张广才岭福兴屯组的形成时代、物源及构造背景

何雨思; 高福红; 修铭; 许文良

doi:10.3799/dqkx.2019.145

张广才岭福兴屯组的形成时代、物源及构造背景

doi: 10.3799/dqkx.2019.145

吉林大学地球科学学院, 吉林长春 130061

基金项目:

国家自然科学基金项目 41272075

详细信息

作者简介:
何雨思(1993—), 女, 硕士研究生, 主要从事岩石学方面研究

通讯作者:
高福红(1963—)

中图分类号: P588
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出版历程
- 收稿日期: 2019-06-13
- 刊出日期: 2019-11-11

Age, Provenance and Tectonic Setting of Fuxingtun Formation in Zhangguangcai Range

College of Earth Sciences, Jilin University, Changchun 130061, China

摘要

摘要: 前人对张广才岭福兴屯组研究程度较低，限制了对区域古生代构造演化的认识.福兴屯组凝灰岩锆石30个测点加权平均年龄为392±3 Ma，砂岩碎屑锆石最小一组年龄为393 Ma，指示福兴屯组形成于中泥盆世.Al₂O₃/TiO₂平均值为19.58，稀土元素球粒陨石标准化曲线具有轻稀土富集、重稀土稳定和负Eu异常特征，结合碎屑锆石年龄峰值，确定福兴屯组物源主要为晚古生代中酸性火成岩和早古生代花岗质岩.地球化学和区域火山岩特征共同揭示福兴屯组形成于伸展构造环境.松嫩-张广才岭地块和佳木斯地块晚古生代早期地层均广泛分布有489~551 Ma的碎屑锆石，暗示两地块在福兴屯组沉积之前已完成拼合，为两地块于早古生代晚期拼合提供了新的证据.
- 张广才岭 /
- 福兴屯组 /
- U-Pb年代学 /
- 地球化学 /
- 物源 /
- 构造背景 /
- 岩石学
Abstract: Previous studies on the Fuxingtun Formation in Zhangguangcai Range are relatively inadequate, which has limited the understanding of regional Paleozoic tectonic evolution. The weighted average age of zircons from tuff of 30 test points in the Fuxingtun Formation is 392±3 Ma, and the minimum age of detrital zircons from arkose is 393 Ma, indicating that the Fuxingtun Formation was formed in the Middle Devonian. Al₂O₃/TiO₂ average value is 19.58, and chondrite-normalized REE patterns have the characteristics of enrichment in light rare earth, stability in heavy rare earth and negative Eu anomaly, which, combined with detrital zircons age populations, indicates that the provenance of the Fuxingtun Formation was mainly derived from the Late Paleozoic intermediate-acid igneous rocks and the Early Paleozoic granitic rocks. The geochemical and regional volcanic characteristics reveal that the Fuxingtun Formation was formed in extensional environment. 489-551 Ma detrital zircons are widely distributed in the Late Paleozoic early strata in Songnen-Zhangguangcai Range massif and Jiamusi massif, suggesting that the two blocks had been combined before the deposition of the Fuxingtun Formation, which provides a new evidence for the combination of the two blocks in the late Early Paleozoic.
- Zhangguangcai Range /
- Fuxingtun Formation /
- U-Pb chronology /
- geochemistry /
- provenance /
- tectonic setting /
- petrology

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图 1 研究区地质简图

Fig. 1. Geological sketch map of the study area

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图 2 福兴屯组岩性柱状图及采样位置

Fig. 2. Column diagram of the Fuxingtun Formation showing lithology and sampling locations

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图 3 福兴屯组野外露头和样品显微照片

Qz.石英；Pl.长石

Fig. 3. Outcrop photographs and photomicrographs of samples from the Fuxingtun Formation

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图 4 福兴屯组锆石样品中典型阴极发光图像

Fig. 4. CL images of the selected typical zircons from the Fuxingtun Formation

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图 5 福兴屯组流纹质晶屑凝灰岩锆石LA-ICP-MS U-Pb年龄谐和图

Fig. 5. U-Pb concordia diagram summarizing the LA-ICP-MS zircon data for the rhyolitic crystalline tuff in the Fuxingtun Formation

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图 6 福兴屯组细粒长石砂岩碎屑锆石LA-ICP-MS U-Pb年龄谐和图

Fig. 6. U-Pb concordia diagrams summarizing the LA-ICP-MS detrital zircon data for the fine-grained arkose in the Fuxingtun Formation

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图 7 福兴屯组风化特征图解

Fig. 7. The characteristics of weathering for the Fuxingtun Formation

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图 8 福兴屯组沉积岩稀土元素PAAS和球粒陨石标准化曲线

Fig. 8. PAAS-normalized and chondrite-normalized REE patterns of sedimentary rocks from the Fuxingtun Formation

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图 9 福兴屯组沉积岩物源区判别图解

Fig. 9. Provenance discrimination diagrams of sedimentary rocks from the Fuxingtun Formation

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图 10 福兴屯组碎屑锆石U-Pb年龄频率

Fig. 10. Relative probability of detrital zircons from the Fuxingtun Formation

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图 11 福兴屯组沉积岩构造环境判别图

PM.被动大陆边缘；ACM.活动大陆边缘；ARC.岛弧；A1.岛弧；A2.演化岛弧

Fig. 11. Tectonic setting discriminate diagrams of sedimentary rocks from the Fuxingtun Formation

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图 12 福兴屯沉积岩和不同构造环境砂岩稀土元素PAAS和球粒陨石标准化曲线

Fig. 12. PAAS-normalized and chondrite-normalized REE patterns of sedimentary rocks from the Fuxingtun Formation and sandstones from various tectonic settings

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表 1 福兴屯组沉积岩主量（%）和微量元素（10^-6）分析结果

Table 1. Major and trace element compositions of the sedimentary rocks from the Fuxingtun Formation

样品号	14HYS-1-1	14HYS-1-2	14HYS-1-3	14HYS-1-4	14HYS-1-5	14HYS-1-6	14HYS-1-7	14HYS-1-8	14HYS-1-9	14HYS-1-10
Fe₂O₃	2.91	1.66	2.56	2.53	0.85	2.59	1.74	3.41	2.46	2.06
FeO	2.80	4.15	3.18	3.47	4.92	4.18	4.31	3.18	4.38	4.43
TFe₂O₃	6.02	6.27	6.09	6.39	6.32	7.23	6.53	6.94	7.33	6.98
MnO	0.12	0.12	0.11	0.10	0.10	0.13	0.11	0.12	0.13	0.20
TiO₂	0.70	0.86	0.79	0.74	0.74	0.81	0.76	0.70	0.84	1.32
CaO	1.86	1.70	1.47	1.74	1.58	1.51	1.55	1.74	1.64	1.67
K₂O	1.87	2.04	1.66	1.73	2.53	1.95	1.96	1.47	2.18	1.56
P₂O₅	0.22	0.22	0.22	0.21	0.19	0.21	0.22	0.22	0.23	0.29
SiO₂	64.22	64.94	65.04	63.38	63.53	61.02	64.56	62.66	62.56	62.90
Al₂O₃	15.33	15.18	15.28	15.48	16.28	16.52	15.33	16.04	15.74	15.49
MgO	2.36	2.66	2.17	2.51	2.28	2.82	2.51	2.29	2.77	2.66
Na₂O	4.64	4.73	4.96	4.84	4.82	5.49	4.80	4.58	4.45	5.18
LOI	2.86	1.60	2.36	2.34	1.35	2.28	1.64	3.06	2.05	1.78
Total	99.89	99.86	99.80	99.07	99.16	99.51	99.49	99.47	99.43	99.54
Al₂O₃/TiO₂	21.90	17.65	19.34	20.92	22.00	20.40	20.17	22.91	18.74	11.73
CIA	54.04	53.72	54.75	54.36	54.59	54.33	54.43	56.62	55.42	53.90
ICV	1.43	1.46	1.37	1.42	1.29	1.45	1.40	1.33	1.43	1.50
PIA	54.71	54.40	55.45	55.02	55.63	55.03	55.21	57.46	56.50	54.42
Sc	13.20	14.30	13.50	13.40	15.60	16.40	14.00	14.20	14.20	17.30
V	108.00	117.00	108.00	112.00	102.00	128.00	117.00	116.00	125.00	149.00
Cr	77.40	106.00	87.40	80.00	53.60	95.60	86.60	86.10	106.00	185.00
Co	16.30	16.20	15.00	16.80	10.70	21.70	15.10	19.60	19.90	14.60
Ni	33.30	37.70	32.40	40.40	27.60	46.60	41.20	40.10	41.10	39.10
Rb	41.10	50.60	32.20	35.50	74.20	52.70	39.70	37.00	46.60	31.20
Sr	244.00	246.00	226.00	259.00	198.00	290.00	245.00	268.00	251.00	204.00
Y	20.30	23.10	18.90	20.90	27.50	29.20	19.50	23.60	22.00	21.30
Zr	171.00	189.00	187.00	167.00	203.00	228.00	190.00	209.00	216.00	260.00
Hf	5.69	5.32	5.12	5.12	6.16	7.19	5.27	6.68	7.12	7.60
Th	6.36	5.24	4.11	4.64	8.54	9.04	4.85	6.05	5.40	3.66
U	1.37	1.33	1.22	1.30	1.65	2.05	1.36	1.63	1.51	1.59
Th/U	4.64	3.94	3.37	3.57	5.18	4.41	3.57	3.71	3.58	2.30
Rb/Sr	0.17	0.21	0.14	0.14	0.37	0.18	0.16	0.14	0.19	0.15
La	23.30	27.60	21.40	22.60	24.30	30.10	23.70	26.10	30.10	23.90
Ce	47.50	57.20	44.80	45.80	50.80	66.40	51.30	53.20	60.70	48.90
Pr	5.99	6.35	5.62	5.61	6.18	7.68	5.83	6.30	7.30	6.07
Nd	24.50	28.70	22.80	24.90	26.80	34.90	25.50	27.10	30.20	26.60
Sm	4.94	5.19	4.40	4.97	5.57	6.81	4.91	5.21	5.96	5.33
Eu	1.25	1.35	1.09	1.26	1.18	1.60	1.22	1.31	1.34	1.43
Gd	4.11	4.57	3.96	4.24	4.53	5.81	3.90	4.52	4.93	4.56
Tb	0.69	0.72	0.67	0.66	0.79	0.94	0.65	0.77	0.74	0.74
Dy	4.26	4.07	3.89	4.02	4.86	5.62	4.00	4.50	4.21	4.34
Ho	0.75	0.82	0.77	0.78	0.97	1.03	0.77	0.90	0.81	0.83
Er	2.15	2.15	1.94	2.27	2.91	3.13	2.14	2.48	2.28	2.20
Tm	0.35	0.32	0.29	0.36	0.46	0.45	0.31	0.37	0.34	0.30
Yb	2.08	1.97	1.74	1.96	2.97	2.65	1.97	2.22	2.08	1.90
Lu	0.36	0.37	0.34	0.36	0.50	0.50	0.34	0.41	0.39	0.34
∑REE	122.23	141.38	113.71	119.79	132.82	167.62	126.54	135.39	151.38	127.44
∑LREE	107.48	126.39	100.11	105.14	114.83	147.49	112.46	119.22	135.60	112.23
∑HREE	14.75	14.99	13.60	14.65	17.99	20.13	14.08	16.17	15.78	15.21
L/H	7.29	8.43	7.36	7.18	6.38	7.33	7.99	7.37	8.59	7.38
La/Yb	11.20	14.01	12.30	11.53	8.18	11.36	12.03	11.76	14.47	12.58
（La/Yb）_N	7.55	9.45	8.29	7.77	5.52	7.66	8.11	7.93	9.76	8.48
（Gd/Yb）_N	1.59	1.87	1.84	1.75	1.23	1.77	1.60	1.64	1.91	1.94
δEu	0.83	0.83	0.78	0.82	0.70	0.76	0.83	0.81	0.74	0.87
δCe	0.95	1.00	0.96	0.95	0.97	1.03	1.02	0.97	0.96	0.95
注：TFe₂O₃=Fe₂O₃+1.111FeO；化学蚀变指数(CIA)=[Al₂O₃/(Al₂O₃+CaO+Na₂O+K₂O)]×100，成分变异指数(ICV)=(Fe₂O₃+K₂O+Na₂O+CaO+MgO+MnO+TiO₂)/Al₂O₃，斜长石风化程度指数(PIA)=[(Al₂O₃－K₂O)/(Al₂O₃+CaO+Na₂O－K₂O)]×100，以上式子中的主要成分指摩尔分数，CaO为碳酸盐中的CaO，即全岩中的CaO扣除掉化学沉积的CaO的摩尔分数（McLennan，1993）；∑REE不包括Sc和Y元素；L/H=∑LREE/∑HREE；N代表球粒陨石标准化值；δEu=2Eu _N/（Sm _N / Gd _N）；δCe=2Ce _N/(La _N /Pr _N).

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表 2 福兴屯组沉积岩与不同构造背景砂岩稀土元素特征比较

Table 2. Geochemical comparison between sedimentary rocks from the Fuxingtun Formation and sandstones from various tectonic settings

构造背景	La(10^-6)	Ce(10^-6)	∑REE(10^-6)	La/Yb	(La/Yb)_N	L/H	δEu
大洋岛弧	8.00±1.70	19.00±3.70	58.00±10.00	4.20±1.30	2.80±0.90	3.80±0.90	1.04±0.11
大陆岛弧	27.00±4.50	59.00±8.20	146.00±20.00	11.00±3.60	7.50±2.50	7.70±1.70	0.79±0.13
活动大陆边缘	37.00	78.00	186.00	12.50	8.50	9.10	0.60
被动大陆边缘	39.00	85.00	210.00	15.90	10.80	8.50	0.56
样品（平均值）	25.31	52.66	133.83	11.94	8.05	7.53	0.80
注：大洋岛弧、大陆岛弧、活动大陆边缘和被动大陆边缘数据据Bhatia(1985).

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