武夷山成矿带桃溪隆起、岩浆侵入和区域铜多金属矿成矿作用

陈世忠; 马明; 陈刚; 周延; 朱筱婷; 邱金亮; 毛建仁

doi:10.3799/dqkx.2010.111

武夷山成矿带桃溪隆起、岩浆侵入和区域铜多金属矿成矿作用

doi: 10.3799/dqkx.2010.111

中国地调局南京地质调查中心, 江苏南京 210016

基金项目:

中国地质调查局项目矿调[2004]12-1号

中国地质调查局项目矿调[2006]13-1号

中国地质调查局项目资[2008]02-13-02号

中国地质调查局项目资[2010]矿评01-17-11

详细信息

作者简介:
陈世忠(1967-), 男, 研究员, 从事地质矿产调查和研究.E-mail: chenshizhong@gmail.com

中图分类号: P611.1
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出版历程
- 收稿日期: 2010-07-05
- 刊出日期: 2010-11-01

Taoxi Uplift of Wuyi Metallogenic Belt, Its Tectonics, Magmatism and Metallogeny

Nanjing Institute of Geology and Mineral Resources, China Geological Survey, Nanjing 210016, China

摘要

摘要: 武夷山成矿带内矿区的最大特征就是分布有老地层和岩浆岩.老地层集中分布区——桃溪隆起区是武夷山隆起的一部分, 表现为变质核杂岩的特征, 其中分布着大中型铜多金属矿床和大量的多金属矿点, 如紫金山铜金矿、岩背锡矿和红山铜矿, 它们是武夷山成矿带乃至中国东部的典型特征.主要矿床的成矿年龄集中于130~90 Ma, 属燕山晚期; 成矿特征表现为斑岩型-岩浆热液型铜多金属矿.成矿斑岩体成岩时代90~140 Ma, 多为燕山期复式杂岩体的中晚期, 桃溪隆起区这种时空一致性是由于中生代晚期岩石圈拆沉的产物.桃溪隆起区在中生代晚期经历了岩石圈加厚期后的拆沉、软流圈物质侵入、岩浆作用及其伴随的成矿作用.这些认识对该区找矿部署具有重要的意义.
- 桃溪隆起区 /
- 变质核杂岩 /
- 紫金山 /
- 燕山晚期 /
- 矿床 /
- 成矿作用
Abstract: Taoxi uplift is a part of Wuyishan uplift and occurs as metamorphic core complexes. There are abundant medium to large scale copper and polymetallic ore deposits distributed in the uplift, such as the super large scale Zijinshan copper-gold deposit, super large Yanbei tin deposit, and large scale Hongshan copper deposit. This area is representative of a rich segment of Wuyi metallogenic belt. The main geochronology dating of mineralization concentrates in the range of 130-90 Ma, the late Yanshan period. The ore deposits, as well as most copper-gold ore deposits located in Taoxi uplift are of porphyry-magmatic hydrothermal type. Geochronology dating of ore bearing porphyry stocks is 94-140 Ma, the middle to late period derivatives of Yanshan magmatic complex resulted from interaction of crust with mantle and the lithosphere delamination in the Late Mesozoic. Taoxi Uplift is characterized by lithosphere thickening and delamination, intrusion of the asthenosphere matter and magmatism, and accompanied mineralization.
- Taoxi uplift region /
- metamorphic core complex /
- Zijinshan /
- Late Yanshan /
- ore deposit /
- metallogeny

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图 1 桃溪隆起区位置示意

Fig. 1. Location of Taoxi Uplift

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图 2 桃溪隆起区地质矿产简图

Fig. 2. Sketch map of geology and mineral resources on Taoxi uplift

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图 3 武平东留桃溪岩组岩层片理中发育的斑岩脉

Fig. 3. Porphyry veins developed in rock schistosity of Taoxiyan Formation in Dongliu, Wuping

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图 4 桃溪变质核杂岩构造剖面略图

1.侏罗纪侵入岩；2.三叠纪侵入岩；3.二叠纪侵入岩；4.白垩系；5.上三叠统一下白垩统；6.上部盖层(上古生界)；7.下部盖层(下古生界)；8.桃溪岩组；9.脆性断层；10.剥离断层上、下盖层间滑脱断层；11.韧性剪切断层；12.韧脆性滑脱断层；13.走滑型韧性剪切带；14.侵入界线、角度不整合界线

Fig. 4. Sketch tectonic section of Taoxi metamorphic core complex

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图 5 桃溪隆起区构造、岩浆和成矿综合模式

Fig. 5. Delamination model of Taoxi Uplift

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表 1 几种矿床同位素年龄

Table 1. Isotope ages of several mineral deposits

矿床名称	成矿年龄(Ma)	同位素测年方法	测试样品	资料来源
紫金山罗卜岭成矿花岗闪长斑岩	105±7.2	Rb-Sr等时线	全岩	张德全等，2001
紫金山铜金矿床	104.54±1.7	⁴⁰Ar/³⁹Ar	蚀变黑云母	张德全等，2005
紫金山铜金矿床金矿石	100±3	流体包裹体Rb-Sr等时线	石英	陈好寿，1996
紫金山矿床碧田金银矿石	91.47±0.39	⁴⁰Ar/³⁹Ar	与矿石矿物共生的冰长石	刘晓东和华仁民，2005
岩背含锡石石英脉	125.5±6.1	Rb-Sr等时线	石英	梅玉萍等，2007
岩背锡矿	120.2±5.3	Re-Os模式年龄	辉钼矿	邱检生等，2005
岩背苦竹岽锡矿	114.0±1.6	Re-Os模式年龄	辉钼矿	邱检生等，2005
红山铜矿大山含铜石英脉	98.8±1.5	K-Ar法	石英	周济元等，1998a
红山铜矿牛牯远含铜石英脉	97.1±1.9	K-Ar法	石英	周济元等，1998a

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表 2 几种矿床成矿岩体同位素年龄

Table 2. Isotope ages of ore-forming porphyry in several mineral deposits

岩体名称	成岩年龄(Ma)	同位素测年方法	测试样品	资料来源
紫金山次火山侵入体	133±6	微量锆石U-Pb法	锆石	陈好寿，1996
紫金山次火山侵入体	118±4	微量锆石U-Pb法	锆石	陈好寿，1996
四坊石英闪长玢岩	102±9	Rb-Sr	全岩	陈好寿，1996
四坊花岗闪长岩	107.8±1.2	U-Pb法	单颗粒锆石	毛建仁等，2004
四坊花岗闪长岩	103.1±0.6	Ar-Ar法	角闪石	毛建仁等，2004
四坊花岗闪长岩	99.4±0.5	Ar-Ar法	钾长石	毛建仁等，2004
罗卜岭花岗闪长岩	100±1	Rb-Sr	全岩	陈好寿，1996
紫金山铜金矿床流纹岩	94±7.7	Rb-Sr等时线	全岩	张德全等，2001
岩背流纹质火山岩	123.3±1.3	Rb-Sr等时线	全岩	刘昌实等，1994
岩背含黄玉花岗斑岩	114.1±0.7	Rb-Sr等时线	全岩	刘昌实等，1994
岩背含黄玉花岗斑岩	128.1±3.3	Rb-Sr等时线	全岩	梅玉萍等，2007
岩背花岗斑岩	114.1±0.6	Rb-Sr等时线	全岩	沈渭洲和凌洪飞，1994
塌山花岗斑岩	117.5±5.6	Rb-Sr等时线	全岩	沈渭洲和凌洪飞，1994
岩背火山岩	138±1	K-Ar法	矿化蚀变绢英岩	黄常立等，1997
岩背清溪花岗岩	134±2	K-Ar法	矿化蚀变绢英岩	黄常立等，1997
岩背花岗岩	128±1	K-Ar法	矿化蚀变绢英岩	黄常立等，1997
岩背矿化蚀变绢英岩	118	K-Ar法	矿化蚀变绢英岩	黄常立等，1997
岩背密坑山花岗岩	124.5±0.7	Rb-Sr等时线	全岩	邱检生等，2005
岩背密坑山花岗斑岩	114.1±0.6	Rb-Sr等时线	全岩	王德滋等，1994

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表 3 3个矿床稳定同位素和放射性同位数特征

Table 3. Isotope ratios of Zijinshan, Hongshan and Yanbei deposits

矿床	δ¹⁸O(‰，SMOW)	δ³⁴S(‰)	其他同位素特征	资料来源
紫金山铜金矿	11.05~12.25(花岗岩类)，9.57~10.61(英安玢岩)，11.20(隐爆角砾岩)，10.80(蚀变矿物绢云母)，11.57(明矾石)，10.17~14.77(英安玢岩中石英斑晶)	-9.25~-5.1(金属硫化物)，25.9(明矾石)		张德全等, 1991, 2001, 2005
红山铜矿		+1.03~3.6(黄铁矿和辉铜矿)	黄铜矿和辉铜矿的²⁰⁶Pb/²⁰⁴Pb、²⁰⁷Pb/²⁰⁴Pb、²⁰⁸Pb/²⁰⁴Pb比值分别为17.986~18.197，15.506~15.697和38.244~38.711	陈世忠等, 1998a, 1998b
岩背锡矿	+9.00(成矿花岗斑岩)，6.0~11.9(石英)	-0.3~-1.5 (锡石)	(⁸⁷Sr/⁸⁶Sr)i: 0.712 8~0.713 0(花岗斑岩)0.709 3(花岗闪长斑岩)，ε_Nd(t)：-3.61~+1.27(花岗斑岩)，+1.09(花岗闪长斑岩)	邱检生等, 2005, Liu et al., 1999

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表 4 红山铜矿成矿岩体主要微量元素的含量

Table 4. Main trace elements content of ore-forming porphyry in Hongshan deposits

序号	样品号	Rb	Ba	Th	Ta	Nb	La	Ce	Sr	Nd
1	NHR-1	17.97	11.02	0.68	8.09	238.23	54.36	115.96	192.28	52.08
2	NHR-2	18.24	7.27	0.48	7.67	225.68	51.56	107.60	197.08	48.63
3	NHR-3	16.69	5.01	0.19	7.51	212.81	56.77	117.72	103.62	53.97
4	NHR-4	20.49	2.56	0.20	9.17	274.90	53.24	114.08	51.17	51.67
5	NHR-5	15.21	3.69	2.35	8.12	237.31	52.22	109.65	145.78	50.37
6	NHR-6	17.87	6.46	0.50	7.10	217.64	48.75	101.20	221.50	46.78
7	NHR-7	19.81	5.17	0.23	6.04	184.15	47.24	98.41	167.72	45.46
8	NHR-8	17.77	3.52	0.61	7.42	224.20	44.38	92.22	112.70	42.28
9	NHR-9	18.59	1.97	0.11	8.23	249.17	50.92	108.61	34.82	48.64
10	NHR-10	18.77	11.63	0.25	6.99	212.39	45.33	94.12	209.25	42.37
11	HSR-1	221.75	634.88	11.01	1.26	10.44	20.28	40.98	841.08	16.88
12	HSR-2	228.37	466.79	11.57	1.49	12.18	18.83	39.98	294.26	18.22
13	HSR-3	234.54	486.88	14.76	1.31	11.51	27.97	55.79	573.61	24.10
14	HSR-4	257.46	367.79	13.82	1.33	11.00	20.42	43.27	713.31	19.35
15	HSR-5	256.68	515.60	13.56	1.38	11.93	24.50	48.86	617.53	21.30
16	HSR-6	221.76	369.43	13.17	1.34	11.23	22.31	43.36	206.87	18.56
17	HSR-7	230.49	438.52	13.41	1.33	10.97	22.31	44.65	585.02	18.82
18	HSR-8	248.55	708.75	14.78	1.44	12.37	25.24	50.56	636.99	21.70
19	HSR-9	247.36	556.03	14.79	1.37	12.56	24.23	49.59	300.65	21.44
20	HSR-10	186.99	435.83	9.81	1.01	10.81	23.31	47.90	679.35	23.66

序号	P₂O₅	Sm	Zr	Hf	Eu	TiO₂	Tb	Y	Yb	Lu
1	0.12	9.38	56.19	0.99	1.32	0.49	1.62	43.70	6.79	0.99
2	0.11	8.91	37.66	0.67	1.24	0.43	1.28	94.96	4.53	0.67
3	0.13	9.46	45.93	0.84	1.28	0.45	1.52	53.31	5.34	0.84
4	0.13	10.18	63.56	1.06	1.30	0.54	1.81	48.85	6.91	1.06
5	0.11	9.15	53.12	0.91	1.20	0.43	1.57	65.19	6.16	0.91
6	0.12	8.50	44.40	0.79	1.18	0.42	1.31	97.65	5.23	0.79
7	0.13	8.39	45.48	0.85	1.20	0.46	1.44	84.46	5.58	0.85
8	0.09	7.78	41.96	0.76	1.28	0.44	1.34	49.82	5.07	0.76
9	0.11	8.57	50.89	0.92	1.28	0.49	1.58	57.09	6.05	0.92
10	0.11	7.69	41.02	0.74	1.27	0.44	1.34	95.90	4.85	0.74
11	0.34	2.31	101.57	3.11	0.70	0.35	0.31	13.66	1.51	0.25
12	0.40	2.87	109.80	3.32	0.71	0.37	0.33	13.36	1.64	0.28
13	0.57	3.40	106.85	3.22	1.03	0.38	0.44	13.77	1.60	0.26
14	0.23	2.74	98.69	3.14	0.75	0.36	0.34	12.60	1.51	0.26
15	0.57	3.23	109.96	3.55	0.84	0.37	0.47	17.45	2.00	0.32
16	0.40	2.45	124.35	3.70	0.77	0.37	0.40	13.53	1.56	0.28
17	0.28	2.69	125.58	3.68	0.73	0.37	0.36	12.89	1.56	0.27
18	0.22	3.25	158.98	4.49	0.91	0.38	0.42	14.97	1.81	0.31
19	0.31	3.29	125.05	3.60	0.88	0.40	0.47	16.86	1.99	0.32
20	0.29	3.51	127.78	3.68	0.79	0.48	0.33	9.17	1.24	0.21
注：主量元素由国土资源部华东矿产资源监督检测中心检测，微量元素和稀土元素由中国科学院地质与地球物理研究所检测；NHR-1-10为花岗岩，HSR-1-10为花岗闪长斑岩；氧化物单位为%，其他单位为10^-6.

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