福建中生代钼矿的辉钼矿矿物学特征

王翠芝; 刘文元

doi:10.3799/dqkx.2013.121

福建中生代钼矿的辉钼矿矿物学特征

doi: 10.3799/dqkx.2013.121

王翠芝^{1, 2,},
刘文元^{1, 2}

1.
福州大学紫金矿业学院, 福建福州 350108
2.
福建省矿产资源重点实验室, 福建福州 350108

基金项目:

福建省自然科学基金 2010J01257

国家自然科学基金项目 41072067

详细信息

作者简介:
王翠芝(1965-), 女, 副教授, 博士, 主要从事矿床成矿规律及矿产开发利用方向研究.E-mail: Wcuizhi@163.com

中图分类号: P578
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出版历程
- 收稿日期: 2012-12-27
- 刊出日期: 2013-06-01

Mineralogical Characterstics of Molybdenite of Mesozoic Molybdenum in Fujian Province

WANG Cui-zhi^{1, 2
,},
LIU Wen-yuan^{1, 2}

1.
College of Zijin Mining, Fuzhou University, Fuzhou 350108, China
2.
Fujian Key Laboratory of Mineral Resources, Fuzhou 350108, China

摘要

摘要: 福建中生代钼矿分布广泛, 并伴生有一定的铼.通过系统研究福建中生代钼矿基本特征, 总结出主要有斑岩型、岩浆期后热液型、火山热液型、构造角砾岩型(热液石英脉型)及少量矽卡岩型, 选择坪地、上西坑、罗卜岭、马坑等4个典型钼矿进行重点研究.在野外地质调查、岩相学的基础上, 进行了矿相学及辉钼矿矿石矿物学的系统研究, 得出福建中生代钼矿中辉钼矿的晶体形态主要表现为颗粒较大(粗到中细粒), 结晶度高, 多呈片状、鳞片状、局部板状, 多色性明显, 个别矿区辉钼矿颗粒较小, 结晶较差, 多色性不明显; 辉钼矿多型主要为2H, 少量2H+3R型、3R型; 辉钼矿矿物化学成分中微量杂质元素(包括Re含量, 一般为(N~N×100)×10^-6, 并以(N~N×10)×10^-6为主)较低.本区辉钼矿的这些矿物学特征说明其形成时的温度条件较高, 多为中高温环境, 其物源可能是壳幔混染源, 且以壳源为主; 中生代钼成矿在福建省内具普遍性, 辉钼矿中的Re作为有益的伴生元素具有一定的综合利用价值.
- 福建省 /
- 中生代 /
- 辉钼矿 /
- 矿物 /
- 指示作用 /
- 地球化学
Abstract: Mesozoic molybdenum deposits are distributed widely in Fujian, and associated with a certain amount of rhenium. This study explores Mesozoic molybdenum deposits in Fujian. It is found by analysis of characteristics of ore petrology and mineralogy of molybdenite of typical molybnum deposits (Pingdi, Shangxikeng, Luobuling, Makeng, etc.) in Fujian Province, five types of the molybdenum deposits have been determined, including the porphyry type, the magmatic hydrothermal type, the volcanic hydrothermal type, the tectonic breccia type and a few skarn type. Our systematic field investigation and petrography study finds that the ores mainly have coarse-medium fine grain, platy texture, small amount of thick tabular texture; the ore mineral(only molybdenite) is of leaden color, obvious polychroism, 2H polymorph (a small amount of 2H+3R, 3R), low contents of impurities including Re((N-N×100)×10^-6, most(N-N×10)×10^-6), which indicates the ores formed in moderate-high temperature condition and the ore originates from crust-mantle mixed source (most crust source); Mesozoic molybdenum mineralization is of universality in Fujian province; and as a kind of accompanying elements, Re is of some comprehensive utilization value.
- Fujian Province /
- Mesozoic /
- molybdenite /
- minerals /
- indication /
- geochemistry

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图 1 福建沿海区域地质构造示意图(据1∶50万福建省地质图修编，1998)

1.主要断层；2.背斜；3.向斜；4.片理化；5.主要水系；6.省界线；7.主要城镇；8.典型钼矿

Fig. 1. Sketch of the regional geological structure in Fujian coastal areas

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图 2 典型钼矿中辉钼矿的形态(本图为二次电子扫描图像)

a.坪地I₁矿体硅化岩中片状辉钼矿；b、c.坪地I₆矿体细粒及厚板状辉钼矿；d~f.上西坑矿段Ⅳ₁矿体硅化岩中细晶辉钼矿及构造角砾岩中弯曲的板状辉钼矿；g.罗卜岭铜钼矿体中片状的辉钼矿；h.马坑铁矿伴生钼矿体中板状辉钼矿

Fig. 2. Shape of molybdenite in typical Mo deposits

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图 3 典型钼矿辉钼矿的X光衍射图谱与标准辉钼矿多型的峰型的对比

(1)~(3)坪地矿段辉钼矿；(4)~(5)上西坑矿段辉钼矿；(6)罗卜岭铜钼矿；(7)马坑铁矿辉钼矿；2H、3R峰位及峰值为Jade5软件加载的PDF卡片中的数据；2H、3R型辉钼矿的峰位及峰值为Jade5软件加载的PDF卡片中的数据；衍射指数(hkl)数据引自文献(毛兴莉等，1988；王奖臻等，2004)；数据对比时，主要依据特征网间距d值来确定特征面网，d_hkl=λ/2sinθ_hkl

Fig. 3. Comparison of X-ray diffraction patterns of molybdenite of the typical molybdenum deposits with patterns of standard molybdenite polymorph

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图 4 辉钼矿中微量元素曲线

PDI₁(12)为坪地12个点平均值；PDI₆(15)为坪地15个点平均值；SXK(12)为上西坑12个点平均值；MK(7)为马坑7个点平均值；LBL(8)为紫金山罗卜岭8个点平均值

Fig. 4. Trace elements of molybdenite

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图 5 福建中生代典型钼矿中辉钼矿的铼含量与其他类型钼矿中的对比

1~6矿床的数据黄典豪(1992)；1.国外斑岩型铜(钼)矿床；2.我国斑岩型铜(钼)矿床；3.国外斑岩岩钼矿床；4.我国斑岩型钼矿床；5.黄龙铺碳酸岩脉型钼(铅)矿床；6.南泥湖-三道庄斑岩-矽卡岩型钼(钨)矿床；7.北岔门铅锌矿辉钼矿；8.福建砺山钼矿(王成辉等，2009)；9.赤路斑岩钼矿(张克尧等，2009)；10.福建省永定山口钼矿(罗锦昌等，2009)；11.坪地钼矿；12.上西坑钼矿；13.罗卜岭铜钼矿；14.马坑铁钼矿；11~14矿床数据为本文实测

Fig. 5. Comparison of Re content of molybdenite of Mesozoic molybdenum deposits in Fujian with others

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表 1 福建中生代主要钼矿统计

Table 1. Statistics of main Mesozoic molybdenum deposits in Fujian

序号	矿床名称	矿床类型	年龄(Ma)	同位素资料来源
1	坪地钼矿	中高温热液型	102.9±1.8	本文Re-Os测年(另文报道)
2	上西坑钼矿	中低温热液型	102.0±1.5	本文Re-Os测年(另文报道)
3	罗卜岭铜钼矿	斑岩型	109.0±1.7	王登红等，2010
4	马坑铁钼矿	热液型(矽卡岩型)	130.5±0.9	邱小平，2008(内部资料)
5	福安赤路钼矿	斑岩型	105.3±1.6	张克尧等，2009
6	周宁咸格钼矿	斑岩型	102.6	王登红等，2010
7	古田三保钨钼矿	岩浆期后热液型	81.5~85.0	郑开旗，1989
8	永泰无岩坑钼矿	岩浆期后热液型	燕山晚期	谭元松，2010
9	漳平北坑场多金属矿	岩浆期后热液型	139.8±2.3~143.7±2.1	张达等，2010
10	平和钟腾铜钼矿	斑岩型	109.0±2.8	王登红等，2010
11	仙游砺山钼矿点	岩浆期后热液型	91.7±4.9	王成辉等，2009
12	宁化行洛坑钨钼矿	含钨石英脉型	156.3±4.8	张家菁，2008
13	永定山口钼矿	火山热液型	165.3±3.5	罗锦昌，2009
14	霞浦大湾铍钼矿	热液充填-交代型	J₃	杨武平，2007

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表 2 福建中生代典型钼矿辉钼矿电子探针结果(%)

Table 2. Electron probe microanalysis of molybdenite of typical Mesozoic molybdenum deposits in Fujian

矿床	矿体(探针点数)	W	As	Se	Re	S	Mo	Cu	Sn	Fe	Mn	Total
坪地	PDI₁(12)	0.016 1	0.000 1	0.002 3	0.005 9	40.148 4	59.490 3	0.022 6	0.002 9	0.069 6	0.002 5	99.850 0
坪地	PDI₆(15)	0.006 4	0.000 5	0.001 7	0.012 6	40.260 7	59.889 1	0.003 9	0.013 1	0.015 6	0.006 3	100.210 8
坪地	PD(27)	0.011 2	0.000 3	0.002 0	0.009 2	40.204 6	59.689 7	0.013 3	0.008 0	0.042 6	0.004 4	100.030 4
上西坑	SXKIV₁(12)	0.009 2	0.001 4	0.014 3	0.010 6	39.904 1	59.271 9	0.006 0	0.003 8	0.028 3	0.003 3	99.402 6
马坑	MK(7)	0.009 4	0.005 2	0.016 1	0.011 6	40.195 7	59.620 1	0.022 4	0.011 1	0.006 9	0.197 4	100.096 0
罗卜岭	LBL(8)	0.080 0	0.001 9	0.009 0	0.000 1	40.207 7	59.712 9	0.003 4	0.005 1	0.018 7	0.006 1	100.045 0
	矿床	Mo+S			Re/Mo			微量元素总和
特征值	坪地	99.86			0.000 155			0.14
特征值	上西坑	99.77			0.000 178			0.23
特征值	马坑	99.72			0.000 194			0.28
特征值	罗卜岭	99.88			0.000 001 7			0.12
注：电子探针数据由福建省矿产资源重点实验室测试，测试人：刘文元；测试时间：2011年12月.测试条件：仪器型号JXA-8230，电压20 kV，电流20 nA，束斑5 μm，标样：金属W、Re、Sn、GaAs、MoS₂、Bi₂S₃、CdSe、FeS₂、CuFeS₂、MnS.微量元素的检测限是50×10^-6，有效数字为3位(小数点后)，仅Re/Mo取6位.

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表 3 不同多型的辉钼矿中化学成分对比

Table 3. Comparison of chemical composition of different polymorph molybdenite

序号	矿床名称	多型	Mo(%)	S(%)	Mo+S(%)	Re(10^-6)	杂质(%)	杂质成分
1	大石沟	2H	58.20	37.80	96.00	381	4.00	Mn、Fe、Ti、Ce、Co、U、Ta、Nb、Sn、Zr、V、La、Yb、Lu、Cr
2	金堆城	2H	58.80	39.40	98.20	21	1.80	Fe、Ti、Mn、Co、Nb、Ce、La、Ta、Bi、W、Ca、Cr、V
3	石家湾	2H	57.90	37.50	95.40	23	4.60	Fe、Ti、Ni、Ce、La、Mn、Co、Cr、Ta、Ca、Sn、Nb、Y、V、Zr、Bi
3	石家湾	2H+3R	56.80	36.90	93.70	42	6.30	Fe、Ti、Ni、Ce、La、Mn、Co、Cr、Ta、Ca、Sn、Nb、Y、V、Zr、Bi
4	南泥湖	2H	54.05	38.94	92.99	38	7.01	Fe、Re
5	马圈	2H	58.87	40.23	99.10	18	0.90	Fe、Re
6	黄背岭	2H	58.23	38.50	96.93	8	3.07	Fe、Re
7	白乃庙	3R	57.66	37.44	95.10	1 800	4.90	Fe、Re
8	三保	2H	59.60	39.88	99.48	30	0.52	Se、Te
9	紫云	2H+3R	59.01	34.20	93.21	50	6.79	Se、Te
10	坪地	2H	59.67	40.19	99.86	92	0.14	W、As、Se、Re、Cu、Sn、Fe、Mn
11	上西坑	2H	59.63	40.14	99.77	106	0.23
12	罗卜岭	2H	59.71	40.21	99.88	1	0.12
13	马坑	3R	59.62	40.20	99.72	116	0.28
注：1~3.陈福根等(1984)；4~7.韩吟文(1988)；8~9.毛兴莉等(1988)；10~13.本文.

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表 4 福建中生代主要钼矿中辉钼矿的矿物学主要特征对比表

Table 4. Comparison of main mineralogical characteristics of molybdenite in major Mesozoic molybdenum deposits in Fujian

序号	矿床名称	成因类型	晶形	多型	形成温度(℃)	Re含量(10^-6)及资料来源
1	坪地钼矿	中高温热液石英脉型	片状	2H		2.354~54.65(本文)
2	上西坑钼矿	中低温热液石英脉型	鳞片状	2H		1.479~34.35(本文)
3	罗卜岭铜钼矿	斑岩型	鳞片状	2H		1.43(本文电子探针)
4	马坑铁钼矿	热液型(矽卡岩型)	鳞片状	3R		116(本文电子探针)
5	福安赤路钼矿	斑岩型	鳞片状	2H	191~224	4.277~16.174(张克尧等，2009)
6	周宁吴山底钼矿	构造蚀变带型	粉末状	2H+3R	260
7	周宁紫云钼矿	蚀变脉型	粉末状	2H+3R	260
8	古田香峰钨钼矿	热液石英脉型	鳞片状	2H
9	古田三保钨钼矿	热液石英脉型	鳞片状	2H
10	永泰犁壁坑钼矿	斑岩型	片状	2H
11	永泰焦坑钼矿	斑岩型	鳞片状	2H
11	永泰焦坑钼矿	热液石英脉型	片状	2H	370
12	永泰无岩坑钼矿	岩浆期后热液型	鳞片状	2H		谭元松，2010
13	永泰犁壁坑钼矿	斑岩型	鳞片状	2H
13	永泰犁壁坑钼矿	热液石英脉型	片状	2H
14	漳平洛阳钼矿	斑岩型	鳞片状	2H	350
14	漳平洛阳钼矿	热液石英脉型	细鳞状	2H+3R	200	97~168
15	漳平北坑场多金属矿	岩浆热液	它形粒状			0.996~7.062(张达等，2010)
16	平和钟腾铜钼矿	斑岩型	片状	2H		王登红等，2010
17	古田香峰钨钼矿	热液石英脉型	鳞片状	3R+2H	205
18	仙游砺山钼矿点	热液石英脉型	粉末状	3R+2H		8.426~14.257(王成辉等，2009)
19	永春东山寨钼矿	热液型	鳞片状	2H
20	南靖南坑钼矿点	热液型	鳞片状	2H
21	宁化行洛坑钨钼矿	含钨石英脉	鳞片状			2.851~4.292(张家菁等，2008)
22	永定山口钼矿	细脉	浸染状			31.131~58.455(罗锦昌等，2009)
23	霞浦大湾铍钼矿	中高温热液型	鳞片状			杨武平，2008
注：表中除有标著引文外，其余毛兴莉等(1988).

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参考文献(86)

[1]	Berzina, A.N., Sotnikov, V.I., Economou-Eliopoulos, M., et al., 2005. Distribution of Rhenium in Molybdenite from Porphyry Mo-Cu Deposits of Russia (Siberia) and Mongolia. Ore Geology Reviews, 26(1-2): 91-113. doi: org/10.1016/j.oregeorew.2004.12.002
[2]	Chen, F.G., Du, B.C., Wu, Q.Z., et al., 1984. Preliminary Study of Molybdenite (Polymorphic) in Shijiawan Molybdenum Ore Deposit, Shaanxi. Geology of Shaanxi, 2(2): 1-19 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SXDY198402000.htm
[3]	Chen, Y.S., 2009. Analysis of Mineralization Group Work Ability of Skarn Molybdenum Ore and Diabase Molybdenum Ore in Makeng Iron Mine. Modern Mining, 478(2): 45-50 (in Chinese with English abstract).
[4]	Fu, S.C., 2005. On Geologic Characteristics and Genesis of the Pingdi Molybdenum Deposit in Wuyishan City, Fujian Province. Geology of Fujian, 24(3): 125-133 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-FJDZ200503000.htm
[5]	Fu, S.C., 2011. Geologic Characters and Genesis of the Pingdi Molybdenum Deposit in the Wuyishan Mountains, Fujian Province. Geology and Exploration, 47(2): 268-276 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT201102019.htm
[6]	Fu, S.C., Su, J.H., 1994. Geological Characteristics of the Xiaochuan Granite-Gneiss of Jinning Period in Pucheng Area of Northern Fujian. Geology of Fujian, 13(4): 227-234 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-FJDZ404.001.htm
[7]	Fujian Exploration Authorities of Ministry of Geology and Mineral Resources, 1998. Instructions of Fujian Geological Map (1∶500 000). Fujian Map Press, Fuzhou(in Chinese).
[8]	Gao, T.J., Wang, Z.M., Wu, K.L., et al., 1999. Tectono-Magmatic Evolution and Mineralization of the Taiwan Strait and the Surrounding Areas. Geological Publishing House, Beijing, 105-148 (in Chinese).
[9]	Han, Y.W., 1988. Molybdenite Polytypes and the Mechanism of Polytype Formation. Earth Science—Journal of China University of Geosciences, 13(4): 385-394 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX198804003.htm
[10]	Hauri, E.H., Hart, S.R., 1997. Rhenium Abundances and Systematics in Oceanic Basalts. Chemical Geology, 139(1-4): 185-205. doi: 10.1016/S0009-2541(97)00035-1
[11]	Huang, D.H., 1992. Rhenium Content and Polytype Characteristics of Molybdenite from Molybdenum Deposits in East Qinling. Acta Petrologica et Mineralogica, 11(1): 74-83 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW199201009.htm
[12]	Huang, D.H., Wang, Y.C., Nie, F.J., et al., 1985. A New Type of Molybdenum Deposit—Geological Characteristics and Metallogenic Mechanism of the Huanglongpu Carbonatite Vein-Type of Molybdenum (Lead) Deposit, Shaanxi. Acta Geologica Sinica, 59: 241-257 (in Chinese with English abstract).
[13]	Liu, G.J., Peng, Z.C., Yang, G., 2006. Abundance and Geological Significance of Rhenium and Osmium in Pyrite Samples from Coals. Earth Science Frontiers, 13(1): 211-215 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200601030.htm
[14]	Liu, N.Z., 2005. On the Geologic Characteristics and Genesis of the Shuangchang Molybdenum Deposit in Pucheng County, Fujian Province. Geology of Fujian, 24(3): 141-146 (in Chinese with English abstract). http://www.researchgate.net/publication/303247166_On_the_Geologic_Characteristics_and_Genesis_of_the_Shangchang_Molybdenum_Deposit_in_Pucheng_County_Fujian_Province
[15]	Liu, S.G., 2005. On the Geologic Characteristics and Genesis of the Dalinkeng Molybdenum-Polymetallic Deposit in Songxi County, Fujian Province. Geology of Fujian, 24(3): 134-140 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-FJDZ200503001.htm
[16]	Luo, J.C., Chen, Z.H., Qu, W.J., 2009. Re-Os Isotopic Dating of Molybdenite from the Shankou Molybdenum Deposit in Yongding County of Fujian Province and Its Geological Significance. Rock and Mineral Analysis, 28(3): 254-258 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YKCS200903020.htm
[17]	Ma, J., Zhang, W.Z., Li, S.B., 2008. Molybdenum Mineral Separation. The Metallurgical Industry Press, Beijing, 1-241 (in Chinese).
[18]	Mao, J.W., Wang, Y.T., Lehmann, B., et al., 2006. Molybdenite Re-Os and Albite ⁴⁰Ar/³⁹Ar Dating of Cu-Au-Mo and Magnetite Porphyry Systems in the Yangtze River Valley and Metallogenic Implications. Ore Geology Reviews, 29(3-4): 307-324. doi: org/ 10.1016/j.oregeorev.2005.11.001
[19]	Mao, J.W., Xie, G.Q., Bierlein, F., et al., 2008. Tectonic Implications from Re-Os Dating of Mesozoic Molybdenum Deposits in the East Qinling-Dabie Orogenic Belt. Geochimica et Cosmochimica Acta, 72(18): 4607-4626. doi: 10.1016/j.gca.2008.06.027
[20]	Mao, J.W., Xie, G.Q., Guo, C.L., et al., 2007. Large-Scale Tungsten-Tin Mineralization in the Nanling Region, South China: Metallogenic Ages and Corresponding Geodynamic Processes. Acta Petrologica Sinica, 23(10): 2329-2338 (in Chinese with English abstract).
[21]	Mao, J.W., Xie, G.Q., Guo, C.L., et al., 2008. Spatial-Temporal Distribution of Mesozoic Ore Deposits in South China and Their Metallogenic Settings. Geological Journal of China Universities, 14(4): 510-526 (in Chinese with English abstract). http://www.researchgate.net/publication/284045978_Spatial-temporal_distribution_of_Mesozoic_ore_deposits_in_South_China_and_their_metallogenic_settings?ev=auth_pub
[22]	Mao, J.W., Zhang, Z.C., Zhang, Z.H., et al., 1999. Re-Os Isotopic Dating of Molybdenites in the Xiaoliugou W-(Mo) Deposit in the Northern Qilian Mountains and Its Geological Significance. Geochimica et Cosmochimica Acta, 63(11-12): 1815-1818. doi: org/10.1016/s0016-7037(99)0165-9
[23]	Mao, X.L., Zhang, Z.S., Zheng, N.L., 1988. A Preliminary Study of Molybdenite Polymorphism in Some Mo Deposits in the Coastal Reginon of Fujian. Journal of Fuzhou University (Natural Sciences Edtion), 1(1): 111-116 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=FZDZ198801019&dbcode=CJFD&year=1988&dflag=pdfdown
[24]	Mathur, R., Brantley, S., Anbar, A., et al., 2010. Variation of Mo Isotopes from Molybdenite in High-Temperature Hydrothermal Ore Deposits. Miner. Deposita, 45: 43-50. doi: 10.1007/s00126-009-0257-z
[25]	Mccandless, T.E., Ruiz, J., Campbell, A.R., 1993. Rhenium Behavior in Molybdenite in Hypogene and Near-Surface Environments: Implications for Re-Os Geochronometry. Geochimica et Cosmochimica Acta, 57: 889-905. doi: org/10.1016/0016-7037(93)90176-w
[26]	Ministry of Geology and Mineral Resources, 1987. Reference Manual of Mineral Industry Requirements. Geological Publishing House, Beijing, 1-672 (in chinese).
[27]	Newberry, R.J., 1979a. Polytypism in Molybdenite (I); A Non-Equilibrium Impurity-Induced Phenomenon. American Mineralogist, 64: 758-767.
[28]	Newberry, R.J., 1979b. Polytypism in Molybdenite (Ⅱ); Relationships between Polytypism, Ore Deposition/Alteration Stages and Rhenium Contents. American Mineralogist, 64: 768-775.
[29]	Peng, J.T., Zhou, M.F., Hu, R.Z., et al., 2006. Precise Molybdenite Re-Os and Ar-Ar Dating of the Mesozoic Yaogangxian Tungstern Deposit, Central Nanling District, South China. Mineralium Deposita, 41: 661-669. doi: 10.1007/s00126-006-0084-4
[30]	Raith, J.G., Stein, H., 2006. Variscan Ore Formation and Metamorphism at the Felbertal Scheelite Deposit (Austria): Constraining Tungsten Mineralization from Re-Os Dating of Molybdenite. Contrib. Mineral. Petrol., 152: 505-521. doi: 10.1007/s00410-006-0118-z
[31]	Selby, D., Creaser, R.A., 2001. Re-Os Geochronology and Systematic in Molybdenite from the Endako Porphyry Molybdenum Deposit, British Columbia, Canada. Econ. Geol., 96(1): 197-204. doi: 10.2113/gsecongeo.96.1.197
[32]	Shao, J.L., 1984. The Development of Polymorph Study of Molybdenum. Geological Science and Technology Information, 2: 37-44 (in Chinese).
[33]	Tan, Y.S., 2010. Geologic Characteristics and Origin Discussion of the Wuyankeng Molybdenum Deposit in Yongtai County, Fujian Province. Geology of Fujian, 29(2): 101-106 (in Chinese with English abstract).
[34]	Terada, k., Osaki, S., Ishihara, S., et al., 1971. Distribution of Rhenium in Molybdenites from Japan. Geochemical Journal, 4: 123-141. doi: 10.2343/geochemj.4.123
[35]	Wang, C.H., Wang, D.H., Chen, Z.H., et al., 2009. Geological Characteristics and Metallogenic Epoch of the Lishan Molybdenum Deposit—A Discussion on Regional Prospecting for Mo in the Southeastern Coast of China. Acta Mineralogica Sinica, 29(1): 63-69 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB200901010.htm
[36]	Wang, D.H., Chen, Z.H., Chen, Y.C., et al., 2010. New Data of the Rock-Forming and Ore-Forming Chronology for China's Important Mineral Resources Areas. Acta Geologica Sinica, 84(7): 1031-1040 (in Chinese with English abstract). http://www.researchgate.net/publication/284594588_New_data_of_the_rock-forming_and_ore-forming_chronology_for_China's_important_mineral_resources_areas
[37]	Wang, J.Z., Li, Z.Q., Liu, J.J., et al., 2004. Polytype and Typomorphic Characteristics of Molybdenite from LaLa Fe-Oxide-Cu-Au-Mo-Co-REE Deposit in Sichuan Province, China. Contributions to Geology and Mineral Resources Research, 19(2): 96-99 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZZK200402006.htm
[38]	Wu, G.G., Zhang, D., Cheng, B.L., et al., 2000. Post-Mesozoic Transformation of Tectonic Domain in Southeast China and Its Geodynamic Mechanism. Journal of China University of Geosciences, 11(3): 288-292. http://qikan.cqvip.com/Qikan/Article/Detail?id=4000690416
[39]	Wu, G.G., Zhang, D., Peng, R.M., et al., 2004. Study on the Evolution Regularity of Mineralization Ages in Southeastern China. Earth Science Frontiers, 11(1): 237-247 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200401031.htm
[40]	Xing, G.F., Yang, Z.F., Mao, J.R., et al., 2002. Characteristics of Early Jurassic Igneous Rocks on the Continental Margin of Southeastern China and Their Tectonic Significance. Regional Geology of China, 21(7): 384-391 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-bulletin-china_thesis/0201252294388.html
[41]	Xu, X.C., Yue, S.C., 1999. Factors Controlling the Metallogenic Evolution and Time-Space Distribution of the Ore Deposits in Zhejiang-Fujian-Guangdong Coastal Areas. Mineral Deposits, 18(4): 373-378 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ199904010.htm
[42]	Yang, W.P., 2008. On Geological Characteristics and Genesis of the Dawan Beryllium and Molybdenum Deposit in Xiapu County, Fujian Province. Geology of Fujian, 27(1): 1-7 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-FJDZ200801002.htm
[43]	Yang, Z.F., Luo, Z.H., Lu, X.X., 2011. Discussion on Significance of Re Content of Molybdenite in Tracing Source of Metallogenic Materials. Mineral Deposits, 30(4): 654-674 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ201104007.htm
[44]	Yuan, Z.X., Wu, L.S., Zhang, Z.Q., et al., 1991. The Sm-Nd, Rb-Sr Isotopic Age-Dating of Mayuan Group in Northern Fujian. Acta Petrologica et Mineralogica, 10(2): 127-132 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW199102003.htm
[45]	Zhang, D., Wu, G.G., Liu, N.Z., et al., 2010. Re-Os Isotopic Age of Molybdenite from the Beikengchang Molybdenite and Polymetal Deposit in Zhangping City, Fujian Province and Its Geological Significance. Acta Geologica Sinica, 84(10): 1428-1437 (in Chinese with English abstract). http://www.researchgate.net/publication/303241787_Re-Os_isotopic_age_of_molybdenite_from_the_beikengchang_molybdenite_and_polymetal_deposit_in_Zhangping_city_Fujian_province_and_its_geological_significance
[46]	Zhang, J.J., Chen, Z.G., Wang, D.H., et al., 2008. Geological Characteristics and Metallogenic Epoch of the Xingluokeng Tungsten Deposit, Fujian Province. Geotectonica et Metallogenia, 116(32): 92-97 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=26509874
[47]	Zhang, K.Y., Wang, J.P., Du, A.D., et al., 2009. Re-Os Isotopic Dating of Molybdenite from the Chilu Molybdenum Deposit in Fuan, Fujian Province. Geology in China, 36(1): 147-155 (in Chinese with English abstract).
[48]	Zhao, G.C., Sun, D.Y., He, T.X., 1996. Buffering of Metamorphic Reaction Temperature by Metamorphic Fluids in Mayuan Group, Northern Fujian Province. Acta Petrologica Sinica, 12(1): 59-69 (in Chinese with English abstract). http://www.researchgate.net/publication/289895672_Buffering_of_metamorphic_reaction_temperature_by_metamorphic_fluids_in_mayuan_group_northern_fujian_province
[49]	Zheng, K.Q., Huang, W.X., Zhou, L.S., 1989. Geology and Geochemistry of the Sanbao Tungsten-Molybdenum Ore Deposit in Gutian County, Fujian Province. Mineral Deposits, 8(1): 29-38 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ198901004.htm
[50]	Zhou, K., Ye, H.S., Mao, J.W., et al., 2009. Geological Characteristics and Molybdenite Re-Os Isotopic Dating of Yuchiling Porphyry Mo Deposit in Western Henan Province. Mineral Deposits, 28(2): 170-184 (in Chinese with English abstract). http://www.cnki.com.cn/article/cjfdtotal-ysxb200902015.htm
[51]	陈福根, 杜本臣, 武清周, 等, 1984. 陕西石家湾钼矿床中辉钼矿(多型)初步研究. 陕西地质, 2(2): 1-19. https://www.cnki.com.cn/Article/CJFDTOTAL-SXDY198402000.htm
[52]	陈跃升, 2009. 马坑铁矿区单钼矿成矿组可采性分析. 现代矿业, 478(2): 45-50. doi: 10.3969/j.issn.1674-6082.2009.02.013
[53]	地矿部福建地质矿产勘查开发局, 1998. 福建省地质图说明书(1∶50万). 福州: 福建省地图出版社.
[54]	地质矿产部, 1987. 矿产工业要求参考手册. 北京: 地质出版社.
[55]	傅树超, 2005. 福建武夷山坪地钼矿床地质特征及成因探讨. 福建地质, 24(3): 125-133. doi: 10.3969/j.issn.1001-3970.2005.03.001
[56]	傅树超, 2011. 福建省武夷山坪地钼矿床地质特征及成因探讨. 地质与勘探, 47(2): 268-276. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201102019.htm
[57]	傅树超, 苏江湖, 1994. 闽北浦城地区晋宁期小串花岗片麻岩地质特征. 福建地质, 13(4): 227-234. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ404.001.htm
[58]	高天钧, 王振民, 吴克隆, 等, 1999. 台湾海峡及其周边地区构造岩浆演化与成矿作用. 北京: 地质出版社, 105-148.
[59]	韩吟文, 1988. 辉钼矿的多型及其成因初探. 地球科学——中国地质大学学报, 13(4): 385-394. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198804003.htm
[60]	黄典豪, 1992. 东秦岭地区钼矿床中辉钼矿的铼含量及多型特征. 岩石矿物学杂志, 11(1): 74-83. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW199201009.htm
[61]	黄典豪, 王义昌, 聂凤军, 等, 1985. 一种新的钼矿床类型——陕西黄龙铺碳酸岩脉型钼(铅)矿床地质特征及成矿机制. 地质学报, 59: 241-257. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198503006.htm
[62]	刘桂建, 彭子成, 杨刚, 2006. 煤中黄铁矿的铼-锇同位素含量及其地质意义. 地学前缘, 13(1): 211-215. doi: 10.3321/j.issn:1005-2321.2006.01.028
[63]	刘乃忠, 2005. 福建浦城上厂钼矿床地质特征及成因初探. 福建地质, 24(3): 141-146. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ200503002.htm
[64]	刘诗光, 2005. 福建松溪大林坑钼多金属矿床地质特征及成因初探. 福建地质, 24(3): 134-140. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ200503001.htm
[65]	罗锦昌, 陈郑辉, 屈文俊, 2009. 福建省永定山口钼矿辉钼矿铼-锇同位素定年及其地质特征. 岩矿测试, 28(3): 254-258. doi: 10.3969/j.issn.0254-5357.2009.03.012
[66]	马晶, 张文钲, 李枢本, 2008. 钼矿选矿. 北京: 冶金工业出版社.
[67]	毛景文, 谢桂青, 郭春丽, 等, 2007. 南岭地区大规模钨锡多金属成矿作用: 成矿时限及地球动力学背景. 岩石学报, 23(10): 2329-2338. doi: 10.3969/j.issn.1000-0569.2007.10.002
[68]	毛景文, 谢桂青, 郭春丽, 等, 2008. 华南地区中生代主要金属矿床时空分布规律和成矿环境. 高校地质学报, 14(4): 510-526. doi: 10.3969/j.issn.1006-7493.2008.04.005
[69]	毛兴莉, 张载三, 郑南来, 1988. 福建沿海一些钼矿床中辉钼矿多型性的初步研究. 福州大学学报(自然科学版), 1(1): 111-116. https://www.cnki.com.cn/Article/CJFDTOTAL-FZDZ198801019.htm
[70]	邵洁涟, 1984. 辉钼矿多型研究的新进展. 地质科技情报, 2: 37-44. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ198402010.htm
[71]	谭元松, 2010. 福建永泰无岩坑钼矿地质特征及成因探讨. 福建地质, 29(2): 101-106. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ201002005.htm
[72]	王成辉, 王登红, 陈郑辉, 等, 2009. 福建砺山钼矿的地质特征、成矿时代及区域找矿前景. 矿物学报, 29(1): 63-69. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB200901010.htm
[73]	王登红, 陈郑辉, 陈毓川, 等, 2010. 我国重要矿产地成岩成矿年代学研究新数据. 地质学报, 84(7): 1031-1040. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201007009.htm
[74]	王奖臻, 李泽琴, 刘家军, 等, 2004. 拉拉铁氧化物-铜-金-钼-钴-稀土矿床辉钼矿的多型及标型特征. 地质找矿论丛, 19(2): 96-99. https://www.cnki.com.cn/Article/CJFDTOTAL-DZZK200402006.htm
[75]	吴淦国, 张达, 彭润民, 等, 2004. 东南沿海成矿带矿床形成的时间演化规律研究. 地学前缘, 11(1): 237-247. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200401031.htm
[76]	邢光福, 杨祝良, 毛建仁, 等, 2002. 东南大陆边缘早侏罗世火成岩特征及其构造意义. 地质通报, 21(7): 384-391. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200207004.htm
[77]	徐晓春, 岳书仓, 1999. 浙闽粤滨海地区成矿演化和矿床时空分布的控制因素. 矿床地质, 18(4): 373-378. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ199904010.htm
[78]	杨武平, 2008. 福建霞浦大湾铍钼矿床地质特征及成因初探. 福建地质, 27(1): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-FJDZ200801002.htm
[79]	杨宗锋, 罗照华, 卢欣祥, 等, 2011. 关于辉钼矿中Re含量示踪来源的讨论. 矿床地质, 30(4): 654-674. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201104007.htm
[80]	袁忠信, 吴良士, 张宗清, 等, 1991. 闽北麻源群Sm-Nd、Rb-Sr同位素年龄研究. 岩石矿物学杂志, 10(2): 127-132. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW199102003.htm
[81]	张达, 吴淦国, 刘乃忠, 等, 2010. 福建漳平北坑场钼多金属矿床辉钼矿Re-Os同位素年龄及其地质意义. 地质学报, 84(10): 1428-1437. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201010004.htm
[82]	张家菁, 陈郑辉, 王登红, 等, 2008. 福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义. 大地构造与成矿学, 116(32): 92-97. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200801013.htm
[83]	张克尧, 王建平, 杜安道, 等, 2009. 福建福安赤路钼矿床辉钼矿Re-Os同位素年龄及其地质意义. 中国地质, 36(1): 147-155. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200901016.htm
[84]	赵国春, 孙德有, 贺同兴, 1996. 闽北麻源群变质流体对变质反应温度缓冲作用研究. 岩石学报, 12(1): 59-69. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB601.004.htm
[85]	郑开旗, 黄维新, 周乐生, 1989. 福建古田县三保钨钼矿床地质地球化学. 矿床地质, 8(1): 29-38. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ198901004.htm
[86]	周珂, 叶会寿, 毛景文, 等, 2009. 豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄. 矿床地质, 28(2): 170-184. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200902007.htm