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Gold Science and Technology ›› 2018, Vol. 26 ›› Issue (4): 465-472.doi: 10.11872/j.issn.1005-2518.2018.04.465

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Geochronology,Geochemical Characteristics of Molybdenum Ore-bearing Syenogranite from Xiaozhaohuo Area in East Kunlun and Its Geological Significance

Jing CHEN(),Jichun HU,Yongzhuo LU,Shiying LU,Shulin WANG,Beibei XU   

  1. 1Qinghai Geological Survey Institue,The Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources Laboratory,Xining 810012,Qinghai,China
  • Received:2018-03-06 Revised:2018-05-23 Online:2018-10-10 Published:2018-10-17

Abstract:

Xiaozaohuo area is located in the northern region of the Middle Kunlun magmatic arc,next to the Qimantage back-arc basin in the north,which is one of the large number of copper molybdenum polymetallic mineralized points in Lalingzaohuo monoblock exploration area.The ore-bearing intrusion is syenogranite.Detailed studies on geochronology,element geochemical were carried out for the syenogranite.The results show that the age of syenogranite is (226±1)Ma,geochemical analysis show that it belongs to shoshonitic series,with weaker Eu negative anomaly (0.75~0.86),depleted of Nb,Ta,Ti,P,Ba,rich in Rb,Th,U,K;Rb/Sr ratios of 1.90 on average,Nb/Ta ratios of 11.33 on average,these characteristics are reflected the crust sources of the magma genesis.Combined with studies of igneous diagenetic assemblages in this area,this paper proposed that the diagenetic mineralization setting in Xiaozaohuo area is post-collision intracontinental orogenic stage in the late Triassic.

Key words: syenogranite, zircon U-Pb age, geochemistry, post-collision stage, molybdenum polymetallic ore, Xiaozaohuo, east Kunlun

CLC Number: 

  • P618.65

Fig.1

Geological sketch map of Xiaozaohuo area in East Kunlun"

Fig.2

Macroscopic(a) and hand specimen (b) photographs of molybdenum bearing syenogranite from Xiaozaohuo area"

Fig.3

CL images of zircon grains for syenogranite (XZHJD1)"

Table 1

Table 1 LA-ICP-MS zircon U- Pb isotopic tset data for ore-bearing syenogranite (XZHJD1) in Xiaozaohuo area"

测点编号 含量(×10-6)及比值 同位素比值及误差 年龄及误差
238U 232Th 232Th/238U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 206Pb/238U 1σ
1 326.94 216.73 0.66 0.05793 0.00263 0.2854 0.01240 0.03572 0.00042 226 3
2 374.34 208.12 0.56 0.05433 0.00383 0.26757 0.01830 0.03571 0.00062 226 4
3 395.31 189.35 0.48 0.05925 0.00201 0.29372 0.00939 0.03595 0.00032 228 2
4 359.78 266.71 0.74 0.04898 0.00168 0.24110 0.00783 0.03570 0.00030 226 2
5 693.50 440.25 0.63 0.04605 0.00277 0.22469 0.01305 0.03539 0.00054 224 3
6 657.32 359.52 0.55 0.06043 0.00269 0.29869 0.01271 0.03584 0.00042 227 3
7 490.92 350.41 0.71 0.05873 0.00649 0.28267 0.03074 0.03491 0.00070 221 4
8 517.31 357.25 0.69 0.05016 0.00178 0.24696 0.00832 0.03571 0.00031 226 2
9 527.93 336.54 0.64 0.05116 0.00126 0.25231 0.00566 0.03576 0.00023 226 1
10 523.05 279.68 0.53 0.05250 0.00207 0.25912 0.00975 0.03579 0.00035 227 2
11 347.92 251.36 0.72 0.05393 0.00163 0.26560 0.00746 0.03571 0.00028 226 2
12 836.68 729.23 0.87 0.05047 0.00353 0.24607 0.01674 0.03536 0.00057 224 4
13 436.40 307.08 0.70 0.05415 0.00305 0.26383 0.01465 0.03534 0.00036 224 2
14 607.12 159.45 0.26 0.05286 0.00246 0.26142 0.01166 0.03586 0.00041 227 3
15 540.32 330.61 0.61 0.06155 0.00294 0.30362 0.01392 0.03577 0.00045 227 3
16 617.61 346.15 0.56 0.06802 0.00321 0.32634 0.01502 0.03480 0.00035 220 2

Fig.4

U-Pb concordia diagram of zircon samples of syenogranite in Xiaozaohuo area"

Fig.5

A/NK-A/CNK(a) and SiO2-K2O diagram(b)"

"

元素 样品编号及元素含量
样品一 样品二 样品三 样品四
SiO2 73.51 73.02 77.20 77.36
TiO2 0.30 0.28 0.09 0.09
Al2O3 13.82 13.77 12.18 11.98
Fe2O3 0.96 1.44 0.64 0.66
FeO 0.77 0.71 0.35 0.38
MnO 0.044 0.042 0.03 0.02
MgO 0.58 0.34 0.19 0.21
CaO 0.86 0.94 0.74 0.75
Na2O 3.29 3.63 3.53 3.42
K2O 4.6 4.96 4.6 4.59
P2O5 0.08 0.066 0.01 0.02
H2O+ 1.14 0.68 0.48 0.80
LOS 0.61 0.17 0.26 0.20
A/CNK 1.156 1.055 1.004 1.002
La 34.5 30.7 23.4 20.8
Ce 61.93 62.04 52.06 43.34
Pr 8.83 7.45 6.03 5.20
Nd 25.90 24.70 20.70 17.30
Sm 4.94 4.27 3.66 3.01
Eu 1.08 1.03 0.83 0.79
Gd 3.62 3.62 2.82 2.48
Tb 0.57 0.54 0.38 0.37
Dy 2.59 2.78 1.70 1.83
Ho 0.59 0.58 0.31 0.35
Er 1.31 1.23 1.542 1.282
Tm 0.25 0.29 0.12 0.15
Yb 1.49 1.93 0.72 0.96
Lu 0.25 0.32 0.11 0.15
Rb 1 90 1 61 203.2 214.3
Ba 897 887 359.1 450.8
Th 8.94 25.00 16.23 16.72
Ta 0.76 1.24 1.633 1.333
Nb 10.60 12.50 16.92 14.57
Hf 4.05 4.89 2.931 2.728
Zr 148 166 72.98 70.65
Sm 4.13 3.79 4.272 3.198
Y 13.00 12.10 16.27 13.81
Sr 206 345 63.82 70.47
ΣREE 147.85 141.48 114.38 98.01
(La/Yb)N 16.61 11.41 23.31 15.54
σEu 0.75 0.78 0.76 0.86

Fig.6

Chondrite-normalized REE diagram (a) and primitive mantle normalized trace element spider-diagram(b)"

Fig.7

Y-Nb (a) and R1- R2 (b) diagrams of samples from Xiaozaohuo area(after Batchlor,et al[17])"

1 莫宣学,罗照华,邓晋福,等.东昆仑造山带花岗岩及地壳生长[J].高校地质学报,2007,13(3):403-414.
Mo Xuanxue , Luo Zhaohua , Deng Jinfu ,et al.Granitoids and crustal growth in the East-Kunlun orogenic belt[J].Geological Journal of China Universities,2007,13(3):403-414.
2 罗照华,柯珊,曹永清,等.东昆仑印支晚期幔源岩浆活动[J].地质通报,2002,21(6):292-297.
Luo Zhaohua , Ke Shan , Cao Yongqing ,et al.Late Indosinian mantle-derived magmatism in the East Kunlun[J].Geological Bulletin,2002,21(6):292-297.
3 王秉璋,陈静,罗照华,等.东昆仑祁漫塔格东段晚二叠世—早侏罗世侵入岩岩石组合时空分布、构造环境的讨论[J].岩石学报,2014,30(11):3213-3228.
Wang Bingzhang , Chen Jing , Luo Zhaohua ,et al.Spatial and temporal distribution of Late Permian–Early Jurassic intursion assemblages in eastern Qimantage,East Kunlun,and their tectonic settings[J].Acta Perologica Sinica,2014,30(11):3213-3228.
4 王秉璋.祁漫塔格地质走廊域古生代—中生代火成岩岩石构造组合研究[D].北京:中国地质大学,2011.
Wang Bingzhang .The Study and Investigation on the Assembly and Coupling Petrotectonic Assemblage During Paleozoic-Mesozoic Period at Qimantage Geological Corridor Domain[D].Beijing:China University of Geosciences,2011.
5 陈静,谢智勇,李彬,等.东昆仑拉陵灶火钼多金属矿床含矿岩体地质地球化学特征及其成矿意义[J].地质与勘探,2013,49(5):813-824.
Chen Jing , Xie Zhiyong , Li Bin ,et al.Geological and gechemical characteristics of the ore-bearing intrusions from the Lalingzaohuo Mo polymetallic deposit and its metallogenic significance[J].Geology and Exploration,2013,49(5):813-824.
6 王富春,陈静,谢志勇,等.东昆仑拉陵灶火钼多金属矿床地质特征及辉钼矿Re-Os同位素定年[J].中国地质,2013,40(4):1209-1217.
Wang Fuchun , Chen Jing , Xie Zhiyong ,et al.Geological features and Re-Os isotopic dating of the Lalingzaohuo molybdenum polymetallic deposit in East Kunlun[J].Geology in China,2013,40(4):1209-1217.
7 佘宏全,张德全,景向阳,等.青海省乌兰乌珠尔斑岩铜矿床地质特征与成因[J].中国地质,2007,34(2):306-312.
She Hongquan , Zhang Dequan , Jing Xiangyang ,et al.Geological characteristics and genesis of Ulan Uzhur porphyry copper deposit in Qinghai[J].Geology in China,2007,34(2):306-312.
8 李世金,孙丰月,丰成友,等.青海东昆仑鸭子沟多金属矿的成矿年代学研究[J].地质学报,2008,82(7):949-955.
Li Shijin , Sun Fengyue , Feng Chengyou ,et al.Geochronological Study on Yazigou Polymetallic Deposit in Eastern Kunlun,Qinghai Province[J].Acta Geologica Sinica,2008,82(7):949-955.
9 许庆林.青海东昆仑造山带斑岩型矿床成矿作用研究2l[D].长春:吉林大学,2014:85-90.
Xu Qinglin .Study on Metallogenesis of Porphyry Deposits in Eastern Kunlun Orogenic Belt,Qinghai Province[D].Changchun:Jilin University,2014:85-90.
10 王松,丰成友,李世金,等.青海祁漫塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMPU-Pb测年及其地质意义[J].中国地质,2009,36(1):74-84.
Wang Song , Feng Chengyou , Li Shijin ,et al.Zircon SHRIMP U-Pb dating of granodiorite in the Kaerqueka polymetallic ore deposit,Qimantage Mountain,Qinghai Province,and its geological implications[J].Geology in China,2009,36(1):74-84.
11 李积清,陈静,史青瑞,等.东昆仑卡尔却卡矿区似斑状二长花岗岩成因:锆石U-Pb年龄及Sr-Nd同位素制约[J].矿物岩石,2016,36(3):87-95.
Li Jiqing , Chen Jing , Shi Qingrui ,et al.The genesis of porphyritic monzogranitie of the Kaerqueka deposit in the East Kunlun:Evidence from zircon U-Pb dating and Sr-Nd isotopic compositions[J].Journal of Mineral and Petrol,2016,36(3):87-95.
12 Anderson T. Correction of common lead in U-Pb analyses that do not report204Pb[J].Chemical Geology,2002,192(1):59-79.
13 Belousova E A , Griffin W L , O'Reilly S Y ,et al.Igneous zircon:Trace element composition as an indicator of source rock type[J].Contributions to Mineralogy and Petrology,2002,143(5):602-622.
14 Boynton W V .Geochemistry of the rare earth elements:Meteorite studies[M]//Henderson.Rare Earth Element Geochemistry.Amsterdam :Elservier,1984:63-114.
15 Sun S S , Mcdonough W F .Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J].Geological Society London Special Publications,1989,42(1):313-345.
16 Taylor S R , Mclennan S M .The geochemical evolution of the continental crust[J].Reviews of Geophysics,1995,33(2):241-265.
17 Batchlor R B , Bowden P. Petrogenetic interpretation of granitiod rock series using multicationic parameters[J].Chemical Geology,1985,48(1):43-55.
18 罗照华,邓晋福,曹永清,等.青海省东昆仑地区晚古生代一早中生代火山活动与区域构造演化[J].现代地质,1999,13(1):51-56.
Luo Zhaohua , Deng Jinfu , Cao Yongqing ,et al.On Late Paleozoic-Early Mesozoic volcanism and regional tectonic evolution of Eastern Kunlun,Qinghai Province[J].Geoscience,1999,13(1):51-56.
19 向鹏.青海省加当根斑岩型铜(钼)矿床成矿特征及成矿条件研究[D].武汉:中国地质大学,2011.
Xiang Peng .Research on Mineralization Characteristics and Metallogenic Conditions of Jiadanggen Porphyry Copper (Molybdenum) Deposit,Qinghai Province[D].Wuhan:China University of Geosciences,2011.
20 鲁海峰,杨延乾,何皎,等.东昆仑哈陇休玛钼(钨)矿床花岗闪长斑岩锆石U-Pb及辉钼矿Re-Os同位素定年及其地质意义[J].矿物岩石,2017,37(2):33-39.
Lu Haifeng , Yang Yanqian , He Jiao ,et al.Zircon U-Pb age dating for granodiorite porphyry and molybdenite Re-Os isotope dating of Halongxiuma molybdenum(tungsten) deposit in the East Kunlun area and its geological significance[J].Journal of Mineral and Petrol,2017,37(2):33-39.
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