新疆西准噶尔早石炭世沉积地层的物源及构造环境

廖婉琳; 肖龙; 张雷; 王国灿

doi:10.3799/dqkx.2015.039

新疆西准噶尔早石炭世沉积地层的物源及构造环境

doi: 10.3799/dqkx.2015.039

廖婉琳^1,,
肖龙^1, ,,
张雷^{1, 2},
王国灿^{1, 3}

1.
中国地质大学地球科学学院，湖北武汉 430074
2.
湖北省地质矿业开发有限责任公司，湖北武汉 430022
3.
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

基金项目:

中国地质调查局项目“西准噶尔克拉玛依后山地区三维地质调查试点” 1212011220245

新疆1∶25万铁厂沟镇幅(L45C002001)与克拉玛依市幅(L45C003001)区调修测项目 1212011120502

详细信息

作者简介:
廖婉琳(1989-)，女，在读硕士，矿物学、岩石学及矿床学专业.E-mail: 369353892@qq.com

通讯作者:
肖龙，E-mail: longxiao@cug.edu.cn

中图分类号: P59
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出版历程
- 收稿日期: 2014-05-07
- 刊出日期: 2015-03-15

Provenance and Tectonic Settings of Early Carboniferous Sedimentary Strata in Western Junggar, Xinjiang

Liao Wanlin^1
,,
Xiao Long^{1
, ,},
Zhang Lei^{1, 2},
Wang Guocan^{1, 3}

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Hubei Geological and Mining Exploration Limited Liability Company, Wuhan 430022, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 沉积物的地球化学和碎屑锆石特征在沉积岩物源分析及构造背景的研究中具有较为重要的作用.对克拉玛依后山地区早石炭世包古图组和太勒古拉组碎屑岩样品(共42个)进行了岩石学和地球化学研究，结果显示，这套碎屑岩的主量元素SiO₂含量为54.64%~73.14%，Al₂O₃含量相对较高(11.89%~19.36%)，(TFe₂O₃+MgO)含量比较高(3.97%~9.99%)，反映岩石化学成熟度偏低.岩石稀土元素含量变化较大，在83×10^-6~252×10^-6之间变化，无Ce异常，Eu呈微弱负异常，具有低的∑REE等特征，与大洋岛弧型砂岩相似.采自这2个组的碎屑锆石U-Pb定年结果表明，包古图组有340 Ma和440 Ma两个主峰值，主要来源于石炭纪、志留纪的源岩；太勒古拉组碎屑锆石主峰值为325 Ma，其年龄与地层年龄很接近，推测其主要来源于同沉积石炭纪岩石.根据主、微量及稀土元素等多个构造环境判别图解的综合分析，结果表明早石炭世包古图组和太勒古拉组沉积物的物源特征及沉积构造背景较为相似，主要为大洋岛弧-大陆岛弧环境下的中酸性火山岩，夹有少量基性火山岩.
- 西准噶尔 /
- 早石炭世 /
- 沉积岩地球化学特征 /
- 构造环境
Abstract: The geochemistry and detrital zircon characteristics of the sediments play an important role in the study of sedimentary provenance and their tectonic settings. This paper presents petrography and geochemical study of the Early Carboniferous Baogutu Group and Tailegula Group clastic rocks in Karamay area, western Junggar, NW Xinjiang. Geochemical data show that the sedimentary rocks have SiO₂ contents (54.64%-73.14%), relatively high Al₂O₃ contents (11.89%-19.36%) and high (TFe₂O₃+MgO) contents (3.97%-9.99%), indicating low chemical maturity. Their total rare earth element contents vary between 83×10^-6 and 252×10^-6, characterized by no Ce anomaly and slightly negative Eu anomalies, which is similar to those of sandstones formed at oceanic island arc setting. U-Pb dating results of detrital zircons show that Baogutu Group has 340 and 440 Ma two peak values. Detrital zircons of Tailegula Group show only one peak (325 Ma) and suggests that they were sourced from the Early Carboniferous rocks. Discrimination diagrams of the major and trace elements show that the provenance and tectonic settings of Early Carboniferous Baogutu and Tailegula groups sedimentary rocks were formed from the oceanic island arc and continental island arc acidic volcanic rocks, with minor mafic volcanic rocks.
- western Junggur /
- Early Carboniferous /
- geochemistry of sedimentary rock /
- tectonic setting

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图 1 中亚造山带构造分区(a)和研究区地质简图(b)及采样点、剖面位置(实测)

图a据Yang et al.(2012)修改

Fig. 1. Simplified tectonic divisions of the Central Asian orogenic belt (a) and geological map of the study area (b) (sampling profiles and locations are marked)

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图 2 克拉玛依后山地区包古图组(a, b)和太勒古拉组(c, d)碎屑岩野外地质特征

Fig. 2. Field geological characteristics of the Baogutu Group (a, b) and Tailegula Group (c, d) from Karamay area

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图 3 克拉玛依后山地区包古图组(a~d)和太勒古拉组(e~h)碎屑岩镜下特征

a、e.微层理构造; b、f.细粒碎屑结构; c、d、g、h.岩石中的岩屑和晶屑; Lv.火山岩岩屑; Ls.沉积岩岩屑; Q.石英; Px.辉石; Am.角闪石(F为正交偏光，其余为单偏光)

Fig. 3. Photomicrograph characteristics of the Baogutu Group (a~d) and Tailegula Group (e~h) from Karamay area

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图 4 克拉玛依后山地区包古图组(a)和太勒古拉组(b)代表碎屑锆石阴极发光图象及分析点表面年龄

Fig. 4. Representative CL images (a) and of detrital zircon from the clastic rock in Karamay area(b)

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图 5 克拉玛依后山地区包古图组(a)和太勒古拉组(b)碎屑锆石和谐曲线

Fig. 5. Concordia plots of detrital zircon of Baogutu Gaogutu (a) and Tailegula Group (b) form Karamny area

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图 6 克拉玛依后山地区包古图组(a)和太勒古拉组(b)碎屑锆石U-Pb谐和年龄频数直方图

Fig. 6. Detrital zircon U-Pb Age distribution histograms of Baogutu Group (a) and Tailegula Group (b) from Karamay area

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图 7 克拉玛依后山地区碎屑岩主要元素与SiO₂关系

Fig. 7. Bivariate diagrams of major elements composition of the clastic rocks from Karamay area

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图 8 碎屑岩微量元素蛛网图和稀土元素球粒陨石标准化与构造背景砂岩对比

a.碎屑岩微量元素蛛网图; b.稀土元素球粒陨石标准化，典型构造背景稀土元素数据来自Bhatia(1985)

Fig. 8. Primitive mantle-normalized spider diagrams of clastic rocks and Chondrite-normalized REE patterns and sandstone from other typical tectonic setting

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图 9 A-CN-K图

各端元为各元素摩尔百分比，据Nesbitt and Young(1982)，Fedo et al.(1995)

Fig. 9. A-CN-K Ternary diagram

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图 10 碎屑岩主量元素与微量元素源区判别

a.碎屑砂岩方程F1对F2物源性质判别图解; P1.基性火山岩源区; P2.中性岩火山岩源区; P3.酸性火山岩源区; P4.成熟大陆石英质源区，计算方法见Roser and Korsch(1988); b.微量元素La/Sc vs Co/Th物源性质判别(Gu et al., 2002)

Fig. 10. Discrimination diagram illustrating sedimentary provenance

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图 11 克拉玛依后山石炭纪包古图组和太勒古拉组碎屑岩构造环境判别

a.TFe₂O₃+MgO-TiO₂判别(Bathia, 1983); b.La-Th图解; c.Th-Sc-Zr/10三角图解; d.La-Th-Sc三角图解(Bathia, 1986)

Fig. 11. Tectonic setting diagrams using major and trace elements

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表 1 克拉玛依后山地区碎屑岩主量元素分析结果

Table 1. Major element compositions of the clastic rocks in Karamay area

组名	样品号	检测项目(%)													CIA
组名	样品号	SiO₂	TiO₂	Al₂O₃	TFe₂O₃	MnO	MgO	CaO	Na₂O	K₂O	P₂O₅	H₂O⁺	CO₂	烧失量	CIA
包古图组	PM003-9-1(b)	66.13	0.65	15.34	3.74	0.08	1.48	1.89	4.25	3.92	0.17	1.80	0.22	1.94	53.19
	PM003-28-1(b)	65.20	0.74	14.46	4.53	0.11	1.40	3.79	3.98	2.74	0.28	2.01	0.34	2.24	49.84
	PM003-67-1(b)	63.76	0.74	15.05	4.40	0.11	1.60	2.83	2.68	5.89	0.24	2.06	0.22	2.11	50.78
	PM003-74-1(b)	55.14	0.79	16.90	6.41	0.14	2.36	6.14	3.65	3.16	0.29	2.55	1.97	4.22	56.43
	PM004-2-2(b)	61.11	0.71	16.35	4.50	0.10	1.66	4.10	2.78	4.28	0.27	2.29	1.35	3.28	59.08
	PM004-3-1(b)	60.48	0.70	17.30	4.81	0.11	1.92	4.21	3.49	3.48	0.26	2.15	0.62	2.40	54.60
	PM004-16-1(b)	57.82	0.74	17.49	5.83	0.11	2.68	5.73	3.24	2.64	0.26	2.86	0.18	2.77	50.19
	PM004-31-1(b)	56.22	0.86	18.39	6.23	0.13	2.66	4.85	3.91	3.09	0.20	2.77	0.22	2.73	51.45
	PM004-42-1(b)	71.09	0.58	12.56	3.57	0.11	1.29	1.65	3.47	2.78	0.21	1.80	0.45	2.31	56.55
	PM004-44-1(b)	73.14	0.52	11.89	2.94	0.08	1.11	1.30	2.29	4.64	0.14	1.56	0.07	1.37	52.93
	PM004-59-1(b)	70.12	0.63	13.66	3.66	0.10	1.24	1.28	4.31	2.38	0.20	1.87	0.11	1.95	55.10
	KP4-35-1	69.62	0.54	13.47	2.91	0.03	1.27	2.27	3.03	2.90	0.20	1.98	1.35	3.26	65.55
	KP4-72-1	60.15	0.80	16.82	5.61	0.04	2.74	1.79	1.94	4.84	0.14	3.40	1.01	4.68	68.21
	H7913-1	64.66	0.74	15.72	4.01	0.11	1.48	2.26	3.35	5.01	0.23	1.69	0.13	1.73	52.82
	H7913-2	65.03	0.58	15.95	3.51	0.09	1.43	2.31	2.67	5.54	0.28	1.88	0.10	1.88	54.03
	H7913-3	72.42	0.49	12.73	3.51	0.09	1.24	1.16	4.58	1.36	0.10	1.75	0.21	2.09	55.65
	b5010-1	60.53	0.89	18.08	5.64	0.04	2.61	0.40	3.61	4.04	0.15	3.23	0.07	3.42	63.40
太勒古拉组	PM002-33-1(b)	63.60	0.89	15.12	6.07	0.11	2.13	2.32	5.06	1.72	0.18	2.31	0.16	2.26	51.12
	PM002-39-1(b)	60.82	0.89	14.81	6.36	0.13	2.57	4.48	3.39	2.63	0.20	2.35	1.01	2.94	54.45
	PM002-41-1(b)	60.94	0.95	14.85	6.61	0.13	2.43	5.12	5.00	0.55	0.23	2.45	0.39	2.54	58.09
	PM002-63-1(b)	63.33	0.61	16.53	3.95	0.07	1.54	2.66	5.00	2.76	0.16	2.20	0.84	2.89	60.50
	PM006-17-1(b)	55.79	0.80	18.28	6.41	0.11	2.87	5.68	3.86	2.36	0.18	2.80	0.38	2.85	51.93
	PM006-19-1(b)	54.64	0.85	19.36	5.74	0.10	2.61	5.60	3.80	2.94	0.21	2.84	0.84	3.20	54.40
	PM006-37-1(b)	71.76	0.58	12.29	3.63	0.08	1.24	1.43	2.33	3.81	0.14	1.90	0.39	2.39	52.80
	PM006-47-1(b)	58.16	0.73	17.58	5.13	0.10	2.00	5.16	2.99	3.34	0.25	2.50	1.68	3.84	54.05
	KP4-14-1	61.29	0.66	16.41	5.40	0.09	2.45	3.50	3.49	3.74	0.14	2.26	0.18	1.92	52.16
	KP4-18-1	57.59	0.86	17.03	6.71	0.12	2.43	3.63	3.25	4.39	0.33	2.74	0.47	2.78	50.74
	KP4-19-1	62.44	0.71	16.50	5.19	0.09	1.53	4.30	2.20	3.79	0.17	2.59	0.11	2.57	64.54
	KP4-22-1	56.34	0.93	17.91	7.22	0.13	2.77	3.15	3.88	4.07	0.35	2.70	0.13	2.23	52.98
	KP4-24-1	56.95	0.82	17.41	6.59	0.10	2.72	3.19	3.64	5.06	0.31	2.59	0.16	2.17	54.07
	KP4-24-2	57.00	0.79	17.50	6.48	0.10	2.86	3.54	5.72	2.54	0.28	2.50	0.27	2.25	47.79
	KP4-71-1	68.84	0.72	12.10	2.84	0.09	1.13	3.88	3.53	2.50	0.14	1.52	2.47	3.93	56.46
	H7911-1	61.48	0.82	16.19	5.67	0.09	2.15	3.17	3.62	2.99	0.32	2.71	0.19	2.89	54.48
	H7914-1	58.39	0.72	18.18	5.45	0.08	2.55	5.69	4.12	1.79	0.24	2.05	0.15	1.92	50.30
	H7914-2	57.40	0.78	16.98	6.12	0.11	2.66	6.16	4.43	2.09	0.23	1.98	0.54	2.15	48.10
	H7915-1	60.54	0.74	19.32	4.13	0.11	1.30	1.34	8.18	1.70	0.29	1.82	0.10	1.80	53.65
	H7915-2	69.49	0.42	15.73	2.42	0.08	0.82	0.97	8.21	0.10	0.13	1.16	0.23	1.23	52.44
	H7915-3	56.94	0.73	18.70	5.44	0.09	2.40	4.91	4.24	2.86	0.22	2.31	0.59	2.63	53.25
	H7915-4	70.59	0.49	14.12	3.22	0.08	0.93	0.96	4.19	3.02	0.12	1.70	0.19	2.22	56.30
	H7916-1	67.39	0.58	15.46	4.54	0.09	1.12	1.11	5.34	1.67	0.12	1.87	0.25	1.94	57.44
	H7916-2	74.42	0.46	12.98	2.40	0.05	0.82	0.51	6.52	0.09	0.10	1.26	0.13	1.43	54.00
	H7916-3	67.61	0.53	13.87	3.66	0.07	1.14	2.81	2.61	2.42	0.12	2.66	2.04	4.80	74.91
注：TFe₂O₃代表全铁，TFeO=FeO+0.899 8×Fe₂O₃.

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表 2 克拉玛依后山地区碎屑岩稀土元素分析结果

Table 2. Rare element compositions of the clastic rocks in Karamay area

组名	样品号	检测项目(10^-6)															总和
组名	样品号	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu	Y
包古图组	PM003-9-1(b)	20.29	45.27	5.70	22.14	4.77	1.23	4.45	0.68	4.23	0.86	2.44	0.37	2.57	0.42	23.52	138.92
	PM003-28-1(b)	18.25	41.82	5.38	21.59	4.66	1.27	4.34	0.68	4.05	0.78	2.26	0.33	2.31	0.35	20.94	129.01
	PM003-67-1(b)	20.31	46.71	6.02	23.73	4.99	1.29	4.42	0.71	4.40	0.86	2.47	0.39	2.57	0.42	22.67	141.95
	PM003-74-1(b)	15.31	31.99	4.33	17.43	3.66	1.23	3.47	0.52	3.06	0.62	1.74	0.27	1.81	0.29	16.36	102.10
	PM004-2-2(b)	16.02	32.66	4.47	17.96	3.79	1.12	3.49	0.55	3.19	0.64	1.79	0.28	1.86	0.30	17.51	105.61
	PM004-3-1(b)	14.31	31.22	4.16	16.53	3.65	1.12	3.16	0.48	2.90	0.59	1.63	0.26	1.69	0.28	15.27	97.25
	PM004-16-1(b)	14.34	30.55	3.97	16.03	3.46	1.15	3.02	0.48	2.88	0.57	1.61	0.25	1.70	0.27	14.83	95.10
	PM004-31-1(b)	13.43	29.65	3.92	15.66	3.33	1.09	2.90	0.46	2.73	0.51	1.48	0.23	1.53	0.24	13.80	90.97
	PM004-42-1(b)	15.06	33.76	4.28	16.48	3.61	1.04	3.49	0.61	3.72	0.75	2.25	0.36	2.40	0.38	19.85	108.03
	PM004-44-1(b)	19.21	42.48	5.30	20.36	4.18	1.05	3.93	0.64	3.84	0.76	2.19	0.33	2.31	0.35	20.44	127.37
	PM004-59-1(b)	19.76	44.25	5.58	21.95	4.67	1.18	4.46	0.74	4.70	0.94	2.83	0.45	3.05	0.50	25.93	140.97
	KP4-35-1	16.20	33.72	4.38	16.99	3.71	0.90	3.45	0.58	3.55	0.71	2.04	0.31	2.16	0.34	20.23	109.26
	KP4-72-1	19.72	44.88	5.68	22.61	4.92	1.40	4.73	0.78	4.58	0.92	2.69	0.41	2.77	0.44	24.40	140.93
	H7913-1	20.80	47.32	5.98	25.23	5.94	1.65	5.50	0.87	5.66	1.06	3.20	0.50	3.27	0.51	31.40	158.87
	H7913-2	25.29	53.33	6.37	25.33	5.20	1.26	4.35	0.63	3.88	0.72	2.25	0.35	2.32	0.36	22.16	153.78
	H7913-3	15.88	33.82	3.89	15.58	3.37	0.82	3.10	0.54	3.28	0.66	1.96	0.28	2.08	0.31	19.50	105.08
	b5010-1	20.28	45.30	5.87	22.68	4.86	1.52	4.66	0.76	4.88	0.94	2.75	0.42	2.87	0.46	24.82	143.07
太勒古拉组	PM002-33-1(b)	10.93	25.00	3.52	14.74	3.71	1.22	3.94	0.69	4.29	0.87	2.52	0.38	2.57	0.42	23.32	98.12
	PM002-39-1(b)	9.00	20.85	2.99	13.34	3.38	1.25	3.71	0.63	3.99	0.81	2.36	0.36	2.43	0.38	21.95	87.43
	PM002-41-1(b)	10.11	23.64	3.47	15.35	3.98	1.30	4.41	0.79	5.00	1.01	2.89	0.44	2.91	0.47	26.80	102.57
	PM002-63-1(b)	19.15	42.31	5.57	21.38	4.49	1.19	4.24	0.70	4.41	0.88	2.52	0.40	2.73	0.43	23.71	134.11
	PM006-17-1(b)	12.57	26.55	3.52	14.31	3.10	1.14	2.85	0.44	2.49	0.48	1.42	0.21	1.41	0.22	12.91	83.63
	PM006-19-1(b)	14.02	30.05	3.92	15.80	3.37	1.23	3.01	0.46	2.68	0.52	1.50	0.23	1.56	0.24	13.68	92.28
	PM006-37-1(b)	13.60	30.98	4.01	15.62	3.39	0.91	3.23	0.52	3.21	0.62	1.77	0.29	1.91	0.31	16.99	97.34
	PM006-47-1(b)	14.43	30.59	4.10	16.42	3.39	1.11	3.03	0.50	2.93	0.58	1.63	0.26	1.78	0.28	15.75	96.78
	KP4-14-1	13.25	29.56	3.87	14.73	3.13	1.01	2.76	0.44	2.62	0.51	1.51	0.23	1.60	0.25	13.25	88.72
	KP4-18-1	16.86	36.86	5.15	21.04	4.67	1.40	4.13	0.68	3.81	0.75	2.05	0.30	2.06	0.32	20.27	120.35
	KP4-19-1	18.04	42.11	5.46	21.16	4.49	1.20	4.08	0.66	4.06	0.80	2.36	0.37	2.52	0.38	20.93	128.61
	KP4-22-1	17.59	39.94	5.32	21.95	4.53	1.32	4.07	0.60	3.44	0.66	1.85	0.28	1.85	0.29	17.54	121.23
	KP4-24-1	15.31	35.52	4.77	19.73	4.13	1.12	3.68	0.53	3.16	0.60	1.70	0.26	1.69	0.27	15.68	108.14
	KP4-24-2	16.40	35.83	4.69	19.09	4.08	1.23	3.60	0.53	3.07	0.60	1.71	0.25	1.69	0.26	15.74	108.77
	KP4-71-1	11.51	24.59	3.34	13.28	3.03	1.00	2.89	0.49	3.08	0.61	1.73	0.27	1.89	0.30	16.27	84.27
	H7911-1	19.51	42.49	5.22	21.75	4.65	1.22	4.00	0.70	4.27	0.82	2.42	0.35	2.56	0.40	23.68	134.04
	H7914-1	17.94	35.77	4.33	17.71	3.90	1.29	3.41	0.48	2.79	0.52	1.57	0.20	1.46	0.23	15.22	106.82
	H7914-2	16.75	34.24	4.45	18.17	4.12	1.24	3.41	0.47	2.66	0.54	1.59	0.22	1.44	0.22	15.50	105.03
	H7915-1	38.95	93.29	11.66	46.45	8.02	1.74	6.28	0.88	5.23	1.01	3.00	0.44	3.21	0.48	31.18	251.83
	H7915-2	19.16	45.81	5.60	22.28	4.68	0.92	3.88	0.60	3.64	0.74	2.30	0.33	2.52	0.38	21.98	134.82
	H7915-3	15.88	32.79	4.12	16.74	3.55	1.19	3.15	0.48	2.81	0.61	1.69	0.24	1.66	0.25	17.04	102.21
	H7915-4	18.62	40.58	4.84	19.38	4.29	1.02	4.02	0.63	3.92	0.82	2.48	0.39	2.50	0.40	23.39	127.30
	H7916-1	7.88	19.28	2.67	11.87	3.22	1.05	3.24	0.55	3.81	0.83	2.46	0.39	2.54	0.40	23.14	83.33
	H7916-2	13.52	31.22	4.06	16.82	3.81	0.87	4.02	0.72	4.79	1.07	3.17	0.50	3.31	0.52	30.77	119.15
	H7916-3	14.34	32.94	4.48	19.06	4.99	1.17	5.22	0.91	5.97	1.23	3.79	0.56	3.65	0.57	34.78	133.66

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表 3 克拉玛依后山地区碎屑岩微量元素分析结果

Table 3. Trace element compositions of the clastic rocks in Karamay area

组名	样品号	检测项目(10^-6)
组名	样品号	Rb	Th	Ta	Nb	Sr	Zr	Hf	Sc	Cr	V	Co	Zn
包古图组	PM003-9-1(b)	45.61	6.10	0.59	6.75	381.55	186.40	4.78	12.19	20.73	76.30	7.24	74.88
	PM003-28-1(b)	45.10	6.14	0.66	6.83	557.60	165.70	4.41	13.77	19.49	117.50	8.37	78.54
	PM003-67-1(b)	85.30	5.24	0.56	6.87	412.05	182.80	4.56	14.40	18.99	104.30	9.04	68.00
	PM003-74-1(b)	53.50	3.68	0.49	4.96	668.65	103.70	2.73	18.16	25.08	183.40	16.32	75.88
	PM004-2-2(b)	82.42	4.08	0.45	4.80	1 025.55	116.50	3.21	15.22	16.11	131.00	9.36	70.44
	PM004-3-1(b)	61.12	4.39	0.44	4.60	821.70	120.60	3.29	14.53	17.90	136.20	9.40	71.95
	PM004-16-1(b)	50.14	3.75	0.51	4.57	775.05	110.70	3.11	17.67	22.59	162.40	16.17	75.49
	PM004-31-1(b)	52.80	4.50	0.48	5.17	623.60	126.30	3.44	17.31	27.20	195.70	16.03	84.21
	PM004-42-1(b)	63.52	4.58	0.43	5.02	258.70	129.70	3.51	12.58	22.95	98.15	4.17	56.11
	PM004-44-1(b)	96.13	4.90	0.48	5.48	260.15	129.50	3.55	10.85	19.08	73.25	3.43	45.41
	PM004-59-1(b)	51.48	5.11	0.49	5.83	336.60	152.50	3.96	13.96	23.39	107.50	4.06	67.01
	KP4-35-1	70.54	4.15	0.43	5.34	291.05	139.60	3.69	11.08	17.68	73.00	3.03	37.14
	KP4-72-1	99.71	5.40	0.58	7.41	232.75	194.90	5.16	16.65	51.71	118.90	6.81	84.46
	H7913-1	81.04	5.95	0.68	8.09	275.95	215.50	5.60	17.11	71.83	123.50	7.13	84.24
	H7913-2	83.40	4.11	0.36	6.84	1 197.13	161.31	4.56	15.79	5.73	59.13	5.48	84.69
	H7913-3	132.73	7.48	0.55	8.83	1 071.30	192.86	5.17	9.76	4.19	100.27	6.41	66.71
	b5010-1	21.24	5.21	0.38	5.57	412.06	122.33	3.12	11.58	17.24	78.20	8.63	69.86
太勒古拉组	PM002-33-1(b)	29.54	2.73	0.58	4.27	257.00	111.40	3.11	23.14	29.32	157.70	16.30	85.54
	PM002-39-1(b)	38.21	1.93	0.38	2.99	246.65	94.20	2.62	22.56	32.44	149.20	16.95	85.45
	PM002-41-1(b)	9.21	1.90	0.36	3.12	214.40	118.00	3.18	24.66	30.95	164.60	16.17	94.85
	PM002-63-1(b)	43.49	4.36	0.70	7.73	382.05	180.30	4.57	11.91	17.02	76.85	7.85	69.69
	PM006-17-1(b)	44.58	3.12	0.38	4.04	795.55	94.80	2.62	18.67	25.35	181.30	16.60	79.19
	PM006-19-1(b)	50.54	4.02	0.46	4.91	904.90	116.40	3.35	17.77	25.25	179.40	16.09	80.86
	PM006-37-1(b)	86.24	5.11	0.46	5.50	248.10	141.80	3.83	11.60	22.10	86.87	6.50	61.80
	PM006-47-1(b)	68.11	3.55	0.42	4.61	540.05	111.80	3.09	16.00	19.20	140.50	10.12	81.57
	KP4-14-1	73.71	7.31	0.41	4.58	623.25	143.20	4.15	14.49	23.27	129.40	12.06	65.34
	KP4-18-1	80.73	3.74	0.40	4.23	745.40	102.50	3.07	18.99	23.46	170.00	15.10	87.15
	KP4-19-1	102.63	6.84	0.58	7.00	572.10	187.90	5.58	14.05	25.80	102.20	5.50	75.64
	KP4-22-1	85.82	5.28	0.37	4.60	729.45	125.90	3.65	17.33	27.89	212.50	14.18	88.53
	KP4-24-1	108.23	5.07	0.41	4.40	887.90	116.50	3.34	16.92	29.19	188.20	13.85	74.82
	KP4-24-2	45.08	3.51	0.39	4.28	811.10	99.60	2.80	18.87	24.25	212.70	15.38	78.73
	KP4-71-1	42.42	2.60	0.31	4.03	286.70	125.10	3.65	13.53	152.00	75.52	11.53	69.85
	H7911-1	62.16	5.81	0.41	6.15	435.10	148.93	4.06	18.18	16.96	164.32	12.12	88.14
	H7914-1	28.45	4.48	0.25	4.25	1 039.42	103.24	2.77	14.34	19.02	162.83	13.82	75.70
	H7914-2	34.69	4.12	0.24	3.98	798.11	95.07	2.61	15.64	23.26	211.34	17.10	87.37
	H7915-1	42.22	10.80	0.80	14.85	495.00	324.48	8.26	8.56	1.83	37.40	3.05	84.62
	H7915-2	0.93	9.89	0.52	7.94	151.17	208.87	5.57	8.00	2.12	30.79	2.97	52.60
	H7915-3	58.28	3.90	0.26	4.71	737.08	110.47	2.98	16.26	10.33	134.74	13.09	78.17
	H7915-4	56.05	6.07	0.54	7.77	292.21	168.41	4.81	10.07	10.88	54.76	4.41	67.46
	H7916-1	21.86	1.80	0.17	2.48	299.02	122.66	3.66	12.21	10.67	64.55	6.73	64.96
	H7916-2	1.19	5.29	0.39	5.58	142.95	193.54	5.31	10.45	14.68	41.76	5.07	56.98
	H7916-3	48.73	3.05	0.29	3.92	158.51	162.79	4.68	12.64	13.26	72.01	6.51	72.03

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表 4 不同沉积盆地构造背景下碎屑岩的REE特征

Table 4. REE characteristics of clastic rock from different sedimentary basins

形成环境	源岩类型	La	Ce	∑REE	La/Yb	LaN/Yb_N	∑LREE/∑HREE	δEu
大洋岛弧	未切割岩浆岛弧(Bhatia, 1985)	8.0±1.7	19.0±3.7	58±10	4.2±1.3	2.8±0.9	3.8±0.9	1.04±0.11
大陆岛弧	已切割岩浆弧(Bhatia, 1985)	27.0±4.5	59.0±8.2	146±20	11.0±3.6	7.5±2.5	7.7±1.7	0.79±0.13
活动大陆边缘	抬升基底(Bhatia, 1985)	37.0	78.0	186.00	12.50	8.50	9.10	0.60
被动大陆边缘	克拉通内核(Bhatia, 1985)	39.0	85.0	210.00	15.90	10.80	8.50	0.56
早石炭世碎屑岩	初始岩浆弧(张雷等，2014)	16.7	36.9	96.99	7.69	5.41	5.99	0.90
注：数据均为平均值，除比值外，含量单位为10^-6.

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