新疆卡拉麦里上-中泥盆统间角度不整合和346.8 Ma后碰撞火山岩的意义

王富明; 廖群安; 樊光明; 程雯娟; 田健; 陈帅; 吴魏伟; 胡朝斌

doi:10.3799/dqkx.2014.107

新疆卡拉麦里上-中泥盆统间角度不整合和346.8 Ma后碰撞火山岩的意义

doi: 10.3799/dqkx.2014.107

王富明^{1, 2,},
廖群安^1, ,,
樊光明¹,
程雯娟³,
田健¹,
陈帅¹,
吴魏伟¹,
胡朝斌¹

1.
中国地质大学地球科学学院, 湖北武汉 430074
2.
四川省地质矿产勘查开发局区域地质调查队, 四川成都 610213
3.
江西省地质矿产勘查开发局赣西北地质大队, 江西九江 332000

基金项目:

中国地质调查局地质调查工作项目 1212011120508

新疆东准噶尔卡拉麦利1:5万区调 L45E016022

新疆东准噶尔卡拉麦利1:5万区调 L45E017020

新疆东准噶尔卡拉麦利1:5万区调 L45E017021

新疆东准噶尔卡拉麦利1:5万区调 L45E018020

新疆东准噶尔卡拉麦利1:5万区调 L45E018021

详细信息

作者简介:
王富明(1987-), 男, 硕士, 主要从事岩浆岩石学方向研究.E-mail: liqinghan55555@126.com

通讯作者:
廖群安, E-mail: qanliao@cug.edu.cn

中图分类号: P581;P588
计量
- 文章访问数: 3123
- HTML全文浏览量: 137
- PDF下载量: 555
- 被引次数: 0
出版历程
- 收稿日期: 2014-03-14
- 刊出日期: 2014-09-01

Geological Implications of Unconformity between Upper and Middle Devonian, and 346.8 Ma Post-Collision Volcanic Rocks in Karamaili, Xinjiang

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Regional Geological Survey Team, Sichuan Bureau of Geology Exploration and Development of Mineral Reesources, Chengdu 610213, China
3.
Northwestern Jiangxi Geological Party, Bureau of Geology and Exploration and Development of Mineral Researches of Jiangxi Province, Jiujiang 332000, China

摘要

摘要: 在东准噶尔卡拉麦里地区的五彩湾一带出露一套具磨拉石特征的火山沉积建造, 下部为具磨拉石特征的砾岩、砂岩, 上部为一套中基性的火山熔岩夹中酸性的火山凝灰岩.1:20万卡拉麦里山幅将其归入下石炭统松喀尔苏组.通过1:5万地质调查研究发现, 该火山沉积建造底部以一套粗砾岩高角度不整合于下-中泥盆统卡拉麦里组之上, 含晚泥盆世植物化石Prelepidodendron sp.(先鳞木), 中上部火山岩LA-ICP-MS锆石U-Pb年龄为346.8±3.3 Ma, 且被年龄为341.1±4.0 Ma~340.9±5.1 Ma后碰撞花岗岩侵入, 表明其形成时代为晚泥盆世-早石炭世, 时代上对应于北准噶尔地层分区的上泥盆统克安库都克组.该套地层中上部的火山岩的岩石组合为玄武岩、玄武安山岩、夹少量的流纹质凝灰岩, 岩石化学特征上属钙碱性-高钾钙碱性系列, (La/Yb)_N=2.97~6.66, Nb、Ta亏损, 部分样品Zr、Ti弱显亏损, Nb/U、Ce/Pb比值分别为7.43~20.88、3.17~12.45.地球化学特征表明其兼具板内火山岩和弧火山岩的某些特点, 形成于后碰撞伸展环境, 是卡拉麦里洋盆于晚泥盆世之前闭合后后碰撞岩浆活动的产物.这一研究成果对广为关注的卡拉麦里洋盆的闭合时间进行了很好的限定.
- 东准噶尔 /
- 卡拉麦里 /
- 角度不整合 /
- 后碰撞 /
- 火山岩 /
- 克安库都克组
Abstract: A set of volcanic sedimentary formation outcrops in Wucaiwan, Karamaili area, eastern Junggar, composed of conglomerate, sandstone characterized by molasse in its lower part, and intermediate-basic lava interbedded with intermediate-acidic tuff in its upper part. The volcanic sedimentary formation is categorized into the Lower Carboniferous Songkaersu Formation in 1:200 000 Karamaili Mountain report. The 1:50 000 geological survey finds that a set of coarse conglomerate in the bottom high angle unconformably overlies the Early-Middle Devonian Karamaili Formation and contains plant fossil Prelepidodendron sp. of Late Devonian to Early Carboniferous. The volcanic rocks in the middle-upper part are intruded by post-collision granite of 341.1±4.0 Ma to 340.9±5.1 Ma, and its zircon U-Pb age is 346.8±3.3 Ma obtained by LA-ICP-MS. It indicates that the age of the volcanic sedimentary formation is Late Devonian-Early Carboniferous which might correspond to the Upper Devonian Keankuduke Formation in northern Junggar stratigraphic group. The volcanic rocks consist of basalt, basaltic andesite, and a handful of rhyolitic tuff, belonging to calc-alkaline and high K calc-alkaline series; and they are enriched in LILE and LREE ((La/Yb)_N=2.97-6.66), depleted slightly in Nb, Ta, and depleted weakly in Zr, Ti in some samples, with Nb/U=7.43-20.88, Ce/Pb=3.17-12.45. These volcanic rocks show both intraplate and arc volcanic rock geochemistry characteristics, formed in post-collision extensional period after the closure of Karamaili Ocean before the Upper Devonian. This study determines the final amalgamation time of Karamali Ocean, an issue of wide concern.
- eastern Junggar /
- Karamaili /
- angular unconformity /
- post-collision /
- volcanic rock /
- Keankuduke Formation

HTML全文

图 1 区域地质简图

a.据Jahn, 2004；b.据李锦轶，2004

Fig. 1. Regional geological sketch map

下载: 全尺寸图片幻灯片

图 2 克安库都克组野外露头、植物化石及火山岩显微照片

a.克安库都克组底部砾岩；b.克安库都克组不整合于卡拉麦里组之上；c.早石炭世花岗质岩体侵入克安库都克组玄武岩当中；d.克安库都克组底部先鳞木化石；e.克安库都克组不整合于卡拉麦里组之上；f.玄武岩(-)；g.玄武安山岩(+)；h.玄武安山岩(+)；i.流纹质凝灰岩(+)；Pl.斜长石；Px.辉石；Mt.磁铁矿；Ilm.钛铁矿；Chl.绿泥石；Q.石英；Pyr.岩屑

Fig. 2. Outcrop photos, plant fossil photos of the Keankuduke Formation and Photomicrographs of volcanic rocks

下载: 全尺寸图片幻灯片

图 3 克安库都克组(PM066)实测剖面

1.砾岩；2.凝灰质砾岩；3.凝灰质含砾长石砂岩；4.岩屑砂岩；5.砂岩；6.凝灰质砂岩；7.粉砂岩；8.流纹质凝灰岩；9.玄武岩；10.玄武安山岩；11.石英正长岩；12.流纹斑岩；13.卡拉麦里组；14.克安库都克组第1段；15.克安库都克组第2段；16.克安库都克组第3段；17.石英正长岩；18.角度不整合界线；19.锆石样品采样点；20.植物化石

Fig. 3. The geological section of the Keankuduke Formation (PM066)

下载: 全尺寸图片幻灯片

图 4 锆石CL图像(a)、U-Pb谐和图(b)及²⁰⁶Pb/²³⁸U年龄加权平均图(c)(图a单位为Ma)

Fig. 4. CL images of zircons (a), U-Pb concordia diagram (b) and ²⁰⁶Pb/²³⁸U age diagram (c)

下载: 全尺寸图片幻灯片

图 5 火山岩TAS(a)和Nb/Y-Zr/TiO₂图解(b)

a.据Le Maitre et al., 1989；b.据Winchester and Floyd, 1977

Fig. 5. TAS plot of volcanic rocks (a) and Nb/Y-Zr/TiO₂ plot (b)

下载: 全尺寸图片幻灯片

图 6 火山岩SiO₂-K₂O关系(据Peccerillo and Taylor, 1976)

Fig. 6. Relation of SiO₂-K₂O of volcanic rocks

下载: 全尺寸图片幻灯片

图 7 样品微量元素蛛网图及稀土元素球粒陨石标准化图

a.MORB值据Pearce, 1983；OIB值据Sun and Mcdonough, 1989；CABI值据李昌年，1992；b.标准化值据Sun and Mcdonough, 1989

Fig. 7. Spider plot of trace element of samples and Chondrite-normalized REE patterns of samples

下载: 全尺寸图片幻灯片

图 8 火山岩Nb/Yb-Th/Yb(a)和Ta/Yb-Th/Yb关系(b)

a.据Pearce, 2008；b.据Pearce, 1982

Fig. 8. Nb/Yb-Th/Yb (a) and Ta/Yb-Th/Yb (b) plot for samples

下载: 全尺寸图片幻灯片

表 1 玄武安山岩锆石U-Pb同位素分析结果

Table 1. Zircon U-Pb Isotopic analysis composition of basaltic andesite

分析点	Th/U	元素含量(10^-6)		同位素比值						同位素年龄(Ma)
分析点	Th/U	Th	U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
01	0.9	1 459	1 594	0.065 8	0.001 7	1.172 0	0.030 7	0.128 4	0.001 2	1 200	54	788	14	779	7
02	1.0	750	787	0.058 1	0.002 7	0.528 2	0.024 3	0.066 2	0.000 9	532	99	431	16	413	5
03	1.3	555	423	0.064 2	0.002 9	1.239 9	0.052 9	0.141 9	0.001 9	750	96	819	24	855	10
04	0.8	228	278	0.066 7	0.003 6	0.819 2	0.047 4	0.088 8	0.002 0	828	107	608	26	549	12
05	1.8	1 658	935	0.083 0	0.002 9	0.868 5	0.033 2	0.074 5	0.000 9	1 278	100	635	18	463	6
06	0.9	1 498	1 723	0.069 7	0.001 8	1.530 7	0.039 3	0.158 2	0.001 6	920	54	943	16	947	9
07	1.3	1 455	1 127	0.055 5	0.002 2	0.493 1	0.019 1	0.064 3	0.000 9	435	89	407	13	402	5
08	0.5	990	1 862	0.059 1	0.002 0	0.669 3	0.022 3	0.081 4	0.000 9	569	72	520	14	505	5
09	0.5	798	1 742	0.061 4	0.001 8	0.701 1	0.020 8	0.082 0	0.000 9	654	63	539	12	508	5
10	1.0	763	795	0.063 0	0.003 0	0.591 0	0.029 0	0.067 2	0.000 8	709	100	472	19	419	5
11	0.7	893	1 285	0.052 4	0.001 4	0.513 6	0.014 4	0.070 4	0.000 7	302	63	421	10	438	4
12	0.7	1 719	2 592	0.054 4	0.001 1	0.541 7	0.012 1	0.071 4	0.000 6	387	46	440	8	445	4
13	1.8	1 490	851	0.065 4	0.002 4	0.629 5	0.023 6	0.069 2	0.000 8	787	77	496	15	431	5
14	1.3	3 486	2 656	0.066 3	0.001 1	1.032 4	0.018 4	0.111 5	0.000 7	817	33	720	9	681	4
15	0.8	461	596	0.058 6	0.001 1	0.565 1	0.010 6	0.069 1	0.000 5	554	36	455	7	431	3
16	0.9	2 036	2 163	0.060 3	0.001 5	0.607 0	0.014 9	0.072 3	0.000 6	613	52	482	9	450	4
17	2.4	1 879	773	0.064 2	0.002 8	0.575 5	0.023 5	0.065 2	0.000 7	746	91	462	15	407	4
18	0.3	760	2 239	0.063 6	0.001 6	0.708 2	0.018 1	0.079 8	0.000 7	728	56	544	11	495	4

下载: 导出CSV

表 2 凝灰岩锆石U-Pb同位素分析结果

Table 2. Zircon U-Pb Isotopic analysis composition of tuff

分析点	Th/U	元素含量(10^-6)		同位素比值						同位素年龄(Ma)
分析点	Th/U	Th	U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
01	0.5	302	572	0.048 0	0.003 6	0.380 8	0.029 1	0.056 9	0.000 9	102	231	328	21	357	6
02	0.9	377	441	0.042 8	0.003 2	0.335 6	0.024 5	0.057 1	0.001 1	error	error	294	19	358	7
03	0.6	441	773	0.060 4	0.003 8	0.445 4	0.028 1	0.053 1	0.000 8	617	137	374	20	334	5
04	0.8	1 056	1 362	0.048 1	0.002 6	0.366 1	0.019 4	0.054 7	0.000 8	106	128	317	14	343	5
05	0.6	475	768	0.062 7	0.004 1	0.468 8	0.029 9	0.054 1	0.000 9	698	140	390	21	340	5
06	0.5	370	679	0.060 2	0.004 5	0.464 1	0.034 6	0.055 3	0.000 9	613	161	387	24	347	6
07	0.6	510	793	0.055 3	0.003 6	0.417 6	0.025 9	0.055 1	0.000 9	433	144	354	19	346	6
08	0.6	325	509	0.052 9	0.003 8	0.424 0	0.031 3	0.057 6	0.000 9	324	165	359	22	361	5
09	0.5	365	675	0.064 1	0.004 3	0.487 6	0.030 8	0.055 8	0.000 9	746	141	403	21	350	6
10	0.7	580	868	0.055 5	0.003 6	0.425 6	0.026 3	0.055 9	0.000 9	432	144	360	19	350	6
11	0.7	608	881	0.054 4	0.003 5	0.410 4	0.026 3	0.054 5	0.000 9	391	144	349	19	342	5
12	0.6	373	624	0.058 8	0.003 9	0.422 9	0.027 7	0.052 4	0.000 9	561	146	358	20	329	6
13	0.5	315	583	0.053 7	0.004 4	0.404 9	0.032 1	0.055 3	0.001 0	367	185	345	23	347	6
14	0.7	763	1 159	0.055 6	0.003 0	0.432 2	0.023 6	0.056 4	0.000 9	439	116	365	17	354	5
15	0.7	559	858	0.048 4	0.002 9	0.361 7	0.021 2	0.054 6	0.000 9	120	133	314	16	343	5
16	0.5	302	630	0.056 6	0.003 7	0.423 5	0.027 7	0.054 6	0.001 0	476	143	359	20	343	6
17	0.7	1 108	1 508	0.055 9	0.002 7	0.421 1	0.020 4	0.054 7	0.000 7	456	103	357	15	344	4
18	0.5	323	606	0.060 4	0.003 6	0.460 0	0.026 4	0.056 3	0.001 0	618	130	384	18	353	6
19	0.7	704	1 018	0.054 6	0.003 4	0.401 5	0.024 0	0.053 7	0.000 8	394	136	343	17	337	5
20	0.6	510	888	0.051 3	0.003 8	0.368 4	0.024 3	0.053 5	0.000 9	257	170	318	18	336	6
21	0.5	163	359	0.064 1	0.005 3	0.487 3	0.037 4	0.056 5	0.001 0	746	181	403	26	354	6
22	0.5	219	417	0.073 0	0.004 8	0.580 0	0.036 9	0.058 2	0.001 1	1 013	132	464	24	365	7
23	0.7	457	673	0.051 4	0.003 4	0.396 0	0.025 7	0.056 5	0.001 0	257	186	339	19	354	6
24	0.9	897	1 015	0.061 6	0.003 4	0.468 7	0.026 1	0.054 8	0.000 8	661	119	390	18	344	5
25	0.6	398	686	0.058 4	0.004 2	0.438 8	0.030 6	0.054 9	0.000 9	546	153	369	22	344	6

下载: 导出CSV

表 3 样品全岩主量(%)及微量元素(10^-6)分析结果

Table 3. Major elements (%) and trace elements (10^-6) analysis data

样品编号	066-18-1	066-18-2	066-22-1	067-9-5	066-25-1	D5462-1	067-9-4	067-16-1	067-16-2	067-16-4	067-18-2	066-24-1	066-24-3
岩性	玄武岩						玄武安山岩
SiO₂	50.40	43.62	51.52	51.73	49.16	46.86	55.01	52.92	52.91	53.32	52.30	53.42	55.56
TiO₂	2.48	2.40	1.46	2.73	1.83	2.27	1.20	1.29	1.27	1.10	1.14	1.46	1.35
Al₂O₃	16.18	16.07	16.09	13.77	16.19	16.82	16.75	17.31	16.73	16.97	16.87	16.20	15.70
FeO	8.42	10.02	6.35	5.98	5.12	7.52	4.48	3.25	5.12	4.75	4.48	5.35	5.38
Fe₂O₃	1.29	1.84	1.70	6.09	4.79	4.36	3.16	3.51	2.99	3.36	3.64	2.99	2.28
Fe₂O₃^T	10.65	12.97	8.76	12.73	10.48	12.72	8.14	7.12	8.68	8.64	8.62	8.93	8.26
FeO^T	9.58	11.67	7.88	11.46	9.43	11.44	7.32	6.41	7.81	7.77	7.75	8.04	7.43
MnO	0.21	0.23	0.14	0.24	0.17	0.20	0.13	0.16	0.14	0.12	0.12	0.16	0.17
MgO	3.27	3.24	4.19	3.65	5.00	6.71	4.03	2.15	3.77	3.63	4.15	4.39	3.59
CaO	9.34	11.62	6.95	5.93	8.26	8.54	6.85	9.90	7.94	6.24	8.16	5.59	5.84
Na₂O	2.72	2.61	2.84	4.49	3.02	3.02	3.50	3.31	3.55	3.33	2.46	4.28	3.98
K₂O	2.52	0.18	1.90	1.83	0.81	0.82	1.57	1.15	1.26	1.43	0.74	2.35	2.53
P₂O₅	0.40	0.40	0.51	1.13	0.30	0.45	0.39	0.47	0.45	0.35	0.35	0.51	0.47
H₂O⁺	2.36	3.23	3.19	2.09	3.15	2.02	2.49	1.41	1.24	2.88	2.96	2.59	2.10
CO₂	0.19	4.34	2.95	0.16	2.00	0.17	0.22	2.95	2.43	2.26	2.43	0.49	0.46
LOI	1.64	6.68	5.54	1.61	4.74	1.65	2.26	3.97	3.17	4.58	4.68	2.46	2.02
Mg^#	41.72	36.79	52.72	40.05	52.65	55.15	53.58	41.30	50.31	49.48	52.88	53.38	50.33
Cr	107.00	106.00	77.80	31.40	139.0	78.40	70.10	66.00	69.10	120.00	97.00	77.60	67.20
Ni	51.10	53.10	40.00	5.66	84.30	66.60	38.80	39.30	35.00	48.40	48.30	40.80	34.00
Rb	48.80	4.18	37.70	38.20	23.10	24.40	38.90	17.90	23.60	28.20	13.10	55.20	37.60
Ba	368.00	103.00	402.00	263.00	156.00	162.00	444.00	323.00	341.00	719.00	279.00	560.00	576.00
Th	1.32	1.10	2.58	3.02	1.79	1.85	3.52	3.99	3.69	2.93	3.15	2.51	2.58
U	0.34	0.35	0.80	1.15	0.64	0.51	0.87	1.15	1.05	0.82	0.95	0.71	0.73
Nb	5.59	6.39	9.29	8.56	5.55	10.70	8.41	10.80	9.18	6.95	7.40	8.49	9.36
Ta	0.36	0.45	0.58	0.54	0.40	0.83	0.56	0.84	0.62	0.47	0.57	0.51	0.67
La	13.70	13.20	23.20	23.00	13.80	14.60	26.50	27.80	27.80	19.70	20.10	20.80	22.40
Ce	34.30	33.30	53.70	57.20	31.90	34.60	57.30	59.20	59.70	42.10	42.60	48.00	52.50
Pr	5.04	5.06	7.34	8.31	4.73	4.91	7.31	7.58	7.58	5.53	5.57	6.54	7.21
Sr	346.00	406.00	445.00	351.00	443.00	463.00	529.00	504.00	457.00	493.00	436.00	416.00	364.00
Nd	22.40	22.40	29.80	36.80	20.20	23.00	28.00	29.20	28.60	21.90	21.50	26.80	29.70
Zr	191.00	190.00	240.00	242.00	203.00	200.00	239.00	267.00	265.00	187.00	190.00	238.00	236.00
Hf	5.05	4.79	5.67	6.04	4.57	7.28	5.50	5.75	5.52	4.42	4.41	5.69	5.65
Sm	6.63	6.82	7.71	10.48	5.86	5.84	6.74	7.12	6.95	5.46	5.29	7.03	7.64
Eu	2.17	2.08	2.41	3.22	1.85	1.81	1.86	1.95	1.90	1.53	1.50	2.15	2.60
Gd	6.90	7.17	7.27	10.9	6.12	6.01	6.04	6.61	6.38	5.05	4.99	6.83	7.31
Tb	1.14	1.16	1.18	1.74	1.01	0.97	0.90	1.02	1.07	0.79	0.79	1.07	1.19
Dy	6.71	6.91	6.79	9.94	6.17	5.65	5.27	6.01	5.70	4.62	4.54	6.17	6.93
Y	32.70	32.60	33.20	48.90	30.80	28.30	26.70	30.40	29.00	23.00	23.00	31.50	34.70
Ho	1.30	1.28	1.31	1.93	1.19	1.10	1.00	1.15	1.14	0.90	0.88	1.20	1.37
Er	3.56	3.63	3.84	5.45	3.48	3.16	2.92	3.36	3.31	2.63	2.57	3.48	3.94
Tm	0.48	0.48	0.54	0.74	0.49	0.45	0.41	0.48	0.48	0.39	0.37	0.48	0.56
Yb	3.03	3.01	3.74	5.01	3.33	2.95	2.85	3.34	3.27	2.61	2.65	3.39	3.88
Lu	0.39	0.39	0.54	0.72	0.49	0.42	0.42	0.49	0.50	0.40	0.39	0.50	0.57
Pb	2.76	0.92	16.90	6.70	7.19	5.75	6.56	10.30	6.84	5.99	8.60	4.58	14.70
Cs	346.00	406.00	445.00	351.00	443.00	463.00	529.00	504.00	457.00	493.00	436.00	416.00	364.00

下载: 导出CSV

参考文献(101)

[1]	Belousova, E.A., Griffin, W.L., O'Reilly, S.Y., et al., 2002. Igneous Zircon: Trace Element Composition as an Indicator of Source Rock Type. Contribution to Mineralogy and Petrology, 143(5): 602-622. doi: 10.1007/s00410-002-0364-7
[2]	Cai, W.J., Li, C.Y., 1983. Preliminary Study on Plate Tectonics of Northern East Junggar in Xinjiang Uighur Autonomous Region. In: Institute of Geology, Chinese Academy of Geological Sciences., ed., Bulletin of the Chinese Academy of Geological Sciences (1983 Bound Volume in Chinese and English). Geological Publishing House, Beijing, 170-171 (in Chinese).
[3]	Chen, S., Zhang, Y.Y., Guo, Z.J., 2009. Zircon SHRIMP U-Pb Dating and Its Implication of Post-Collisional Volcanic Rocks in Santanghu Basin, Xinjiang. Acta Petrologica Sinica, 25(3): 527-538 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200903006.htm
[4]	Han, B.F., Ji, J.Q., Song, B., et al., 2006. Late Paleozoic Vertical Growth of Continental Crust around the Junggar Basin, Xinjiang, China (PartⅠ): Timing of Post-Collisional Plutonism. Acta Petrologica Sinica, 22(5): 1077-1086 (in Chinese with English abstract). http://www.researchgate.net/publication/269710583_Late_Paleozoic_vertical_growth_of_continental_crust_around_the_Junggar_Basin_Xinjiang_China_Part_I_Timing_of_post-collisional_plutonism
[5]	He, G.Q., Li, M.S., Jia, J.D., et al., 2001. A Discussion on Age and Tectonic Significance of Ophiolite in Eastern Junggar, Xinjiang. Acta Scientiarum Naturalium Universitatis Pekinensis, 37(6): 852-858 (in Chinese with English abstract). http://www.researchgate.net/publication/282736819_A_discussion_on_age_and_tectonic_significance_of_ophiolite_in_Eastern_Junggar_Xinjiang
[6]	Hofmann, A., Jochum, K.P., Seufert, M., et al., 1986. Nb and Pb in Oceanic Basalts: New Constraints on Mantle Evolution. Earth and Planetary Science Letters, 79(1-2): 33-45. doi:10.1016/0012-821 X (86)90038-5
[7]	Hole, M.J., Saunders, A.D., Marriner, G.F., et al., 1984. Subduction of Pelagio Sediments: Implications for the Origin of Ce-Anomalous Basalts from the Manana Islands. Journal of the Geological Society, London, 141(3): 453-472. doi: 10.1144/gsjgs.141.3.0453
[8]	Huang, G., Niu, G.Z., Wang, X.L., et al., 2012. Formation and Emplacement Age of Karamaili Ophiolite: LA-ICP-MS Zircon U-Pb Age Evidence from the Diabase and Tuff in Eastern Junggar, Xinjiang. Geological Bulletin of China, 31(8): 1267-1278 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201208006.htm
[9]	Jahn, B.M., 2004. The Central Asian Orogenic Belt and Growth of the Continental Crust in the Phanerozoic. Geological Society, Special Publication, 226: 73-100. doi: 10.1144/GSL.SP.2004.262.01.05
[10]	Le Maitre, R.W., Bateman. P., Dudek. A., et al., 1989. A Classification of Igneous Rocks and Glossary of Terms. Blackwell, Oxford, 130-171.
[11]	Li, C.N., 1992. Trace Elements Petrology of Volcanic Rocks. China University of Geosciences Press, Wuhan, 181-182 (in Chinese).
[12]	Li, D., He, D.F., Fan, C., et al., 2012. Geochemical Characteristics and Tectonic Significance of Carboniferous Basalt in the Karamaili Gas Field of Junggar Basin. Acta Petrologica Sinica, 28(3): 981-992 (in Chinese with English abstract).
[13]	Li, J.L., Sun, S., Hao, J., et al., 1999. Time Limit of Collision Event of Collision Orogens. Acta Petrologica Sinica, 15(2): 315-320 (in Chinese with English abstract). http://www.oalib.com/paper/1473027
[14]	Li, J.Y., 1991. Early Paleozoic Evolution of Lithosphere Plate, East Junggar, Xinjiang. Bulletin of the Chinese Academy of Geological Sciences, 1-12 (in Chinese with English abstract). http://www.researchgate.net/publication/285162161_Early_Paleozoic_evolution_of_lithosphere_plate_East_Junggar_Xinjiang
[15]	Li, J.Y., 2004. Late Neoproterozoic and Paleozoic Tectonic Framework and Evolution of Eastern Xinjiang, NW China. Geological Review, 50(3): 304-322 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200403015
[16]	Li, J.Y., He, G.Q., Xu, X., et al., 2006. Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation. Acta Geologica Sinica, 80(1): 148-168 (in Chinese with English abstract). http://www.researchgate.net/publication/286884899_Crustal_tectonic_framework_of_northern_Xinjiang_and_adjacent_regions_and_its_formation
[17]	Li, J.Y., Xiao, X.C., Tang, Y.Q., et al., 1988. Progress in Study of Ancient Plate Tectonics in Karamaili Region, Eastern Junggar, Xinjiang. Chinese Science Bulletin, 33(10): 762-764 (in Chinese). doi: 10.1360/csb1988-33-10-762
[18]	Li, J.Y., Xiao, X.C., Tang, Y.Q., et al., 1990. Main Characteristics of Late Paleozoic Plate Tectonics in the Southern Part of East Junggar, Xinjiang. Geological Review, 36(4): 305-316 (in Chinese with English abstract). http://www.researchgate.net/publication/313240678_The_main_characteristics_of_Late_Paleozoic_plate_tectonics_in_the_southern_part_of_East_Junggar_Xinjiang
[19]	Li, J.Y., Yang, T.N., Li, Y.P., et al., 2009. Geological Features of the Karamaili Faulting Belt, Eastern Junggar Region, Xinjiang, China and Its Constraints on the Reconstruction of Late Paleozoic Ocean-Continental Framework of the Central Asian Region. Geological Bulletin of China, 28(12): 1817-1826 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200912015.htm
[20]	Li, W., Liu, Y.Q., Dong, Y.P., et al., 2012. The Geochemical Characteristics, Geochronology and Tectonic Significance of the Carboniferous Volcanic Rocks of the Santanghu Area in Northeastern Xinjiang, China. Science in China (Series D), 42(11): 1716-1728 (in Chinese). doi: 10.1007/s11430-012-4483-3
[21]	Liégeois, J.P., 1998. Some Words on the Post-Collisional Magmatism. Lithos, 45: 15-18: xv-xvii. doi: 10.1016/S0024-4937(98)00023-1
[22]	Liu, Y.S., Gao, S., Hu. Z.C., et al., 2010. 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 of Mantle Xenoliths. Journal of Petrology, 51(1-2): 537-571. doi: 10.1093/petrology/egp082
[23]	Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1-2): 34-43. doi: 10.1016/j.chemgeo.2008.08.004
[24]	Long, X.P., Yuan, C., Sun, M., et al., 2012. Geochemistry and U-Pb Detrital Zircon Dating of Paleozoic Graywackes in East Junggar, NW China: Insights into Subduction-Accretion Processes in the Southern Central Asian Orogenic Belt. Gondwana Research, 21(2-3): 637-653. doi: 10.1016/j.gr.2011.05.015
[25]	Ludwig, K.R., 2003. Users Manual for Isoplot 3.0: A Geochronological Toolkit for Microsoft Exccel. Berkeley Geochronology Center, Berkeley, 1-39.
[26]	Mao, Z.G., Zou, C.N., Zhu, R.K., et al., 2010. Geochemical Characteristics and Tectonic Settings of Carboniferous Volcanic Rocks in Junggar Basin. Acta Petrologica Sinica, 26(1): 207-216 (in Chinese with English abstract).
[27]	Ouyang, S., Zhu, H.C., Zhan, J.Z., et al., 2004. Comparison of Permian Palynofloras from the Junggar and Tarim Basins and Its Bearing on Phytoprovincialism and Stratigraphy. Journal of Stratigraphy, 28(3): 193-207 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ200403000.htm
[28]	Pearce, J.A., 1982. Trace Element Characteristics of Lava from Destructive Plate Boundaries. In: Thorpe, R.S., ed., Orogenic Andesites and Related Rocks. John Wiley and Sons, Chichester, 528-548.
[29]	Pearce, J.A., 1983. The Role of Sub-Continental Lithosphere in Magma Genesis at Active Plate Margins. In: Hawkesworth, C.J., Norry, M.J., eds., Continental Basalts and Mantle Xenoliths. Shiva Publications, Cheshire, 230-249.
[30]	Pearce, J.A., 2008. Geochemical Fingerprinting of Oceanic Basalts with Applications to Ophiolite Classification and the Search for Archean Oceanic Crust. Lithos, 100(1-4): 14-48. doi: 10.1016/j.lithos.2007.06.016
[31]	Peccerillo, R., Taylor, S.R., 1976. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey. Contribution to Mineralogy and Petrology, 58(1): 63-81. doi: 10.1007/BF00384745
[32]	Plank, T., Langmuir, C.H., 1998. The Chemical Composition of Subducting Sediment and Its Consequences for the Crust and Mantle. Chemical Geology, 145(3-4): 325-394. doi: 10.1016/S0009-2541(97)00150-2
[33]	Seghedi, I., Downes, H., Vaselli, O., et al., 2004. Post-Collisional Tertiary-Quaternary Mafic Alkalic Magmatism in the Carpathian-Pannonian Region: A Review. Tectonophysics, 393(1-4): 43-62. doi: 10.1016/j.tecto.2004.07.051
[34]	Shu, L.S., Wang, Y.J., 2003. Late Devonian-Early Carboniferous Radiolarian Fossils from Siliceous Rocks of Kelameili Ophiolite, Xinjiang. Geological Review, 49(4): 408-412 (in Chinese with English abstract). http://www.researchgate.net/publication/284318300_Late_Devonian-Early_Carboniferous_radiolarian_fossils_from_siliceous_rocks_of_the_Kelameili_ophiolite_Xinjiang
[35]	Su, Y.P., Zheng, J.P., Griffin, W.L., et al., 2010. Zircon U-Pb and Hf Isotopes of Volcanic Rocks from the Batamayineishan Formation in the Eastern Junggar Basin. Chinese Science Bulletin, 55(30): 2931-2943. doi: 10.1007/s11434-010-4151-y
[36]	Su, Y.P., Zheng, J.P., Griffin, W.L., et al., 2012. Geochemistry and Geochronology of Carboniferous Volcanic Rocks in the Eastern Junggar Terrane, NW China: Implication for a Tectonic Transition. Gondwana Research, 22(3-4): 1009-1029. doi: 10.1016/j.gr.2012.01.004
[37]	Sun, S.S., McDonough, W.F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. Geological Society London, Special Publication, 42(1): 313-345. doi: 10.1144/GSL.SP.1989.042.01.19
[38]	Tan, J.Y., Wu, R.J., Zhang, Y.Y., et al., 2009. Characteristics and Geochronology of Volcanic Rocks of Batamayineishan Formation in Kalamaily, Eastern Junggar, Xinjiang. Acta Petrologica Sinica, 25(3): 539-546 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200903007.htm
[39]	Wang, B.Y., Jiang, C.Y., Li, Y.J., et al., 2009. Geochemistry and Tectonic Implications of Karamaili Ophiolite in East Junggar of Xinjiang. Journal of Mineralogy and Petrology, 29(3): 74-82 (in Chinese with English abstract). http://www.researchgate.net/publication/283773982_Geochemistry_and_tectonic_implications_of_Karamaili_ophiolite_in_East_Junggar_of_Xinjiang
[40]	Wang, D.Y., Deng, J.H., 1995. Characteristics and Evolution of the Plate Tectonics in Eastern Junggar, Xinjiang. Journal of Chengdu Institute of Technology, 22(4): 38-45 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG504.007.htm
[41]	Wang, T., Hong, D.W., Jahn, B., et al., 2006. Timing, Petrogenesis, and Setting of Paleozoic Synorogenic Intrusions from the Altai Mountains, Northwest China: Implications for the Tectonic Evolution of an Accretionary Orogen. Journal of Geology, 114(6): 735-751. doi: 10.1086/507617
[42]	Wang, Z.H., Sun, S., Li, J.L., et al., 2003. Paleozoic Tectonic Evolution of the Northern Xinjiang, China: Geochemical and Geochronological Constraints from the Ophiolites. Tectonics, 22(2): 1014-1023. doi: 10.1029/2002TC001396
[43]	Wilson, M., 1989. Igneous Petrogenesis. Springer, Netherlands, 173-174.
[44]	Winchester, J.A., Floyd, P.A., 1977. Geochemical Discrimination of Different Magma Series and Their Differentiation Products Using Immobile Elements. Chemical Geology, 20: 325-343. doi: 10.1016/0009-2541(77)90057-2
[45]	Windley, B.F., Alexeiev, D., Xiao, W.J., et al., 2007. Tectonic Models for Accretion of the Central Asian Orogenic Belt. Journal of the Geological Society, 164(1): 31-47. doi: 10.1144/0016-76492006-022
[46]	Wu, Q., Qu, X., Chang, G.H., et al., 2012. Geochronology of the Hongliuxia Ductile Shear Zone and Its Constraint on the Closure Time of the Junggar Ocean. Acta Petrologica Sinica, 28(8): 2331-2339 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201208004.htm
[47]	Wu, R.J., Zhang, Y.Y., Tan, J.Y., et al., 2009. The Characteristics of Different Structure Layers and Tectonic Implications since Late Paleozoic in Kalamaily Area, Xinjiang. Earth Science Frontiers, 16(3): 102-109 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200903011.htm
[48]	Wu, X.Q., Liu, D.L., Li, Z.S., 2009a. Post-Collisional Volcanism of Karamaili Suture Zone. Earth Science Frontiers, 16(3): 220-230 (in Chinese with English abstract). doi: 10.1016/S1872-5791(08)60086-X
[49]	Wu, X.Q., Liu, D.L., Wei, G.Q., et al., 2009b. Geochemical Characteristics and Tectonic Setting of Carboniferous Volcanic Rocks from Ludong-Wucaiwan Area, Junggar Basin. Acta Petrologica Sinica, 25(1): 55-66 (in Chinese with English abstract).
[50]	Wu, Y.B., Zheng, Y.F., 2004. Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age. Chinese Science Bulletin, 49(15): 1554-1569. doi: 10.1007/BF03184122
[51]	Xiao, W.J., Han, C.M., Yuan, C., et al., 2006. Unique Carboniferous-Permian Tectonic-Metallogenic Framework of Northern Xinjiang (NW China): Constraints for the Tectonics of the Southern Paleoasian Domain. Acta Petrologica Sinica, 22(05): 1062-1076 (in Chinese with English abstract). http://www.oalib.com/paper/1472010
[52]	Xiao, W.J., Han, C.M., Yuan, C., et al., 2008. Middle Cambrian to Permian Subduction-Related Accretionary Orogenesis of Northern Xinjiang, NW China: Implications for the Tectonic Evolution of Central Asia. Journal of Asian Earth Sciences, 32(2-4): 102-117. doi: 10.1016/j.jseaes.2007.10.008
[53]	Xiao, W.J., Windley, B.F., Huang, B. C, et al., 2009. End-Permian to Mid-Triassic Termination of the Accretionary Processes of the Southern Altaids: Implications for the Geodynamic Evolution, Phanerozoic Continental Growth, and Metallogeny of Central Asia. International Journal of Earth Sciences, 98(6): 1189-1217. doi: 10.1007/s00531-008-0407-z
[54]	Xiao, W.J., Zhang, L.C., Qin, K.Z., et al., 2004. Paleozoic Accretionary and Collisional Tectonics of the Eastern Tianshan (China): Implications for the Continental Growth of Central Asia. American Journal of Science, 304(4): 370-395. doi: 10.2475/ajs.304.4.370
[55]	Xiao, Y., Zhang, H.F., Shi, J.A., et al., 2011. Late Paleozoic Magmatic Record of East Junggar, NW China and Its Significance: Implication from Zircon U-Pb Dating and Hf Isotope. Gondwana Research, 20(2-3): 532-542. doi: 10.1016/j.gr.2010.12.008
[56]	Yang, G.X., Li, Y.J., Li, Z.C., et al., 2010. Genesis and Tectonic Setting of Post-Collison Volcanic Rocks in North Eastern Margin of East Junggar. Earth Science Frontiers, 17(1): 49-60 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY201001006.htm
[57]	Yang, G.X., Li, Y.J., Yan, J., et al., 2011. Geochemistry Characteristics of Volcanic Rocks of Heishantou Formation in Karamaili, East Junggar, and Tectonic Settings Implication. Xinjiang Geology, 29(3): 257-262 (in Chinese with English abstract).
[58]	Yang, P.R., Yang, W.Q., Meng, Y.Y., et al., 2007. Lower Carboniferous Stratigraphic System of Karamaili Orogenic Belt, Xinjiang and Its Tectonic Setting. Geological Science and Technology Information, 26(5): 6-10 (in Chinese with English abstract). http://www.researchgate.net/publication/291153400_Lower_carboniferous_stratigraphic_system_of_kelamaili_oogenic_belt_Xinjiang_and_its_tectonic_setting
[59]	Zhang, W.S., Gao, H.Z., 1999. The Residual Sea Basin of Karamaili Orogenic Belt, Eastern Junggar, Xinjiang. Earth Science Frontiers, 6(4): 294 (in Chinese).
[60]	Zhang, Y.Y., Pe-Piper, G., Piper, D, J.W., et al., 2013. Early Carboniferous Collision of the Kalamaili Orogenic Belt, North Xinjiang, and Its Implications: Evidence from Molasse Deposits. Geological Society of America Bulletin, 125(5-6): 932-944. doi: 10.1130/B30779.1
[61]	Zhao, H.L., Xu, F., Zhang, J., et al., 2012. The Karamaili Ophiolites: Age, Geological Characteristics and Tectonic Significance. Xinjiang Geology, 30(2): 161-164 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XJDI201202012.htm
[62]	Zhao, L., Ji, J.Q., Xu, Q.Q., et al., 2012. Karamaili Strike-Slipping Fault and Deformational Sequence since Late Paleozoic in the Northern Xinjiang. Acta Petrologica Sinica, 28(7): 2257-2268 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201207026.htm
[63]	Zhao, X., Jia, C.Z., Zhang, G.Y., et al., 2008. Geochemistry and Tectonic Settings of Carboniferous Intermediate-Basic Volcanic Rocks in Ludong-Wucaiwan, Junggar Basin. Earth Science Frontiers, 15(2): 272-279 (in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/S187257910960004X
[64]	Zhao, Z.H., Guo, Z.J., Han, B.F., et al., 2006. The Geochemical Characteristics and Tectonic-Magmatic Implications of the Latest-Paleozoic Volcanic Rocks from Santanghu Basin, Eastern Xinjiang, Northwest China. Acta Petrologica Sinica, 22(1): 199-214 (in Chinese with English abstract). http://www.researchgate.net/publication/286792823_The_geochemical_characteristics_and_tectonic-magmatic_implications_of_the_latest-Paleozoic_volcanic_rocks_from_Santanghu_basin_eastern_Xinjiang_northwest_China
[65]	Zheng, Y.F., Yang, J.H., Song, S.G., et al., 2013. Progress in Study of Chemical Geodynamics. Bulletin of Mineralogy, Petrology and Geochemistry, 32(1): 1-24 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KYDH201301002.htm
[66]	蔡文俊, 李春昱, 1983. 新疆东准噶尔北缘板块构造初步研究. 见: 中国地质科学院地质研究所编, 中国地质科学院文集(1983中英文合订本). 北京: 地质出版社, 170-171.
[67]	陈石, 张元元, 郭召杰, 2009. 新疆三塘湖盆地后碰撞火山岩的锆石SHRIMP U-Pb定年及其地质意义. 岩石学报, 25(3): 527-538. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200903006.htm
[68]	韩宝福, 季建清, 宋彪, 等, 2006. 新疆准噶尔晚古生代陆壳垂向生长(Ⅰ)—后碰撞深成岩浆活动的时限. 岩石学报, 22(5): 1077-1086. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605003.htm
[69]	何国琦, 李茂松, 贾进斗, 等, 2001. 论新疆东准噶尔蛇绿岩的时代及其意义. 北京大学学报(自然科学版), 37(6): 852-858. doi: 10.3321/j.issn:0479-8023.2001.06.017
[70]	黄岗, 牛广智, 王新录, 等, 2012. 新疆东准噶尔卡拉麦里蛇绿岩的形成和侵位时限—来自辉绿岩和凝灰岩LA-ICP-MS锆石U-Pb年龄的证据. 地质通报, 31(8): 1267-1278. doi: 10.3969/j.issn.1671-2552.2012.08.006
[71]	李昌年, 1992. 火成岩微量元素岩石学. 武汉: 中国地质大学出版社, 181-182.
[72]	李涤, 何登发, 樊春, 等, 2012. 准噶尔盆地克拉美丽气田石炭系玄武岩的地球化学特征及构造意义. 岩石学报, 28(3): 981-992. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201203027.htm
[73]	李继亮, 孙枢, 郝杰, 等, 1999. 碰撞造山带的碰撞事件时限的确定. 岩石学报, 15(2): 315-320. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB902.019.htm
[74]	李锦轶, 1991. 试论新疆东准噶尔早古生代岩石圈板块构造演化. 中国地质科学院院报, 23: 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB199102000.htm
[75]	李锦轶, 2004. 新疆东部新元古代晚期和古生代构造格局及其演变. 地质论评, 50(3): 304-322. doi: 10.3321/j.issn:0371-5736.2004.03.015
[76]	李锦轶, 何国琦, 徐新, 等, 2006. 新疆北部及邻区地壳构造格架及其形成过程的初步探讨. 地质学报, 80(1): 148-168. doi: 10.3321/j.issn:0001-5717.2006.01.017
[77]	李锦轶, 肖序常, 汤耀庆, 等, 1988. 新疆东准噶尔卡拉麦里地区古板块构造研究的新进展. 科学通报, 33(10): 762-764. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB198810012.htm
[78]	李锦轶, 肖序常, 汤耀庆, 等, 1990. 新疆东准噶尔卡拉麦里地区晚古生代板块构造的基本特征. 地质论评, 36(4): 305-316. doi: 10.3321/j.issn:0371-5736.1990.04.003
[79]	李锦轶, 杨天南, 李亚萍, 等, 2009. 东准噶尔卡拉麦里断裂带的地质特征及其对中亚地区晚古生代洋陆格局重建的约束. 地质通报, 28(12): 1817-1826. doi: 10.3969/j.issn.1671-2552.2009.12.014
[80]	李玮, 柳益群, 董云鹏, 等, 2012. 新疆三塘湖地区石炭纪火山岩年代学、地球化学及其大地构造意义. 中国科学(D辑), 42(11): 1716-1728. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201211010.htm
[81]	毛治国, 邹才能, 朱如凯, 等, 2010. 准噶尔盆地石炭纪火山岩岩石地球化学特征及其构造环境意义. 岩石学报, 26(1): 207-216. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201001025.htm
[82]	欧阳舒, 朱怀诚, 詹家桢, 等, 2004. 新疆准噶尔盆地和塔里木盆地二叠纪孢粉组合的比较及其植物区系和地层意义. 地层学杂志, 28(3): 193-207. doi: 10.3969/j.issn.0253-4959.2004.03.001
[83]	舒良树, 王玉净, 2003. 新疆卡拉麦里蛇绿岩带中硅质岩的放射虫化石. 地质论评, 49(4): 408-412. doi: 10.3321/j.issn:0371-5736.2003.04.011
[84]	苏玉平, 郑建平, Griffin, W.L., 等, 2010. 东准噶尔盆地巴塔玛依内山组火山岩锆石U-Pb年代及Hf同位素研究. 科学通报, 55(30): 2931-2943. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201030009.htm
[85]	谭佳奕, 吴润江, 张元元, 等, 2009. 东准噶尔卡拉麦里地区巴塔玛依内山组火山岩特征和年代确定. 岩石学报, 25(3): 539-546. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200903007.htm
[86]	汪帮耀, 姜常义, 李永军, 等, 2009. 新疆东准噶尔卡拉麦里蛇绿岩的地球化学特征及大地构造意义. 矿物岩石, 29(3): 74-82. doi: 10.3969/j.issn.1001-6872.2009.03.012
[87]	王道永, 邓江红, 1995. 东准噶尔地区板块构造特征及演化. 成都理工学院学报, 22(4): 38-45. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG504.007.htm
[88]	吴琪, 屈迅, 常国虎, 等, 2012. 红柳峡韧性剪切带形成时代及其对准噶尔洋盆闭合时限的约束. 岩石学报, 28(8): 2331-2339. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201208004.htm
[89]	吴润江, 张元元, 谭佳奕, 等, 2009. 新疆卡拉麦里地区晚古生代以来不同构造层特征及大地构造意义. 地学前缘, 16(3): 102-109. doi: 10.3321/j.issn:1005-2321.2009.03.006
[90]	吴小奇, 刘德良, 李振生, 2009a. 卡拉麦里缝合带后碰撞期火山活动. 地学前缘, 16(3): 220-230. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200903025.htm
[91]	吴小奇, 刘德良, 魏国齐, 等, 2009b. 准噶尔盆地陆东-五彩湾地区石炭系火山岩地球化学特征及其构造背景. 岩石学报, 25(1): 55-66. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200901006.htm
[92]	肖文交, 韩春明, 袁超, 等, 2006. 新疆北部石炭纪-二叠纪独特的构造-成矿作用: 对古亚洲洋构造域南部大地构造演化的制约. 岩石学报, 22(05): 1062-1076. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605002.htm
[93]	杨高学, 李永军, 李注苍, 等, 2010. 东准噶尔东北缘后碰撞火山岩成因与构造环境. 地学前缘, 17(1): 49-60. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201001006.htm
[94]	杨高学, 李永军, 严镜, 等, 2011. 卡拉麦里地区黑山头组火山岩地球化学特征及构造环境分析. 新疆地质, 29(3): 257-262. doi: 10.3969/j.issn.1000-8845.2011.03.003
[95]	杨品荣, 杨文强, 蒙有言, 等, 2007. 新疆克拉麦里造山带下石炭统地层系统及其沉积构造背景. 地质科技情报, 26(5): 6-10. doi: 10.3969/j.issn.1000-7849.2007.05.002
[96]	张旺生, 高怀忠, 1999. 新疆东准卡拉麦里造山带的陆间残余海盆. 地学前缘, 6(4): 294. doi: 10.3321/j.issn:1005-2321.1999.04.031
[97]	赵恒乐, 许凡, 张冀, 等, 2012. 东准噶尔卡拉麦里蛇绿岩形成时代、地质特征及构造意义. 新疆地质, 30(2): 161-164. doi: 10.3969/j.issn.1000-8845.2012.02.008
[98]	赵磊, 季建清, 徐芹芹, 等, 2012. 新疆北部卡拉麦里晚古生代走滑构造及其叠加变形序次. 岩石学报, 28(7): 2257-2268. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201207026.htm
[99]	赵霞, 贾承造, 张光亚, 等, 2008. 准噶尔盆地陆东-五彩湾地区石炭系中、基性火山岩地球化学及其形成环境. 地学前缘, 15(2): 272-279. doi: 10.3321/j.issn:1005-2321.2008.02.030
[100]	赵泽辉, 郭召杰, 韩宝福, 等, 2006. 新疆三塘湖盆地古生代晚期火山岩地球化学特征及其构造-岩浆演化意义. 岩石学报, 22(1): 199-214. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200601020.htm
[101]	郑永飞, 杨进辉, 宋述光, 等, 2013. 化学地球动力学研究进展. 矿物岩石地球化学通报, 32(1): 1-24. doi: 10.3969/j.issn.1007-2802.2013.01.001