Sources of Ore-Forming Fluids from Tianbaoshan and Huize Pb-Zn Deposits in Yunnan-Sichuan-Guizhou Region, Southwest China: Evidence from Fluid Inclusions and He-Ar Isotopes
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摘要: 为限定川滇黔地区大型铅锌矿床成矿流体来源，选择天宝山大型铅锌矿床和会泽超大型铅锌矿床中热液矿物进行流体包裹体及氦氩同位素研究.结果显示：（1）天宝山矿床为中低温、中等盐度流体成矿，成矿流体主要来源于盆地卤水；会泽矿床为中高温、中等盐度流体成矿，成矿流体也主要来源于盆地卤水，但具有不同性质流体混合特征；（2）两矿床硫化物3He/4He值范围介于0.02~0.32 Ra，证明成矿流体以地壳流体为主，但混有少量（< 5.3%）地幔成分，40Ar/36Ar值（345.0~1 698.8）表明成矿流体以饱和大气水为主；（3）综合两个矿床地质特征、流体包裹体及氦氩同位素研究认为天宝山矿床和会泽矿床的形成与右江盆地演化及峨眉山大火成岩省的岩浆活动有关.Abstract: In order to constrain the source of the ore-forming fluids in large Pb-Zn deposits in the Sichuan-Yunnan-Guizhou region, fluid inclusions and He-Ar isotopes have been analyzed in ore-forming fluids trapped in sulphide minerals from the large Tianbaoshan Pb-Zn deposit and the super large Huize Pb-Zn deposit. The results are summarized as follows:(1) Fluid inclusions in Tianbaoshan deposit have medium-low homogenization temperatures and medium salinities, and ore-forming fluids are mainly derived from basin brine, whereas fluid inclusions in Huize deposit represent high-medium homogenization temperatures and medium salinities, and ore-forming fluids are dominantly derived from basin brine, but with evidence for mixing of different fluids. (2) The values of 3He/4He in Tianbaoshan deposit and Huize deposit range from 0.02 to 0.32 Ra (where Ra is the atmospheric value; 3He/4He=1.4×10-6), indicating that the ore-forming fluids are dominated by continental crust fluids, where as a small but clear mantle helium contribution is present. And the measurements of 40Ar/36Ar ratio (345.0-1 698.8) indicate that the ore-forming fluids mainly consist of saturated atmospheric water. (3) Combined with geological features, fluid inclusion trapped in sulphide minerals and He-Ar isotopes, it is concluded that the ore-forming processes of Tianbaoshan deposit and Huize deposit are related to the evolution of Youjiang sedimentary basin and the magmatic activities of the Emeishan large igneous province.
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图 1 川滇黔地区地质与主要铅锌矿床分布简图
Fig. 1. Simplified regional geological and distribution map of typical Pb-Zn deposits at the Sichuan-Yunnan-Guizhou region
图 3 天宝山铅锌矿床矿石主要组构的构造特征
a.块状铜铅锌矿石，主要矿物为黄铜矿、方铅矿、闪锌矿；b.块状铅锌矿石，矿物主要为闪锌矿、方铅矿、方解石；c.角砾状铅锌矿石，方铅矿、闪锌矿、方解石胶结硅化白云岩角砾；d.细脉状铅锌矿石，闪锌矿、方铅矿、方解石沿白云岩裂隙分布；e.黄铜矿(Ⅰ)被稍晚方铅矿(Ⅰ)、闪锌矿(Ⅰ)交代；f.晚阶段细脉状方铅矿(Ⅲ)沿裂隙穿插闪锌矿(Ⅱ)；g.晚阶段细粒浅色闪锌矿(Ⅲ)穿插早期细粒闪锌矿(Ⅱ1)与粗粒闪锌矿(Ⅱ2)；h.方解石(Ⅲ)胶结早期形成的闪锌矿角砾(Ⅱ)和围岩白云岩角砾(Dol)；Ⅰ.方铅矿(Ⅰ)、闪锌矿(Ⅰ)交代黄铜矿(Ⅰ)；j.黄铜矿(Ⅱ)、方铅矿(Ⅱ)呈固溶体赋存于闪锌矿(Ⅱ)中；k.稍晚形成的方铅矿(Ⅱ)交代稍早形成的闪锌矿(Ⅱ)；l.晚阶段的方铅矿－黄铁矿－方解石(Ⅲ)细脉穿插较早的闪锌矿(Ⅱ)；Cc.方解石；Ccp.黄铜矿；Dol.白云岩；Py.黄铁矿；Gn.方铅矿；Sph.闪锌矿；Ⅰ第一阶段；Ⅱ第二阶段；Ⅲ第三阶段).
Fig. 3. Typical ore structures from Tianbaoshan Pb-Zn deposit
图 4 会泽铅锌矿床地质图
上二叠统(P2)包括峨眉山玄武岩(P2β)；下二叠统(P1)包括栖霞－茅口组(P1q+m)灰岩、白云质灰岩夹白云岩，梁山组(P1l)炭质页岩和石英砂岩；石炭系(C)包括马平组(C3m)角砾状灰岩，威宁组(C2w)鲕粒状灰岩，摆佐组(C1b)粗晶白云岩及灰岩及白云质灰岩，大唐组(C1d)隐晶灰岩及粒状灰岩；泥盆系(D)包括宰格组(D3zg)灰岩、硅质白云岩，海口组(D2h)粉砂岩和泥质页岩；寒武系()包括筇竹寺组(1q)泥质页岩夹砂质泥岩；Z震旦系(Z)包括灯影组(Z2d)硅质白云岩；据韩润生等(2000)修改
Fig. 4. Simplified geological map of the Huize Pb-Zn deposit
图 5 会泽铅锌矿床矿石组构特征
a.黄铁矿、闪锌矿、方解石依次由矿脉边缘向中心生长；b.块状矿石，由方铅矿、闪锌矿、方解石构成；c.橘红色闪锌矿与他形－半自形方铅矿共生，形成块状矿石；d.晚阶段方解石(Ⅲ)胶结早阶段黄铁矿、闪锌矿(Ⅰ)、方铅矿(Ⅰ)角砾形成角砾状矿石；e.Ⅰ阶段矿物生长顺序，由早到晚依次为黄铁矿(Ⅰ)、深棕色闪锌矿(Ⅰ)、方解石(Ⅰ)；f.Ⅱ阶段的深棕色粗晶闪锌矿(Ⅱ)－方解石(Ⅱ)组合交代早阶段黄铁矿(Ⅰ)；g.Ⅱ阶段深棕色闪锌矿(Ⅱ)、浅棕色闪锌矿(Ⅱ)、橘红色闪锌矿(Ⅱ)、浅黄色闪锌矿(Ⅱ)与方铅矿(Ⅱ)、方解石(Ⅱ)共生；h.Ⅱ阶段闪锌矿胶结早阶段黄铁矿(Ⅱ)角砾，而被晚阶段闪锌矿(Ⅲ)－方解石(Ⅲ)胶结；i.闪锌矿(Ⅰ)、方铅矿(Ⅰ)交代较早形成的黄铁矿(Ⅰ)；j.黄铜矿(Ⅰ)固溶体出溶于闪锌矿(Ⅱ)晶体中；k.闪锌矿(Ⅱ)交代黄铁矿(Ⅱ)颗粒；l.黄铜矿(Ⅱ)出溶于闪锌矿(Ⅱ)中；Cc.方解石；Ccp.黄铜矿；Gn.方铅矿；Py.黄铁矿；Sph.闪锌矿
Fig. 5. Field photographs of different textures from Huize Pb-Zn deposit
图 6 天宝山矿床流体包裹体特征
a.Ⅰ阶段闪锌矿中V型包裹体；b.Ⅱ阶段闪锌矿中(V+L)ⅰ型包裹体；c.Ⅱ阶段闪锌矿中(V+L)ⅱ型包裹体成群分布；d.Ⅱ阶段闪锌矿中孤立分布的(V+L)ⅱ型包裹体；e.闪锌矿中孤立分布的(V+L)ⅱ型包裹体；f.Ⅱ阶段闪锌矿中L型包裹体
Fig. 6. Photomicrographs of fluid inclusions in sphalerit in the Tianbaoshan deposit
图 7 会泽矿床流体包裹体特征
a.Ⅰ阶段闪锌矿中V型包裹体(白平衡后照片)；b.Ⅱ阶段棕色闪锌矿中S+V+L型包裹体(白平衡后照片)；c.Ⅱ阶段棕色闪锌矿中(L+V)ⅰ型包裹体(白平衡后照片)；d.Ⅱ阶段橘红色闪锌矿中成群分布的(L+V)ⅱ型包裹体与L型包裹体共生；e.Ⅱ阶段方解石中成群分布的(L+V)ⅱ型包裹体(白平衡后照片)；f.Ⅱ阶段方解石中负晶形(L+V)ⅱ型包裹体；g.Ⅲ阶段闪锌矿中孤立分布的(L+V)ⅱ型包裹体
Fig. 7. Photomicrographs of fluid inclusions in the Huize deposit
图 8 天宝山矿床和会泽矿床流体包裹体均一温度、盐度直方图
a.天宝山矿床不同阶段热液矿物流体包裹体均一温度直方图；b.天宝山矿床不同阶段热液矿物流体包裹体盐度直方图；c.会泽矿床不同阶段热液矿物流体包裹体均一温度直方图；d.会泽矿床不同阶段热液矿物流体包裹体盐度直方图；TBS Sph Ⅱ.天宝山矿床Ⅱ阶段闪锌矿；TBS Sph Ⅲ.天宝山矿床Ⅲ阶段闪锌矿；TBS CcⅡ.天宝山矿床Ⅱ阶段方解石；TBS Cc Ⅲ.天宝山矿床Ⅲ阶段方解石；HZ Sph Ⅰ.会泽矿床Ⅰ阶段闪锌矿；HZ Sph Ⅱ.会泽矿床Ⅱ阶段闪锌矿；HZ Sph Ⅲ.会泽矿床Ⅲ阶段闪锌矿；HZ Cc Ⅰ.会泽矿床Ⅰ阶段方解石；HZ Cc Ⅱ.会泽矿床Ⅱ阶段方解石；HZ Cc Ⅲ.会泽矿床Ⅲ阶段方解石
Fig. 8. Histograms of microthermometric and salinity for each stage of Tianbaoshan and Huize deposits
图 9 天宝山铅锌矿床、会泽铅锌矿床流体包裹体成分K/Na vs. Ca/K(a)，Na/Ca vs. Na/K(b)，Na/K vs. Na/(Ca+Mg)(c)和Na/Ca vs. Na/Mg(d)图解
a.底图来源于Samson et al.(2008)；b、d.底图来源于Hofstra et al.(2016)；c.底图来源于谢树成和殷鸿福(1997).1数据来源于韩润生(2002)；2数据来源于王小春(1992)；Na/K、Na/Ca、Na/Mg、Na/(Ca+Mg)值为摩尔比值
Fig. 9. Plots of K/Na vs. Ca/K(a), Na/Ca vs. Na/K(b), Na/K vs. Na/(Ca+Mg)(c) and Na/Ca vs. Na/Mg(d) of inclusion-trapped fluids in the Tianbaoshan Pb-Zn deposit and Huize Pb-Zn deposit
图 10 天宝山矿床和会泽矿床硫化物3He/4He(Ra)-40Ar/36Ar(a)及3He-4He含量(b)
a图MVT铅锌矿床3He/4He(Ra)-40Ar/36Ar数据范围统计于美国(Illinois-Kentucky、Viburnum Trend、Tri-State)(Kendrick et al., 2002)，摩洛哥(Touissit-Bou Beker)(Bouabdellah et al., 2015)、英国(Irish)(Davidheiser-Kroll et al., 2014)MVT铅锌矿床.40Ar/36Ar值地壳范围引自Stuart et al.(1995)，地幔范围胡瑞忠(1997)；3He/4He值范围引自Stuart et al.(1995)
Fig. 10. Plots of 3He/4He (Ra) vs.40Ar/36Ar (a) and 3He vs. 4He (b) of inclusion-trapped fluids from the Tianbaoshan deposit and Huize deposit
图 11 世界MVT矿床与川滇黔地区会泽矿床、天宝山矿床热液矿物流体包裹体均一温度、盐度统计汇总
典型MVT矿床均一温度、盐度数据来自于闪锌矿流体包裹体；天宝山矿床、会泽矿床均一温度、盐度分别来自不同阶段的闪锌矿和方解石.典型MVT矿床数据引自Leach et al.(2005)；HZ.会泽矿床；TBS.天宝山矿床；Sph.闪锌矿；Cc.方解石；Ⅰ、Ⅱ、Ⅲ.成矿阶段
Fig. 11. Summary of homogenization temperatures and salinity data for Tianbaoshan deposit, Huize deposit and selected MVT deposits based on fluid inclusion studies
表 1 天宝山矿床和会泽矿床各阶段流体包裹体显微测温数据
Table 1. Summary of fluid inclusion data in minerals from different stages of Tanbaoshan and Huize deposits
矿床 成矿阶段 测试矿物(数据个数n) 均一温度(℃) 冰点(℃) 盐度(% NaCl eqv) 分布范围 峰值区间 平均值 分布范围 主要区间 平均值 天宝山 Ⅱ 闪锌矿(n=59) 101.8~267.0 100~180 140.4 -14.4~-1.9 3.2~18.1 8~16 11.1 Ⅱ 方解石(n=31) 102.6~193.1 100~160 133.2 -16.6~-4.1 6.6~19.9 8~20 14.3 Ⅲ 闪锌矿(n=15) 98.4~162.2 100~160 129.7 -8.2~-2.2 3.7~11.9 8~12 8.3 Ⅲ 方解石(n=12) 95.6~158.3 100~140 119.2 -1.2~-6.4 2.1~9.7 4~10 6.7 会泽 Ⅰ 闪锌矿(n=33) 246.0~420.0 250~300，325~400 315.5 -12.1~-0.5 0.9~16.1 0~2，8~16 8.2 Ⅰ 方解石(n=37) 184.0~420.0 175~300，325~375 259.2 -3.6~-20.1 5.9~22.4 10~16，18~23 15.0 Ⅱ 闪锌矿(n=43) 167.8~400.0 175~325 255.7 -2.6~19.2 4.3~21.8 12~16，18~22 13.5 Ⅱ 方解石(n=49) 132.1~330.3 150~275 213.0 -0.3~-11.6 0.5~15.6 0~6，8~14 6.5 Ⅲ 闪锌矿(n=20) 160.5~231.6 160~225 182.5 -0.5~-3.7 0.9~6.0 0~4 2.7 Ⅲ 方解石(n=17) 152.0~217.0 150~200 178.1 -0.3~-2.3 0.5~3.9 - 2.2 
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表 2 天宝山铅锌矿床和会泽铅锌矿床矿物流体包裹体液相成分及离子比值
Table 2. Compositions and cationic ratios of fluid inclusions in minerals from the Tianbaoshan Pb-Zn deposit and Huize Pb-Zn deposit
矿床 样号 矿物 K+(106) Na+(106) Ca2+(106) Mg2+(106) K/Na Ca/K Na/K Na/Ca Na/Mg Na/(Ca+Mg) 天宝山 T-1 闪锌矿 1.39 19.98 22.32 15.72 0.07 16.06 24.45 1.56 1.34 0.72 T-2 闪锌矿 2.489 46.05 30.55 14.71 0.05 12.27 31.46 2.63 3.31 1.46 T-3 闪锌矿 2.764 57.49 35.61 13.15 0.05 12.88 35.37 2.81 4.62 1.75 T-4 方解石 0.755 2 8.242 19.8 2.11 0.09 26.22 18.56 0.73 4.13 0.62 TB0492 闪锌矿 2.6 10 83.4 28.3 0.26 32.08 6.54 0.21 0.37 0.13 会泽 H5S 闪锌矿 0.84 8.03 3.18 0.37 0.10 3.79 16.26 4.40 22.94 3.69 H2S 闪锌矿 1.46 0.92 7.75 0.73 1.59 5.31 1.07 0.21 1.33 0.18 A-4 闪锌矿 0.15 4.74 2.06 0.21 0.03 13.73 53.74 4.01 23.86 3.43 A-5 闪锌矿 0.04 5.40 2.11 0.21 0.01 52.75 229.59 4.46 27.19 3.83 H2C 方解石 Nd 0.30 39.29 2.42 - - - - 0.13 0.01 H5C 方解石 Nd 0.47 39.32 1.28 - - - - 0.39 0.02 B-4 方解石 Nd 0.86 18.3 1.22 - - - - 0.75 0.07 B-5 方解石 Nd 0.73 12.76 0.96 - - - - 0.80 0.09 1751/9/91 黄铁矿 0.87 0.25 0.65 0.25 3.48 0.75 0.49 0.67 1.06 0.41 MQ/9111 黄铁矿 0.181 3.66 51.74 8.15 0.05 285.86 34.39 0.12 0.47 0.10 MQ/9151 黄铁矿 0.73 3.07 1.39 0.51 0.24 1.90 7.15 3.85 6.36 2.40 1751/21 闪锌矿 0.81 8.90 26.8 2.06 0.09 33.09 18.69 0.58 4.57 0.51 28-21 闪锌矿 0.28 1.50 0.60 0.01 0.19 2.14 9.11 4.36 158.58 4.24 28-31 闪梓矿 0.75 4.27 6.32 0.73 0.18 8.43 9.68 1.18 6.18 0.99 HQ99/11 方解石 0.53 3.56 108.8 4.16 0.15 205.28 11.42 0.06 0.90 0.05 HQ109/41 方解石 1.31 7.21 81.5 4.39 0.18 62.21 9.36 0.15 1.74 0.14 HQ/841 方解石 1.23 7.14 81.44 4.70 0.17 66.21 9.87 0.15 1.61 0.14 1631/381 方解石 2.45 11.42 72.65 5.56 0.21 29.65 7.93 0.27 2.17 0.24 1751/21 方解石 1.57 9.30 74.52 4.70 0.17 47.46 10.07 0.22 2.09 0.20 注：Na/K、Na/Ca、Na/Mg、Na/(Ca+Mg)值为摩尔比值；K/Na、Ca/K值为质量百分比值.上标1数据来源于韩润生(2002)；上标2数据来源于王小春(1992)；测试工作在国土资源部中南矿产资源监督检测中心(武汉地质矿产研究所)完成.
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表 3 天宝山铅锌矿床及会泽铅锌矿床硫化物矿物流体包裹体He-Ar同位素
Table 3. He-Ar isotopic compositions of fluid inclusions in sulphide minerals from the Tianbaoshan and Huize Pb-Zn deposit
矿床 样品名称 矿物 重量(g) 4He(10-7 ccSTP/g) 3He/4He(Ra) 40Ar(10-7 ccSTp/g) 40Ar*(10-7 ccSTp/g) 40Ar/36Ar 38Ar/36Ar 4He地幔(%) 天宝山 TBCP-1 黄铜矿 0.3 28.9 0.04±0.01 13.0 5.9 539.0±3.3 0.189±0.001 0.5 TBCP-2 黄铜矿 0.3 23.0 0.21±0.01 14.4 2.1 345.0±2.1 0.187±0.001 3.3 TBCP-3 黄铜矿 0.3 32.0 0.05±0.01 12.2 6.8 669.1±4.1 0.188±0.001 0.7 TBCP-4 黄铜矿 0.3 27.4 0.03±0.01 6.5 1.7 402.7±2.5 0.189±0.001 0.4 TBCP-5 黄铜矿 0.2 16.0 0.32±0.04 6.7 1.4 373.7±2.3 0.189±0.001 5.3 TBCP-6 黄铜矿 0.4 27.5 0.04±0.01 13.6 7.0 612.1±3.7 0.188±0.001 0.6 会泽 Hhe-1 黄铁矿 0.2 21.9 0.02±0.01 5.9 4.9 1 698.8±10.5 0.191±0.003 0.2 Hhe-2 黄铁矿 0.2 29.7 0.03±0.01 17.0 2.7 354.6±2.2 0.188±0.003 0.3 Hhe-3 黄铁矿 0.2 9.6 0.04±0.01 3.0 1.7 679.2±4.2 0.186±0.003 0.4 Hhe-4 黄铁矿 0.3 13.9 0.14±0.02 3.9 2.9 1 194.2±2.2 0.188±0.003 2.1 Hhe-5 黄铁矿 0.2 13.7 0.16±0.02 3.1 2.4 1 165.2±2.2 0.188±0.003 2.5 Hhe-6 黄铁矿 0.1 12.6 0.06±0.01 2.9 2.0 918.5±1.7 0.187±0.003 0.8 注：Ra为大气3He/4He=1.4×10-6；40Ar*为非大气氩40Ar，40Ar*=40Ar样-295.5×36Ar样；4He地幔值代表地幔氦份额，4He地幔(%)=100[(3He/4He)样品-(3He/4He)地壳]/[(3He/4He)地幔-(3He/4He)地壳]，假设地幔R/Ra=6.00和地壳R/Ra=0.01(Anderson，2000).测试工作在中国科学院地质与地球物理研究所完成.
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表 4 典型MVT铅锌矿床与川滇黔地区铅锌矿床主要特征
Table 4. Comparison of characteristics between typical MVT Pb-Zn deposits in the world and Pb-Zn deposits in Sichuan-Yunnan-Guizhou region
典型MVT铅锌矿床 川滇黔地区铅锌矿床 资料来源 总体特征 典型矿床 成因 后生 后生 TBSD：后生；HZD：后生 1~6，本文 成矿背景 造山带内侧600 km内的前陆盆地边缘为主，少数在前陆逆冲带中，极少数产于伸展环境 与古特提斯洋闭合过程中右江盆地演化有关 TBSD、HZD：与古特提斯洋闭合过程中右江盆地演化及峨眉山大火成岩省岩浆活动有关 1~3，6，8，21~22 赋矿围岩 台地碳酸盐岩，主要为白云岩 台地碳酸盐岩，主要为白云岩 TBSD：白云岩HZD：白云岩 1~4，本文 控矿构造 溶蚀坍塌角砾岩，断层和裂隙，岩性转化界面 张性断裂，逆冲断裂，褶皱－顺层活动带 TBSD：张性断裂HZD：逆冲断裂 1~4，9 主要矿物 闪锌矿、方铅矿、黄铁矿、白铁矿、(黄铜矿)、白云石、方解石、(重晶石)、(萤石) 闪锌矿、方铅矿、黄铁矿、(黄铜矿)、白云石、方解石、(重晶石)、(萤石) TBSD：闪锌矿、方铅矿、黄铜矿、方解石、白云石HZD：闪锌矿、方铅矿、黄铁矿、方解石、白云石 1~4，10~12，本文 围岩蚀变 围岩溶解，角砾岩化，碳酸盐化+硅化±粘土化±有机质化±长石化 碳酸盐化+硅化±粘土化±有机质化 TBSD：碳酸盐化+硅化±黄铁矿化HZD：碳酸盐化+黄铁矿化+硅化±粘土化 1~4，10~12 成矿时代 泥盆纪－三叠纪，白垩纪－第三纪 晚三叠世－早侏罗世 TBSD：无年代学数据，推断为晚三叠世－早侏罗世HZD：晚三叠世 2，8~10 与岩浆活动关系 存在争议 争议较大 TBSD：提供部分流体；可能提供热源HZD：提供部分流体；可能提供热源 1~8，10，16~18，本文 成矿温度及盐度 成矿温度介于50~250 ℃，以90~150 ℃为主，Irish型温度为70~280 ℃；盐度主要区间介于(10~30)% NaCl eqv，Irish型盐度(4~28)% NaCl eqv 140~360 ℃；(4.2~13.5)% NaCl eqv TBSD：95.6~267 ℃，2.1~19.9% NaCl eqvHZD：132.1~420 ℃，0.5~22.4% NaCl eqv 1~3，13~15，24，本文 成矿流体来源 盆地卤水为主，少量地幔流体 争议较大 TBSD：盆地卤水为主，少量地幔流体HZD：盆地卤水为主，少量地幔流体，存在其他性质流体 1~3，23~24，本文 He-Ar同位素 3He/4He：地壳为主，少量的地幔流体加入；40Ar/39Ar：大气降水为主，有少量的剩余氩 — TBSD、HZD：3He/4He：地壳为主，少量的地幔流体加入；40Ar/39Ar：大气降水为主，有少量的剩余氩 16~18，本文 物质来源 Pb：地壳；S：地壳；Zn：未知 Pb：地壳；S：地壳；Zn：未知 TBSD：地壳HZD：地壳 1~4，10~11 矿床规模 具有群聚性，单个为中小型，矿区可达大型－超大型 具有群聚性，单个多为中小型或矿化体，少量为(超)大型，矿区规模不等 TBSD：大型HZD：超大型 1~4，19~20 注：TBSD为天宝山矿床，HZD为会泽矿床.1. Leach et al.(1993) ；2.Leach et al.(2001) ；3.Leach et al.(2005) ；4.柳贺昌和林文达(1999)；5.王奖臻等(2002)；6.张长青(2008)；7.吴越(2013)；8.Zhang et al.(2015) ；9.张志斌等(2006)；10.黄智龙(2004b)；11.孙海瑞等(2016)；12.王小春(1992)；13.Zhu et al.(2016) ；14.喻磊(2014)；15.韩润生等(2012)；16.Kendrick et al.(2002) ；17.Bouabdellah et al.(2015) ；18.Davidheiser-Kroll et al.(2014) ；19.Li et al(2007a) ；20.Zhou et al.(2013a) ；21.Liu et al.(2017) ；22.Hu et al.(2017) ；23.叶霖等(2016)；24.念红良等(2017).
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