云南老君山矿集区的晚侏罗世-早白垩世成矿事件

李建康; 王登红; 李华芹; 陈郑辉; 梅玉萍

doi:10.3799/dqkx.2013.100

云南老君山矿集区的晚侏罗世-早白垩世成矿事件

doi: 10.3799/dqkx.2013.100

1.
中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室, 北京 100037
2.
中国地质调查局武汉地质矿产研究所, 湖北宜昌 443003

基金项目:

国家深部探测技术与实验研究专项 SinoProbe-03-01

中央公性科研院所基本科研业务费 K1001

中国地质大调查项目 1212011220805

详细信息

作者简介:
李建康(1976-), 副研究员, 主要从事矿床学研究.E-mail: Li9968@126.com

中图分类号: P612
计量
- 文章访问数: 4195
- HTML全文浏览量: 711
- PDF下载量: 1188
- 被引次数: 0
出版历程
- 收稿日期: 2012-10-16
- 刊出日期: 2013-09-15

Late Jurassic-Early Cretaceous Mineralization in the Laojunshan Ore Concentration Area, Yunnan Province

1.
Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Wuhan Institute of Geology and Mineral Resources, Yichang 443003, China

摘要

摘要: 云南省老君山矿集区产出南秧田、花石头、茶叶山等众多钨矿床, 是南岭成矿带西段为数不多的以钨为主的矿集区.由于受到多期构造热事件的影响, 该矿集区的成矿年龄存在较大的争议.为此, 选择白钨矿Sm-Nd同位素体系测定了南秧田钨矿田中长石石英脉型矿体的年龄, 用白云母和黑云母Ar-Ar方法厘定了区域花岗伟晶岩的形成时代及其变质围岩的变质时限.研究表明, 南秧田钨矿田中长石石英脉型白钨矿矿体的形成年龄为159±14 Ma, 明显晚于印支期形成的矽卡岩型矿体; 两花岗伟晶岩及其围岩变质作用的时代分别为144~141 Ma和121~112 Ma, 说明老君山矿集区存在晚侏罗世-早白垩世的构造热事件和成矿作用.综合前人的研究成果, 老君山矿集区受到区域花岗片麻岩和花岗岩产出特征的制约, 成矿时代分布与南岭成矿带一致, 存在晚三叠世、晚侏罗世-早白垩世和晚白垩世3个成矿高峰期.而且, 老君山矿集区的成矿特点与南岭东段的钨矿床有一定的可类比性, 是"东钨西扩"的典型实例, 这可能与老君山矿集区遭受了较高的剥蚀程度有关, 暗示南岭西段的高剥蚀区是寻找晚侏罗世钨矿床的远景区.
- 晚侏罗世-早白垩世成矿事件 /
- 南秧田钨矿田 /
- 老君山矿集区 /
- 南岭成矿带 /
- 构造 /
- 矿床
Abstract: The Laojunshan ore concentration area, containing many tungsten deposits of Nanyangtian, Huashitou and Chayeshan, is one of the few tungsten concentration areas in the western Nanling metallogenic belt. But, its regional ore-forming ages are controversial due to multi-stage tectono-thermal events. In this paper, the scheelite Sm-Nd dating method was used to determine the ore-forming age of the feldspar quartz vein type ore bodies in the Nanyangtian ore field, and the muscovite and biotite Ar-Ar dating method were used to determine the crystallization ages of the regional granitic pegmatites and the metamorphic age of their wall rocks respectively. The dating results show that the feldspar quartz veins type ore bodies formed at 159±14 Ma, younger than the skarn type ore bodies, and the pegmatite crystallization ages and the wall rock's metamorphic ages are 144-141 Ma and 121-112 Ma respectively. So the Late Jurassic-Early Cretaceous tectono-thermal event and tungsten mineralization occurred in Laojunshan area. The metallogenic regularity in the Laojunshan areas illustrates that the regional ore deposits or spots are constrained by the regional granite gneiss and granitic intrusion, and the ore-forming period is consistent with the three ore-forming peaks in the Nanling minerallenic belt. Furthermore, the mineralization features in Laojunshan area are similar with that in the eastern Nanling metallogenic belt, which may be due to the high denudation degree. It is concluded that the great denudation area in the western Nanling region has great potential to find tungsten deposit formed in Late Triassic and Indo-Chinese and Late Jurassic-Early Cretaceous.
- Late Jurassic-Early Cretaceous mineralization /
- Nanyangtian tungsten ore field /
- Laojunshan ore concentration area /
- Nanling mierallenic belt /
- tectonics /
- ore deposits

HTML全文

图 1 云南省老君山矿集区矿产地质图(据云南省地质局，1:20万地质矿产报告·马关幅，1976编制)

1.三叠系；2.二叠系；3.泥盆系；4.寒武系歇场组白云质灰岩；5.寒武系龙哈组白云岩；6.寒武系田蓬组白云质灰岩；7.寒武系未分层中下统片岩、片麻岩；8.花岗片麻岩；9.燕山晚期第1期中粗粒花岗岩；10.燕山晚期第2期中细粒花岗岩；11.断裂；12.超大型矿床；13.大型矿床；14.中型矿床；15.小型矿床；16.矿(化)点；17.白钨矿矿床；18.黑钨矿矿床；19.锡矿；20.钨锡矿；21.锡多金属矿；22.铍矿；23.钨铍矿；24.铜矿；25.铅锌矿；26.白云母矿；27.晚三叠世成矿；28.晚三叠世和晚侏罗-早白垩世多阶段成矿；29.晚侏罗世-早白垩世成矿；30.晚白垩世成矿；31.本文工作区

Fig. 1. Geological map of the Laojunshan ore concentration area in Yunnan Province

下载: 全尺寸图片幻灯片

图 2 南秧田矿田地质图(据云南省317地质分队，1984)

1.第四系；2.下寒武统冲庄组太阳坪段白云母斜长片麻岩；3.下寒武统冲庄组南秧田段大理岩、片岩和片麻岩；4.下寒武统冲庄组戈岭段角闪变粒岩和片麻岩；5.下寒武统冲庄组戈岭段花岗片麻岩；6.下寒武统冲庄组南秧田段石英电气石岩；7.二云二长花岗岩；8.断层；9.花岗斑岩脉；10.矽卡岩；11.钠长伟晶岩脉；12.白钨矿体；13.采样位置

Fig. 2. Geological map of the Nanyangtian ore field

下载: 全尺寸图片幻灯片

图 3 南秧田钨矿田中产出的长石石英脉型白钨矿矿体

a.穿过矽卡岩矿体和变质围岩的长石石英矿脉；b.长石石英矿脉切过沿石英黑云母片岩片理产出的石英细脉，石英细脉未发现明显的白钨矿化

Fig. 3. The feldspar quartz veins of Nanyangtian tungsten ore filed

下载: 全尺寸图片幻灯片

图 4 云南老君山矿集区花岗伟晶岩的产出状态

a.沿黑云闪长片麻岩片理产出的保良街伟晶岩脉；b.与黑云斜长片麻岩呈侵入式接触关系上阳坡伟晶岩脉

Fig. 4. The granitic pegmatite veins exists in regional metamorphic rock

下载: 全尺寸图片幻灯片

图 5 用于白云母和黑云母Ar-Ar定年的岩石照片

BLJ-2、BLJ-3分别为保良街伟晶岩脉与其黑云闪长片麻岩围岩的岩石样品；BLJ-LB-8、BLJ-LB-2分别为上阳坡某伟晶岩脉与其黑云斜长片麻岩围岩的岩石样品

Fig. 5. Pictures of rock samples for Ar-Ar dating of muscovite and biotite

下载: 全尺寸图片幻灯片

图 6 南秧田矿田法瓦矿床白钨矿Sm-Nd同位素等时线

Fig. 6. The Sm-Nd isochron of scheelite in the Fawa tungsten deposit, Nanyangtian ore field

下载: 全尺寸图片幻灯片

图 7 云南老君山矿集区保良街伟晶岩中白云母(BLJ-2)及其围岩中黑云母(BLJ-3)Ar-Ar定年的坪年龄和反等时线

Fig. 7. The ⁴⁰Ar/³⁹Ar plateau age spectra and inverse isochron age spectra for muscovite (BLJ-2) and biotite (BLJ-3) from the Baoliangjie pegmatite and it's wall rock respectively

下载: 全尺寸图片幻灯片

图 8 云南老君山矿集区上阳坡伟晶岩中白云母(BLJ-LB-8)及其围岩中黑云母(BLJ-LB-2)Ar-Ar定年的坪年龄和反等时线

Fig. 8. The ⁴⁰Ar/³⁹Ar plateau age spectra and inverse isochron age spectra for muscovite (BLJ-LB-8) and biotite (BLJ-LB-2) from the Shangyangpo pegmatite and it's wall rock repectively

下载: 全尺寸图片幻灯片

表 1 南秧田矿田法瓦矿床的白钨矿Sm-Nd定年结果

Table 1. Sm-Nd dating results of scheelite in the Fawa tungsten deposit, Nanyangtian ore field

原送样号	W(Sm)(10^-6)	W(Nd)(10^-6)	¹⁴⁷Sm/¹⁴⁴Nd	¹⁴³Nd/¹⁴⁴Nd	1σ
YF-2-1	12.15	38.38	0.191 6	0.511 980	0.000 003
YF-2-2	12.40	37.44	0.200 3	0.511 990	0.000 002
YF-2-3	13.56	35.87	0.228 7	0.512 020	0.000 003
YF-2-4	11.82	30.01	0.238 2	0.512 028	0.000 003
YF-2-5	9.49	26.88	0.213 6	0.512 004	0.000 002
YF-2-6	9.15	27.67	0.200 1	0.511 989	0.000 004
YF-2-7	15.15	46.58	0.196 8	0.511 985	0.000 004
YF-2-8	9.42	23.04	0.247 3	0.512 038	0.000 003
YF-2-9	12.17	37.56	0.196 1	0.511 985	0.000 004

下载: 导出CSV

表 2 云南老君山矿集区保良街伟晶岩脉的白云母(BLJ-2)⁴⁰Ar/³⁹Ar逐步加热分析结果

Table 2. The ⁴⁰Ar/³⁹Ar step-heating data of muscovite (BLJ-2) from the Baoliangjie pegmatite

T(℃)	(⁴⁰Ar/³⁹Ar)_m	(³⁶Ar/³⁹Ar)_m	(³⁷Ar/³⁹Ar)_m	(³⁸Ar/³⁹Ar)_m	⁴⁰Ar(%)	⁴⁰Ar/³⁹Ar	³⁹Ar(10^-14 mol)	³⁹Ar(Cum.)(%)	年龄(Ma)	±1σ(Ma)
400	21.218 2	0.055 8	0.246 0	0.048 9	22.28	4.728 2	23.29	0.34	82.0	11.0
500	11.645 1	0.028 9	0.091 9	0.033 6	26.67	3.105 7	25.18	0.70	54.0	10.0
600	10.724 5	0.019 5	0.040 7	0.0249	46.16	4.951 1	75.78	1.80	85.4	4.3
700	7.876 8	0.006 6	0.025 5	0.020 5	75.23	5.926 1	169.17	4.24	101.8	2.7
800	8.015 2	0.001 3	0.008 0	0.014 5	95.29	7.637 8	757.85	15.20	130.1	1.4
900	7.958 9	0.000 5	0.003 7	0.013 3	98.16	7.812 3	1013.71	29.86	133.0	1.3
1 000	7.985 5	0.000 3	0.000 6	0.012 7	98.74	7.884 7	2258.82	62.53	134.2	1.3
1 100	8.328 6	0.000 4	0.003 6	0.013 4	98.59	8.211 6	1077.28	78.11	139.5	1.5
1 200	8.501 4	0.000 4	0.001 2	0.014 9	98.62	8.384 2	997.64	92.54	142.3	1.6
1 300	8.543 3	0.000 8	0.017 0	0.014 5	97.16	8.300 7	479.43	99.47	141.0	1.6
1 400	10.692 7	0.008 2	0.079 0	0.027 6	77.34	8.270 6	36.58	100.00	140.5	2.7
注：下标m表示样品中测定的同位素比值，总的年龄=134.3 Ma，⁴⁰Ar/³⁹Ar为放射性⁴⁰Ar与³⁹Ar的比值，W=45.90 mg，J=0.009 792.

下载: 导出CSV

表 3 云南老君山矿集区保良街伟晶岩脉围岩(黑云闪长片麻岩)的黑云母(BLJ-3)⁴⁰Ar/³⁹Ar逐步加热分析结果

Table 3. The ⁴⁰Ar/³⁹Ar step-heating data of biotite (BLJ-3) from the wall rock (biotite diorite gneiss) of the Baoliangjie pegmatite

T(℃)	(⁴⁰Ar/³⁹Ar)_m	(³⁶Ar/³⁹Ar)_m	(³⁷Ar/³⁹Ar)_m	(³⁸Ar/³⁹Ar)_m	⁴⁰Ar(%)	⁴⁰Ar/³⁹Ar	³⁹Ar(10^-14 mol)	³⁹Ar(Cum.)(%)	年龄(Ma)	±1σ(Ma)
400	174.087 4	0.586 0	0.092 4	0.133 2	0.53	0.917 6	58.96	0.72	15.9	9.6
500	24.185 9	0.077 2	0.057 9	0.031 5	5.67	1.372 0	119.15	2.18	23.7	8.7
600	19.984 4	0.047 9	0.012 0	0.023 0	29.13	5.822 1	275.66	5.54	98.3	2.4
700	8.783 3	0.007 1	0.007 4	0.014 9	76.19	6.692 0	1 137.23	19.44	112.5	1.9
800	7.459 9	0.002 5	0.005 2	0.013 2	90.13	6.723 9	707.81	28.08	113.0	1.3
900	6.971 7	0.001 1	0.006 8	0.013 4	95.48	6.656 3	1 423.19	45.47	111.9	1.2
1 000	7.148 4	0.001 6	0.025 1	0.013 8	93.37	6.674 9	841.15	55.75	112.2	1.3
1 100	6.775 0	0.000 7	0.011 1	0.013 2	97.07	6.576 9	1 993.39	80.10	110.7	1.2
1 200	6.861 2	0.000 8	0.007 5	0.013 1	96.58	6.626 5	1 349.50	96.58	111.5	1.2
1 300	7.219 5	0.001 7	0.069 1	0.015 5	93.08	6.720 5	264.77	99.82	113.0	2.1
1 400	9.719 8	0.010 6	0.257 2	0.037 6	67.82	6.593 2	14.88	100.00	110.9	3.8
注：下标m表示样品中测定的同位素比值，总的年龄=109.4 Ma，⁴⁰Ar/³⁹Ar为放射性⁴⁰Ar与³⁹Ar的比值，W=47.04 mg，J=0.009 618.

下载: 导出CSV

表 4 云南老君山矿集区上阳坡伟晶岩脉的白云母(BLJ-LB-8)⁴⁰Ar/³⁹Ar逐步加热分析结果

Table 4. The ⁴⁰Ar/³⁹Ar step-heating data of muscovite (BLJ-LB-8) from the Shangyangpo pegmatite

T(℃)	(⁴⁰Ar/³⁹Ar)_m	(³⁶Ar/³⁹Ar)_m	(³⁷Ar/³⁹Ar)_m	(³⁸Ar/³⁹Ar)_m	⁴⁰Ar(%)	⁴⁰Ar/³⁹Ar	³⁹Ar(10^-14 mol)	³⁹Ar(Cum.)(%)	年龄(Ma)	±1σ(Ma)
400	22.144 5	0.051 8	0.232 5	0.037 2	30.87	6.838 0	37.23	0.41	122.4	7.6
500	23.978 8	0.055 9	0.125 2	0.031 2	31.18	7.476 3	59.66	1.08	133.4	8.9
600	26.045 7	0.063 7	0.090 2	0.032 3	27.73	7.224 2	51.99	1.66	129.1	9.3
700	12.976 7	0.019 2	0.025 3	0.017 6	56.27	7.302 5	401.56	6.12	130.4	2.1
800	8.605 8	0.001 8	0.007 1	0.013 8	93.81	8.072 7	894.53	16.07	143.7	1.6
900	8.298 4	0.000 4	0.007 2	0.013 4	98.47	8.171 6	2 774.91	46.92	145.3	1.4
1 000	8.159 8	0.000 5	0.008 6	0.013 4	98.07	8.002 1	1 968.16	68.80	142.5	1.4
1 100	8.281 4	0.000 6	0.026 3	0.012 9	97.89	8.106 8	1 165.88	81.77	144.2	1.6
1 200	8.180 6	0.000 4	0.015 7	0.013 0	98.49	8.057 3	1 499.16	98.44	143.4	1.4
1 300	9.281 5	0.004 3	0.243 1	0.022 7	86.60	8.039 1	125.85	99.83	143.1	1.9
1 400	13.715 1	0.019 2	0.269 3	0.043 0	58.67	8.048 2	14.87	100.00	143.2	6.1
注：下标m表示样品中测定的同位素比值，总的年龄=143.1 Ma，⁴⁰Ar/³⁹Ar为放射性⁴⁰Ar与³⁹Ar的比值，W=46.36 mg，J=0.010 268.

下载: 导出CSV

表 5 云南老君山矿集区上阳坡伟晶岩脉的围岩(黑云斜长片麻岩)的黑云母(BLJ-LB-2)⁴⁰Ar/³⁹Ar逐步加热分析结果

Table 5. The ⁴⁰Ar/³⁹Ar step-heating data of biotite (BLJ-LB-2) from the wall rock (biotite plagiogneiss gneiss) of the Shangyangpo pegmatite

T(℃)	(⁴⁰Ar/³⁹Ar)_m	(³⁶Ar/³⁹Ar)_m	(³⁷Ar/³⁹Ar)_m	(³⁸Ar/³⁹Ar)_m	⁴⁰Ar(%)	⁴⁰Ar/³⁹Ar	³⁹Ar(10^-14 mol)	³⁹Ar(Cum.)(%)	年龄(Ma)	±1σ(Ma)
400	13.165 0	0.020 1	0.093 7	0.021 7	54.82	7.217 7	205.05	3.15	127.1	3.1
500	8.241 4	0.005 2	0.011 6	0.015 3	81.45	6.712 8	258.56	7.11	118.5	2.2
600	7.440 1	0.001 6	0.003 7	0.012 7	93.41	6.949 5	621.57	16.65	122.6	1.5
700	7.160 6	0.000 4	0.003 6	0.012 9	98.38	7.044 7	1 614.86	41.43	124.2	1.8
800	7.035 7	0.000 5	0.002 6	0.013 1	97.97	6.893 1	1 280.27	61.07	121.6	1.3
900	6.971 3	0.000 5	0.009 2	0.014 1	97.83	6.820 1	412.60	67.40	120.4	1.5
1 000	7.035 6	0.000 7	0.014 4	0.015 2	97.13	6.833 9	255.26	71.32	120.6	1.5
1 100	7.056 8	0.000 8	0.007 3	0.013 5	96.73	6.825 8	722.85	82.41	120.5	1.3
1 200	7.114 8	0.000 7	0.007 9	0.013 6	97.12	6.909 6	890.97	96.08	121.9	1.4
1 300	7.179 9	0.001 1	0.023 5	0.014 8	95.50	6.857 0	239.51	99.76	121.0	1.6
1 400	9.185 7	0.014 5	0.123 9	0.038 0	53.39	4.904 5	15.92	100.00	87.4	7.5
注：下标m表示样品中测定的同位素比值，总年龄=122.1 Ma，⁴⁰Ar/³⁹Ar为放射性⁴⁰Ar与³⁹Ar的比值，W=46.90 mg，J=0.010 116.

下载: 导出CSV

表 6 云南老君山矿集区主要地质体的年龄数据

Table 6. The dating results of main geological bodies in the Laojunshan ore concentration area

矿床名称	地质体	定年方法	年龄(Ma)	参考文献
南秧田钨矿	矽卡岩	辉钼矿Re-Os	209~214	冯佳睿等，2011a
	矽卡岩	金云母Ar-Ar	114~129	谭洪旗等，2011
	长石石英脉	白钨矿Sm-Nd	159±14	本文
新寨锡矿	矽卡岩	金云母Ar-Ar	209	冯佳睿等，2011a
花石头钨矿	石英脉	白云母Ar-Ar	85	刘玉平等，2011
洒西钨铍矿	矽卡岩	金云母Ar-Ar	120	刘玉平等，2011
都龙锡多金属矿床	矽卡岩	锡石TIMS U-Pb	80	刘玉平等，2007
保良街伟晶岩	白云母钠长石伟晶岩	白云母Ar-Ar	141	本文
保良街伟晶岩	黑云闪长片麻岩	黑云母Ar-Ar	112	本文
上阳坡伟晶岩	白云母钠长石伟晶岩	白云母Ar-Ar	144	本文
上阳坡伟晶岩	黑云斜长片麻岩	黑云母Ar-Ar	121	本文

下载: 导出CSV

参考文献(65)

Cai, D.K., 1983. Formation, Evolution and Tungsten-Tin Mineralization of Granitoid in Laojunshan, Southeastern Yunnan Province. Yunnan Geology, 2(2): 102-113 (in Chinese).
Cai, M.H., Chen, K.X., Qu, W.J., et al., 2006. Geological Characteristics and Re-Os Dating of Molybdenites in Hehuaping Tin-Polymetallic Deposit, Southern Hunan Province. Mineral Deposits, 25(3): 263-268 (in Chinese with English abstract).
Chen, W., Zhang, Y., Ji, Q., et al., 2002. The Magmatism and Deformation Times of the Xidatan Rock Series, East Kunlun Mountain. Science in China(Series B), 45(Suppl. ): 20-27. doi: 10.3969/j.issn.1674.2002.zl.003
Chen, Y.C., 1983. The Metallogenetic Series of the Rare-Earth, Rare and Nonferrous Metal Deposits Related to the Yanshanian Granites in South China. Mineral Deposits, (2): 15-24 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ198302002.htm
Feng, J.R., Mao, J.W., Pei, R.F., et al., 2011a. A Tentative Discussion on Indosinian Ore-Forming Events in Laojunshan Area of Southeastern Yunnan: A Case Study of Xinzhai Tin Deposit and Nanyangtian Tungsten Deposit. Mineral Deposits, 30(1): 57-73 (in Chinese with English abstract).
Feng, J.R., Mao, J.W., Pei, R.F., et al., 2011b. Ore-Forming Fluids and Metallogenesis of Nanyangtian Tungsten Deposit in Laojunshan, Southeastern Yunnan Province. Mineral Deposits, 30(3): 403-419 (in Chinese with English abstract). http://www.researchgate.net/publication/285467339_Ore-forming_fluids_and_metallogenesis_of_Nanyangtian_tungsten_deposit_in_Laojunshan_southeastern_Yunnan_Province
Feng, J.R., Zhou, Z.H., Cheng, Y.B., 2010. Characteristics and Significance of the Fluid Inclusions from the Nanyangtian Tungsten Deposit in Yunnan Province. Acta Petrologica et Mineralogica, 29(1): 50-58 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201001008.htm
Guo, L.G., 2006. Primary Research on Geochemistry and Geochronology of the Laojunshan Metamorphic Core Complex, Sourtheastern Yunnan (Dissertation). Institute of Geochemistry, Chinese Academy of Science, Guiyang (in Chinese with English abstract).
Hua, R.M., Chen, P.R., Zhang, W.L., et al., 2005. Three Major Metallogenic Events in Mesozoic in South China. Mineral Deposits, 24(2) : 99-107 (in Chinese with English abstract).
Hua, R.M., Li, G.L., Zhang, W.L., et al., 2010. A Tentative Discussion on Differences between Large-Scale Tungsten and Tin Mineralizations in South China. Mineral Deposits, 29(1): 9-22 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ201001004.htm
Hua, R.M., Mao, J.W., 1999. A Preliminary Discussion on the Mesozoic Metallogenic Explosion in East China. Mineral Deposits, 18(4): 300-308 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ199904001.htm
Li, D.X., Xu, S.S., 2000. Rotation-Shearing Genesis of Metamorphic Core Complex—Structural Analysis of Metamorphic Core Complex in Laojunshan, Southeastern Yunnan Province. Geological Review, 46(2): 113-120 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-review_thesis/0201253282262.html
Li, H.Q., Xie, C.F., Chang, H.L., et al., 1998. Study on Metallogenetic Chronology of Nonferrous and Precious Metallic Ore Deposits in North Xinjiang, China. Geological Publishing House, Beijing, 10-24 (in Chinese with English abstract).
Li, J.K., Wang, D.H., Liang, T., et al., 2013. The Research Progress of Nanling Regional Mineralization and Deep Exploration and Its Indication to Find Tungsten and Tin Deposits in Tibet. Acta Geoscientica Sinica, 34(1): 58-74 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB201301009.htm
Li, J.K., Wang, D.H., Zhang, D.H., et al., 2007. Mineralizing Mechanism and Continental Geodynamics of Typical Pegmatite Deposits in Western Sichuan, China. Atomic Energy Press, Beijing, 59-97 (in Chinese with English abstract).
Li, S.R., Wang, D.H., Liang, T., et al., 2008. Metallogenic Epochs of the Damingshan Tungsten Deposit in Guangxi and Its Prospecting Potential. Acta Geologica Sinica, 82(7): 873-879 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=28044490
Liang, T., Wang, D.H., Hou, K.J., et al., 2011. LA-MC-ICP-MS Zircon U-Pb Dating of Longxianggai Pluton in Dachang of Guangxi and Its Geological Significance. Acta Petrologica Sinica, 27(6): 1624-1636 (in Chinese with English abstract). http://www.oalib.com/paper/1475196
Liu, S.B., Wang, D.H., Chen, Y.C., et al., 2008. ⁴⁰Ar/³⁹Ar Ages of Muscovite from Different Types Tungsten-Bearing Quartz Veins in the Chong-Yu-You Concentrated Mineral Area in Gannan Region and Its Geological Significance. Acta Geologica Sinica, 82(7): 932-940 (in Chinese with English abstract). http://www.researchgate.net/publication/279652096_40Ar39Ar_ages_of_muscovite_from_different_types_tungsten-bearing_quartz_veins_in_the_Chong-Yu-You_concentrated_mineral_area_in_Gannan_region_and_its_geological_significance
Liu, Y.P., Li, Z.X., Li, H.M., et al., 2007. U-Pb Geochronology of Cassiterite and Zircon from the Dulong Sn-Zn Deposit: Evidence for Cretaceous Large-Scale Granitic Magmatism and Mineralization Events in Southeastern Yunnan Province, China. Acta Petrologica Sinica, 23(5): 967-976 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200705011.htm
Liu, Y.P., Li, Z.X., Ye, L., et al., 2011. Ar-Ar Geochronology of Tungsten Mineralization in the Laojunshan Ore Concentration Area, Yunnan Province. Acta Mineralogica Sinica, (S1): 617-618 (in Chinese).
London, D., 2008. Pegmatites. Can Mineral, Special Publication 10, QuÉBec, 347
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). http://www.researchgate.net/publication/279556851_large-scale_tungsten-tin_mineralization_in_the_nanling_region_south_china_metallogenic_ages_and_corresponding_geodynamic_processes
Raimbauh, L., Baumer, A., Dubru, M., et al., 1993. REE Fractionation Between Scheelite and Apatite in Hydrothermal Conditions. American Mineralogist, 78(11-12): 1275-1285. http://search.ebscohost.com/login.aspx?direct=true&db=aph&AN=9410070016&site=ehost-live
Tan, H.Q., Liu, Y.P., Ye, L., et al., 2011. ⁴⁰Ar/³⁹Ar Ages of Phlogopite of the Nanyangtian Tungsten and Tin Deposit in Southeastern Yunnan Province. and Its Geological Significance. Acta Mineralogica Sinica, (S1): 639-640 (in Chinese).
Tan, X.H., Li, Z.J., Du, Z.F., 2010. On the Stratoid Scheelite of Kata-Metamorphite in Nanwenhe Area of SE Yunnan. Yunnan Geology, 29(4): 382-387 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTotal-YNZD201004002.htm
Wang, D.H., Chen, Z.H., Chen, Y.C., et al., 2010a. New Data of the Rock-Forming and Ore-Forming Chronology for China's Important Mineral Resources Areas. Acta Geologica Sinica, 84(7): 1030-1040 (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
Wang, D.H., Chen, Z.H., Huang, G.C., et al., 2012. Northwards and Westwards Prospecting for Tungsten and Its Significance in South China. Geotectonica et Metallogenia, 36(3): 322-239 (in Chinese with English abstract). http://www.cqvip.com/QK/90781X/201203/42988795.html
Wang, D.H., Tang, J.X., Ying, L.J., et al., 2010b. Application of "Five Levels+Basement" Model for Prospecting Deposits into Depth. Journal of Jilin University (Earth Science Edition), 40(4): 733-738 (in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_journal-jilin-university-earth-science-edition_thesis/0201247972302.html
Wang, D.H., Zou, T.R., Xu, Z.G., et al., 2004. Advance in the Study of Using Pegmatite Deposits As the Tracer of Orogenic Process. Advance in Earth Sciences, 19(4): 614-620 (in Chinese with English abstract). http://www.researchgate.net/publication/303261921_Advance_in_the_study_of_using_pegmatite_deposits_as_the_tracer_of_orogenic_process
Wang, P.X., 1998. Deformation of Asia and Global Cooling: Searching Links between Climate and Tectonics. Quaternary Sciences, 3: 213-221 (in Chinese with English abstract).
Wang, X.K., 1994. Geological-Geochemical Characteristics of Xinzhai Tin Deposit in Malipo. Yunnan Geology, 13(1): 1-16 (in Chinese with English abstract). http://www.researchgate.net/publication/284873542_Geological-geochemical_characteristics_of_Xinzhai_Tin_Deposit_in_Malipo
Yang, F., Li, X.F., Feng, Z.H., et al., 2009. ⁴⁰Ar/³⁹Ar Dating of Muscovite from Greisenized Granite and Geological Significance in Limu Tin Deposit. Journal of Guilin University of Technology, 29(1): 21-24 (in Chinese with English abstract).
Zeng, Z.G., Li, Z.Y., Liu, Y.P., et al., 1998. REE Geochemistry of Scheelite of Two Genetic Types from Nanyangtian, Southeastern Yunnan. Geology-Geochemistry, 26(2): 34-38 (in Chinese with English abstract).
Zhang, L.G., Lan, Y., 1999. Gemological Characteristics and Deposit Geology of Yunnan Emerald. Acta Mineralogica Sinica, 19(2): 189-197 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB199902009.htm
蔡德坤, 1983. 滇东南老君山花岗岩类岩石的形成演化与锡、钨的矿化富集作用. 云南地质, 2(2): 102-113. https://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198302001.htm
蔡明海, 陈开旭, 屈文俊, 等, 2006. 湘南荷花坪锡多金属矿床地质特征及辉钼矿Re-Os测年. 矿床地质, 25(3): 263-268. doi: 10.3969/j.issn.0258-7106.2006.03.005
陈毓川, 1983. 华南与燕山期花岗岩类有关的稀土、稀有、有色金属矿床成矿作用. 矿床地质, (2): 15-24.
冯佳睿, 毛景文, 裴荣富, 等, 2011a. 滇东南老君山地区印支期成矿事件初探——以新寨锡矿床和南秧田钨矿床为例. 矿床地质, 30(1): 57-73. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201101007.htm
冯佳睿, 毛景文, 裴荣富, 等, 2011b. 滇东南老君山南秧田钨矿床的成矿流体和成矿作用. 矿床地质, 30(3): 403-419. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201103004.htm
冯佳睿, 周振华, 程彦博, 2010. 云南南秧田钨矿床流体包裹体特征及其意义. 岩石矿物学杂质, 29(1): 50-58. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201001008.htm
郭利果, 2006. 滇东南老君山变质核杂岩地球化学和年代学初步研究(硕士学位论文). 贵阳: 中国科学院地球化学研究所.
华仁民, 陈培荣, 张文兰, 等, 2005. 论华南地区中生代3次规模成矿作用. 矿床地质, 24(2): 99-107. doi: 10.3969/j.issn.0258-7106.2005.02.002
华仁民, 李光来, 张文兰, 等, 2010. 华南钨和锡大规模成矿作用的差异及其原因初探. 矿床地质, 29(1): 9-22. doi: 10.3969/j.issn.0258-7106.2010.01.003
华仁民, 毛景文, 1999. 试论中国东部中生代成矿大爆发. 矿床地质, 18(4): 300-308. doi: 10.3969/j.issn.0258-7106.1999.04.002
李东旭, 许顺山, 2000. 变质核杂岩的旋扭成因——滇东南老君山变质核杂岩的构造解析. 地质论评, 46(2): 113-119. doi: 10.3321/j.issn:0371-5736.2000.02.001
李华芹, 谢才富, 常海亮, 等, 1998. 新疆北部有色贵金属矿床成矿作用年代学. 北京: 地质出版社, 10-24.
李建康, 王登红, 粱婷, 等, 2013. 南岭区域成矿与深部探测的研究进展及其对西藏钨锡找矿的指示. 地球学报, 34(1): 58-74. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201301009.htm
李建康, 王登红, 张德会, 等, 2007. 川西伟晶岩型矿床的形成机制及大陆动力学背景. 北京: 原子能出版社, 59-97.
李水如, 王登红, 梁婷, 等, 2008. 广西大明山钨矿区成矿时代及其找矿前景分析. 地质学报, 82(7): 873-879. doi: 10.3321/j.issn:0001-5717.2008.07.002
梁婷, 王登红, 侯可军, 等, 2011. 广西大厂笼箱盖复式岩体的LA-MC-ICP-MS锆石U-Pb年龄及其地质意义. 岩石学报, 27(6): 1624-1636. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201106005.htm
刘善宝, 王登红, 陈毓川, 等, 2008. 赣南崇-余-犹矿集区不同类型含矿石英中白云母⁴⁰Ar/³⁹Ar年龄及其地质意义. 地质学报, 82(7): 932-940. doi: 10.3321/j.issn:0001-5717.2008.07.011
刘玉平, 李正祥, 李惠民, 等, 2007. 都龙锡锌矿床锡石和锆石U-Pb年代学: 滇东南白垩纪大规模花岗岩成岩-成矿事件. 岩石学报, 23(5): 967-976. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200705011.htm
刘玉平, 李正祥, 叶霖, 等, 2011. 滇东南老君山矿集区钨成矿作用Ar-Ar年代学. 矿物学报, (S1): 617-618. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2011S1320.htm
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
谭洪旗, 刘玉平, 叶霖, 等, 2011. 滇东南南秧田钨锡矿床金云母⁴⁰Ar-³⁰Ar定年及意义. 矿物学报, (S1): 639-640. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2011S1332.htm
谭筱虹, 李志均, 杜再飞, 2010. 滇东南南温河地区深变质岩中似层状白钨矿. 云南地质, 29(4): 382-387. doi: 10.3969/j.issn.1004-1885.2010.04.002
王登红, 陈郑辉, 陈毓川, 等, 2010a. 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): 1030-1040. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201007009.htm
王登红, 陈郑辉, 黄国成, 等, 2012. 华南"南钨北扩"、"东钨西扩"及其找矿方向探讨. 大地构造与成矿学, 36(3): 322-239. doi: 10.3969/j.issn.1001-1552.2012.03.003
王登红, 唐菊兴, 应立娟, 等, 2010b. "五层楼+地下室"找矿模型的适用性及其对深部找矿的意义. 吉林大学学报(地球科学版), 40(4): 733-738. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201004003.htm
王登红, 邹天人, 徐志刚, 等, 2004. 伟晶岩矿床示踪造山过程的研究进展. 地球科学进展, 19(4): 614-620. doi: 10.3321/j.issn:1001-8166.2004.04.019
汪品先, 1998. 亚洲形变与全球变冷——探索气候与构造的关系. 第四纪研究, 3: 213-221. doi: 10.3321/j.issn:1001-7410.1998.03.004
王学焜, 1994. 麻栗坡新寨锡矿床地质地球化学特征. 云南地质, 13(1): 1-16. https://www.cnki.com.cn/Article/CJFDTOTAL-YNZD401.000.htm
杨锋, 李晓峰, 冯佐海, 等, 2009. 栗木锡矿云英岩化花岗岩白云母³⁹Ar/⁴⁰Ar年龄及其地质意义. 桂林工学院学报, 29(1): 21-24. doi: 10.3969/j.issn.1674-9057.2009.01.003
曾志刚, 李朝阳, 刘玉平, 等, 1998. 滇东南南秧田两种不同成因类型白钨矿的稀土元素地球化学特征. 地质地球化学, 26(2): 34-38. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ199802005.htm
张良钜, 兰延, 1999. 云南祖母绿的矿床地质及宝石学特征. 矿物学报, 19(2): 189-197. doi: 10.3321/j.issn:1000-4734.1999.02.010