桂中都安-马山煌斑岩成因及其构造意义

唐远兰; 时毓; 王永强; 孙艺容; 刘希军

doi:10.3799/dqkx.2020.306

桂中都安-马山煌斑岩成因及其构造意义

doi: 10.3799/dqkx.2020.306

唐远兰^{1, 2, ,},
时毓^{1, 2, ,},
王永强^{1, 2},
孙艺容^{1, 2},
刘希军^{1, 2}

1.
桂林理工大学广西隐伏金属矿产勘查重点实验室, 广西桂林 541006
2.
桂林理工大学有色金属矿产勘查与资源高效利用协同创新中心, 广西桂林 541006

基金项目:

国家自然科学基金项目 41862003

国家自然科学基金项目 41562005

广西杰出自然科学基金项目 2019GXNSFFA245005

广西杰出自然科学基金项目 2018GXNSFFA281009

详细信息

作者简介:
唐远兰(1995-), 女, 硕士, 现主要从事岩石学研究.ORCID: 0000-0003-0496-7756.E-mail: 1132726253@qq.com

通讯作者:
时毓, E-mail: shiyu_61@163.com

中图分类号: P581;P597.3
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出版历程
- 收稿日期: 2020-09-20
- 刊出日期: 2021-06-15

Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi

Tang Yuanlan^{1, 2
,
,},
Shi Yu^{1, 2
, ,},
Wang Yongqiang^{1, 2},
Sun Yirong^{1, 2},
Liu Xijun^{1, 2}

1.
Guangxi Key Laboratory of Exploration for Hidden Metallic Ore Deposits, Guilin University of Technology, Guilin 541006, China
2.
Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources, Guilin University of Technology, Guilin 541006, China

摘要

摘要: 为精确厘定桂中地区都安-马山带煌斑岩的形成时代并探讨其源区属性、构造环境及其动力学背景，对其进行了LA-ICP-MS锆石U-Pb定年、⁴⁰Ar-³⁹Ar金云母定年、Hf同位素分析测试和全岩地球化学研究.结果表明，锆石U-Pb定年未能成功限定煌斑岩的成岩年龄，但煌斑岩中发育大量2 578~1 650 Ma的捕获锆石，指示其存在太古宙-古元古代变质基底.金云母⁴⁰Ar-³⁹Ar定年结果限定了煌斑岩的侵位年龄为100.4±0.99 Ma.Hf同位素研究表明，ε_Hf（t）有正有负，且正值多于负值，表明岩浆源区主要以新生地壳为主，存在部分古老地壳的再循环.全岩地球化学分析显示，煌斑岩具有较低的SiO₂含量（47.66%~50.93%）及高的K₂O含量（4.98%~6.77%）、富集LILE和LREE而亏损HFSE（如Nb、Ta和Ti），表现出富集地幔和俯冲流体交代作用的特征.桂中煌斑岩形成过程中，地壳混染作用十分有限，主要形成过程为：流体交代的富集地幔，在燕山晚期岩石圈的拉张-伸展背景下，部分熔融形成煌斑岩岩浆，同时NNW向的南丹-昆仑关大断裂为岩浆的侵位提供了通道.研究区煌斑岩形成于太平洋和印度板块向欧亚板块俯冲碰撞的动力学背景下.
- 煌斑岩 /
- ⁴⁰Ar-³⁹Ar年龄 /
- 地球化学 /
- 燕山期 /
- 动力学背景
Abstract: In order to determine the formation age of lamprophyre accurately in Du'an-Mashan belt, Central Guangxi, and to discuss its source property, tectonic environment and dynamic setting, LA-ICP-MS zircon U-Pb dating, ⁴⁰Ar-³⁹Ar phlogopite dating, ε_Hf isotope and whole-rock geochemistry were obtained. It shows that zircon U-Pb dating fails to determine the fomation age of lamprophyres, however, a mass of captured zircons ranging from 2 578 Ma to 1 650 Ma indicates the existence of the Archean-Paleoproterozoic metamorphic basement. The phlogopite ⁴⁰Ar/³⁹Ar age of 100.4±0.99 Ma displayes the formation age of the lamprophyres. Zircons yield both positive and negative ε_Hf(t) values (with mostly positive), suggesting that the protolith was derived from newborn crust that incorporated a few evolved ancient continental crustal components. Geochemical data exhibit that lamprophyres have low SiO₂ (47.66%-50.93%) and high K₂O (4.98%-6.77%) contents, with relatively high LILE and LREE and low HFSE (such as Nb, Ta and Ti) contents, indicating the characteristics of enriched mantle and subducted fluid metasomatism. During the formation of lamprophyres in Central Guangxi, crustal contamination is very limited, and the main formation process is as follows: under the background of lithospheric extension in the Late Yanshanian, the enriched mantle which was metasomatic was partially melted to form lamprophyre magma, and the Nandan-Kunlunguan fault extending in the NNW direction provided a channel for the magma fluid. The lamprophyres formed under the dynamic setting of subduction and collision of Pacific and Indian plate to Eurasian plate.
- lamprophyre /
- ⁴⁰Ar-³⁹Ar dating /
- geochemistry /
- Yanshanian /
- dynamic setting

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图 1 华南构造格局简图

①澜沧江缝合带; ②昌宁-孟连缝合带; ③金沙江缝合带; ④哀牢山缝合带; ⑤八布缝合带; ⑥SongMa缝合带; ⑦勉略缝合带; ⑧商丹缝合带; 据Yang et al.(2012)

Fig. 1. Simplified tectonic framework of South China

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图 2 桂中地区地质简图及采样位置

图a中，1.二级构造单元; 2.三级构造单元; 3.四级构造单元; 4.区域断裂; 5.研究区; 6.煌斑岩分布区; Ⅰ.都阳山褶皱; Ⅱ.灵马褶皱; Ⅲ.来宾褶皱; Ⅳ.西大明山凸起; V.十万大山断陷; VI.大瑶山隆起; a.改自广西壮族自治区地质矿产局（1992）；b.改自Yang et al.（2012）

Fig. 2. Simplified geological map of Central Guangxi and the sampling locations

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图 3 河池都安煌斑岩(17DA-01)的野外和手标本照片及镜下特征

Bt.黑云母；Phl.金云母；Pl.斜长石

Fig. 3. Photographs of field, hand specimen and microscope features of the lamprophyre from Du'an in Hechi (17DA-01)

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图 4 河池都安煌斑岩(17DA-02)的野外和手标本照片及镜下特征

Bt.黑云母；Phl.金云母

Fig. 4. Photographs of field, hand specimen and microscope features of the lamprophyre from Du'an in Hechi (17DA-02)

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图 5 河池都安煌斑岩(15DA-02)的野外和手标本照片及镜下特征

Bt.黑云母；Pl.斜长石；Px.普通辉石

Fig. 5. Photographs of field, hand specimen and microscope features of the lamprophyre from Du'an in Hechi (15DA-02)

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图 6 马山百龙滩煌斑岩(GX1506)的野外和手标本照片及镜下特征

Bt.黑云母；Phl.金云母；Ol.橄榄石；Pl.斜长石

Fig. 6. Photographs of field, hand specimen and microscope features of the lamprophyre from Bailongtan in Mashan (GX1506)

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图 7 桂中煌斑岩TAS分类图(a)和K/Al-K/(K+Na)图(b)

a据Le Maitre et al.（1989）；Rock（1987）；b据路凤香等（1991）；CAL.钙碱性煌斑岩；AL.碱性煌斑岩；UML.超基性煌斑岩；LL.钾镁煌斑岩；Pc.苦橄玄武岩；B.玄武岩；O1.玄武安山岩；O2.安山岩；S1.粗面玄武岩；S2.玄武质粗面安山岩；S3.粗面安山岩；U1.碱玄岩、碧玄岩；U2.响岩质碱玄岩；U3.碱玄质响岩；L1.钠质煌斑岩；L2.弱钾质煌斑岩；L3.钾质煌斑岩；L4.超钾质煌斑岩；L5.过铝质煌斑岩；L6.钾镁煌斑岩

Fig. 7. TAS classification diagram (a) and K/Al vs. K/(K+Na) diagram (b) of the lamprophyre from Central Guangxi

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图 8 桂中煌斑岩REE球粒陨石标准化分布图(a)和原始地幔标准化微量元素蛛网图(b)

球粒陨石和原始地幔标准化数据引自Sun and McDonough（1989）

Fig. 8. Spider diagrams for trace elements (a) and REE patterns (b) of the lamprophyre from Central Guangxi

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图 9 桂中煌斑岩锆石阴极发光(CL)照片

Fig. 9. Cathode luminescence (CL) images for zircons of the lamprophyres from Central Guangxi

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图 10 桂中煌斑岩锆石U-Pb年龄谐和图

Fig. 10. U-Pb concordia diagrams for zircons of the lamprophyres from Central Guangxi

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图 11 广西都安和马山煌斑岩中锆石的(¹⁷⁶Hf/¹⁷⁷Hf)_i-U-Pb年龄(a)和ε_Hf(t)-U-Pb年龄图(b)

DM.亏损地幔；NC.新生地壳；CHUR.球粒陨石均一源

Fig. 11. Plots of (¹⁷⁶Hf/¹⁷⁷Hf)_i vs. U-Pb ages (a) and ε_Hf(t) vs. U-Pb ages (b) for zircon grains of the lamprophyres from Du'an and Mashan in Guangxi

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图 12 桂中马山煌斑岩金云母⁴⁰Ar/³⁹Ar坪年龄(a)和等时线年龄(b)

Fig. 12. Phlogopite ⁴⁰Ar/³⁹Ar plateau ages (a) and normal isochron ages (b) of the lamprophyre in Mashan, Central Guangxi

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图 13 桂中煌斑岩中锆石U-Pb年龄直方图

Fig. 13. U-Pb age histogram of zircons from lamprophyres in central Guangxi

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图 14 都安-马山煌斑岩Zr与U (a)、Th (b)、Rb (c)、Ti (d)、Ba (e)、Y (f)、ΣREE (g)、Nb (h)和LOI (i)相关性图解

Fig. 14. The correlations of Zr vs. U (a), Th (b), Rb (c), Ti (d), Ba (e), Y (f), ΣREE (g), Nb (h) and LOI (i) for the Du'an-Mashan lamprophyres

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图 15 Zr/Nb-Y/Nb (a)、Ta/Yb-Th/Yb (b)、La/Yb-Nb/Ta (c)、MgO-Th (d)、MgO-Al₂O₃ (e)、MgO-Cr (f)、MgO-Sr (g)、La-La/Yb (h)和La-La/Sm (i)图解

a，b.底图据Hofmann（1988）；h，i.底图据Imaoka et al.（2014）

Fig. 15. Zr/Nb-Y/Nb (a), Ta/Yb-Th/Yb (b), La/Yb-Nb/Ta (c), MgO-Th (d), MgO-Al₂O₃ (e), MgO-Cr (f), MgO-Sr (g), La-La/Yb (h) and La-La/Sm (i) diagrams

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图 16 Th/Zr-Nb/Zr图解(a)和(Ta/La)_N-(Hf/Sm)_N图解(b)

DM.亏损地幔；MORB.洋中脊玄武岩；N-MORB.大洋拉斑玄武岩；OIB.洋岛玄武岩；a据Jia et al., 2004；b据Gutscher et al.（2000）

Fig. 16. Th/Zr-Nb/Zr diagram (a) and (Ta/La)_N-(Hf/Sm)_N illustration (b)

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图 17 Ba/Rb-Rb/Sr图解(底图据Furman and Graham, 1999)

Fig. 17. Ba/Rb-Rb/Sr diagram (modified after Furman and Graham, 1999)

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图 18 La-La/Yb图解(a)和Nb-Yb图解(b)

a据Sun et al.（2015）修改；b底图据Hardarson and Fitton（1991）

Fig. 18. La-La/Yb diagram (a) and Nb-Yb diagram (b)

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图 19 桂中煌斑岩的Zr-Zr/Y(a)图解与Ta/Hf-Th/Hf图解(b)

a底图据Meschede（1986）；b底图据汪云亮等（2001）；IAB.洋岛玄武岩；MORB.洋中脊玄武岩；WPB.板内玄武岩

Fig. 19. Zr-Zr/Y (a) diagram and Ta/Hf-Th/Hf illustration (b) from lamprophyres in Central Guangxi

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表 1 桂中煌斑岩主量(%)和微量(10^-6)分析结果

Table 1. Major (%) and trace element (10^-6) compositions of the lamprophyres from central Guangxi

样品	15GX6	15GX9	LCH-01	LCH-04	LCH-05	LCH-06	LCH-07	LCH-08	LCH-09	17DA-01	17DA-02	15DA-02	GX1506
样品	云斜煌岩	辉石闪长玢岩	超钾质煌斑岩							煌斑岩
主量元素(%)
SiO₂	53.92	58.49	53.01	50.65	54.6	52.92	54.53	51.16	52.65	40.45	40.78	48.42	57.23
TiO₂	0.95	0.97	0.97	0.9	0.92	0.91	0.92	0.88	0.94	1.01	1.02	1.85	1.04
Al₂O₃	12.66	16.25	13.36	12.55	13.11	12.6	12.79	12.25	12.9	11.21	11.09	12.91	13.76
Fe₂O₃	4.85	5.75	4.53	4.49	4.9	4.41	4.71	4.23	4.21	4.76	4.76	10.69	4.47
MnO	0.1	0.09	0.08	0.08	0.08	0.08	0.08	0.08	0.08	0.24	0.22	0.17	0.07
MgO	6.18	4.12	4.5	4.44	5.69	4.88	5.9	4.61	4.62	3.88	3.84	8.21	4.22
CaO	6.6	5.62	7.19	9.42	5.62	7.51	5.63	9.33	7.12	16.26	15.50	8.07	4.27
Na₂O	2.18	3.41	2.05	1.76	1.93	1.58	1.81	1.65	1.84	1.35	1.32	3.39	2.83
K₂O	5.46	2.74	6.08	5.65	5.74	6.01	6.03	5.94	6.26	7.28	7.22	2.21	6.63
P₂O₅	0.91	0.28	1.00	0.93	0.94	0.95	0.94	0.93	1.00	1.45	1.43	0.58	0.65
LOI	5.86	1.59	6.7	8.51	5.93	6.17	5.16	8.02	6.12	11.16	11.90	2.97	4.42
TOTAL	99.67	99.31	99.47	99.38	99.46	98.02	98.49	99.07	97.94	99.05	99.07	99.47	99.59
Na₂O/K₂O	0.40	1.24	0.34	0.31	0.34	0.26	0.30	0.28	0.29	0.19	0.18	1.54	0.43
Na₂O+K₂O	7.64	6.15	8.13	7.41	7.67	7.59	7.84	7.59	8.10	8.63	8.54	5.60	9.46
微量元素(10^-6)
Sc	18	18.5	17.7	16.3	18.7	16	16.5	16.1	16.8	26.03	29.70	15.20	27.44
Ti	6 050	5 909	6 234	5 900	5 864	5 821	5 819	5 739	6 010	6 210	6 509	6 550	10 831
V	110	137	117	111	127	104	107	104	109	0.00	0.00	110	214
Cr	351	154	396	365	414	345	351	349	381	189	201	419	367
Ni	234	82	242	206	349	256	326	213	247	152	146	222	172
Zn	71.2	63.3	81.4	91.8	82.1	80.6	79.7	71.7	81.4	82.47	109	108	100
Ga	25.5	23.2	17	19.7	16.8	17.3	16.7	17.6	17	15.06	14.45	18.93	16.58
Rb	239	117	237	272	259	263	255	263	237	491	546	281	57.81
Sr	499	402	434	488	428	441	440	484	434	514	536	387	714
Y	41.9	36.6	39.1	43.5	38.3	38.6	38.9	40.1	39.1	33.33	37.28	27.86	26.77
Zr	478	269	433	500	475	493	471	502	433	468	488	532	351
Nb	22.2	20.7	21.8	25.4	22.3	22.8	21.9	23.3	21.8	50.13	51.20	23.55	26.88
Cs	9.56	4.27	12.7	12.8	11.4	11	12.1	8.2	12.7	15.03	14.28	10.57	427
Ba	2 467	935	2 387	2 638	2 559	2 570	2 579	2 761	2 387	4 444	4 617	2 835	2 164
La	69	58	67	72.19	66.57	66.32	67.84	78.48	67	74.47	77.32	52.11	65.57
Ce	162	104	155	165	158	157	163	181	155	176	181	119	132
Pr	21.3	12.6	20.65	22.12	20.25	19.94	20.55	22.67	20.65	18.66	19.40	14.98	15.80
Nd	97.5	49.6	87.7	93.53	87.3	86.16	89.32	97.72	87.7	69.91	74.99	66.10	64.25
Sm	21	8.31	20.77	22.38	20.57	20.72	21.25	22.9	20.77	14.46	15.35	15.30	11.66
Eu	4.08	1.89	3.99	4.53	4.10	4.11	4.19	4.54	3.99	2.84	3.01	3.17	2.90
Gd	16.7	7.56	16.22	17.58	15.53	14.82	15.35	16.61	16.22	11.58	12.31	11.62	8.87
Tb	2.00	1.12	1.85	2.04	1.88	1.88	1.92	1.99	1.85	1.46	1.54	1.47	1.16
Dy	8.46	6.12	7.94	8.69	8.28	8.36	8.45	8.59	7.94	6.91	7.35	6.84	6.02
Ho	1.36	1.23	1.29	1.43	1.31	1.34	1.35	1.36	1.29	1.19	1.25	1.12	1.13
Er	3.46	3.58	3.11	3.41	3.06	3.03	3.05	3.21	3.11	3.12	3.31	2.69	3.00
Tm	0.43	0.51	0.42	0.47	0.41	0.42	0.41	0.41	0.42	0.40	0.42	0.35	0.42
Yb	2.54	3.12	2.39	2.67	2.53	2.53	2.58	2.57	2.39	2.58	2.74	2.25	2.72
Lu	0.36	0.47	0.33	0.38	0.33	0.31	0.29	0.33	0.33	0.38	0.41	0.33	0.42
Hf	11.7	6.31	11.27	13.05	11.56	12.02	11.32	12.31	11.27	13.34	13.80	14.35	8.42
微量元素(10^-6)
Ta	1.54	1.19	1.56	1.88	1.71	1.75	1.66	1.73	1.56	2.40	2.48	1.60	1.05
Pb	73.3	29	71.11	92.44	70.35	86.91	73.41	77.47	71.11	103	103	73.80	31.42
Th	69.2	23.2	64.87	75.75	68.29	70.15	66.85	70.3	64.87	60.99	68.46	76.31	23.71
U	13.7	3.4	12.3	14.77	11.48	12.93	11.93	11.68	12.3	11.00	10.47	13.23	2.91
ΣREE	410	258	388	417	390	387	400	442	388	384	401	297	316
LREE	375	234	355	380	357	354	367	407	355	356	371	270	293
HREE	35.31	23.71	33.55	36.67	33.32	32.69	33.4	35.07	33.55	27.61	29.34	26.67	23.73
LREE/HREE	10.62	9.89	10.58	10.36	10.71	10.85	10.98	11.61	10.58	12.92	12.67	10.16	12.35
La_N/Yb_N	19.49	13.33	22.81	20.11	19.40	18.87	18.80	18.86	21.90	20.72	20.25	16.62	17.31
δEu	0.67	0.73	0.67	0.66	0.70	0.70	0.72	0.71	0.71	0.65	0.65	0.70	0.84
δCe	1.04	0.94	1.00	1.02	1.01	1.06	1.06	1.07	1.05	1.13	1.12	1.03	0.98
注：样品15GX6和15GX9数据来源高秦等(2019), 来源地区分别为马山和都安；LCH-01, LCH-04~LCH-09数据来源Li et al.(2014)，来源地区为马山；17DA-01，17DA-02，15DA-02和GX1506数据来源本文，其中GX1506来源地区为马山，其他为都安.

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表 2 桂中煌斑岩LA-ICP-MS锆石U-Pb定年分析结果

Table 2. LA-ICP-MS U-Pb dating results for zircons of lamprophyres from Central Guangxi

分析点号	同位素比值						定年结果(Ma)						谐和度(%)	Th (10^-6)	U (10^-6)	Th/U
分析点号	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	谐和度(%)	Th (10^-6)	U (10^-6)	Th/U
17DA-01(煌斑岩)
1	0.054 3	0.001 5	0.518 7	0.014 3	0.069 5	0.000 7	387	66	424	10	433	4	97	196	1 159	0.17
2	0.063 9	0.001 1	1.149 2	0.022 3	0.130 7	0.001 2	737	38	777	11	792	7	98	232	1 841	0.13
3	0.053 5	0.001 3	0.509 4	0.012 7	0.069 1	0.000 7	350	84	418	9	431	4	96	296	1 409	0.21
4	0.075 2	0.001 1	0.852 8	0.016 5	0.082 1	0.000 9	1 072	30	626	9	509	6	79	1 801	4 080	0.44
5	0.142 9	0.004 9	2.881 7	0.111 7	0.144 5	0.001 4	2 263	59	1 377	29	870	8	54	586	824	0.71
6	0.064 0	0.001 2	1.076 6	0.025 6	0.121 1	0.001 5	743	44	742	13	737	8	99	326	1 263	0.26
7	0.064 7	0.001 1	1.150 8	0.024 0	0.128 7	0.001 5	765	234	778	11	781	9	99	686	1 796	0.38
8	0.053 1	0.001 1	0.490 9	0.011 4	0.067 1	0.000 7	332	53	406	8	419	4	96	263	1 878	0.14
9	0.064 9	0.001 6	1.210 5	0.029 9	0.135 8	0.001 4	770	51	805	14	821	8	98	364	653	0.56
10	0.056 7	0.001 7	0.546 6	0.016 4	0.070 3	0.000 8	480	65	443	11	438	5	98	393	941	0.42
11	0.089 6	0.002 9	0.885 8	0.031 0	0.071 4	0.000 8	1 417	63	644	17	445	5	63	289	702	0.41
12	0.068 1	0.002 6	1.212 3	0.073 8	0.125 7	0.001 4	872	78	806	34	763	8	94	247	1 524	0.16
13	0.060 7	0.001 8	0.902 9	0.035 2	0.107 7	0.002 3	628	69	653	19	660	13	99	480	778	0.62
14	0.200 0	0.018 3	3.053 9	0.407 6	0.075 2	0.003 5	2 828	150	1 421	102	467	21	33	360	466	0.77
15	0.058 5	0.001 1	0.601 9	0.014 6	0.074 1	0.000 9	546	41	478	9	461	5	96	1 533	4 185	0.37
16	0.065 2	0.001 6	1.124 6	0.028 2	0.125 5	0.001 3	781	52	765	14	762	7	99	229	644	0.36
17	0.138 9	0.002 4	7.744 5	0.153 2	0.404 4	0.004 2	2 213	30	2 202	18	2 189	19	99	206	365	0.56
18	0.067 2	0.001 3	1.185 2	0.025 4	0.127 7	0.001 2	843	40	794	12	775	7	97	243	1 151	0.21
19	0.117 8	0.002 3	2.326 3	0.050 2	0.142 9	0.001 2	1 924	35	1 220	15	861	7	65	254	2 035	0.13
20	0.146 7	0.005 6	1.705 3	0.073 7	0.083 6	0.000 9	2 309	66	1 011	28	518	5	35	419	1 586	0.26
21	0.057 8	0.001 4	0.558 7	0.013 8	0.070 2	0.000 6	524	47	451	9	437	4	96	377	1 434	0.26
22	0.068 4	0.001 2	1.316 4	0.027 0	0.139 4	0.001 4	883	39	853	12	841	8	98	494	1 421	0.35
23	0.062 5	0.001 7	0.579 5	0.016 2	0.067 5	0.000 7	700	59	464	10	421	4	90	1 221	1 183	1.03
24	0.064 8	0.001 9	0.643 8	0.018 4	0.072 6	0.000 8	769	61	505	11	452	5	88	325	855	0.38
25	0.063 5	0.002 4	0.635 7	0.024 6	0.072 7	0.000 9	726	80	500	15	452	5	90	353	408	0.87
26	0.070 3	0.001 5	1.320 9	0.029 8	0.136 2	0.001 2	939	47	855	13	823	7	96	533	1 066	0.50
27	0.067 5	0.001 2	1.248 1	0.025 9	0.133 8	0.001 3	854	35	823	12	809	7	98	481	1 711	0.28
28	0.169 3	0.003 8	2.485 6	0.061 6	0.108 3	0.002 0	2 551	38	1 268	18	663	12	37	553	1 037	0.53
29	0.231 1	0.006 3	2.757 7	0.094 4	0.085 1	0.001 1	3 061	43	1 344	26	526	6	12	505	636	0.79
30	0.056 6	0.001 3	0.554 4	0.014 0	0.071 0	0.000 7	476	45	448	9	442	4	98	1 269	1 712	0.74
31	0.116 2	0.006 6	1.277 0	0.087 1	0.074 5	0.001 1	1 898	101	836	39	463	6	42	866	1 160	0.75
32	0.078 5	0.001 9	1.565 6	0.038 4	0.144 5	0.001 3	1 161	42	957	15	870	7	90	195	832	0.23
33	0.068 9	0.001 5	1.372 8	0.031 8	0.144 6	0.001 3	894	45	877	14	870	7	99	184	1 150	0.16
34	0.069 2	0.001 3	1.238 6	0.027 1	0.129 6	0.001 4	906	39	818	12	786	8	95	531	1 152	0.46
35	0.113 5	0.002 2	2.115 1	0.044 9	0.135 0	0.001 2	1 855	40	1 154	15	816	7	65	283	1 506	0.19
36	0.066 7	0.001 2	1.217 1	0.024 2	0.132 1	0.001 2	828	37	808	11	800	7	98	937	1 519	0.62
37	0.065 3	0.001 1	1.162 7	0.022 4	0.129 0	0.001 2	783	36	783	11	782	7	99	333	1 790	0.19
38	0.078 3	0.002 4	0.725 9	0.023 8	0.067 0	0.000 6	1 154	59	554	14	418	4	71	277	2 292	0.12
39	0.067 0	0.001 3	1.180 7	0.024 7	0.127 9	0.001 2	837	41	792	11	776	7	97	1 337	1 635	0.82
40	0.089 9	0.001 9	1.643 7	0.037 4	0.132 6	0.001 3	1 433	41	987	14	803	7	79	295	911	0.32
17DA-02(煌斑岩)
1	0.056 9	0.001 4	0.557 9	0.014 8	0.071 1	0.000 7	487	56	450	10	443	4	98	708	1 757	0.40
2	0.062 6	0.001 6	0.860 4	0.023 4	0.099 9	0.001 1	694	56	630	13	614	6	97	120	766	0.16
3	0.051 7	0.001 7	0.478 5	0.015 7	0.067 4	0.000 7	272	74	397	11	420	4	94	177	729	0.24
4	0.062 1	0.001 1	0.793 8	0.016 6	0.092 6	0.001 1	676	42	593	9	571	6	96	855	2 108	0.41
5	0.054 8	0.001 2	0.514 2	0.012 0	0.068 0	0.000 6	467	48	421	8	424	4	99	1 799	2 386	0.75
6	0.066 7	0.001 2	1.274 3	0.027 4	0.138 2	0.001 3	828	44	834	12	835	7	99	425	1 304	0.33
7	0.055 8	0.001 4	0.525 4	0.014 2	0.068 4	0.000 8	443	56	429	9	427	5	99	1 175	1 242	0.95
8	0.054 1	0.001 8	0.495 5	0.016 6	0.066 8	0.000 8	376	74	409	11	417	5	98	450	656	0.69
9	0.063 4	0.001 3	0.773 7	0.019 7	0.088 5	0.001 3	722	44	582	11	547	7	93	489	1 311	0.37
10	0.055 9	0.001 4	0.373 2	0.012 6	0.048 7	0.001 2	456	54	322	9	306	8	95	67	1 724	0.04
11	0.064 7	0.001 4	0.947 7	0.026 9	0.105 6	0.001 8	765	44	677	14	647	10	95	301	1 069	0.28
12	0.054 8	0.000 9	0.588 0	0.011 4	0.077 7	0.000 9	406	37	470	7	483	5	97	1 924	4 045	0.48
13	0.063 1	0.001 2	0.602 0	0.011 9	0.069 3	0.000 7	722	41	478	8	432	4	89	2 298	3 486	0.66
14	0.077 8	0.001 5	1.336 3	0.032 6	0.124 0	0.001 5	1 143	44	862	14	754	9	86	231	1 090	0.21
15	0.056 8	0.001 9	0.531 9	0.018 0	0.068 3	0.000 8	483	81	433	12	426	5	98	319	624	0.51
16	0.073 6	0.001 4	1.548 1	0.030 9	0.152 4	0.001 4	1 031	69	950	12	914	8	96	125	1 807	0.07
17	0.060 4	0.001 3	0.733 1	0.017 6	0.088 0	0.000 9	617	47	558	10	544	5	97	224	1 260	0.18
18	0.052 5	0.001 5	0.460 5	0.014 2	0.063 5	0.000 7	306	65	385	10	397	4	96	398	1 013	0.39
19	0.055 9	0.001 1	0.521 4	0.010 8	0.067 6	0.000 6	456	47	426	7	422	4	99	1 600	2 467	0.65
20	0.064 6	0.002 3	1.205 8	0.045 2	0.135 8	0.001 6	761	75	803	21	821	9	97	202	268	0.75
21	0.086 9	0.002 5	1.572 4	0.089 4	0.119 1	0.0044	1 359	56	959	35	725	25	72	860	1 619	0.53
22	0.067 8	0.001 6	1.218 1	0.033 2	0.130 4	0.001 8	861	49	809	15	790	10	97	162	562	0.29
23	0.065 9	0.001 8	0.629 4	0.017 2	0.069 6	0.000 7	806	57	496	11	434	4	86	364	990	0.37
24	0.070 3	0.001 5	1.271 9	0.029 5	0.131 4	0.001 3	939	44	833	13	796	8	95	222	797	0.28
25	0.113 8	0.002 4	2.927 2	0.083 5	0.184 5	0.002 9	1 861	33	1 389	22	1 091	16	76	272	591	0.46
26	0.080 3	0.002 6	0.772 5	0.025 2	0.070 1	0.000 8	1 206	69	581	14	437	5	71	664	990	0.67
27	0.117 9	0.005 5	1.132 2	0.061 7	0.066 7	0.000 8	1 924	83	769	29	416	5	40	2 005	1 845	1.09
28	0.057 3	0.001 2	0.499 1	0.011 4	0.0631	0.000 6	506	46	411	8	395	4	95	1 057	2 112	0.50
29	0.061 8	0.001 2	0.587 5	0.012 1	0.069 1	0.000 7	666	37	469	8	431	4	91	1 337	2 775	0.48
30	0.057 5	0.001 2	0.503 2	0.011 4	0.063 5	0.000 6	522	51	414	8	397	3	95	991	1 909	0.52
31	0.082 3	0.001 5	1.443 2	0.038 8	0.126 7	0.002 4	1 254	35	907	16	769	14	83	206	958	0.21
32	0.064 3	0.002 0	0.913 4	0.030 4	0.103 3	0.001 5	754	65	659	16	634	9	96	176	496	0.36
33	0.067 7	0.001 1	1.272 6	0.023 7	0.136 3	0.001 2	857	33	834	11	824	7	98	910	1 569	0.58
34	0.065 2	0.001 6	1.118 6	0.029 4	0.124 4	0.001 4	783	50	762	14	756	8	99	241	682	0.35
35	0.056 9	0.001 9	0.549 9	0.018 1	0.070 6	0.000 8	487	77	445	12	440	5	98	394	599	0.66
36	0.055 1	0.001 2	0.537 1	0.012 7	0.070 7	0.000 7	417	46	436	8	440	4	99	431	1 400	0.31
37	0.061 5	0.002 2	0.593 4	0.024 0	0.069 5	0.000 9	657	84	473	15	433	5	91	211	448	0.47
38	0.135 2	0.009 3	1.435 1	0.116 0	0.069 8	0.001 2	2 166	121	904	48	435	7	29	720	944	0.76
39	0.057 1	0.001 6	0.544 4	0.015 5	0.069 3	0.000 7	494	61	441	10	432	5	97	605	1 092	0.55
40	0.058 0	0.001 5	0.579 3	0.016 9	0.072 9	0.001 0	528	55	464	11	453	6	97	688	1 121	0.61
15DA-02(煌斑岩)
1	0.053 8	0.001 9	0.393 7	0.013 7	0.053 0	0.000 8	364	51	337	10	333	5	99	98	81	1.21
2	0.113 9	0.002 5	5.251 7	0.116 6	0.334 5	0.0050	1 862	20	1 861	19	1 860	24	100	83	35	2.39
3	0.070 0	0.001 2	1.608 1	0.028 9	0.166 7	0.002 1	928	18	973	11	994	12	102	288	446	0.65
4	0.060 6	0.001 0	0.733 6	0.013 4	0.087 8	0.001 2	626	19	559	8	542	7	97	520	325	1.60
5	0.056 2	0.000 9	0.552 3	0.009 4	0.071 2	0.000 9	461	18	446	6	444	5	100	572	407	1.41
6	0.055 3	0.001 7	0.379 9	0.011 3	0.049 9	0.000 7	422	40	327	8	314	5	96	156	242	0.64
7	0.067 7	0.001 3	0.669 1	0.013 9	0.071 7	0.001 0	858	22	520	8	447	6	86	1 501	794	1.89
8	0.105 9	0.002 2	4.570 7	0.093 8	0.313 1	0.004 2	1 729	19	1 744	17	1 756	21	101	93	83	1.12
9	0.076 3	0.001 2	1.750 0	0.029 2	0.166 4	0.002 1	1 102	16	1 027	11	992	11	97	379	353	1.07
10	0.053 6	0.001 7	0.495 9	0.015 4	0.067 1	0.001 0	355	43	409	10	419	6	102	174	124	1.40
11	0.075 2	0.001 4	1.734 4	0.031 8	0.167 4	0.002 1	1 073	18	1 021	12	998	12	98	374	223	1.68
12	0.057 3	0.001 1	0.590 1	0.011 2	0.074 7	0.001 0	503	21	471	7	464	6	99	334	257	1.30
13	0.064 4	0.001 5	1.053 7	0.023 8	0.118 7	0.001 6	754	26	731	12	723	9	99	41	95	0.43
14	0.051 9	0.001 0	0.267 8	0.005 5	0.037 4	0.000 5	282	24	241	4	237	3	98	98	300	0.33
15	0.098 5	0.001 6	2.070 2	0.035 0	0.152 5	0.002 0	1 596	15	1 139	12	915	11	80	368	1 039	0.35
16	0.236 9	0.003 2	17.616 7	0.271 3	0.539 4	0.0070	3 099	11	2 969	15	2 781	29	94	203	865	0.23
17	0.056 2	0.001 2	0.494 5	0.011 1	0.063 9	0.000 9	459	27	408	8	399	5	98	70	159	0.44
18	0.076 8	0.001 2	1.135 2	0.019 3	0.107 2	0.001 5	1 115	16	770	9	657	8	85	1 218	2 932	0.42
19	0.106 2	0.001 5	4.427 6	0.070 1	0.302 4	0.003 9	1 735	13	1 718	13	1 703	19	99	115	146	0.79
20	0.051 9	0.001 2	0.278 1	0.006 6	0.038 9	0.000 5	281	30	249	5	246	3	99	171	206	0.83
21	0.162 7	0.0131	1.783 0	0.138 8	0.079 5	0.001 6	2 484	140	1 039	51	493	10	47	267	1 070	0.25
22	0.073 9	0.001 5	1.623 5	0.034 9	0.159 3	0.002 4	1 039	22	979	13	953	13	97	691	1 826	0.38
23	0.072 9	0.001 2	1.593 2	0.029 1	0.158 5	0.002 1	1 012	18	968	11	948	12	98	184	113	1.63
24	0.094 8	0.002 0	3.234 1	0.071 4	0.247 6	0.003 6	1 523	21	1 465	17	1 426	19	97	159	157	1.01
25	0.105 7	0.002 7	2.236 1	0.056 5	0.153 4	0.002 2	1 727	26	1 192	18	920	12	77	278	756	0.37
26	0.072 1	0.001 5	1.585 4	0.033 9	0.159 6	0.002 2	988	22	964	13	954	12	99	241	125	1.92
27	0.079 3	0.001 3	1.730 4	0.030 7	0.158 4	0.002 1	1 179	17	1 020	11	948	12	93	195	1 050	0.19
28	0.058 6	0.009 7	0.171 2	0.028 2	0.021 2	0.000 5	552	371	160	24	135	3	84	407	169	2.40
29	0.074 0	0.001 0	1.610 3	0.025 2	0.157 8	0.002 1	1 043	14	974	10	945	12	97	237	258	0.92
30	0.128 5	0.002 3	5.480 9	0.105 9	0.309 4	0.004 6	2 078	16	1 898	17	1 738	22	92	545	539	1.01
31	0.065 6	0.001 2	1.069 7	0.020 4	0.118 3	0.001 7	794	19	739	10	721	10	98	777	565	1.38
32	0.093 5	0.001 3	3.210 0	0.052 0	0.249 3	0.003 5	1 497	14	1 460	13	1 435	18	98	336	968	0.35
33	0.201 2	0.002 6	10.435 9	0.156 0	0.376 3	0.005 0	2 836	11	2 474	14	2 059	23	83	481	1 121	0.43
34	0.080 6	0.001 5	1.261 3	0.024 1	0.113 5	0.001 6	1 213	18	828	11	693	9	84	360	428	0.84
35	0.077 8	0.001 2	1.225 9	0.022 1	0.114 4	0.001 6	1 140	16	812	10	698	9	86	1 105	959	1.15
36	0.059 4	0.001 8	0.476 0	0.012 5	0.058 1	0.000 8	582	66	395	9	364	5	92	297	1 304	0.23
37	0.208 7	0.003 0	15.604 0	0.250 4	0.542 3	0.007 4	2 896	12	2 853	15	2 793	31	98	74	64	1.15
38	0.060 9	0.001 7	0.201 0	0.005 7	0.023 9	0.000 4	636	34	186	5	152	2	82	412	499	0.83
GX1506(煌斑岩)
1	0.121 1	0.001 5	5.961 3	0.082 9	0.357 0	0.004 3	1 973	11	1 970	12	1 968	21	100	121	482	0.25
2	0.089 6	0.001 2	3.039 9	0.045 7	0.246 1	0.003 1	1 417	13	1 418	11	1 418	16	100	709	524	1.35
3	0.104 6	0.001 4	4.380 3	0.062 8	0.303 7	0.003 7	1 708	12	1 709	12	1 709	18	100	852	582	1.46
4	0.052 9	0.001 2	0.374 9	0.008 8	0.051 4	0.000 7	326	29	323	6	323	4	100	512	281	1.82
5	0.059 5	0.001 5	0.416 2	0.010 4	0.050 7	0.000 7	587	30	353	7	319	5	90	339	198	1.71
6	0.052 4	0.000 9	0.364 5	0.006 5	0.050 5	0.000 7	301	19	316	5	318	4	101	4 689	1 732	2.71
7	0.066 3	0.000 9	1.102 6	0.016 9	0.120 7	0.001 5	815	15	755	8	735	9	97	400	567	0.71
8	0.070 4	0.001 0	1.472 3	0.023 0	0.151 7	0.001 9	940	15	919	9	910	11	97	296	284	1.04
9	0.072 1	0.001 2	1.524 8	0.026 8	0.153 3	0.001 9	990	18	940	11	919	11	98	249	294	0.85
10	0.171 3	0.003 5	11.360 4	0.238 7	0.481 0	0.006 9	2 570	18	2 553	20	2 532	30	99	273	481	0.57
12	0.147 2	0.002 5	8.684 2	0.155 6	0.428 1	0.005 8	2 313	14	2 305	16	2 297	26	100	108	108	1.01
13	0.138 3	0.002 0	4.885 8	0.076 0	0.256 3	0.003 2	2 205	12	1 800	13	1 471	16	82	702	867	0.81
14	0.066 3	0.001 4	1.163 5	0.021 3	0.127 2	0.001 1	817	24	784	10	772	6	98	100	121	0.83
15	0.512 5	0.0439	4.906 0	0.306 7	0.069 4	0.004 2	4 277	42	1 803	53	433	25	24	10	2	4.79
16	0.066 9	0.001 5	1.206 1	0.024 7	0.130 7	0.001 3	836	27	803	11	792	7	99	621	476	1.30
17	0.056 9	0.000 9	0.263 4	0.003 3	0.033 6	0.000 2	488	16	237	3	213	1	90	3 626	1 409	2.57
18	0.066 5	0.001 2	1.165 0	0.018 2	0.127 1	0.001 0	821	19	784	9	771	6	98	1 953	526	3.71
19	0.057 5	0.001 5	0.577 6	0.013 9	0.072 9	0.000 7	510	35	463	9	453	4	98	215	164	1.31
20	0.068 7	0.001 5	1.203 8	0.023 5	0.127 0	0.001 1	891	26	802	11	771	6	96	120	134	0.89
21	0.068 3	0.002 1	1.296 5	0.037 3	0.137 8	0.001 7	876	39	844	17	832	10	99	91	110	0.83
22	0.108 6	0.001 8	4.726 4	0.066 9	0.315 7	0.002 6	1 776	14	1 772	12	1 769	13	100	38	43	0.89
23	0.056 8	0.001 4	0.574 1	0.012 9	0.073 3	0.000 7	484	33	461	8	456	4	99	73	109	0.68
24	0.064 4	0.002 2	1.037 0	0.033 3	0.116 8	0.001 5	753	46	722	17	712	9	99	236	139	1.70
25	0.059 9	0.001 8	0.620 9	0.016 8	0.075 2	0.000 8	599	39	490	11	468	5	96	1 637	1 368	1.20
26	0.076 1	0.001 2	1.936 8	0.025 8	0.184 7	0.001 4	1 097	15	1 094	9	1 092	7	100	139	326	0.43
27	0.049 7	0.000 9	0.118 4	0.001 8	0.017 3	0.000 1	181	22	114	2	110	1	97	1 097	2 389	0.46

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表 3 广西都安和马山煌斑岩中锆石Hf同位素组成

Table 3. Hf isotopic compositions for zircons of the lamprophyres from Du'an and Mashan in Guangxi

测点号	¹⁷⁶Hf/¹⁷⁷Hf	2σ	¹⁷⁶Lu/¹⁷⁷Hf	2σ	¹⁷⁶Yb/¹⁷⁷Hf	2σ	(¹⁷⁶Hf/¹⁷⁷Hf)_i	年龄(Ma)	ε_Hf(t)	2σ	T_DM1(Ga)	T_DM2(Ga)
15DA-02(煌斑岩)
1	0.282 925	0.000 019	0.001 495	0.000 022	0.034 269	0.000 405	0.282 916	333	12.05	0.67	0.47	0.55
2	0.281 443	0.000 019	0.000 236	0.000 005	0.006 299	0.000 114	0.281 435	1 862	-5.74	0.65	2.48	2.90
3	0.282 301	0.000 019	0.001 058	0.000 057	0.029 028	0.001 510	0.282 281	994	4.44	0.66	1.34	1.57
4	0.282 454	0.000 019	0.000 860	0.000 005	0.019 869	0.000 232	0.282 445	542	0.08	0.65	1.12	1.48
5	0.282 469	0.000 020	0.000 931	0.000 011	0.023 257	0.000 340	0.282 461	444	-1.58	0.72	1.11	1.51
6	0.282 923	0.000 020	0.001 355	0.000 006	0.034 280	0.000 211	0.282 915	314	11.59	0.70	0.47	0.57
8	0.281 601	0.000 021	0.000 596	0.000 018	0.018 326	0.000 673	0.281 581	1 729	-3.59	0.74	2.29	2.66
9	0.281 908	0.000 016	0.000 704	0.000 003	0.018 685	0.000 037	0.281 895	992	-9.29	0.57	1.87	2.43
10	0.282 629	0.000 018	0.000 681	0.000 001	0.016 719	0.000 053	0.282 624	419	3.64	0.63	0.87	1.16
11	0.281 861	0.000 018	0.000 343	0.000 020	0.009 795	0.000 534	0.281 854	998	-10.60	0.63	1.92	2.52
12	0.282 527	0.000 020	0.000 428	0.000 007	0.010 771	0.000 205	0.282 523	464	1.07	0.70	1.01	1.36
14	0.282 344	0.000 019	0.001 796	0.000 030	0.046 725	0.000 755	0.282 336	237	-10.63	0.67	1.31	1.92
22	0.281 921	0.000 017	0.001 257	0.000 020	0.0385 47	0.000 703	0.281 898	953	-10.05	0.61	1.88	2.45
23	0.282 145	0.000 024	0.001 293	0.000 024	0.038 778	0.000 603	0.282 122	948	-2.24	0.83	1.57	1.95
26	0.282 028	0.000 019	0.000 804	0.000 008	0.023 740	0.000 122	0.282 013	954	-5.95	0.67	1.71	2.19
GX1506(煌斑岩)
1	0.281 500	0.000 018	0.000 623	0.000 004	0.017 245	0.000 138	0.281 477	1 973	-1.68	0.63	2.43	2.73
2	0.281 769	0.000 017	0.000 733	0.000 004	0.017 861	0.000 132	0.281 749	1 417	-4.78	0.58	2.07	2.49
3	0.282 297	0.000 020	0.001 061	0.000 057	0.029 094	0.001 507	0.282 263	1 708	20.11	0.68	1.35	1.12
4	0.282 123	0.000 023	0.001 694	0.000 014	0.040 214	0.000 319	0.282 113	323	-16.58	0.79	1.62	2.36
5	0.282 118	0.000 020	0.001 636	0.000 017	0.038 915	0.000 506	0.282 109	319	-16.83	0.70	1.62	2.37
6	0.282 741	0.000 019	0.002 751	0.000 033	0.087 060	0.000 987	0.282 725	318	4.94	0.68	0.76	1.00
7	0.282 282	0.000 018	0.001 318	0.000 009	0.035 887	0.000 325	0.282 264	735	-2.02	0.63	1.38	1.77
8	0.282 135	0.000 019	0.000 960	0.000 005	0.025 916	0.000 168	0.282 118	910	-3.23	0.65	1.57	1.99
9	0.282 098	0.000 016	0.000 672	0.000 001	0.017 947	0.000 057	0.282 086	919	-4.16	0.56	1.61	2.05
10	0.281 184	0.000 017	0.000 449	0.000 013	0.012 037	0.000 413	0.281 162	2 570	1.00	0.60	2.84	3.03
12	0.281 339	0.000 019	0.000 726	0.000 003	0.018 686	0.000 162	0.281 307	2 313	0.17	0.65	2.65	2.88
14	0.282 371	0.000 019	0.000 727	0.000 011	0.018 985	0.000 196	0.282 361	772	2.24	0.66	1.24	1.53
16	0.282 484	0.000 022	0.001 625	0.000 005	0.040 610	0.000 132	0.282 460	792	6.20	0.78	1.10	1.29
17	0.282 675	0.000 024	0.002 647	0.000 122	0.067 438	0.003 293	0.282 664	213	0.47	0.84	0.85	1.20
20	0.282 405	0.000 021	0.001 471	0.000 009	0.035 360	0.000 190	0.282 384	771	3.05	0.73	1.21	1.48
21	0.282 072	0.000 018	0.000 830	0.000 002	0.020 753	0.000 073	0.282 059	832	-7.07	0.64	1.65	2.17
25	0.282 510	0.000 023	0.001 264	0.000 045	0.029 966	0.001 144	0.282 499	468	0.30	0.82	1.06	1.41

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表 4 桂中马山煌斑岩金云母⁴⁰Ar/³⁹Ar测年结果

Table 4. Phlogopite ⁴⁰Ar/³⁹Ar dating results of the lamprophyres veins in Mashan, central Guangxi

分段加热		³⁶Ar(a) FA	³⁷Ar(a) FA	³⁸Ar(ca) FA	³⁹Ar(k) FA	⁴⁰Ar(r) FA	年龄±2σ(Ma)	⁴⁰Ar(r) %	³⁹Ar(k) %
GX1506煌斑岩，J= 0.009 505 09±0.000 0475 3，Tp坪年龄=100.4±0.99 Ma
002	3.6 %	0.707 217	5.185 83	0.355 858	165.982	1 179.932	118.24±0.67	84.93	1.44
003	4.0 %	0.699 562	6.875 89	0.505 287	306.167	2 155.999	117.16±0.55	91.22	2.66
004	4.5 %	0.840 834	6.040 99	1.602 537	992.781	8 364.545	139.31±0.55	97.09	8.64
005	5.0 %	0.572 124	3.555 41	0.648 611	411.263	2 777.402	112.50±0.49	94.23	3.58
006	5.6 %	0.735 265	5.130 10	0.987 578	654.704	4 293.628	109.35±0.45	95.15	5.69
001	6.4 %	0.974 426	7.612 97	1.383 390	931.945	5 962.277	106.75±0.43	95.36	8.11
002	7.2 %	0.644 404	0.555 43	1.143 274	763.200	4 799.365	104.98±0.42	96.15	6.64
003	8.0 %	1.348 542	18.668 55	2.498 288	1 674.823	10 292.218	102.66±0.41	96.24	14.57
004	9.0 %	1.062 488	14.625 13	2.067 031	1 337.220	8 012.337	100.16±0.40	96.19	11.63
005	10.0 %	0.656 970	9.917 16	1.194 158	757.249	4 555.494	100.55±0.41	95.88	6.59
006	11.0 %	0.747 882	11.718 10	1.320 806	839.227	5 045.532	100.49±0.43	95.77	7.30
001	12.0 %	0.544 354	6.791 59	0.970 608	564.059	3 380.094	100.17±0.41	95.42	4.91
002	14.0 %	0.956 625	13.196 49	1.375 792	850.141	5 115.196	100.57±0.42	94.73	7.39
003	17.0 %	1.144 011	9.701 81	1.349 841	792.061	4 754.919	100.35±0.45	93.33	6.89
004	20.0 %	0.482 542	1.496 40	0.488 011	274.894	1 659.188	100.88±0.46	92.05	2.39
005	25.0 %	0.526 213	0.000 00	0.305 764	145.589	915.811	105.01±0.75	85.46	1.27
006	30.0 %	0.557 759	0.000 00	0.152 314	35.185	230.879	109.41±1.84	58.34	0.31

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表 5 桂中都安-马山周缘燕山晚期岩浆活动

Table 5. The Late Yanshanian magmatism around Du'an-Mashan, Central Guangxi

产地	岩石	年龄(Ma)	测试方法	资料来源
广西都安丹桃	云煌岩	104	黑云母K-Ar	陆刚等(2013)
广西都安东庙	煌斑岩	93.6±0.6	金云母Ar-Ar	王新宇等(2019)
广西凌云-凤山县明山金矿附近	石英斑岩脉	89	白云母K-Ar	广西壮族自治区地质矿产局(1985)
广西凌云-凤山县明山金矿附近	石英斑岩脉	80.9~84.9	全岩K-Ar	广西壮族自治区地质矿产局(1992)
广西凤山县弄黄	石英斑岩脉	96.5±0.7	白云母斑晶Ar-Ar	陈懋弘等(2012)
广西巴马县县城	石英斑岩脉	95.6±0.7	白云母斑晶Ar-Ar
广西都安县保安	煌斑岩墙	99.02±0.78	金云母Ar-Ar
广西大厂龙箱盖	黑云母花岗岩	93±1	SHRIMP锆石U-Pb	蔡明海等(2006)
	斑状黑云母花岗岩	91±1
	花岗斑岩墙	91±1
	闪长玢岩墙	91±1
广西大明山	中酸性岩墙群	89~90	白云母K-Ar	广西壮族自治区地质矿产局(1985)
广西大瑶山	花岗斑岩	91.3±0.6	LA-ICP-MS锆石U-Pb	毕诗健等(2015)
广西大瑶山龙头山	流纹斑岩	103.3±2.4	LA-ICP-MS锆石U-Pb	陈富文等(2008)
广西大瑶山龙头山	花岗斑岩	103.3±1.5	LA-ICP-MS锆石U-Pb	陈富文等(2008)
广西大瑶山平天山	中酸性侵入岩	96.1±3.0	LA-ICP-MS锆石U-Pb	段瑞春等(2011)
广西大瑶山平天山	中酸性侵入岩	96.2±0.4	LA-ICP-MS锆石U-Pb	段瑞春等(2011)
广西大瑶山大黎	石英二长岩	102.8±0.9	LA-ICP-MS锆石U-Pb	胡升奇等(2012)
广西大瑶山大黎	石英二长岩	101.7±1.2	LA-ICP-MS锆石U-Pb	胡升奇等(2012)
广西昆仑关	斑状黑云母花岗岩	93±1	LA-ICP-MS锆石U-Pb	谭俊等(2008)
广西昆仑关	A型花岗岩	97.7±1.3	LA-ICP-MS锆石U-Pb	刘飞等(2018)
广西罗城	煌斑岩	100±14	LA-ICP-MS锆石U-Pb	王磊等(2015)
广西大明山	那宁石英斑岩	93.11±0.64	LA-ICP-MS锆石U-Pb	肖昌浩等(2018)
	罗维二长花岗岩	92.92±0.69
	罗维黑云母花岗岩	92.5±1.1
广西马山	龙昌钾质煌斑岩	89±0.76	云母K-Ar	Li et al., (2014)
广西马山	百龙滩煌斑岩	100.4±0.99	金云母Ar-Ar	本文
广西大瑶山	二长花岗岩	99±2	LA-ICP-MS锆石U-Pb	王强等(2005)

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桂中都安-马山煌斑岩成因及其构造意义

doi: 10.3799/dqkx.2020.306

作者简介:
唐远兰(1995-), 女, 硕士, 现主要从事岩石学研究.ORCID: 0000-0003-0496-7756.E-mail: 1132726253@qq.com

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时毓, E-mail: shiyu_61@163.com

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Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi

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桂中都安-马山煌斑岩成因及其构造意义

doi: 10.3799/dqkx.2020.306

作者简介: 唐远兰(1995-), 女, 硕士, 现主要从事岩石学研究.ORCID: 0000-0003-0496-7756.E-mail: 1132726253@qq.com

通讯作者: 时毓, E-mail: shiyu_61@163.com

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Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi

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作者简介:
唐远兰(1995-), 女, 硕士, 现主要从事岩石学研究.ORCID: 0000-0003-0496-7756.E-mail: 1132726253@qq.com

通讯作者:
时毓, E-mail: shiyu_61@163.com