黔东震旦-寒武系转换期碎屑锆石年龄及其地质意义

杨恩林; 吕新彪; 石平; 吴波; 刘文; 狄永宁

doi:10.3799/dqkx.2014.037

黔东震旦-寒武系转换期碎屑锆石年龄及其地质意义

doi: 10.3799/dqkx.2014.037

杨恩林^{1, 2,},
吕新彪^1, ,,
石平²,
吴波²,
刘文³,
狄永宁⁴

1.
中国地质大学资源学院，湖北武汉 430074
2.
贵州省地质矿产勘察开发局117地质大队，贵州贵阳 550018
3.
中国地质大学地质调查研究院，湖北武汉 430074
4.
贵州师范大学地理与环境科学学院，贵州贵阳 550001

基金项目:

“十二五”国家科技支撑计划项目05子课题 2011BAB06B04-05

贵州地矿局地质科研项目 200901

详细信息

作者简介:
杨恩林(1978-)，男，工程师，博士生，主要从事沉积学研究.E-mail: 155060162@qq.com

通讯作者:
吕新彪，E-mail: lvxb_01@163.com

中图分类号: P597
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- 被引次数: 0
出版历程
- 收稿日期: 2013-07-19
- 刊出日期: 2014-04-15

Detrital Zircon Age of Stratigraphic Sinian-Cambrian in East Guizhou and Its Geological Significance

Yang Enlin^{1, 2
,},
Lü Xinbiao^{1
, ,},
Shi Ping²,
Wu Bo²,
Liu Wen³,
Di Yongning⁴

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
117 Geological Team, Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang 550018, China
3.
Geological Survey, China University of Geosciences, Wuhan 430074, China
4.
School of Geographic and Environmental Sciences, Guizhou Normal University, Guiyang 550001, China

摘要

摘要: 通过对注溪地层剖面岩性、含矿性及接触关系进行详细考察，及对其黑色岩系中长石岩屑砂岩进行碎屑锆石LA-ICP-MS U-Pb测年，获得84组有效年龄，其中864~742 Ma年龄最集中，表明新元古代黔东地区存在大规模的岩浆活动.江南造山带为黔东早寒武世黑色岩系的主要沉积物源区，而钒等成矿元素源于基性-超基性侵入岩体.雪峰运动导致这些含矿岩体剥顶，大量金属元素注入海洋.海侵海底缺氧，富含这些成矿元素藻类死亡，钒等金属元素随同有机质进入沉积物中，在利于其沉淀富集的留茶坡和九门冲组地层成矿.536 Ma为留茶坡组最后接受沉积时限和九门冲组最大沉积年龄，震旦与寒武系界线位于留茶坡组中上部硅质岩中，清水江组地层岩性的变形、变质和角度不整合于上覆、下伏地层的现象为雪峰运动地质效应.
- 地层学 /
- 碎屑锆石 /
- 沉积 /
- 地质年代学 /
- 注溪剖面
Abstract: Lithology, ore-bearing potential and contact relation in Zhuxi stratigraphic section are studied in detail. 84 groups of effective ages concentrated in 864-742 Ma are obtained from U-Pb dating of detrital zircon by LA-ICP-MS in feldspar lithic sandstone in the black shales, which indicates the presence of large-scale magmatic activity of the East Guizhou at the Neoproterozoic. All zircon U-Pb ages indicate that sediments within Lower Cambrian black shales in East Guizhou are mainly from the Jiangnan orogen. Metal elements such as vanadium are derived from the basic-ultrabasic rocks. The Xuefeng movement peeled the top of ore-bearing rock off the basic-ultrabasic rocks, pouring a great amount of metal into the ocean. The anoxic submarine caused the death of algae whose bodies were rich of metallogenic elements, which introduced vanadium into the sediments along with the organic matter. The mineralization occurred in the Liuchapo and Jiumenchong formations that were favorable to sedimentation of metals. 536 Ma is the final depositional time of the Jiumenchong Formation, and maximum depositional age of the Liuchapo Formation. The boundary between Sinian and Cambrian is located in the upper siliceous rocks of the Liuchapo Formation. Lithology deformation, metamorphism, and unconformity with other strata of the Qingshuijiang Formation are the geological responses of the Xuefeng movement.
- stratigraphy /
- detrital zircon /
- sedimentology /
- geochronology /
- Zhuxi section

HTML全文

图 1 注溪钒矿床地质略图(a)和研究区大地构造单元(b) (图a据贵州地矿局117地质队资料，2011修改)

Fig. 1. The simplified geological map of the Zhuxi vanadium deposit (a), and the tectonic location and tectonic units division of the studied area (b)

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图 2 注溪钒矿床老屋基地层柱状剖面

Fig. 2. Stratigraphic in Laowuji of the Zhuxi vanadium deposit

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图 3 长石岩屑砂岩露头(a)和显微镜下照片(b)

Fig. 3. Photos of the feldspar lithic sandstone in outcrop and under microscope

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图 4 长石岩屑砂岩代表性锆石CL图像(图中圆为锆石U-Pb测年位置，其编号与表 1中一致)

Fig. 4. CL images of selected zircons from Jiumenchong Formation

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图 5 九门冲组碎屑锆石U-Pb年龄谐和图

Fig. 5. U-Pb concordia plots of detrital zircon from Jiumenchong Formation

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图 6 九门冲组碎屑锆石U-Pb年龄图谱

Fig. 6. U-Pb histograms and relative probability plots of detrital zircon from Jiumenchong Formation

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图 7 江南造山带新元古代部分岩体分布(据王敏，2012修改)

Fig. 7. The distribution of partly igneous rocks in Neroproterozoic from the Jiangnan orogen

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图 8 江南造山带新元古代岩体年龄统计直方图(数据来源李献华等, 1999, 2002；葛文春等，2001；王敏，2012)

a.所统计岩体年龄；b.中酸性岩体年龄；c.基性-超基性岩体年龄

Fig. 8. Age histograms of igneous rocks in Neroproterozoic from the Jiangnan orogen

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表 1 九门冲组碎屑锆石U-Pb年龄测试结果

Table 1. U-Pb isotopic data for detrital zircons from Jiumenchong Formation

测点号	含量(10^-6)				²⁰⁷Pb/²⁰⁶Pb							²⁰⁶Pb/²³⁸U(Ma)						谐和度(%)
测点号	Pb	Th	U		比值	1σ	比值	1σ	比值	1σ		年龄	1σ	年龄	1σ	年龄	1σ	谐和度(%)
1	132	412	408		0.062 86	0.002 90	1.061 73	0.047 04	0.122 44	0.001 90		702	94	735	23	745	11	98
2	145	288	426		0.069 98	0.003 16	1.488 85	0.066 18	0.153 29	0.002 13		928	93	926	27	919	12	99
3	35	72	117		0.079 01	0.005 47	1.373 37	0.094 38	0.127 16	0.003 06		1 172	138	878	40	772	17	87
4	177	455	562		0.066 20	0.003 13	1.189 95	0.052 61	0.129 64	0.001 77		813	100	796	24	786	10	98
5	115	353	256		0.067 91	0.004 48	1.188 03	0.074 88	0.127 13	0.002 30		865	137	795	35	771	13	96
6	67	179	217		0.066 49	0.003 95	1.175 87	0.065 50	0.128 51	0.002 30		822	124	789	31	779	13	98
7	184	427	600		0.066 64	0.002 88	1.324 83	0.052 80	0.143 45	0.001 94		828	85	857	23	864	11	99
8	52	147	140		0.075 08	0.005 54	1.376 59	0.097 03	0.135 07	0.002 92		1 072	149	879	41	817	17	92
9	35	73	143		0.072 93	0.005 31	1.330 88	0.088 63	0.134 93	0.003 33		1 013	148	859	39	816	19	94
10	326	824	1 204		0.065 53	0.002 42	1.169 33	0.043 75	0.127 56	0.001 58		791	78	786	20	774	9	98
11	148	317	623		0.066 00	0.002 74	1.254 27	0.049 92	0.136 89	0.001 74		806	92	825	22	827	10	99
12	250	909	352		0.063 47	0.003 04	1.132 99	0.054 15	0.128 23	0.002 01		724	106	769	26	778	11	98
13	265	735	420		0.068 99	0.003 14	1.462 46	0.065 46	0.152 33	0.002 46		898	-105	915	27	914	14	99
14	107	270	369		0.061 50	0.003 28	1.042 38	0.052 77	0.123 09	0.002 28		657	115	725	26	748	13	96
15	295	772	848		0.060 11	0.002 23	1.144 73	0.045 60	0.137 19	0.002 30		609	81	775	22	829	13	93
16	252	504	421		0.088 03	0.004 62	1.707 72	0.100 44	0.137 36	0.002 83		1 383	100	1 011	38	830	16	80
17	227	608	780		0.063 62	0.002 58	1.086 82	0.041 96	0.122 89	0.001 72		728	86	747	20	747	10	99
18	64	160	190		0.067 15	0.004 31	1.199 49	0.070 61	0.129 84	0.002 66		843	135	800	33	787	15	98
19	83	223	235		0.058 71	0.003 91	1.168 81	0.067 02	0.142 32	0.003 02		567	114	786	31	858	17	91
20	172	356	634		0.062 80	0.003 34	1.280 24	0.051 90	0.140 48	0.001 83		702	114	837	23	847	10	98
21	43	124	162		0.077 10	0.007 37	1.088 86	0.084 02	0.108 23	0.004 00		1124	192	748	41	662	23	87
22	174	408	686		0.065 99	0.002 80	1.215 79	0.045 50	0.130 79	0.001 86		806	90	808	21	792	11	98
23	159	387	472		0.064 81	0.003 14	1.282 27	0.056 92	0.143 06	0.002 26		769	108	838	25	862	13	97
24	114	334	242		0.070 46	0.004 03	1.263 83	0.074 68	0.129 71	0.002 56		943	117	830	34	786	15	94
25	61	141	215		0.067 77	0.004 06	1.179 98	0.070 49	0.127 24	0.002 55		861	125	791	33	772	15	97
26	64	127	235		0.068 33	0.003 56	1.334 47	0.068 95	0.142 12	0.002 63		880	107	861	30	857	15	99
27	247	630	902		0.070 81	0.004 66	1.243 21	0.079 16	0.126 80	0.001 49		954	135	820	36	770	9	93
28	93	299	221		0.071 33	0.004 89	1.167 84	0.072 31	0.122 06	0.002 56		969	141	786	34	742	15	94
29	157	498	431		0.067 40	0.003 05	1.141 34	0.050 68	0.122 89	0.001 93		850	94	773	24	747	11	96
30	135	345	473		0.063 34	0.002 76	1.080 20	0.047 26	0.122 95	0.001 64		720	88	744	23	748	9	99
31	144	557	621		0.060 17	0.002 96	0.740 59	0.035 21	0.089 49	0.001 26		609	112	563	21	553	7	98
32	110	223	425		0.070 59	0.003 27	1.321 23	0.060 71	0.134 82	0.001 87		946	96	855	27	815	11	95
33	280	656	728		0.062 96	0.002 60	1.244 23	0.050 16	0.142 28	0.001 91		706	88	821	23	858	11	95
34	231	593	654		0.066 33	0.002 64	1.296 01	0.050 30	0.140 70	0.001 88		817	83	844	22	849	11	99
35	226	699	907		0.059 73	0.002 29	0.900 70	0.035 21	0.108 34	0.001 49		594	83	652	19	663	9	98
36	66	168	195		0.062 13	0.003 77	1.169 11	0.070 19	0.136 30	0.002 33		680	130	786	33	824	13	95
37	131	301	596		0.070 27	0.003 28	1.039 65	0.047 68	0.107 62	0.001 51		936	95	724	24	659	9	90
38	117	354	322		0.063 76	0.003 20	1.123 19	0.058 88	0.127 92	0.002 36		744	102	765	28	776	13	98
39	70	185	191		0.066 92	0.005 10	1.219 83	0.085 00	0.134 78	0.003 03		835	127	810	39	815	17	99
40	69	176	196		0.065 35	0.004 28	1.246 62	0.073 01	0.142 17	0.003 17		787	137	822	33	857	18	95
41	113	257	388		0.064 00	0.003 08	1.273 94	0.061 61	0.142 58	0.002 28		743	102	834	28	859	13	97
42	135	367	343		0.067 76	0.003 19	1.327 40	0.060 81	0.140 80	0.001 98		861	103	858	27	849	11	98
43	99	244	296		0.072 26	0.004 29	1.275 24	0.073 10	0.127 57	0.001 98		994	116	835	33	774	11	92
44	261	235	388		0.106 64	0.003 96	4.995 41	0.179 71	0.335 70	0.005 58		1 743	68	1 819	30	1 866	27	97
45	87	231	271		0.071 28	0.004 33	1.338 01	0.077 69	0.136 16	0.002 37		965	125	862	34	823	13	95
46	95	248	331		0.064 28	0.003 35	1.128 41	0.057 16	0.127 28	0.002 06		750	111	767	27	772	12	99
47	102	275	269		0.071 74	0.003 97	1.378 09	0.071 66	0.142 35	0.004 23		989	113	880	31	858	24	97
48	269	501	843		0.073 38	0.003 06	1.567 88	0.062 60	0.153 73	0.001 95		1 033	84	958	25	922	11	96
49	79	188	478		0.068 84	0.003 82	0.856 33	0.046 47	0.089 74	0.001 41		894	115	628	25	554	8	87
50	216	375	726		0.084 66	0.003 64	1.615 59	0.070 29	0.136 69	0.001 72		1 309	84	976	27	826	10	83
51	235	456	648		0.063 83	0.002 23	1.260 08	0.043 27	0.142 46	0.001 90		744	74	828	19	859	11	96
52	112	283	299		0.061 84	0.003 38	1.138 09	0.060 12	0.134 36	0.002 26		733	119	772	29	813	13	94
53	109	298	726		0.053 70	0.002 63	0.643 82	0.033 02	0.086 68	0.001 50		367	111	505	20	536	9	94
54	92	214	285		0.072 16	0.003 72	1.333 64	0.065 26	0.136 09	0.002 11		991	104	860	28	823	12	95
55	100	158	413		0.065 29	0.003 04	1.285 42	0.058 35	0.142 41	0.001 73		783	98	839	26	858	10	97
56	162	373	605		0.062 59	0.002 39	1.110 58	0.043 24	0.127 52	0.001 52		694	81	758	21	774	9	98
57	157	310	745		0.061 14	0.002 57	1.075 71	0.043 54	0.127 64	0.001 83		643	91	742	21	774	10	95
58	46	98	152		0.062 99	0.003 95	1.159 08	0.075 03	0.133 88	0.003 09		709	133	782	35	810	18	96
59	28	45	106		0.091 43	0.006 51	1.923 96	0.135 16	0.156 92	0.004 09		1 455	137	1 089	47	940	23	85
60	54	98	210		0.060 50	0.003 24	1.321 99	0.070 52	0.156 99	0.002 72		620	116	855	31	940	15	90
61	103	141	478		0.061 67	0.003 46	1.207 62	0.063 14	0.142 26	0.002 48		663	125	804	29	857	14	93
62	127	321	463		0.067 81	0.003 27	1.009 87	0.049 38	0.107 53	0.001 71		863	100	709	25	658	10	92
63	222	410	850		0.067 25	0.002 56	1.337 00	0.052 23	0.141 85	0.002 02		856	80	862	23	855	11	99
64	210	529	511		0.068 35	0.003 08	1.301 88	0.058 38	0.136 03	0.001 75		880	93	847	26	822	10	97
65	87	201	319	0.065 99	0.003 74	1.158 59	0.066 08	0.126 88	0.002 12	806	119	781	31	770	12	98
66	271	665	783	0.063 53	0.002 64	1.200 41	0.049 04	0.135 73	0.001 65	728	89	801	23	820	9	97
67	99	229	297	0.082 58	0.004 26	1.378 71	0.066 20	0.122 22	0.002 02	1261	106	880	28	743	12	83
68	334	30	905	0.113 69	0.003 47	5.346 99	0.167 63	0.338 92	0.004 10	1859	55	1 876	27	1 881	20	99
69	65	196	345	0.058 67	0.004 22	0.715 93	0.049 66	0.090 01	0.001 71	554	157	548	29	556	10	98
70	146	345	335	0.085 84	0.004 35	1.559 60	0.069 77	0.134 30	0.002 43	1 400	97	954	28	812	14	83
71	135	426	446	0.071 40	0.004 15	0.991 78	0.056 91	0.101 51	0.001 51	969	114	700	29	623	9	88
72	325	880	646	0.076 44	0.003 29	1.480 49	0.061 51	0.140 42	0.002 12	1 106	86	922	25	847	12	91
73	119	306	266	0.070 26	0.003 97	1.276 65	0.065 39	0.133 83	0.002 38	1 000	116	835	29	810	14	96
74	188	429	513	0.070 67	0.003 39	1.334 17	0.068 09	0.135 68	0.002 29	948	94	861	30	820	13	95
75	192	402	521	0.075 49	0.003 34	1.423 50	0.063 76	0.136 01	0.002 01	1 083	89	899	27	822	11	91
76	114	281	318	0.068 42	0.003 62	1.334 90	0.071 48	0.142 10	0.002 62	881	109	861	31	857	15	99
77	970	2 885	2 544	0.068 13	0.002 03	1.166 93	0.035 57	0.123 24	0.001 60	872	62	785	17	749	9	95
78	39	89	99	0.079 58	0.006 51	1.398 63	0.106 96	0.133 71	0.003 78	1 187	162	888	45	809	21	90
79	303	478	913	0.069 60	0.002 40	1.731 65	0.060 89	0.178 93	0.002 44	917	71	1 020	23	1 061	13	96
80	104	244	393	0.062 54	0.003 58	1.097 78	0.060 98	0.127 58	0.002 17	692	122	752	30	774	12	97
81	331	778	1 029	0.067 59	0.002 89	1.280 92	0.052 46	0.136 60	0.001 75	857	89	837	23	825	10	98
82	213	334	1 285	0.072 16	0.002 72	1.084 47	0.039 86	0.108 33	0.001 53	991	71	746	19	663	9	88
83	173	497	457	0.065 50	0.003 19	1.199 77	0.062 41	0.130 13	0.002 17	791	108	800	29	789	12	98
84	103	146	470	0.063 54	0.002 95	1.254 28	0.059 43	0.142 29	0.002 31	728	94	825	27	858	13	96

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