漠河地区黑云母花岗闪长岩地球化学、Hf同位素特征及其成因

李良; 孙丰月; 李碧乐; 陈广俊; 许庆林; 张雅静; 钱烨; 王琳琳

doi:10.3799/dqkx.2018.022

漠河地区黑云母花岗闪长岩地球化学、Hf同位素特征及其成因

doi: 10.3799/dqkx.2018.022

1.
吉林大学地球科学学院, 吉林长春 130061
2.
山东科技大学地球科学与工程学院, 山东青岛 266590

基金项目:

中国地质调查局项目 1212011085485

国家自然科学基金项目 41272093

详细信息

作者简介:
李良(1986-), 男, 博士研究生, 主要从事矿床成矿理论与预测方面的研究

通讯作者:
孙丰月

中图分类号: P581;P591.1
计量
- 文章访问数: 4996
- HTML全文浏览量: 1490
- PDF下载量: 40
- 被引次数: 0
出版历程
- 收稿日期: 2017-07-12
- 刊出日期: 2018-02-15

Geochemistry, Hf Isotopes and Petrogenesis of Biotite Granodiorites in the Mohe Area

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China

摘要

摘要: 以往学者的研究多集中在印支期出露于漠河县城南的黑云母花岗闪长岩，而对该地区燕山早期构造演化的研究相对薄弱.运用LA-ICP-MS锆石U-Pb年代学、全岩地球化学与Hf同位素分析的方法确定其形成时代、岩浆源区性质及成岩构造背景.结果表明：该岩石的加权平均年龄分别为185±2 Ma和182±2 Ma，表明其形成于早侏罗世；岩石属于高钾钙碱性系列，A/CNK介于0.90~1.03，Mg^#值为42~48，具有高Sr（489×10^-6~653×10^-6）低Yb（1.33×10^-6~1.99×10^-6）的特征，判定其属于埃达克岩类；岩石具有弧岩浆的微量元素特征，轻重稀土元素分馏明显（（La/Yb）_N=8.36~15.6），较弱的Eu负异常（Eu/Eu^*=0.79~0.95），富集Rb、K等大离子亲石元素，明显亏损Nb、Ta、Ti等高场强元素；岩石的ε_Hf（t）值为-3.26~-1.46，二阶段模式年龄介于1.25~1.59 Ga，结合该时期的地幔特征认为该岩石岩浆起源于中元古代亏损地幔新增生的下地壳部分熔融.综合认为岩石形成于蒙古-鄂霍茨克洋板块向南俯冲的活动大陆边缘环境.
- 花岗闪长岩 /
- 锆石U-Pb定年 /
- Hf同位素 /
- 埃达克岩 /
- 亏损地幔 /
- 漠河地区 /
- 地球化学 /
- 地质年代学
Abstract: Previous studies are mostly concentrated on the biotite granodiorites exposed during the Indosinian period in southern Mohe county, while the research on the Early Yanshanian tectonic evolution in this area is relatively weak. This paper presents new zircon U-Pb dating, Hf isotope, major and trace elements for biotite granodiorites in southern Mohe County for the discussion in their geochronology, magma sources and tectonic setting. Zircon dating results demonstrate that biotite granodiorites were formed in Early Jurassic (185±2 Ma and 182±2 Ma). Geochemically, these rocks have A/CNK=0.90~1.03, Mg^#=42~48, belonging to the high-K calc-alkaline series. The pluton has features similar to adakitic rock with high Sr (489×10^-6~653×10^-6) and low Yb (1.33×10^-6~1.99×10^-6). They have the geochemistry of arc magmatic rocks, which are enriched LREE and LILE (e.g., Rb and K), depleted HREE and HFSE (e.g., Nb, Ta and Ti), as well as very weak negative Eu anomalies (Eu/Eu^*=0.79~0.95), indicating that the magma source was derived from the partial melting of lower crust. Zircon ε_Hf(t) values and two-stage Hf model ages (t_DM2) of doitite granodoirites range from -3.26 to-1.46 and 1.25 Ga to 1.59 Ga, respectively, indicative of formation from primary magmas generated by partial melting of thickened low crust that formed from the depleted mantle during the Meso-to Neoproterozoic. Considering the regional tectonic revolution, we suggest that the diotite granodiorite was formed in the setting of continuous southward subduction of Mongol-Okhotsk oceanic plate during the Early Mesozoic.
- granodiorite /
- zircon U-Pb dating /
- Hf isotope /
- Adakite /
- depleted mantle /
- Mohe area /
- geochemistry /
- geochronology

HTML全文

图 1 中国东北地区构造分区图(a)和漠河地区地质简图(b)

图a中主要断裂：①牡丹江断裂，②敦化—密山断裂，③伊通—伊兰断裂，④索伦—西拉木伦—长春断裂，⑤贺根山—黑河断裂，⑥喜桂图—塔源断裂，⑦蒙古—鄂霍茨克缝合带；图b：1.中生代沉积岩, 2.古生代沉积岩, 3.前寒武纪基底, 4.中生代火山岩, 5.中生代花岗岩, 6.中生代花岗闪长岩, 7.时代不明的花岗岩, 8.主要断裂, 9.采样地点；图a据Wu et al.(2007)，图b据黑龙江省地质矿产局(1993)和李良等(2015)改编

Fig. 1. Simplified geological map of NE China, showing the main tectonic subdivisions (a) and detailed geological map of the Mohe area, Heilongjiang province (b)

下载: 全尺寸图片幻灯片

图 2 研究区黑云母花岗闪长岩手标本(a，b)和显微镜下照片(c~f)

Aln.褐帘石；Ap.磷灰石；Bi.黑云母；Or.正长石；Pl.斜长石；Pth.条纹长石；Q.石英；Spn.榍石

Fig. 2. Hand specimen photographs (a, b) and micrographs (c-f) of the biotite granodiorites in the study area

下载: 全尺寸图片幻灯片

图 3 黑云母花岗闪长岩部分锆石阴极发光图像

实线圆圈代表U-Pb分析点，虚线圆圈代表相应的Hf同位素分析点；MH-N3样品的锆石图中第一排数值为二阶段模式年龄，第二排数值为锆石U-Pb表面年龄

Fig. 3. CL images of zircons selected for analysis from biotite granodiorites

下载: 全尺寸图片幻灯片

图 4 漠河县城南黑云母花岗闪长岩样品锆石U-Pb年龄谐和图

Fig. 4. Zircon U-Pb concordia diagrams for biotite granodiorites in southern Mohe county

下载: 全尺寸图片幻灯片

图 5 黑云母花岗闪长岩QAP图解(a)、SiO₂-K₂O图解(b)和A/CNK-A/NK图解(c)

图a底图据Streckeisen(1976)；图b底图据Peccerillo and Taylor(1976)；图c底图据Maniar and Piccoli(1989)

Fig. 5. QAP (a), SiO₂ vs. K₂O (b) and A/CNK vs. A/NK (c) diagrams of biotite granodiorites

下载: 全尺寸图片幻灯片

图 6 黑云母花岗闪长岩稀土元素球粒陨石标准化配分图(a)和微量元素原始地幔标准化蛛网图(b)

图a底图据Boynton (1984)；图b底图据Sun and McDonough (1989)

Fig. 6. Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagrams (b) for biotite granodiorites

下载: 全尺寸图片幻灯片

图 7 黑云母花岗闪长岩锆石Hf同位素特征

兴-蒙造山带东段与燕山褶皱带Hf同位素组成引自Yang et al.(2006)；额尔古纳地块早中生代花岗质岩石的Hf同位素组成引自Tang et al.(2016)

Fig. 7. Hf isotopic compositions of zircons from biotite granodiorites

下载: 全尺寸图片幻灯片

图 8 黑云母花岗闪长岩Yb_N-(La/Yb)_N判别图解

底图据Defant and Drummond (1990)

Fig. 8. Yb_N vs. (La/Yb)_N diagram for biotite granodiorites

下载: 全尺寸图片幻灯片

图 9 黑云母花岗闪长岩Sr/Y-(La/Yb)_N(a)、Sr-10Y-Zr(b)和Y/Yb-Sr/Y-La/Yb(c)判别图解

图a底图据Liu et al.(2010)；图b和c的底图据朱弟成等(2002)

Fig. 9. The discrimination diagrams of Sr/Y-(La/Yb)_N (a), Sr-10Y-Zr (b) and Y/Yb-Sr/Y-La/Yb (c) for biotite granodiorites

下载: 全尺寸图片幻灯片

图 10 黑云母花岗闪长岩源区判别图解

底图据Patiño(1999)

Fig. 10. Discriminant diagrams of source regions for biotite granodiorites

下载: 全尺寸图片幻灯片

图 11 黑云母花岗闪长岩(Yb+Ta)-Rb(a)、(Y+Nb)-Rb(b)和R₁-R₂(c)构造判别图解

图a和b底图据Pearce et al.(1984)；图c底图据Batchelor and Bowden(1985)

Fig. 11. Tectonic discrimination diagrams of (Yb+Ta)-Rb (a), (Y+Nb)-Rb (b) and R₁-R₂ (c) for biotite granodiorites

下载: 全尺寸图片幻灯片

表 1 漠河县城南黑云母花岗闪长岩锆石LA-ICP-MS U-Pb同位素分析结果

Table 1. Zircon LA-ICP-MS U-Pb dating results for biotite granodiorites in southern Mohe county

分析点	含量(10^-6)			Th/U	同位素比值								同位素年龄(Ma)
分析点	Pb	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁸Pb/²³²Th	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁸Pb/²³²Th	1σ
MH-N3-01	17.3	406	473	0.86	0.052 4	0.002 3	0.207 7	0.007 1	0.028 8	0.000 4	0.008 9	0.000 2	301	52	192	6	183	3	180	3
MH-N3-02	9.32	67.4	262	0.26	0.054 0	0.003 9	0.216 5	0.014 2	0.029 1	0.000 6	0.010 5	0.000 6	370	112	199	12	185	4	210	11
MH-N3-03	12.5	176	372	0.47	0.050 9	0.002 4	0.203 0	0.009 2	0.028 9	0.000 4	0.009 1	0.000 1	237	111	188	8	184	3	183	2
MH-N3-04	10.7	177	304	0.58	0.050 1	0.002 4	0.200 2	0.007 5	0.029 0	0.000 4	0.008 4	0.000 2	199	60	185	6	184	3	169	3
MH-N3-05	22.6	49.5	595	0.08	0.049 9	0.001 9	0.199 8	0.006 9	0.029 0	0.000 4	0.009 2	0.000 1	190	88	185	6	185	3	184	2
MH-N3-06	9.23	77	269	0.29	0.051 3	0.002 6	0.204 6	0.008 4	0.028 9	0.000 4	0.010 5	0.000 3	256	66	189	7	184	3	211	6
MH-N3-07	8.96	78.1	225	0.35	0.052 0	0.002 8	0.207 5	0.009 5	0.028 9	0.000 5	0.009 7	0.000 3	287	76	191	8	184	3	196	6
MH-N3-08	7.52	93.8	220	0.43	0.053 8	0.002 7	0.215 9	0.009 0	0.029 1	0.000 4	0.010 3	0.000 3	363	66	199	7	185	3	207	5
MH-N3-09	12.7	95.2	356	0.27	0.050 8	0.002 7	0.204 7	0.009 2	0.029 2	0.000 5	0.009 9	0.000 3	231	75	189	8	186	3	199	6
MH-N3-10	12.8	125	369	0.34	0.051 9	0.002 8	0.211 5	0.009 6	0.029 6	0.000 5	0.008 9	0.000 3	279	74	195	8	188	3	179	5
MH-N3-11	16.7	370	459	0.81	0.050 3	0.002 0	0.202 9	0.005 7	0.029 3	0.000 4	0.008 6	0.000 1	209	40	188	5	186	3	172	3
MH-N3-12	8.73	68.8	270	0.25	0.053 3	0.002 9	0.213 1	0.009 8	0.029 0	0.000 5	0.009 2	0.000 3	342	74	196	8	184	3	185	6
MH-N3-13	14.7	252	430	0.59	0.051 1	0.002 4	0.203 8	0.007 4	0.028 9	0.000 4	0.009 1	0.000 2	245	56	188	6	184	3	184	4
MH-N3-14	18.7	207	525	0.39	0.053 2	0.002 3	0.212 1	0.006 8	0.028 9	0.000 4	0.009 3	0.000 2	337	47	195	6	184	3	188	4
MH-N3-15	16.4	248	432	0.57	0.051 6	0.003 1	0.207 5	0.012 1	0.029 2	0.000 5	0.009 2	0.000 1	268	141	191	10	185	3	185	2
MH-N3-16	96.4	643	1144	0.56	0.057 6	0.001 8	0.579 5	0.008 5	0.072 9	0.000 9	0.020 5	0.000 2	516	15	464	5	454	5	410	5
MH-N3-17	51.5	146	630	0.23	0.063 1	0.002 1	0.634 9	0.011 6	0.073 0	0.001 0	0.031 4	0.000 5	710	19	499	7	454	6	625	9
MH-N3-18	8.96	78.1	225	0.35	0.055 8	0.002 2	0.403 6	0.011 5	0.052 5	0.000 7	0.025 8	0.000 7	443	39	344	8	330	5	515	13
MH-N3-19	39.7	173	725	0.24	0.058 0	0.002 1	0.420 2	0.009 5	0.052 5	0.000 7	0.021 9	0.000 4	530	27	356	7	330	4	437	8
MH-N3-20	24.5	205	442	0.46	0.057 2	0.002 1	0.412 0	0.009 8	0.052 2	0.000 7	0.012 2	0.000 2	500	30	350	7	328	4	245	4
MH-N4-01	10.2	55.5	291	0.19	0.051 8	0.002 9	0.197 3	0.010 0	0.027 6	0.000 6	0.010 3	0.000 4	275	79	183	8	176	4	206	9
MH-N4-02	7.61	47.5	213	0.22	0.050 2	0.002 4	0.198 5	0.007 9	0.028 7	0.000 5	0.008 9	0.000 3	204	59	184	7	182	3	179	6
MH-N4-03	15.7	312	449	0.70	0.052 0	0.006 1	0.200 6	0.022 5	0.028 0	0.000 9	0.007 9	0.000 5	286	194	186	19	178	6	159	11
MH-N4-04	11.4	166	311	0.53	0.050 6	0.002 1	0.201 1	0.006 7	0.028 9	0.000 5	0.008 9	0.000 2	220	45	186	6	183	3	179	4
MH-N4-05	10.2	152	281	0.54	0.054 5	0.004 7	0.215 0	0.017 6	0.028 6	0.000 7	0.009 2	0.000 5	390	138	198	15	182	5	185	10
MH-N4-06	11	158	305	0.52	0.051 0	0.002 3	0.202 8	0.007 4	0.028 8	0.000 5	0.007 8	0.000 2	240	51	187	6	183	3	158	4
MH-N4-07	15.8	48.3	470	0.10	0.052 2	0.002 1	0.210 5	0.006 5	0.029 2	0.000 5	0.012 9	0.000 5	294	39	194	5	186	3	258	9
MH-N4-08	11.8	166	330	0.50	0.049 8	0.002 1	0.196 9	0.006 5	0.028 7	0.000 5	0.008 6	0.000 2	186	45	183	6	182	3	173	4
MH-N4-09	11.3	154	269	0.57	0.055 7	0.004 8	0.225 8	0.018 1	0.029 4	0.000 8	0.009 5	0.000 5	440	133	207	15	187	5	192	9
MH-N4-10	10.1	127	282	0.45	0.051 5	0.002 5	0.205 8	0.008 6	0.029 0	0.000 5	0.008 4	0.000 2	264	62	190	7	184	3	168	5
MH-N4-11	8.04	124	193	0.64	0.050 6	0.005 7	0.198 2	0.021 3	0.028 4	0.000 9	0.009 3	0.000 5	223	186	184	18	181	5	187	10
MH-N4-12	14.6	366	360	1.02	0.050 0	0.004 8	0.189 7	0.017 8	0.027 5	0.000 6	0.008 7	0.000 1	197	219	176	15	175	4	175	3
MH-N4-13	11.9	177	323	0.55	0.055 3	0.003 1	0.218 8	0.010 6	0.028 7	0.000 6	0.009 2	0.000 3	424	73	201	9	182	4	186	5
MH-N4-14	29.7	915	704	1.30	0.051 5	0.002 1	0.203 3	0.006 3	0.028 6	0.000 5	0.008 3	0.000 1	262	40	188	5	182	3	167	3
MH-N4-15	19.8	381	519	0.73	0.052 1	0.002 5	0.207 8	0.008 2	0.028 9	0.000 5	0.009 3	0.000 2	289	56	192	7	184	3	188	4
MH-N4-16	13.9	154	394	0.39	0.054 7	0.004 4	0.215 0	0.016 1	0.028 5	0.000 7	0.011 8	0.000 7	400	125	198	13	181	4	238	13
MH-N4-17	12.4	32	371	0.09	0.051 4	0.002 3	0.204 2	0.007 4	0.028 8	0.000 5	0.011 8	0.000 5	258	51	189	6	183	3	237	10
MH-N4-18	58.5	193	843	0.23	0.060 6	0.002 3	0.599 6	0.014 9	0.071 7	0.001 0	0.018 9	0.000 4	625	31	477	9	447	6	378	8
MH-N4-19	55.9	97.8	841	0.12	0.054 9	0.001 8	0.483 6	0.008 1	0.063 9	0.000 8	0.022 0	0.000 4	406	18	401	6	399	5	440	8

下载: 导出CSV

表 2 漠河县城南黑云母花岗闪长岩主量(%)、微量元素(10^-6)分析结果

Table 2. Major elements (%) and trace elements (10^-6) compositions for biotite granodiorites in southern Mohe county

样品号	MH-N3-B1	MH-N3-B2	MH-N3-B3	MH-N3-B4	MH-N4-B1	MH-N4-B2	MH-N4-B3
SiO₂	65.00	64.38	64.56	63.56	63.82	63.90	66.32
TiO₂	0.73	0.66	0.64	0.55	0.80	0.76	0.63
Al₂O₃	16.82	16.58	16.96	16.76	17.10	17.34	16.63
FeO^T	3.90	4.05	4.11	3.87	3.75	3.53	2.96
MnO	0.06	0.12	0.10	0.10	0.05	0.04	0.04
MgO	1.98	1.70	1.81	1.96	1.58	1.54	1.22
CaO	3.54	3.97	3.89	3.95	3.80	3.93	3.35
Na₂O	4.13	4.40	3.96	4.68	4.15	4.29	4.02
K₂O	2.89	2.68	2.71	3.39	2.98	2.74	3.13
P₂O₅	0.21	0.21	0.23	0.18	0.22	0.21	0.17
LOI	0.53	0.55	0.30	0.22	0.43	0.44	0.39
Total	99.91	99.40	99.40	99.40	99.28	99.27	99.34
ALK	7.02	7.08	6.67	8.07	7.14	7.03	7.15
Na₂O/K₂O	1.43	1.64	1.46	1.38	1.39	1.57	1.29
A/CNK	1.03	0.96	1.03	0.90	1.01	1.01	1.03
Mg^#	48	43	44	47	43	44	42
La	17.5	19.2	27.1	15.5	41.0	38.2	25.4
Ce	46.6	53.0	61.2	41.8	83.7	75.6	62.4
Pr	5.71	5.84	7.07	4.74	10.8	9.74	7.98
Nd	24.9	25.3	30.4	21.0	39.7	36.3	30.7
Sm	4.50	4.60	5.42	3.95	6.55	6.13	5.92
Eu	1.16	1.23	1.39	0.96	1.81	1.67	1.43
Gd	3.48	3.58	4.28	3.41	5.20	4.92	5.13
Tb	0.45	0.45	0.54	0.47	0.66	0.62	0.71
Dy	2.49	2.40	2.80	2.70	3.25	3.11	3.85
Ho	0.45	0.43	0.49	0.48	0.65	0.59	0.75
Er	1.37	1.29	1.51	1.47	1.82	1.67	2.10
Tm	0.20	0.19	0.23	0.21	0.28	0.26	0.30
Yb	1.39	1.35	1.58	1.33	1.99	1.76	1.83
Lu	0.20	0.21	0.24	0.19	0.31	0.29	0.27
ΣREE	111	119	144	98.1	198	181	149
HREE	10.0	9.89	11.7	10.3	14.2	13.2	14.9
(La/Yb)_N	9.08	10.2	12.3	8.36	14.8	15.6	10.0
Eu/Eu^*	0.90	0.92	0.88	0.80	0.95	0.93	0.79
V	82.3	76.9	81.5	58.9	85.0	79.0	69.0
Cr	6.24	7.63	9.01	7.06	6.56	8.34	7.83
Co	8.15	7.88	8.70	6.51	6.87	6.65	8.22
Ni	7.00	6.16	6.08	4.89	6.52	5.37	6.21
Sn	2.64	2.51	2.69	2.76	3.00	3.00	3.00
Cs	2.88	2.45	2.42	3.22	3.00	2.74	4.11
Rb	47.0	41.4	50.0	59.3	114	100	118
Sr	541	504	563	489	653	622	587
Y	11.3	12.6	15.3	11.9	19.4	17.3	21.7
Ba	649	604	620	614	987	823	943
Zr	204	88.2	261	43.9	250	220	210
Nb	12.8	12.1	13.1	12.2	16.5	14.5	15.1
Hf	3.52	1.81	4.53	1.03	6.60	6.10	5.30
Ta	0.94	0.92	1.01	0.94	1.50	1.40	1.40
Ga	28.2	26.5	27.8	26.4	27.9	26.3	26.4
Pb	14.4	14.2	14.8	15.4	18.6	17.3	20.7
Th	5.26	4.84	6.24	4.60	8.77	8.46	8.24
U	2.01	1.97	2.25	1.92	2.59	2.17	2.03

下载: 导出CSV

表 3 漠河县城南黑云母花岗闪长岩锆石Hf同位素分析结果

Table 3. Zircon Lu-Hf isotopic data for biotite granodiorites in southern Mohe county

分析点	t(Ma)	¹⁷⁶Yb/¹⁷⁷Hf	2σ	¹⁷⁶Lu/¹⁷⁷Hf	2σ	¹⁷⁶Hf/¹⁷⁷Hf	2σ	ε_Hf(0)	ε_Hf(t)	2σ	t_DM1(Hf)	t_DM2(Hf)	f_Lu/Hf
MH-N3-1	183	0.019 292	0.000 218	0.000 582	0.000 004	0.282 592	0.000 014	-6.36	-2.41	0.50	924	1 378	-0.98
MH-N3-2	185	0.013 751	0.000 062	0.000 434	0.000 002	0.282 582	0.000 014	-6.71	-2.70	0.49	934	1 398	-0.99
MH-N3-3	184	0.025 231	0.000 089	0.000 723	0.000 001	0.282 595	0.000 015	-6.26	-2.31	0.53	923	1 372	-0.98
MH-N3-4	184	0.011 502	0.000 151	0.000 376	0.000 003	0.282 574	0.000 015	-6.98	-2.99	0.52	943	1 416	-0.99
MH-N3-5	185	0.014 551	0.000 385	0.000 452	0.000 010	0.282 605	0.000 015	-5.92	-1.91	0.53	903	1 348	-0.99
MH-N3-6	184	0.022 926	0.000 311	0.000 697	0.000 013	0.282 613	0.000 016	-5.61	-1.65	0.56	897	1 331	-0.98
MH-N3-7	184	0.042 380	0.001 638	0.001 156	0.000 044	0.282 610	0.000 018	-5.74	-1.85	0.63	913	1 343	-0.97
MH-N3-8	185	0.028 355	0.000 905	0.000 768	0.000 021	0.282 618	0.000 018	-5.43	-1.46	0.63	891	1 319	-0.98
MH-N3-9	186	0.057 628	0.000 663	0.001 457	0.000 022	0.282 607	0.000 018	-5.85	-1.94	0.63	925	1 351	-0.96
MH-N3-10	188	0.025 143	0.000 246	0.000 757	0.000 008	0.282 592	0.000 013	-6.35	-2.32	0.46	928	1 376	-0.98
MH-N3-11	186	0.013 000	0.000 183	0.000 391	0.000 002	0.282 571	0.000 015	-7.12	-3.09	0.52	949	1 423	-0.99
MH-N3-12	184	0.022 687	0.000 141	0.000 679	0.000 004	0.282 617	0.000 017	-5.49	-1.53	0.60	892	1 323	-0.98
MH-N3-13	184	0.007 467	0.000 080	0.000 283	0.000 001	0.282 567	0.000 015	-7.26	-3.26	0.54	952	1 433	-0.99
MH-N3-14	184	0.020 418	0.000 221	0.000 590	0.000 005	0.282 617	0.000 016	-5.49	-1.52	0.57	889	1 322	-0.98
MH-N3-15	185	0.016 438	0.000 132	0.000 493	0.000 004	0.282 577	0.000 017	-6.88	-2.88	0.60	942	1 410	-0.99

下载: 导出CSV

参考文献(131)

Andersen, T., 2002.Correction of Common Lead in U-Pb Analyses that Do Not Report ²⁰⁴Pb.Chemical Geology, 192(1-2):59-79. https://doi.org/10.1016/s0009-2541(02)00195-x
Atherton, M.P., Petford, N., 1993.Generation of Sodium-Rich Magmas from Newly Underplated Basaltic Crust.Nature, 362:144-146. https://doi.org/10.1038/362144a0
Batchelor, R.A., Bowden, P., 1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology, 48(1-4):43-55. https://doi.org/10.1016/0009-2541(85)90034-8
Boynton, W. V, 1984. Geochemistry of the Rare Earth Elements: Meteorite Studies. In: Henderson, P., ed., Rare Earth Element Geochemistry. Elsevier, Amsterdam.
Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Region (BGMRI), 1991.Regional Geology of Inner Mongolia Autonomous Region.Geological Publishing House, Beijing (in Chinese).
Bureau of Geology and Mineral Resources of Heilongjiang Province (BGMRH), 1993.Regional Geology of Heilongjiang Province.Geological Publishing House, Beijing (in Chinese).
Castillo, P.R., Janney, P.E., Solidum, R.U., 1999.Petrology and Geochemistry of Camiguin Island, Southern Philippines:Insights to the Source of Adakites and Other Lavas in a Complex Arc Setting.Contributions to Mineralogy and Petrology, 134(1):33-51. https://doi.org/10.1007/s004100050467
Chen, Z.G., Zhang, L.C., Lu, B.Z., et al., 2010.Geochronology and Geochemistry of the Taipingchuan Copper-Molybdenum Deposit in Inner Mongolia, and Its Geological Significances.Acta Petrologica Sinica, 26(5):1437-1449 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201005010.htm
Chen, Z.G., Zhang, L.C., Wan, B., et al., 2011.Geochronology and Geochemistry of the Wunugetushan Porphyry Cu-Mo Deposit in NE China, and Their Geological Significance.Ore Geology Reviews, 43:92-105. https://doi.org/10.1016/j.oregeorev.2011.08.007
Chu, N.C., Taylor, R.N., Chavagnac, V., et al., 2002.Hf Isotope Ratio Analysis Using Multi-Collector Inductively Coupled Plasma Mass Spectrometry:An Evaluation of Isobaric Interference Corrections.Journal of Analytical Atomic Spectrometry, 17(12):1567-1574. https://doi.org/10.1039/b206707b
Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347:662-665. https://doi.org/10.1038/347662a0
Ding, H.X., Hou, Q.Y., Zhang, Z.M., 2016.Petrogenesis and Tectonic Significance of the Eocene Adakite-Like Rocks in Western Yunnan, Southeastern Tibetan Plateau.Lithos, 245:161-173. https://doi.org/10.1016/j.lithos.2015.09.024
Dong, Z.C., Gu, P.Y., Chen, R.M., et al., 2015.Geochronlogy, Geochemistry, and Hf Isotope of Yanchangbeishan Adamellite of Lenghu Area in Qinghai.Earth Science, 40(1):130-144(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2015.009
Francalanci, L., Taylor, S.R., McCulloch, M.T., et al., 1993.Geochemical and Isotopic Variations in the Calc-Alkaline Rocks of Aeolian Arc, Southern Tyrrhenian Sea, Italy:Constraints on Magma Genesis.Contributions to Mineralogy and Petrology, 113(3):300-313. https://doi.org/10.1007/bf00286923
Gao, S., Jin, Z.M., 1997.Delamination and Its Geodynamical Significance for the Crust-Mantle Evolution.Geological Scince and Technology Information, 16(1):1-8 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ701.000.htm
Gao, S., Rudnick, R.L., Yuan, H.L., et al., 2004.Recycling Lower Continental Crust in the North China Craton.Nature, 432:892-897. https://doi.org/10.1038/nature03162
Geng, J.Z., Li, H.K., Zhang, J., et al., 2011.Zircon Hf Isotope Analysis by Means of LA-MC-ICP-MS.Geological Bulletin of China, 30(10):1508-1513 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201110005.htm
Gill, J.B., 1987.Early Geochemical Evolution of an Oceanic Island Arc and Back Arc:Fiji and the South Fiji Basin.The Journal of Geology, 95(5):589-615. doi: 10.1086/629158
Gou, J., Sun, D.Y., Ren, Y.S., et al., 2013.Petrogenesis and Geodynamic Setting of Neoproterozoic and Late Paleozoic Magmatism in the Manzhouli-Erguna Area of Inner Mongolia, China:Geochronological, Geochemical and Hf Isotopic Evidence.Journal of Asian Earth Sciences, 67-68:114-137. https://doi.org/10.1016/j.jseaes.2013.02.016
Griffin, W.L., Wang, X., Jackson, S.E., et al., 2002.Zircon Chemistry and Magma Mixing, SE China:In-Situ Analysis of Hf Isotope, Tonglu and Pingtan Igneous Complexes.Lithos, 61(3-4):237-269. https://doi.org/10.1016/s0024-4937(02)00082-8
Hou, H.X., Zhang, D.H., Zhang, R.Z., 2016.The Chronology, Geochemical Characteristics and Geological Significance of the Mesozoic Shiyaogou Hidden Granite at the East Qinling.Earth Science, 41(10):1665-1682 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.122
Jiang, S.H., Nie, F.J., Su, Y.J., et al., 2010.Geochronology and Origin of the Erdenet Superlarge Cu-Mo Deposit in Mongolia.Acta Geoscientia Sinica, 31(3):289-306 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB201003005.htm
Kay, S.M., Mpodozis, C., 2001.Central Andean Ore Deposits Linked to Evolving Shallow Subduction Systems and Thickening Crust.GSA Today, 11(3):4-9.https://doi.org/10.1130/1052-5173(2001)011<0004:caodlt>2.0.co;2 doi: 10.1130/1052-5173(2001)011<0004:caodlt>2.0.co;2
Kravchinsky, V.A., Cogné, J.P., Harbert, W.P., et al., 2002.Evolution of the Mongol-Okhotsk Ocean as Constrained by New Palaeomagnetic Data from the Mongol-Okhotsk Suture Zone, Siberia.Geophysical Journal International, 148(1):34-57. https://doi.org/10.1046/j.1365-246x.2002.01557.x
Lai, S.C., Liu, C.Y., Yi, H.S., 2003.Geochemistry and Petrogenesis of Cenozoic Andesite-Dacite Associations from the Hoh Xil Region, Tibetan Plateau.International Geology Review, 45(11):998-1019. https://doi.org/10.2747/0020-6814.45.11.998
Li., B.L., Sun, Y.G., Chen, G.J., et al., 2016.Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition and Its Geological Implication of the Fine-Grained Syenogranite in Dong'an Goldfield from the Lesser Xing'an Mountains.Earth Science, 41(1):1-16 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.001
Li, J.Y., He, Z.J., Mo, S.G., et al., 2004a.The Age of Conglomerates in the Lower Part of the Xiufeng Formation in the Northern Da Hinggan Mountains, NE China, and Their Tectonic Implications.Geological Bulletin of China, 23(2):120-129(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200402003.htm
Li, J.Y., Mo, S.G., He, Z.J., et al., 2004b.The Timing of Crustal Sinistral Strike-Slip Movement in the Northern Great Khing'an Ranges and Its Constraint on Reconstruction of the Crustal Tectonic Evolution of NE China and Adjacent Areas since the Mesozoic.Earth Science Frontiers, 11(3), 157-167 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200403022.htm
Li, J.Y., Zhang, J., Yang, T.N., et al., 2009.Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas.Journal of Jilin University (Earth Science Edition), 39(4):584-605 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200904002.htm
Li, L., Sun, F.Y., Li, B.L., et al., 2015.Ore-Forming Fluid Features and Genesis of Shabaosi Gold Deposit in Mohe County, Heilongjiang Province.Earth Science, 40(7):1163-1176 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2015.097
Li, L., Sun, F.Y., Li, B.L., et al., 2017.Geochronology of Ershi'erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance.Earth Science, 42(1):35-52 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.003
Li, Y., Ding, L.L., Xu, W.L., et al., 2015.Geochronology and Geochemistry of Muscovite Granites in Sunwu Area, NE China:Implications for the Timing of Closure of the Mongol-Okhotsk Ocean.Acta Petrologica Sinica, 31(1):56-66 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201501004.htm
Liu, J.L., Sun, F.Y., Li, L., et al., 2015a.Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone.Earth Science, 40(6):965-981 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2015.081
Liu, J.L., Sun, F.Y., Lin, B.L., 2015b.Geochronology, Geochemistry and Zircon Hf Isotope of Miantian Granodiorite Intrusion in Yanbian Region, Southern Jilin Province and Its Geological Significance.Earth Science, 40(1):49-60 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2015.004
Liu, J.L., Sun, F.Y., Zhang, Y.J., et al., 2016.Zircon U-Pb Geochronology, Geochemistry and Hf Isotopes of Nankouqian Granitic Intrusion in Qingyuan Region, Liaoning Province.Earth Science, 41(1):55-66 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.004
Liu, S.A., Li, S.G., He, Y.S., et al., 2010.Geochemical Contrasts between Early Cretaceous Ore-Bearing and Ore-Barren High-Mg Adakites in Central-Eastern China:Implications for Petrogenesis and Cu-Au Mineralization.Geochimica et Cosmochimica Acta, 74(24):7160-7178. https://doi.org/10.1016/j.gca.2010.09.003
Ludwig, K. R., 2003. User's Manual for Isoplot 3. 00: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication, Berkeley.
Macpherson, C.G., Dreher, S.T., Thirlwall, M.F., 2006.Adakites Without Slab Melting:High Pressure Differentiation of Island Arc Magma, Mindanao, the Philippines.Earth and Planetary Science Letters, 243(3-4), 581-593. doi: 10.1016/j.epsl.2005.12.034
Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2 doi: 10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
Martin, H., 1999.Adakitic Magmas:Modern Analogues of Archaean Granitoids.Lithos, 46(3):411-429. https://doi.org/10.1016/s0024-4937(98)00076-0
McKenzie, D., 1989.Some Remarks on the Movement of Small Melt Fractions in the Mantle.Earth and Planetary Science Letters, 95(1-2):53-72. https://doi.org/10.1016/0012-821x(89)90167-2
Meng, E., Xu.W, L., Yang, D.B., et al., 2011.Zircon U-Pb Chronology, Geochemistry of Mesozoic Volcanic Rocks from the Lingquan Basin in Manzhouli Area, and Its Tectonic Implications.Acta Petrologica Sinica, 27(4):1209-1226 (in Chinese with English abstract). http://www.oalib.com/paper/1475699
Mo, S.G., Han, M.L., Li, J.Y., 2005.Compositions and Orogenic Processes of Mongolia-Okhotsk Orogen.Journal of Shandong University of Science and Technology (Natural Science), 24(3):50-52 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SDKY200503013.htm
Orolmaa, D., Erdenesaihan, G., Borisenko, A.S., et al., 2008.Permian-Triassic Granitoid Magmatism and Metallogeny of the Hangayn (central Mongolia).Russian Geology and Geophysics, 49(7):534-544. https://doi.org/10.1016/j.rgg.2008.06.008
Oyarzun, R., Márquez, A., Lillo, J., et al., 2001.Giant Versus Small Porphyry Copper Deposits of Cenozoic Age in Northern Chile:Adakitic Versus Normal Calc-Alkaline Magmatism.Mineralium Deposita, 36(8):794-798. https://doi.org/10.1007/s001260100205
Parfenov, L.M., Popeko, L.I., Tomurtogoo, O., 2001.Problems of Tectonics of the Mongolia-Okhotsk Orogenic Belt.Geology of the Pacific Ocean, 16(5):797-830. https://elibrary.ru/item.asp?id=13370628
Patchett, P.J., Tatsumoto, M., 1980.A Routine High-Precision Method for Lu-Hf Isotope Geochemistry and Chronology.Contributions to Mineralogy and Petrology, 75(3):263-267. https://doi.org/10.1007/bf01166766
Patiño, D.A.E., 1999.What do Experiments Tell Us about the Relative Contributions of Crust and Mantle to the Origin of Granitic Magmas? In:Castro, A., Fernandez, C., Vigneressese, J.L., eds., Understanding Granites:Intergrating New and Classical Techniques.Geological Society, London, Special Publication, 168:55-75. doi: 10.1144/GSL.SP.1999.168.01.05
Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology, 25(4):956-983. https://doi.org/10.1093/petrology/25.4.956
Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81. https://doi.org/10.1007/bf00384745
Qin, K.Z., Li, H.M., Li, W.S., et al., 1999.Intrusion and Mineralization Ages of the Wunugetushan Porphyry Cu-Mo Deposit, Inner Mongolia, Northwestern China.Geological Review, 45(2):180-185 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199902014.htm
Qin, X.F., Yin, Z.G., Wang, Y., et al., 2007.Early Paleozoic Adakitic Rocks in Mohe Area at the Northern End of the Da Hinggan Mountains and Their Geological Significance.Acta Petrologica Sinica, 23(6):1501-1511 (in Chinese with English abstract). https://doi.org/10.3969/j.issn.1000-0569.2007.06.024
Qiu, J.X., 2004.Opening-Closing Tectonics and Magmatic Activity.Geological Bulletin of China, 23(3):222-231 (in Chinese with English abstract). https://doi.org/10.3969/j.issn.1671-2552.2004.03.008
Rabbia, O.M., Correa, K.J., Hernández, L.B., et al., 2017."Normal" to Adakite-Like Arc Magmatism Associated with the El Abra Porphyry Copper Deposit, Central Andes, Northern Chile.International Journal of Earth Sciences, 106(8):2687-2711. https://doi.org/10.1007/s00531-017-1454-0
Rapp, R.P., Watson, E.B., 1995.Dehydration Melting of Metabasalt at 8-32 Kbar:Implications for Continental Growth and Crust-Mantle Recycling.Journal of Petrology, 36(4):891-931. https://doi.org/10.1093/petrology/36.4.891
Richards, J.P., Kerrich, R., 2007.Special Paper:Adakite-Like Rocks:Their Diverse Origins and Questionable Role in Metallogenesis.Economic Geology, 102(4):537-576. https://doi.org/10.2113/gsecongeo.102.4.537
Sajona, F.G., Maury, R.C., 1998.Association of Adakites with Gold and Copper Mineralization in the Philippines.Comptes Rendus de I'Académie des Sciences-Series ⅡA-Earth and Planetary Science, 326(1):27-34. https://doi.org/10.1016/s1251-8050(97)83200-4
Stern, C.R., Kilian, R., 1996.Role of the Subducted Slab, Mantle Wedge and Continental Crust in the Generation of Adakites from the Andean Austral Volcanic Zone.Contributions to Mineralogy and Petrology, 123:263-281. doi: 10.1007/s004100050155
Streckeisen, A.L., 1976.Classification of the Common Igneous Rocks by Means of Their Chemical Composition:A Provisional Attempt.Neues Jahrbuch für Mineralogie-Monatshefte, 1:1-15. https://eurekamag.com/research/018/290/018290717.php
Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.In:Saunders, A.D., Norry, M.J., eds., Magmatism in Ocean Basins.Geological Society, London, Special Publications, 42(1):313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
Tang, J., Xu, W.L., Wang, F., et al., 2014.Geochronology and Geochemistry of Early-Middle Triassic Magmatism in the Erguna Massif, NE China:Constraints on the Tectonic Evolution of the Mongol-Okhotsk Ocean.Lithos, 184-187:1-16. https://doi.org/10.1016/j.lithos.2013.10.024
Tang, J., Xu, W.L., Wang, F., et al., 2016.Early Mesozoic Southward Subduction History of the Mongol-Okhotsk Oceanic Plate:Evidence from Geochronology and Geochemistry of Early Mesozoic Intrusive Rocks in the Erguna Massif, NE China.Gondwana Research, 31:218-240. https://doi.org/10.1016/j.gr.2014.12.010
Thiéblemont, D., Stein, G., Lescuyer, J.L., 1997.Gisements Épithermaux et Porphyriques:La Connexion Adakite.Comptes Rendus de I'Académie des Sciences-Series ⅡA-Earth and Planetary Science, 325(2):103-109. https://doi.org/10.1016/s1251-8050(97)83970-5
Tomurtogoo, O., Windley, B.F., Kroner, A., et al., 2005.Zircon Age and Occurrence of the Adaatsag Ophiolite and Muron Shear Zone, Central Mongolia:Constraints on the Evolution of the Mongol-Okhotsk Ocean, Suture and Orogen.Journal of the Geological Society, 162(1):125-134. https://doi.org/10.1144/0016-764903-146
Wang, Q., Zhao, Z.H., Bai, Z.H., et al., 2003a.Carboniferous Adakites and Nb-Enriched Arc Basaltic Rocks Association in the Alataw Mountains, North Xinjiang:Interactions between Slab Melt and Mantle Peridotite and Implications for Crustal Growth.Chinese Science Bulletin, 48(19):2108-2115. https://doi.org/10.1007/bf03037015
Wang, Q., Zhao, Z.H., Xu, J.F., et al., 2003b.Petrologenesis and Metallogenesis of the Yanshanian Adakite-Like Rocks in the Eastern Yangtze Block.Science China Earth Sciences, 46(Supp.):164-176. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxg2003s2013&dbname=CJFD&dbcode=CJFQ
Wang, Q., Zhao, Z.H., Xu, J.F., et al., 2006.Carboniferous Adakite-High-Mg Andesite-Nb-Enriched Basaltic Rock Suites in the Northern Tianshan Area:Implications for Phanerozoic Crustal Growth in the Central Asia Orogenic Belt and Cu-Au Mineralization.Acta Petrologica Sinica, 22(1):11-30 (in Chinese with English abstract). http://www.oalib.com/paper/1471327
Wang, Z.L., Jin, J., Li, Z.L., et al., 2010.Zircon U-Pb Ages and Hf Isotopic Characteristics of Mineralized Porphyries in the Mordaoga Area, Northern-Central Da Hinggan Mountains, and Their Metallogenic Significance.Acta Petrologica et Mineralogica, 29(6):796-810 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201006015.htm
Wei, Z.L., Zhang, H., Guo, W.M., et al., 2008.LA-ICP-MS Zircon U-Pb Dating:Constraints on Late Mesozoic Regional Unconformity Timing in the Northern Hebei-Western Liaoning Provinces.Progress in Natural Science, 18(10):1119-1127 (in Chinese).
Weng, W.F., Zhi, L.G., Cai, L.Y., et al., 2011.Geochemical Characteristics and Petrogenesis of the Mesozoic Adakite in South Anhui Province.Geological Survey and Research, 34(2):98-107 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ201102001.htm
Wu, F.Y., Sun, D.Y., Ge, W.C., et al., 2011.Geochronology of the Phanerozoic Granitoids in Northeastern China.Journal of Asian Earth Sciences, 41(1):1-30. https://doi.org/10.1016/j.jseaes.2010.11.014
Wu, F.Y., Zhao, G.C., Sun, D.Y., 2007.The Hulan Group:Its Role in the Evolution of the Central Asian Orogenic Belt of NE China.Journal of Asian Earth Sciences, 30(3-4):542-556. https://doi.org/10.1016/j.jseaes.2007.01.003
Wu, G., Chen, Y.C., Chen, Y.J., et al., 2012.Zircon U-Pb Ages of the Metamorphic Supracrustal Rocks of the Xinghuadukou Group and Granitic Complexes in the Argun Massif of the Northern Great Hinggan Range, NE China, and Their Tectonic Implications.Journal of Asian Earth Sciences, 49:214-233. https://doi.org/10.1016/j.jseaes.2011.11.023
Wu, G., Chen, Y.J., Sun, F.Y., et al., 2008.Geochemistry of the Late Jurassic Granitoids in the Northern End Area of Da Hinggan Mountains and Their Geological and Prospecting Implications.Acta Petrologica Sinica, 24(4):899-910 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200804029.htm
Wu, G., Sun, F.Y., Zhao, C.S., et al., 2005.Discovery of the Early Paleozoic Post-Collisional Granites in Northern Margin of Erguna Massif and Its Geological Significance.Chinese Science Bulletin, 50(20):2278-2288 (in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jxtw200523012&dbname=CJFD&dbcode=CJFQ
Wu, G., Sun, F.Y., Zhao, C.S., et al., 2007.Fluid Inclusion Study on Gold Deposits in Northwestern Erguna Metallogenic Belt, China.Acta Petrologica Sinica, 23(9):2227-2240 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200709021.htm
Xiao, L., Clemens, J.D., 2007.Origin of Potassic (C-Type) Adakite Magmas:Experimental and Field Constraints.Lithos, 95(3-4):399-414. https://doi.org/10.1016/j.lithos.2006.09.002
Xiong, X.L., Adam, J., Green, T.H., et al., 2005.Trace Element Characteristics of Partial Melts Produced by Melting of Metabasalts at High Pressures:Constraints on the Formation Condition of Adakitic Melts.Science China Earth Sciences, 49(9):915-925. https://doi.org/10.1007/s11430-006-0915-2
Xiong, X.L., Li, X.H., Xu, J.F., et al., 2003.Extremely High Na Adakite-Like Magmas Derived from Lower Crust Basaltic Underplate:the Zhantang Andesitc Rocks from Huichang Basin, SE China.Geochemical Journal, 37:233-252. https://doi.org/10.2343/geochemj.37.233
Xu, W.L., Pei, F.P., Wang, F., et al., 2013.Spatial-Temporal Relationships of Mesozoic Volcanic Rocks in NE China:Constraints on Tectonic Overprinting and Transformations between Multiple Tectonic Regimes.Journal of Asian Earth Sciences, 74:167-193. https://doi.org/10.1016/j.jseaes.2013.04.003
Xu, W.L., Wang, F., Pei, F.P., et al., 2013.Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations.Acta Petrologica Sinica, 29(2):339-353(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201302002.htm
Yang, J.H., Wu, F.Y., Shao, J.A., et al., 2006.Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt, North China.Earth and Planetary Science Letters, 246(3-4):336-352. https://doi.org/10.1016/j.epsl.2006.04.029
Yuan, H.L., Gao, S., Liu, X.M., et al., 2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 28(3):353-370. https://doi.org/10.1111/j.1751-908x.2004.tb00755.x
Zeng, W.S., Zhou, J.B., Dong, C., et al., 2014.Subduction Record of Mongol-Okhotsk Ocean:Constraints from Badaguan Metamorphic Complexes in the Erguna Massif, NE China.Acta Petrologica Sinica, 30(7):1948-1960 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201407010.htm
Zhang, J.F., Li, Z.T., Jin, C.Z., 2004.Adakites in Northeastern China and Their Mineralized Implications.Acta Petrologica Sinica, 20(2):361-368 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200402015.htm
Zhang, J.H., Ge, W.C., Wu, F.Y., et al., 2008.Large-Scale Early Cretaceous Volcanic Events in the Northern Great Xing'an Range, Northeastern China.Lithos, 102(1-2):138-157. https://doi.org/10.1016/j.lithos.2007.08.011
Zhang, Q., Wang, Y., Qian, Q., et al., 2001.The Characteristics and Tectonic-Meltallogenic Significances of the Adakites in Yanshan Period from Eastern China.Acta Petrologia Sinica, 17(2):236-244 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200102007.htm
Zhang, Q., Xu, J.F., Wang, Y., et al., 2004.Diversity of Adakite.Geological Bulletin of China, 23(9-10):959-965 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD2004Z2019.htm
Zhang, Q., Yin, X.M., Yin, Y., et al., 2009.Issues on Metallogenesis and Prospecting of Gold and Copper Deposits Related to Adakite and Himalayan Type Granite in West Qinling.Acta Petrologica Sinica, 25(12):3103-3122 (in Chinese with English abstract). http://www.oalib.com/paper/1470976
Zhao, S., Xu, W.L., Tang, J., et al., 2016.Timing of Formation and Tectonic Nature of the Purportedly Neoproterozoic Jiageda Formation of the Erguna Massif, NE China:Constraints from Field Geology and U-Pb Geochronology of Detrital and Magmatic Zircons.Precambrian Research, 281:585-601. https://doi.org/10.1016/j.precamres.2016.06.014
Zhao, X., Coe, R.S., Zhou, Y.X., et al., 1990.New Paleomagnetic Results from Northern China:Collision and Suturing with Siberia and Kazakhstan.Tectonophysics, 181(1-4):43-81. https://doi.org/10.1016/0040-1951(90)90008-v
Zhu, D.C., Duan, L.P., Liao, Z.L., et al., 2002.Discrimination for Two Kinds of Adakites.Journal of Mineralogy and Petrology, 22(3):5-9 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KWYS200203001.htm
Zonenshain, L. P., Kuzmin, M. I., Natapov, L. M., et al., 1990. Geology of the USSR: A Plate-Tectonic Synthesis. American Geophysical union, Washington, D. C. .
Zorin, Y.A., 1999.Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt, Trans-Baikal Region (Russia) and Mongolia.Tectonophysics, 306(1):33-56. https://doi.org/10.1016/s0040-1951(99)00042-6
陈志广, 张连昌, 卢百志, 等, 2010.内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义.岩石学报, 26(5):1437-1449. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201005010&dbname=CJFD&dbcode=CJFQ
董增产, 辜平阳, 陈锐明, 等, 2015.柴北缘西端盐场北山二长花岗岩年代学、地球化学及其Hf同位素特征.地球科学, 40(1):130-144.doi: 10.3799/dqkx.2015.009
高山, 金振民, 1997.拆沉作用(delamination)及其壳-幔演化动力学意义.地质科技情报, 16(1):1-9. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkq701.000&dbname=CJFD&dbcode=CJFQ
耿建珍, 李怀坤, 张健, 等, 2011.锆石Hf同位素组成的LA-MC-ICP-MS测定.地质通报, 30(10):1508-1513.doi: 10.3969/j.issn.1671-2552.2011.10.004
黑龙江省地质矿产局, 1993.黑龙江省区域地质志.北京:地质出版社.
侯红星, 张德会, 张荣臻, 2016.东秦岭中生代石瑶沟隐伏花岗岩年代学、地球化学特征及地质意义.地球科学, 41(10):1665-1682.doi: 10.3799/dqkx.2016.122
江思宏, 聂凤军, 苏永江, 等, 2010.蒙古国额尔登特特大型铜-钼矿床年代学与成因研究.地球学报, 31(3):289-306. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqxb201003005&dbname=CJFD&dbcode=CJFQ
李碧乐, 孙永刚, 陈广俊, 等, 2016.小兴安岭东安金矿区细粒正长花岗岩U-Pb年龄、岩石地球化学、Hf同位素组成及地质意义.地球科学, 41(1):1-16.doi: 10.3799/dqkx.2016.001
李锦轶, 和政军, 莫申国, 等, 2004a.大兴安岭北部绣峰组下部砾岩的形成时代及其大地构造意义.地质通报, 23(2):120-129. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd200402003&dbname=CJFD&dbcode=CJFQ
李锦轶, 莫申国, 何政军, 等, 2004b.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约.地学前缘, 11(3):157-168. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy200403022&dbname=CJFD&dbcode=CJFQ
李锦轶, 张进, 杨天南, 等, 2009.北亚造山区南部及其毗邻地区地壳构造分区与构造演化.吉林大学学报(地球科学版), 39(4):584-605. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ccdz200904002&dbname=CJFD&dbcode=CJFQ
李良, 孙丰月, 李碧乐, 等, 2015.黑龙江省漠河县砂宝斯金矿床流体特征及矿床成因.地球科学, 40(7):1163-1176.doi: 10.3799/dqkx.2015.097
李良, 孙丰月, 李碧乐, 等, 2017.漠河盆地二十二站组砂岩形成时代及物源区构造环境判别.地球科学, 42(1):35-52.doi: 10.3799/dqkx.2017.003
李宇, 丁磊磊, 许文良, 等, 2015.孙吴地区中侏罗世白云母花岗岩的年代学与地球化学:对蒙古-鄂霍茨克洋闭合时间的限定.岩石学报, 31(1):56-66. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201501004&dbname=CJFD&dbcode=CJFQ
刘金龙, 孙丰月, 李良, 等, 2015a.青海阿尼玛卿蛇绿混杂岩带西段哥日卓托杂岩体年代学、地球化学及Hf同位素.地球科学, 40(6):965-981.doi: 10.3799/dqkx.2015.081
刘金龙, 孙丰月, 林博磊, 等, 2015b.吉林延边地区棉田岩体锆石U-Pb年代学、地球化学及Hf同位素.地球科学, 40(1):49-60.doi: 10.3799/dqkx.2015.004
刘金龙, 孙丰月, 张雅静, 等, 2016.辽宁省清原县南口前岩体锆石U-Pb年代学、地球化学及Hf同位素.地球科学, 41(1):55-66.doi: 10.3799/dqkx.2016.004
孟恩, 许文良, 杨德彬, 等, 2011.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学、地球化学及其地质意义.岩石学报, 27(4):1209-1226. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201104029&dbname=CJFD&dbcode=CJFQ
莫申国, 韩美莲, 李锦轶, 2005.蒙古-鄂霍茨克造山带的组成及造山过程.山东科技大学学报(自然科学版), 24(3):50-52. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=sdky200503013&dbname=CJFD&dbcode=CJFQ
内蒙古自治区地质矿产局, 1991.内蒙古自治区区域地质志.北京:地质出版社.
秦克章, 李惠民, 李伟实, 等, 1999.内蒙古乌奴格吐山斑岩铜钼矿床的成岩、成矿时代.地质论评, 45(2):180-185. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzlp199902014&dbname=CJFD&dbcode=CJFQ
秦秀峰, 尹志刚, 汪岩, 等, 2007.大兴安岭北端漠河地区早古生代埃达克质岩特征及地质意义.岩石学报, 23(6):1501-1511. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200706023&dbname=CJFD&dbcode=CJFQ
邱家骧, 2004.开合构造与岩浆活动.地质通报, 23(3):222-231. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd200403005&dbname=CJFD&dbcode=CJFQ
王强, 赵振华, 许继峰, 等, 2006.天山北部石炭纪埃达克岩-高镁安山岩-富Nb岛弧玄武质岩:对中亚造山带显生宙地壳增生与铜金成矿的意义.岩石学报, 22(1):11-30. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200601002&dbname=CJFD&dbcode=CJFQ
王召林, 金浚, 李占龙, 等, 2010.大兴安岭中北段莫尔道嘎地区含矿斑岩的锆石U-Pb年龄、Hf同位素特征及成矿意义.岩石矿物学杂志, 29(6):796-810. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=yskw201006015&dbname=CJFD&dbcode=CJFQ
韦忠良, 张宏, 郭文敏, 等, 2008.LA-ICP-MS锆石U-Pb测年对辽西-冀北地区晚中生代区域性角度不整合时代的约束.自然科学进展, 18(10):1119-1127. doi: 10.3321/j.issn:1002-008X.2008.10.005
翁望飞, 支利庚, 蔡连友, 等, 2011.皖南中生代高钾钙碱性埃达克岩地球化学特征及岩石成因.地质调查与研究, 34(2):98-107. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=qhwj201102001&dbname=CJFD&dbcode=CJFQ
武广, 孙丰月, 赵财胜, 等, 2005.额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义.科学通报, 50(20):2278-2288. doi: 10.3321/j.issn:0023-074X.2005.20.017
武广, 孙丰月, 赵财胜, 等, 2007.额尔古纳成矿带西北部金矿床流体包裹体研究.岩石学报, 23(9):2227-2240. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200709021&dbname=CJFD&dbcode=CJFQ
武广, 陈衍景, 孙丰月, 等, 2008.大兴安岭北端晚侏罗世花岗岩类地球化学及其地质和找矿意义.岩石学报, 24(4):899-910. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200804029&dbname=CJFD&dbcode=CJFQ
许文良, 王枫, 裴福萍, 等, 2013.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约.岩石学报, 29(2):339-353. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201302002&dbname=CJFD&dbcode=CJFQ
曾维顺, 周建波, 董策, 等, 2014.蒙古-鄂霍茨克洋俯冲的记录:额尔古纳地区八大关变质杂岩的证据.岩石学报, 30(7):1948-1960. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201407010&dbname=CJFD&dbcode=CJFQ
张炯飞, 李之彤, 金成洙, 2004.中国东北部地区埃达克岩及其成矿意义.岩石学报, 20(2):361-368. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200402015&dbname=CJFD&dbcode=CJFQ
张旗, 王焰, 钱青, 等, 2001.中国东部燕山期埃达克岩的特征及其构造-成矿意义.岩石学报, 17(2):236-244. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200102007&dbname=CJFD&dbcode=CJFQ
张旗, 许继峰, 王焰, 等, 2004.埃达克岩的多样性.地质通报, 23(9-10):959-965. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd2004z2019&dbname=CJFD&dbcode=CJFQ
张旗, 殷先明, 殷勇, 等, 2009.西秦岭与埃达克岩和喜马拉雅型花岗岩有关的金铜成矿及找矿问题.岩石学报, 25(12):3103-3122. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200912003&dbname=CJFD&dbcode=CJFQ
朱弟成, 段丽萍, 廖忠礼, 等, 2002.两类埃达克岩的判别.矿物岩石, 22(3):5-9. http://www.cnki.com.cn/Article/CJFDTOTAL-KWYS200203001.htm