34(3):545-553.
[52]	郑昭昌, 李玉珍. 贺兰山奥陶系研究的新进展[J]. 现代地质, 1991,5(2):119-137.