江西弋阳晚白垩世塘边组风成砂岩碎屑锆石U-Pb定年及其物源意义

王宇佳; 陈留勤; 李文灏; 李鹏程

江西弋阳晚白垩世塘边组风成砂岩碎屑锆石U-Pb定年及其物源意义

1.
东华理工大学核资源与环境国家重点实验室, 江西南昌 330013

2.
东华理工大学地球科学学院, 江西南昌 330013

基金项目:
国家自然科学基金项目《赣东北地区晚白垩世圭峰群古土壤特征与古气候研究》（批准号：41602113）

详细信息

作者简介: 王宇佳(1992-), 女, 在读硕士生, 矿物学、岩石学、矿床学专业。E-mail:1054891477@qq.com

通讯作者: 陈留勤(1983-), 男, 博士, 副教授, 沉积学专业。E-mail:liuqincheen@163.com

中图分类号: P534.53;P597⁺.3

收稿日期: 2018-06-07

修回日期: 2018-08-20

刊出日期: 2019-04-15

Detrital zircon U-Pb dating of the Late Cretaceous aeolian sandstones from the Tangbian Formation in the Yiyang area of Jiangxi Province and its provenance significance

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China

2.
School of Earth Sciences, East China University of Technology, Nanchang 330013, Jiangxi, China

More Information

Corresponding author: CHEN Liuqin, liuqincheen@163.com

Received Date: 07 June 2018

Revised Date: 20 August 2018

Publish Date: 15 April 2019

摘要

摘要:
赣东北信江盆地晚白垩世圭峰群塘边组以发育大型高角度交错层理的风成砂岩为特征，总体为干旱气候条件下沙漠沉积环境的产物。该地区所采砂岩样品为紫红色中-细粒长石石英砂岩，碎屑颗粒主要包括石英、长石、云母和岩屑，多呈次圆状，分选性较好。利用碎屑锆石LA-ICP-MS测年法，对塘边组风成砂岩进行U-Pb同位素定年，分析物源。碎屑锆石颗粒大多数大于100μm，Th/U值为0.1~2.1，且大部分锆石内部具有清晰的振荡环带结构，表明多数为岩浆锆石。²⁰⁶Pb/²³⁸U年龄加权平均值为141.4±1.2Ma。锆石U-Pb年龄主要集中于5个年龄段，分别是137~170Ma、431~506Ma、798~1172Ma、1268~2493Ma、2501~3488Ma。这些主要年龄区间与中国东南地区已知的岩浆事件对应，分别为燕山运动、加里东运动、晋宁运动、吕梁运动。其中，燕山期酸性火山-侵入杂岩提供了主要物源。结合风成砂岩交错层理反映的古风向数据，认为弋阳塘边组碎屑物质主要来自盆地北西部的九岭地区及北东部地区。
- 碎屑锆石 /
- 晚白垩世 /
- 塘边组 /
- 风成砂岩 /
- 信江盆地
Abstract:
The Tangbian Formation of the Late Cretaceous Guifeng Group in the Xinjiang Basin of northeastern Jiangxi Province is characterized by large-scale cross-bedded sandstones. They are generally products of a desert depositional environment under arid climate. The sandstone samples are purple red, fine-to medium-grained feldspar quartz sandstones. Sand particles are mainly composed of quartz, feldspar, mica and rock fragments, which are subangular to subrounded and well sorted. In order to analyze the source rocks of the Tangbian Formation, LA-ICP-MS zircon U-Pb analysis was performed. The zircon grains are mostly larger than 100μm. The results show that the Th/U ratios range from 0.1 to 2.1, and most of the zircons have a clear internal shock band structure, indicating that most of them were magmatic zircons. The mean age of ²⁰⁶Pb/²³⁸U is 141.4±1.2Ma. The age of zircon U-Pb ages are mainly concentrated in five zones of 137~170Ma, 431~506Ma, 798~1172Ma, 1268~2493Ma, 2501~3488Ma, corresponding to the major magmatic events in Southeast China, namely Yanshanian, Caledonian, Jinning, and Lvliang movements, with the Yanshanian volcanic-intrusive complex providing the dominant sediments. In combination with the paleo-wind directions from the aeolian sandstones, the sediments are interpreted to be largely from the northwestern Jiuling mountain area and the northeastern areas.
- detrital zircon /
- Late Cretaceous /
- Tangbian Formation /
- aeolian sandstone /
- Xinjiang Basin

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图 1 信江盆地地质简图^[6]和采样位置

Figure 1.

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图 2 信江盆地晚白垩世圭峰群岩性柱简图

Figure 2.

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图 3 弋阳卧佛塘边组风成砂岩露头和镜下照片

Figure 3.

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图 4 碎屑锆石阴极发光（CL）照片

Figure 4.

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图 5 碎屑锆石U-Pb年龄谐和图

Figure 5.

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图 6 信江盆地样品碎屑锆石U-Pb年龄分布直方图

Figure 6.

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图 7 信江盆地与上饶珍珠山锆石年龄频率图

Figure 7.

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图 8 信江盆地塘边组沉积模式

Figure 8.

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表 1 江西弋阳塘边组风成砂岩样品碎屑锆石U-Th-Pb定年结果

Table 1. Detrital zircon U-Th-Pb dating results of the aeolian sandstone sample from the Tangbian Formation in the Yiyang area of Jiangxi Province

点号	Th	U	Pb		同位素比值										同位素年龄/Ma
点号	l0^-6				Th/U	²⁰⁷Pb/²⁰⁶Pb	1 σ	²⁰⁷Pb/²³⁵U	1 σ	²⁰⁷Pb/²³⁸U	1 σ	₂₀₈Pb/232_Th	1 σ		²⁰⁷Pb/ ²⁰⁶Pb	1 σ	²⁰⁷Pb/²³⁵U	1 σ	²⁰⁶Pb/²³⁸U	1 σ	²⁰⁸Pb/232_Th	1 σ	谐和度/%
01	33	25	59		1.34	0.1441	0.0025	8.4260	0.1273	0.4243	0.0038	0.1363	0.0014		2277	14	2278	14	2280	17	2583	25	100
02	148	514	581		0.29	0.0923	0.0013	3.2613	0.0356	0.2562	0.0016	0.0361	0.0010		1474	12	1472	8	1470	8	717	19	100
03	109	153	110		0.71	0.0701	0.0012	1.4988	0.0206	0.1552	0.0011	0.04744	0.00041		931	17	930	8	930	6	937	8	100
04	90	218	21		0.41	0.0484	0.0020	0.1465	0.0058	0.0220	0.0002	0.0072	0.0002		117	75	139	5	140	1	144	3	99
05	193	229	24		0.84	0.0490	0.0025	0.1485	0.0072	0.0220	0.0002	0.00737	0.00013		150	95	141	6	140	1	148	3	101
06	91	132	121		0.69	0.0790	0.0011	2.1703	0.0239	0.1993	0.0013	0.0615	0.0005		1172	12	1172	8	1172	7	1206	9	100
07	928	601	62		1.54	0.0496	0.0053	0.1523	0.0161	0.0223	0.0004	0.0066	0.0002		175	204	144	14	142	3	133	4	101
08	96	226	475		0.42	0.1554	0.0018	9.6558	0.0768	0.4509	0.0029	0.1222	0.0011		2406	6	2403	7	2399	13	2330	20	100
09	128	214	147		0.60	0.0692	0.0010	1.4320	0.0173	0.1501	0.0010	0.04786	0.00039		905	15	902	7	902	5	945	8	100
10	70	185	128		0.38	0.0693	0.0014	1.4299	0.0254	0.1497	0.0011	0.04456	0.0007		907	25	902	11	899	6	881	14	100
11	80	125	39		0.64	0.0557	0.0015	0.5544	0.0137	0.0722	0.0006	0.0218	0.0003		440	40	448	9	450	3	435	5	100
12	44	228	150		0.19	0.0682	0.0010	1.4111	0.0164	0.1500	0.0010	0.0476	0.0006		876	14	894	7	901	5	939	12	99
13	407	234	78		1.74	0.0558	0.0013	0.5323	0.0110	0.0692	0.0005	0.0207	0.0002		446	33	433	7	431	3	413	3	100
14	204	144	17		1.42	0.0487	0.0041	0.1506	0.0124	0.0225	0.0004	0.0072	0.0002		131	152	142	11	143	2	145	4	99
15	164	102	147		1.60	0.3683	0.0043	10.5716	0.0835	0.2083	0.0014	0.1503	0.0008		3784	5	2486	7	1219	7	2829	15	310
16	310	391	67		0.79	0.0494	0.0040	0.1726	0.0139	0.0253	0.0003	0.0074	0.0002		168	160	162	12	161	2	149	4	101
17	54	55	145		0.99	0.1772	0.0021	12.2875	0.1031	0.5030	0.0034	0.1548	0.0010		2627	6	2627	8	2627	14	2909	18	100
18	203	565	63		0.36	0.0488	0.0025	0.1483	0.0074	0.0221	0.0002	0.0077	0.0002		139	98	140	7	141	1	156	4	99
19	129	181	347		0.71	0.1262	0.0016	6.5246	0.0590	0.3750	0.0025	0.1089	0.0008		2046	8	2049	8	2053	11	2090	15	100
20	66	296	228		0.22	0.0693	0.0016	1.4249	0.0296	0.1492	0.0011	0.0479	0.0010		906	30	899	12	897	6	946	19	100
21	217	308	510		0.70	0.1145	0.0018	5.3249	0.0716	0.3375	0.0024	0.0751	0.0010		1871	14	1873	11	1875	12	1463	18	100
22	134	144	94		0.93	0.0663	0.0016	1.2091	0.0274	0.1322	0.0011	0.0347	0.0004		817	34	805	13	801	6	690	8	100
23	105	213	64		0.49	0.1650	0.0028	1.1776	0.0160	0.0518	0.0004	0.04212	0.00039		2508	13	790	7	325	2	834	8	119
24	45	50	125		0.89	0.1643	0.0020	10.7626	0.0912	0.4752	0.0031	0.1364	0.0010		2501	7	2503	8	2506	14	2585	18	100
25	230	285	26		0.80	0.0511	0.0068	0.1535	0.0200	0.0218	0.0005	0.00668	0.00029		243	248	145	18	139	3	135	6	104
26	42	216	374		0.19	0.1233	0.0014	6.2700	0.0443	0.3690	0.0022	0.13195	0.00103		2004	6	2014	6	2025	10	2505	18	99
27	180	149	708		1.21	0.2616	0.0036	23.7814	0.2710	0.6596	0.0060	0.28563	0.00268		3256	8	3259	11	3266	23	5078	42	100
28	114	182	444		0.62	0.1636	0.0018	10.7365	0.0767	0.4760	0.0029	0.1378	0.0009		2493	5	2501	7	2510	13	2609	15	99
29	150	162	63		0.92	0.0566	0.0018	0.6371	0.0190	0.0816	0.0007	0.0235	0.0003		476	51	500	12	506	4	470	7	99
30	71	107	247		0.66	0.1463	0.0055	8.5822	0.3166	0.4256	0.0061	0.0018	0.0029		2303	44	2295	34	2286	28	37	59	101
31	196	158	30		1.24	0.0502	0.0069	0.1839	0.0250	0.0266	0.0003	0.0075	0.0002		206	270	171	21	169	2	150	5	101
32	109	182	22		0.60	0.0496	0.0034	0.1830	0.0122	0.0268	0.0004	0.0084	0.0002		176	126	171	10	170	2	168	5	101
33	92	155	23		0.59	0.0496	0.0052	0.1496	0.0156	0.0219	0.0002	0.0031	0.0003		178	216	142	14	139	1	62	6	102
34	156	173	114		0.90	0.0675	0.0010	1.3128	0.0157	0.1412	0.0009	0.0415	0.0003		852	15	851	7	851	5	821	6	100
35	203	565	63		0.28	0.1450	0.0024	8.4615	0.1325	0.4233	0.0047	0.1024	0.0008		2288	13	2282	14	2275	21	1970	15	101
36	62	116	273		0.54	0.1643	0.0022	10.6118	0.1073	0.4685	0.0034	0.1276	0.1643		2501	$	2490	9	2477	15	2427	25	101
37	150	272	37		0.55	0.0486	0.0051	0.1500	0.0157	0.0224	0.0003	0.0091	0.0486		127	211	142	14	143	2	183	6	99
38	123	204	31		0.60	0.0485	0.0047	0.1488	0.0142	0.0222	0.0002	0.0087	0.0485		125	196	141	13	142	1	174	7	99
39	100	405	655		0.25	0.1205	0.0016	5.8337	0.0566	0.3511	0.0023	0.1152	0.1205		1964	9	1951	8	1940	11	2203	24	101
40	177	205	77		0.86	0.2654	0.0045	1.8908	0.0255	0.0517	0.0004	0.0423	0.2654		3279	11	1078	9	325	3	838	7	143
41	259	338	281		0.76	0.0749	0.0009	1.8562	0.0167	0.1798	0.0011	0.0533	0.0749		1065	9	1066	6	1066	6	1050	6	100
42	150	400	1308		0.37	0.3034	0.0033	29.1938	0.1925	0.6979	0.0042	0.1781	0.3034		3488	5	3460	6	3413	16	3312	19	102
43	198	227	181		0.87	0.0676	0.0019	1.3088	0.0353	0.1404	0.0010	0.0403	0.0676		858	44	850	16	847	6	799	10	100
44	176	99	293		1.78	0.1795	0.0041	12.5054	0.2738	0.5054	0.0058	0.1301	0.1795		2648	21	2643	21	2637	25	2471	34	100
45	75	507	736		0.145	0.1132	0.0016	5.1941	0.0572	0.3328	0.0023	0.0871	0.1132		1852	10	1852	9	1852	11	1687	31	100
46	85	842	1018		0.10	0.1135	0.0015	5.2125	0.0542	0.3333	0.0024	0.0829	0.1135		1856	9	1855	9	1854	12	1611	109	100
47	109	92	82		1.18	0.2241	0.0032	4.8564	0.0540	0.1572	0.0012	0.08272	0.2241		3010	9	1795	9	941	7	1606	12	137
48	155	289	564		0.54	0.1336	0.0027	7.2298	0.1309	0.3926	0.0037	0.07060	0.1336		2146	19	2140	16	2135	17	1379	29	101
49	255	139	113		1.84	0.0700	0.0011	1.4937	0.0185	0.1549	0.0010	0.04361	0.0700		927	15	928	8	928	6	863	5	100
50	327	194	543		1.68	0.1663	0.0019	11.1392	0.0846	0.4859	0.0030	0.12162	0.1663		2521	6	2535	7	2553	13	2320	12	99
51	46	336	198		0.14	0.0664	0.0019	1.2053	0.0331	0.1317	0.0012	0.04420	0.0664		819	42	803	15	798	7	874	30	101
52	62	116	273		0.54	0.0501	0.0010	0.1549	0.0028	0.0224	0.0001	0.00669	0.0501		200	31	146	2	143	0.9	135	1	102
53	153	583	829		0.26	0.1510	0.0017	5.6001	0.0387	0.2690	0.0016	0.10823	0.00080		2357	5	1916	6	1536	8	2077	15	147
54	95	226	519		0.42	0.1904	0.0022	12.7502	0.0961	0.4858	0.0031	0.19463	0.00146		2746	6	2661	7	2552	13	3594	25	103
55	204	450	696		0.45	0.1290	0.0021	6.5451	0.0922	0.3682	0.0032	0.11391	0.00162		2084	13	2052	12	2021	15	2180	29	101
56	187	872	1241		0.21	0.1208	0.0018	5.8641	0.0698	0.3521	0.0026	0.01662	0.00314		1968	11	1956	10	1945	12	333	62	101
57	272	293	243		0.93	0.0664	0.0015	1.2520	0.0261	0.1368	0.0009	0.03832	0.00036		819	33	824	12	826	5	760	7	100
58	65	128	123		0.51	0.0830	0.0019	2.5038	0.0541	0.2190	0.0017	0.04200	0.00103		1268	30	1273	16	1276	9	832	20	99
59	89	129	281		0.68	0.1401	0.0026	7.9586	0.1347	0.4121	0.0036	0.09047	0.00227		2229	17	2226	15	2224	16	1751	^2	100
60	37	149	161		0.25	0.0882	0.0013	2.8679	0.0324	0.2360	0.0015	0.06395	0.00105		1386	12	1374	8	1366	8	1253	20	101
61	85	400	266		0.21	0.0669	0.0015	1.2815	0.0269	0.1390	0.0010	0.03571	0.00092		834	32	838	12	839	6	709	18	100
62	113	182	439		0.62	0.1686	0.0019	11.0205	0.0735	0.4743	0.0028	0.12940	0.00072		2543	5	2525	6	2502	12	2460	13	102
63	258	276	146		0.93	0.3927	0.0059	3.8195	0.0431	0.0706	0.0006	0.07507	0.00059		3881	8	1597	9	440	4	1463	11	167
64	218	282	534		0.77	0.1350	0.0016	7.3403	0.0557	0.3945	0.0024	0.09912	0.00060		2164	6	2154	7	2144	11	1910	11	101
65	61	182	287	0.33	0.1178	0.0014	5.7077	0.0479	0.3516	0.0022	0.09974	0.00082	1923	7	1933	7	1942	10	1922	15	99
66	56	51	33	1.11	0.0669	0.0023	1.2191	0.0400	0.1323	0.0011	0.04183	0.00042	834	55	809	18	801	6	828	3	101
67	40	379	362	0.11	0.07136	0.0031	1.55796	0.06589	0.15839	0.00141	0.09396	0.00848	968	72	954	26	948	8	1815	157	101
68	52	87	81	0.59	0.16469	0.00289	3.59998	0.05342	0.15858	0.00134	0.09S74	0.0011	2504	14	1550	12	949	7	1903	20	119
69	276	509	53	0.54	0.04907	0.00194	0.15292	0.00582	0.02261	0.00018	0.00742	0.00014	151	74	144	5	144	1	149	3	100
70	197	144	45	1.37	0.0522	0.00326	0.34259	0.02111	0.04762	0.0004	0.01564	0.0002	294	127	299	16	300	2	314	4	100
71	57	310	446	0.18	0.11639	0.00149	5.47014	0.0516	0.34097	0.00222	0.09871	0.00117	1902	8	1896	8	1891	11	1903	22	101
72	103	241	44	0.43	0.04841	0.01218	0.14287	0.03587	0.02141	0.00034	0.00964	0.001	119	411	136	32	137	2	194	20	99
73	77	158	16	0.48	0.04949	0.00297	0.15368	0.00898	0.02253	0.00028	0.00721	0.00021	171	110	145	8	144	2	145	4	101
74	162	317	361	0.51	0.46979	0.0059	5.94982	0.05013	0.09188	0.00065	0.20098	0.00132	4149	6	1969	7	567	4	3702	22	165
75	115	183	245	0.63	0.2557	0.00323	6.62758	0.05893	0.18804	0.00128	0.18141	0.00123	3220	7	2063	8	1111	7	3370	21	118
76	107	439	634	0.24	0.11361	0.00151	5.30494	0.05363	0.33877	0.00226	0.07789	0.00098	1858	9	1870	9	1881	11	1516	18	99
77	123	405	252	0.30	0.06656	0.00131	1.29938	0.02258	0.14163	0.00104	0.04054	0.0006	824	24	845	10	854	6	803	12	99
78	714	327	869	2.19	0.16536	0.00315	10.91654	0.19558	0.47894	0.00538	0.10259	0.00092	2511	16	2516	17	2523	23	1974	17	100
79	134	1111	1977	0.12	0.12644	0.00217	6.51166	0.0975	0.37363	0.00313	0.00185	0.00211	2049	15	2047	13	2046	15	37	上3	100
80	159	375	81	0.42	0.21516	0.00356	0.89397	0.01176	0.03014	0.00023	0.03551	0.00031	2945	12	648	6	191	1	705	6	135

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