Magmatism, metallogenic characteristics, and prospecting prediction for gold deposits in the north of Kunlun River area, Qinghai, China
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摘要: 青海昆仑河北地区靠近昆中断裂带，经历早古生代、晚古生代—中生代多期岩浆活动，近年来自西至东陆续发现黑海北、拉陵灶火、苏海图、加祖它士西、向阳沟、加祖它士东、大灶火、黑刺沟等多个金矿床（点），形成一条东西长度近150 km长的成矿带。文章在总结带内金矿成矿基本特征基础上，选取黑海北金矿和加祖它士东金矿的赋矿围岩开展锆石U-Pb定年，结果显示黑海北硅化二长花岗岩锆石206Pb/238U加权平均年龄为443±8 Ma，形成于原特提斯洋向柴达木地块俯冲碰撞后伸展环境；加祖它士东的花岗闪长岩脉含有较多的继承锆石，锆石206Pb/238U加权平均年龄为250±1 Ma，继承锆石206Pb/238U加权平均年龄为420±2 Ma，加祖它士东花岗闪长岩侵位于古特提斯洋向北俯冲背景下的大陆弧构造环境。综合分析认为昆仑河北地区金矿成矿作用与早中生代三叠纪岩浆活动关系更为密切，其矿床类型存在造山型金矿与岩浆热液型金矿两种不同认识。昆仑河北地区土壤化探异常、低阻高极化激电异常、主要断裂（穿矿区）的次级断裂形成的蚀变破碎带等可以作为区内主要的找矿标志，推测该成矿带具有较大的找矿前景。Abstract: The north of Kunlun River area, which is close to the central Kunlun Fault Zone, has experienced multi-stage magmatic activities of early Paleozoic and Paleozoic-Mesozoic. A number of gold deposits (occurrences) have been discovered successively in this area for the past few years from west to east, such as Heihaibei, Lalingzaohuo, Suhaitu, Jiazutashixi, Xiangyanggou, Jiazutashidong, Dazaohuo and Heicigou, forming a metallogenic belt with an EW-length of nearly 150 km. In consideration of the basic characteristics of gold deposits in the belt, the ore-hosting wall rocks from the Heihaibei and Jiazutashidong gold deposits were selected to carry out zircon U-Pb dating in this study. The results show the silicified monzonitic granites from the Heihaibei deposit yield zircon weighted mean 206Pb/238U age of 443±8 Ma, which should be formed under the stretching environment after the collision of the Proto-Tethys Ocean to the Qaidam block. The diorite dikes from the Jiazutashidong deposit, which bears more inherited zircon, yield the zircon weighted mean 206Pb/238U age of 250±1 Ma and 420±2 Ma for primary zircon and inherited zircon, respectively, indicating a continental arc tectonic setting under the northward subduction of the Paleo-Tethys Ocean during the emplacement of diorites. Overall, it is believed that the gold mineralization in the northern Kunlun River area is more closely related to the Early Mesozoic Triassic magmatic activity, but opinions vary about the deposit types on whether it belongs to the orogenic or magmatic hydrothermal. Soil geochemical anomalies, low-resistance and high-polarization IP anomalies, and altered fracture zones formed by secondary faults can be used as the main ore prospecting markers in the northern of Kunlun River. It is considered that this metallogenic belt has good prospects for gold deposits.
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图 1 研究区地质简图(a据Dong et al., 2018修改；b据王秉璋等，2008修改)
a—研究区地质构造图；b—昆仑河北地区区域地质图(1—第四系；2—三叠系洪水川组；3—奥陶系纳赤台群；4—寒武纪变砂岩；5—金水口群；6—万宝沟群；7—三叠纪钾长花岗岩；8—三叠纪二长花岗岩；9—二叠纪花岗闪长岩；10—金矿床(点)；11—逆断层；12—走滑断层；13—性质不明断层；14—背斜；15—向斜；16—地层产状)
Figure 1. Geological sketch of the study area (a is modified from Dong et al., 2018; b is modified from Wang et al., 2008)
(a) Tectonic map of the study area; (b) Geological map of the northern Kunlun River area; 1-Quaternary; 2-Triassic Hongshuichuan Formation; 3-Ordovician Nachitai Group; 4-Cambrian metamorphic sandstone; 5-Jinshuikou Group; 6-Wanbaogou Group; 7-Triassic potassium feldspar granite; 8-Triassic monzonite granite; 9-Permian granodiorite; 10-Gold deposit (occurrence); 11-Reverse fault; 12-Strike-slip fault; 13-Unidentified fault; 14-Anticline; 15-Syncline; 16-Strata occurrence
图 2 黑海北金矿床地质简图(底图据焦和等，2020修改)
1—第四系；2—长石石英砂岩；3—砂质板岩；4—含砾岩屑砂岩；5—二长花岗岩；6—花岗闪长岩；7—闪长岩脉；8—蚀变破碎带及编号；9—逆冲断层；10—矿体及编号；11—矿化体
Figure 2. Geological map of the Heihaibei gold deposit (modified from Jiao et al., 2020)
1-Quaternary; 2-Feldspathic quartz sandstone; 3-Sandy slate; 4-Pebbly lithic sandstone; 5-Monzonite granite; 6-Granodiorite; 7-Diorite vein; 8-Altered fracture zones and their numbers; 9-Thrust fault; 10-Orebodies and their numbers; 11-Mineralized bodies
图 3 黑海北矿区04勘查线剖面图(底图据焦和等，2020修改)
1—花岗岩；2—长石石英砂岩；3—断层；4—矿体；5—矿化体；6—褐铁矿化/黄铁矿化；7—硅化；8—破碎带；9—采样点；10—钻孔及编号
Figure 3. Profile map of No.04 exploration line in the Heihaibei mining area (modified from Jiao et al., 2020)
1-Granite; 2-Feldspathic quartz sandstone; 3-Fault; 4-Orebodies; 5-Mineralized bodies; 6-Ferritization/; 7-Diorite vein; 8-Altered fracture zone and their numbers; 9-Thrust fault; 10-Orebodies and their numbers; 11-Mineralized bodies
图 4 黑海北和加祖它士东金矿矿体矿石特征
矿物代号：Qz—石英；Pl—斜长石；Amp—角闪石；Ser—绢云母；Py—黄铁矿
a—黑海北矿区矿化破碎带野外照片；b—黑海北矿区典型硅化矿石；c—黑海北矿区硅化黄铁矿化花岗岩显微照片(反射光)；d—黑海北矿区二长花岗岩；e—黑海北矿区二长花岗岩显微照片(透射，单偏光)；f—加东矿区矿化破碎带野外照片；g—加东矿区含团块状黄铁矿矿石照片；h—加东矿区花岗闪长岩；i—加东矿区花岗闪长岩显微照片(透射，单偏光)。Figure 4. Field pictures and micrographs showing the ore characteristics of the Heihaibei and Jiazutashidong gold deposits
(a) Field picture of the mineralized fracture zone in the Heihaibei mining area; (b) Specimen of a typical silicified ore from the Heihaibei mining area; (c) Micrograph of a silicified pyritized granite in the Heihaibei mining area (reflection); (d) Field picture of a monzogranite from the Heihaibei mining area; (e) Micrograph of a monzogranite from the Heihaibei mining area (transmission, plane-polarized light); (f) Field picture of the mineralized fracture zone in the Jiazutashidong mining area; (g) Specimen of an agglomerated pyrite from the Jiazutashidong mining area; (h) Specimen of a granodiorite from the Jiazutashidong mining area; (i) Micrograph of a granodiorite from the Jiazutashidong mining area (transmission, plane-polarized light)
Mineral code: Qz-Quartz; Pl-Plagioclase; Amp-Amphibole; Ser-Sericite; Py-Pyrite
图 5 加祖它士东金矿床地质简图(底图据焦和等，2020修改)
1—第四纪；2—三叠纪砂砾岩；3—含碳质板岩；4—灰岩夹板岩；5—绿片岩化安山岩；6—晚三叠纪花岗闪长岩；7—金矿体；8—蚀变破碎带及编号；9—逆冲断层；10—不整合接触
Figure 5. Geological map of the Jiazutashidong gold deposit (modified from Jiao et al., 2020)
1-Quaternary; 2-Triassic glutenite; 3-Carbonaceous slate; 4-Limestone interbedded with slate; 5-Green schistized andesite; 6-Late Triassic granodiorite; 7-Gold orebody; 8-Altered fracture zone and its number; 9-Thrust fault; 10-Uunconformable contact
图 6 加东矿区0勘探线剖面图(底图据焦和等，2020修改)
1—第四系残坡积；2—砂砾岩；3—长石石英砂岩；4—炭质板岩；5—砂质板岩；6—安山岩；7—变余长石石英砂岩；8—灰岩；9—花岗闪长岩；10—断层；11—矿体；12—矿化体；13—采样点；14—钻孔及编号
Figure 6. Profile map of No.0 exploration line in the Jiazutashidong mining area (modified from Jiao et al., 2020)
1-Quaternary residual slope accumulation; 2-Glutenite; 3-Feldspathic quartz sandstone; 4-Carbonaceous slate; 5-Sandy slate; 6-Andesite; 7-Palimpsest feldspathic quartz sandstone; 8-Limestone; 9-Granodiorite; 10-Fault; 11-Orebodies; 12-Mineralized bodies; 13-Sampling site; 14-Boreholes and their numbers
图 7 测试样品锆石阴极发光照片及点位年龄
Figure 7. Zircon cathodoluminescence photos and point U-Pb ages of the samples
图 8 黑海北二长花岗岩(HHB01)和加祖它士东花岗闪长岩(CY01)锆石U-Pb加权平均年龄图及和谐图
Figure 8. Zircon U-Pb weighted mean ages and concordia diagram of the Heihaibei monzonite (HHB01) and the Jiazutashidong granodiorite (CY01)
图 9 昆仑河北地区1:5万化探异常图(底图据王秉章等，2008修改，图例同图 1)
Figure 9. 1:50000 scale geochemical anomaly in the northern Kunlun River area (The source of the base map is modified from Wang et al., 2008, and the legends are the same as in Fig. 1)
图 10 昆仑河北地区航磁异常图(底图据焦和等，2020修改)
1—超基性岩类引起的异常；2—基性岩类引起的异常；3—中基性岩类引起的异常；4—酸性岩类引起的异常；5—中酸性岩类引起的异常；6—异常轴向
Figure 10. Aeromagnetic anomalies of the northern Kunlun River area (modified from Jiao et al., 2020)
(1) Anomalies caused by ultra-basic rocks; (2) Anomalies caused by basic rocks; (3) Anomalies caused by intermediate-basic rocks; (4) Anomalies caused by acidic rocks; (5) Anomalies caused by intermediate-acid rocks; (6) Abnormal axial
图 11 黑海北地区1:1万土壤测量异常分布图
Figure 11. 1:10000 scale soil geochemical anomalies in the Heihaibei area
图 12 黑海北00勘查线地物综合剖面图
Figure 12. Geological and geophysical comprehensive profile map of No.00 exploration line in the Heihaibei gold deposits
表 1 昆仑河地区已发现金矿床(点)地质特征
Table 1. Geological characteristics of gold deposits discovered in the Kunlun River area
矿床(点)名称 大灶火金矿 老道沟口金矿 没草沟金矿 铜金山金矿 黑海南金矿 黑刺沟金矿 黑海北金矿 苏海图金矿点 拉陵灶火金矿点 加祖它士西金矿点 加祖它士东金矿点 向阳沟金矿点 矿化组合 Au Au-Pb Au Au-Cu Au Au Au Au Au Au Au Au 围岩 二叠系马尔争组炭质千枚状板岩、三叠系洪水川组石英砂岩、岩屑砂岩 奥陶—志留系纳赤台群碎屑岩组灰绿色砂岩 下三叠统洪水川组长石砂岩、粉砂岩、板岩，奥陶—志留系纳赤台群碎屑岩 中新元古界万保沟群碳酸盐岩、下寒武统沙松乌拉组石英砂岩 中二叠统马尔争组与早—中三叠统昌马河组砂板岩接触带附近 奥陶—志留系纳赤台群碎屑岩组灰绿色砂岩 早志留二长花岗岩 奥陶系上统纳赤台群碎屑岩组灰绿色砂岩 奥陶系上统纳赤台群碎屑岩组灰绿色砂岩 中晚元古代万宝沟群灰白色硅质白云岩、暗绿灰色蚀变玄武岩夹白云岩、灰—灰绿色变长石砂岩夹粉砂岩 奥陶—志留系纳赤台群长石石英砂岩及泥质灰岩 中下三叠统洪水川组、晚寒武统沙松乌拉组碎屑岩 岩浆岩 晚三叠世花岗闪长岩 矿区未见出露 少量花岗岩脉发育 矿点处岩浆岩不发育，矿点北侧晚三叠世斑状二长花岗岩发育 少量二长花岗岩 少量花岗岩脉发育 早志留二长花岗岩构造大量发育 矿区未见出露 矿区未见出露 发育大量花岗岩 发育大量花岗闪长岩脉 发育大量花岗岩 控矿构造 北西西向构造破碎带受1条北西—南东向正断层控制，矿化产于宽约40 m的构造蚀变破碎带 受北西—南东向脆韧性断裂构造控制，矿区平卧褶皱发育 2条倾向南西的北西西向逆断层贯穿矿区，构造蚀变破碎带发育 昆中断裂带南侧北西西向、近东西向压扭性断裂构造发育 金矿体严格受断裂蚀变带控制，走向北西、北西西，矿体有分枝、复合与尖灭现象 2条近东西向压扭性断裂构造发育 区内发育2组断裂(F52、F53)，呈近东西向延伸；F53断裂被后期二长花岗岩侵入破坏，形成含矿蚀变破碎带，是区内主要的控矿及容矿构造 主要断裂有3条，走向为北西、北西西向，与之相关的张裂隙大量发育 2条近东西向压扭性断裂构造发育 各方位断裂构造发育，主构造方向为近东西向压扭性断裂构造 区内构造活动强烈，主要分布4条主断裂构造，均为北西西向具挤压性质的逆断层，倾向北，具多期次活动特征 2条近东西向压扭性断裂构造发育 矿体 呈北西西向带状展布，主矿带长约2.24 km，金矿体9条，厚度0.95~144.3 m不等，延伸长度达到478 m，品位1.6~12.5 g/t不等 呈透镜状断续产出，长大于350 m，宽1.0~3.7 m不等 呈北西西—南东东向透镜状、串珠状展布于黄褐色构造破碎带中，长大于1 km，宽10~40 m不等，厚0.6~10.2 m 呈透镜状、串珠状断续展布于强片理化蚀变带中，长度大于1.5 km，宽10~30 m不等 9条，其中主要矿体MⅡ-1和MⅡ-7、8、9；MⅡ-1呈似层状产出，走向约120°，视厚度为4.0 m 圈定金矿体7条，与断层走向基本一致 在近东西向Sb-1构造带中圈定金矿体11条，矿化体27条；矿体主要表现为地表整体品位高、厚度大、连续性好等特点；其中主矿体M3控制长度为660 m，控制斜深80~160 m不等，产状192°∠73°~86°，水平厚度4.90 m 在区内共发现金矿(化)点19处，圈定金矿化体13条(Au1~Au 13)、金矿体2条(M1和M2) 圈定3条含矿蚀变带，带内圈定金矿体13条；主矿体走向长度为480 m，控制斜深118~235 m不等，矿体平均真厚度为3.93 m，矿体北倾，倾角51°~60°，其形态为大透镜体状，展布方向为北西西向，地表未能揭露到该矿体 圈定规模较小的金矿体3条，金矿化体6条，长度一般在80 m以内，厚度2 m以内。 圈定1条宽17~22 m，长400米金矿化带，在该条矿化带中共圈定出金矿体2条，后期通过钻探工程验证，该条矿化带近直立；深部圈定厚大隐伏矿化带，在这条矿化带内圈定金矿体4条(M1、M2、M3、M4)，长160~320 m，视厚度2~26.08 m 圈定金矿(化)体7条，宽0.55~6 m，长20~610 m，矿(化)体走向多数为北西西向，M6为北北西向 矿石类型 构造蚀变岩型+石英脉型 石英脉型+蚀变岩型 蚀变岩型+石英脉型 蚀变岩型+石英脉型 蚀变岩型+石英脉型 构造蚀变岩型 石英脉型 石英脉型 蚀变岩型+石英脉型 构造蚀变岩型 蚀变岩型+石英脉型 蚀变岩型+石英脉型 矿物组合 黄铁矿、褐铁矿、黄钾铁矾、方解石、绿泥石、高岭土 黄铁矿、方铅矿、褐铁矿 褐铁矿、孔雀石、黄铁矿 黄铁矿、黄铜矿、褐铁矿、石英、方解石 黄铁矿和毒砂为主，其余为少量的黄铜矿、孔雀石等 黄铁矿、方铅矿、褐铁矿 黄铁矿、褐铁矿、毒砂、黄铜矿、方铅矿、磁黄铁矿等 黄铁矿、方铅矿、褐铁矿 黄铁矿、黄铜矿、褐铁矿、石英、方解石 黄铁矿、方铅矿、褐铁矿 黄铁矿、黄铜矿、褐铁矿、石英、方解石 黄铁矿、褐铁矿、毒砂、黄铜矿、方铅矿、磁黄铁矿等 矿物组构 他形—半自形粒状结构、鳞片变晶结构、碎裂结构，浸染状构造、细网脉状构造、团块状构造 自形—半自形粒状晶，局部他形粒状晶，细脉状、侵染状、团块状构造 他形粒状结构、交代残余结构，团块状构造、条带状构造 半自形—他形粒状结构，浸染状、块状构造 自形—半自形粒状结构、他形粒状结构、交代残余结构、反应边结构、交代网状结构 他形粒状结构、交代残余结构，团块状构造、条带状构造 区内肉眼可见矿石矿物主要为黄铁矿，粒状结构，呈他形—半自形粒状、偶见自形粒状结构，以细粒为主，粒径一般0.1~1mm 半自形—他形粒状结构，浸染状、块状构造 半自形—他形粒状结构，浸染状、块状构造 半自形—他形粒状结构，浸染状、块状构造 半自形—他形粒状结构，浸染状、块状构造 自形—半自形粒状结构、他形粒状结构、交代残余结构、反应边结构、交代网状结构 矿体品位 Au 1.6~12.5 g/t Au 1.16~7.26 g/t；Pb 1.39%~6.36% Au 0.91~2.58 g/t，最高品位13 g/t Au 0.6~3.0 g/t，最高17 g/t；Cu 0.07%~1.11% 最高4.34 g/t 1.45~3.31 g/t，最高品位13.0 g/t 7.70 g/t，最高品位65.90 g/t 0.33~9.74 g/t最高品位27.6 g/t 平均品位2.23 g/t，最高品位5.43 g/t 最高品位6.34 g/t 1.14~3.55 g/t，最高品位7.88 g/t 1.56~11.1 g/t 金赋存形态 主要以不可见金形式赋存于硫化物中 明金不发育，以超微粒形式赋存于黄铁矿中为主 以不可见金形式赋存于硫化物中 以独立矿物自然金和类质同象形式产出 以微细粒状态赋存在黄铁矿中 主要以不可见金形式赋存于硫化物中 以独立矿物自然金为主 以独立矿物自然金为主，局部可见明金 以不可见金形式赋存于硫化物中 主要以不可见金形式赋存于硫化物中 主要以不可见金形式赋存于硫化物中 主要以不可见金形式赋存于硫化物中 围岩蚀变 硅化、碳酸盐化、绿泥石化 高岭土化 硅化，局部弱碳酸盐化、绿泥石化 碳酸盐化、硅化、绢云母化 硅化、黄铁矿化、绢云母化、碳酸盐化以及绿泥石化等 碳酸盐化、硅化、绢云母化 褐铁矿化、硅化、绢云母化、高岭土化 褐铁矿化、硅化、绢云母化 褐铁矿化、硅化、绢云母化、高岭土化 硅化、黄铁矿化、绢云母化、碳酸盐化以及绿泥石化等 褐铁矿化、硅化、绢云母化、高岭土化 褐铁矿化、硅化、绢云母化、高岭土化 金金属量/t (333+334) 3.6 3.2 1.75 6.05(332+333) 4.88 1.7 资料来源 冯李强，2017；安海西等，2018 逯永卓等，2020 刘彩乐等，2018 李升阳等，2013 申浩，2016 冯李强，2017 黄国彪等，2021 拜红奎等，2019 黄国彪等，2019 潘存钢，2019 雷延祥等，2019 潘鑫等，2019 
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表 2 黑海北二长花岗岩(HHB01)和加祖它士东花岗闪长岩(CY01)锆石LA-ICPMS U-Pb同位素年龄测试结果
Table 2. Zircon LA-ICP-MS U-Pb data of the Heihaibei monzonite (HHB01) and the Jiazutashidong granodiorite (CY01)
测点 含量/×10-6 同位素比值 同位素年龄/Ma Pb Th U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 黑海北HHB01 1 33.83 130.78 388.42 0.0565 0.0013 0.5888 0.0153 0.0754 0.0009 478 52 470 10 469 6 2 38.39 151.12 445.45 0.0566 0.0012 0.5329 0.0113 0.0682 0.0007 476 46 434 8 425 4 3 46.06 194.54 529.60 0.0564 0.0010 0.5677 0.0119 0.0728 0.0009 478 41 457 8 453 5 4 59.02 159.55 681.07 0.0550 0.0009 0.5593 0.0107 0.0736 0.0009 409 40 451 7 458 6 5 40.12 180.06 447.24 0.0596 0.0017 0.5880 0.0226 0.0703 0.0009 591 63 470 15 438 5 6 46.81 236.10 521.28 0.0553 0.0009 0.5266 0.0099 0.0689 0.0008 433 37 430 7 430 5 7 20.68 104.75 231.99 0.0573 0.0013 0.5512 0.0139 0.0697 0.0010 506 48 446 9 434 6 8 24.97 103.24 281.50 0.0572 0.0012 0.5636 0.0127 0.0715 0.0009 498 44 454 8 445 5 9 33.59 141.62 379.61 0.0584 0.0011 0.5813 0.0123 0.0720 0.0008 546 39 465 8 448 5 10 20.58 87.55 228.29 0.0579 0.0013 0.5755 0.0131 0.0726 0.0010 524 50 462 9 452 6 11 31.82 181.33 348.26 0.0579 0.0013 0.5575 0.0128 0.0700 0.0008 528 46 450 8 436 5 12 35.06 166.81 397.83 0.0589 0.0012 0.5575 0.0109 0.0689 0.0007 565 46 450 7 429 4 13 50.56 216.94 543.65 0.0626 0.0012 0.6096 0.0102 0.0712 0.0008 695 47 483 6 444 5 14 67.56 147.77 794.42 0.0570 0.0008 0.5644 0.0100 0.0716 0.0009 495 28 454 7 446 5 15 25.13 103.23 286.54 0.0601 0.0013 0.5927 0.0159 0.0710 0.0009 609 45 473 10 442 6 16 87.64 270.66 1065.25 0.0656 0.0010 0.5943 0.0107 0.0655 0.0006 794 32 474 7 409 4 加祖它士东CY01 1 22.96 240.36 443.52 0.0522 0.0013 0.2847 0.0075 0.0395 0.0004 295 56 254 6 250 3 2 73.51 665.87 1433.60 0.0526 0.0008 0.2853 0.0048 0.0393 0.0004 322 35 255 4 248 2 3 18.55 137.47 363.24 0.0531 0.0013 0.2929 0.0075 0.0401 0.0005 345 56 261 6 253 3 4 26.73 195.03 538.01 0.0505 0.0012 0.2806 0.0068 0.0404 0.0004 217 86 251 5 255 3 5 19.80 182.47 394.40 0.0502 0.0012 0.2698 0.0066 0.0390 0.0004 206 54 243 5 246 2 6 9.61 92.07 185.65 0.0495 0.0021 0.2655 0.0111 0.0393 0.0006 169 94 239 9 249 3 7 41.12 249.92 472.52 0.0565 0.0009 0.5226 0.0103 0.0668 0.0007 472 37 427 7 417 4 8 16.48 80.51 195.72 0.0559 0.0014 0.5105 0.0132 0.0665 0.0008 456 54 419 9 415 5 9 30.14 130.11 360.82 0.0572 0.0012 0.5298 0.0121 0.0670 0.0007 502 46 432 8 418 4 10 20.37 87.85 238.74 0.0569 0.0015 0.5379 0.0153 0.0684 0.0008 487 57 437 10 426 5 11 24.30 104.08 280.29 0.0564 0.0012 0.5343 0.0132 0.0685 0.0008 465 53 435 9 427 5 12 31.37 136.90 363.56 0.0552 0.0011 0.5206 0.0112 0.0684 0.0008 420 44 426 7 426 5 13 57.27 209.82 689.19 0.0556 0.0008 0.5179 0.0092 0.0672 0.0007 439 36 424 6 419 4 14 29.27 152.32 341.28 0.0539 0.0010 0.4973 0.0103 0.0667 0.0007 369 43 410 7 416 4 15 30.18 130.12 357.27 0.0554 0.0010 0.5157 0.0112 0.0673 0.0008 428 45 422 8 420 5
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