世界地质 2017, 36(2) 507-519 DOI:   10.3969/j.issn.1004-5589.2017.02.017  ISSN: 1004-5589 CN: 22-1111/P

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流体包裹体
钼矿床
辉钼矿Re-Os定年
中古公路
斑岩型矿床
本文作者相关文章
PubMed
大兴安岭中北段古中公路钼矿床形成时代与矿床成因
刘大中1, 郝宇杰1, 杨群1, 赵书跃2, 任云生1
1. 吉林大学地球科学学院, 长春 130061;
2. 黑龙江省地质调查研究总院 齐齐哈尔分院, 哈尔滨 150036
摘要

古中公路钼矿床含矿岩体为碎裂硅化片麻状二长花岗岩体,蚀变呈带状分布,成矿过程可划分为钾长石+石英、石英+辉钼矿及石英+黄铁矿3个阶段。2件辉钼矿样品的Re-Os同位素模式年龄分别为(142.4±2.9)Ma和(142.3±2.0)Ma,表明矿床为早白垩世构造-岩浆活动的产物;辉钼矿中w(Re)含量分别为11.894×10-6和11.584×10-6,暗示成矿物质主要为地壳来源,可能有地幔物质的参与。流体包裹体研究表明:主成矿阶段的石英中主要以气液两相包裹体为主,其次为含子晶三相包裹体,CO2三相包裹体最少;不同类型包裹体的均一温度范围为196.3℃~>450℃,盐度可分为0.18%~12.62%和45.33%~>53.26%两个不同区间。因此,成矿流体为中高温、高盐度的NaCl-H2O-CO2体系,在热液成矿阶段可能发生过流体沸腾作用,且是钼矿的主要形成机制。综合成矿地质条件、矿床地质特征及成矿流体特征认为,该矿床成因上属斑岩型,形成于区域伸展的构造环境。

关键词 流体包裹体   钼矿床   辉钼矿Re-Os定年   中古公路   斑岩型矿床  
Mineralization age and ore genesis of Guzhonggonglu molybdenum deposit in central-northern Great Xing'an Range
LIU Da-zhong1, HAO Yu-jie1, YANG Qun1, ZHAO Shu-yue2, REN Yun-sheng1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Qiqihaer Branch of Heilongjiang Institute of Geological Survey, Harbin 150036, China
Abstract:

The ore-hosting intrusion of Guzhonggonglu molybdenum deposit is the fragmented silication gneissic monzogranite, and the alterations are distributed in belt. The metallogenic process can be divided into K-feldspar+quartz, quartz+molybdenite and quartz+pyrite stages. The Re-Os isotope model age of two molybdenite samples are (142.4±2.9)Ma and (142.3±2.0)Ma, respectively, indicating that the deposit was caused by the Early Cretaceous tectonic-magmatic activities. The content of Re in the molybdenite are 11.894×10-6 and 11.584×10-6, respectively, suggesting that the ore-forming materials are mainly derived from the crust, and probably affected by the mantle. The preliminary study of fluid inclusions demonstrates that the fluid inclusions in the quartz are mainly gas-liquid two phase inclusions, secondly gas-liquid-solid three phase inclusions, minor CO2-bearing three phase inclusions. The homogenization temperature of all type of inclusions are of 196.3~>450℃, while the salinities can be divided into two groups: 0.18%~12.62% and 45.33%~>53.26%. Thus, the ore-forming fluid belongs to the medium-high temperature, and high salinity NaCl-H2O-CO2 fluid system, and the fluid boiling might occur during the ore-forming stage and be the major metallogenic mechanism. Combined with the characteristics of ore-forming conditions, ore deposit geology and fluid inclusions, the study indicate that the Guzhonggonglu molybdenum deposit is of porphyry type, and formed under a regional extension tectonic settings.

Keywords: fluid inclusion   molybdenum deposit   molybdenite Re-Os dating   Guzhonggonglu   porphyry deposit  
收稿日期 2017-01-22 修回日期 2017-04-27 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2017.02.017
基金项目:

古亚洲构造域成矿背景与成矿机制(2013CB429802).

通讯作者: 任云生(1969,男,教授,博士生导师,主要从事矿床学与区域成矿规律的教学与科研工作.E-mail:renys@jlu.edu.cn
作者简介:
作者Email: renys@jlu.edu.cn

参考文献:

[1] 张连昌,吴华英,相鹏,等. 中生代复杂构造体系的成矿过程与成矿作用:以华北大陆北缘西拉木伦钼铜多金属成矿带为例[J]. 岩石学报,2010,26(5): 1351-1362. ZHANG Lian-chang, WU Hua-ying, XIANG Peng, et al. Ore-forming processes and mineralization of complex tectonic system during the Mesozoic: a case from Xilamulun Cu-Mo metallogenic belt [J]. Acta Petrologica Sinica, 2010, 26(5): 1351-1362.
[2] 佘宏全,李红红,李进文,等. 内蒙古大兴安岭中北段铜铅锌金银多金属矿床成矿规律与找矿方向[J]. 地质学报,2009,83(10): 1456-1472. SHE Hong-quan, LI Hong-hong, LI Jin-wen, et al. The metallogenetical characteristics and prospecting direction of the copper-lead-zinc polymetal deposits in the northern-central Daxing'anling Mountain, Inner Monglia [J]. Acta Geologica Sinica, 2009, 83(10): 1456-1472.
[3] 陈衍景,张成,李诺,等. 中国东北钼矿床地质[J]. 吉林大学学报: 地球科学版,2012,42(5): 1223-1268. CHEN Yan-jing, ZHANG Chen, LI Nuo, et al. Geology of the Mo deposits in Northeast China [J]. Journal of Jilin University: Earth Science Edition, 2012, 42(5): 1223-1268.
[4] 黄凡,王登红,王平安,等. 大兴安岭北段宜里钼矿岩石成因及成岩成矿年代学[J]. 地质学报,2014,88(3): 361-379. HUANG Fan, WANG Deng-hong, WANG Ping-an, et al. Petrogenesis and metallogenic chronology of the Yili Mo deposit in the northern Great Khing'an Ranges [J]. Acta Geologica Sinica, 2014, 88(3): 361-379.
[5] 李双林,欧阳自远. 兴蒙造山带及邻区的构造格局与构造演化[J]. 海洋地质与第四纪地质,1998,18(3): 45-54. LI Shuang-lin, OUYANG Zi-yuan. Tectonic framework and evolution of Xing'anling-Mongolian orogenic belt (XMOB) and its adjacent region [J]. Marine Geology & Quaternary Geology,1998, 18(3): 45-54.
[6] 郭志军,周振华,李贵涛,等. 内蒙古敖尔盖铜矿中-酸性侵入岩体SHRIMP锆石U-Pb定年与岩石地球化学特征研究[J]. 中国地质,2012,39(6): 1486-1500. GUO Zhi-jun, ZHOU Zhen-hua, LI Gui-tao, et al. SHRIMP U-Pb zircon dating and petrogeochemistral characteristics of the intermediate-acid intrusive rocks in the Aoergai copper deposit of Inner Mongolia[J]. Geology in China, 2012, 39(6): 1486-1500.
[7] Dolgopolova A, Seltmann R, Armstrong R, et al. Sr-Nd-Pb-Hf isotope systematics of the Hugo Dummett Cu-Au porphyry deposit (Oyu Tolgoi, Mongolia)[J]. Lithos, 2013, 164(4): 47-64.
[8] 王东方,权恒.大兴安岭中生代构造岩浆作用[J]. 地球科学,1984(3): 81-90. WANG Dong-fang, QUAN Huan. Mesozoic tectonics-magmatism in Daxing'anling, China [J]. Earth Science, 1984(3): 81-90.
[9] 陈志广,张连昌,万博,等. 内蒙古乌奴格吐山斑岩铜钼矿床低Sr-Yb型成矿斑岩地球化学特征及地质意义. 岩石学报,2008,24(1): 115-128. CHEN Zhi-guang, ZHANG Lian-chang, WAN Bo, et al. Geochemistry and geological significances of ore-forming porphyry with low Sr and Yb value in Wunugetushan copper-molybdenum deposit, Inner Mongolia [J]. Acta Petrologica Sinica, 2008, 24(1): 115-128.
[10] 陈志广,张连昌,卢百志,等. 内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义[J].岩石学报,2010, 26(5): 1437-1449. CHEN Zhi-guang, ZHANG Lian-chang, LU Bai-zhi, et al. Geochronology and geochemistry of the Taipingchuan copper-molybdenum deposit in Inner Mongolia, and its geological significances [J]. Acta Petrologica Sinica, 2010, 26(5): 1437-1449.
[11] 许文良,王枫,裴福萍,等. 中国东北中生代构造体制与区域成矿背景: 来自中生代火山岩组合时空变化的制约[J]. 岩石学报,2013,29(2): 339-353. XU Wen-liang, WANG Feng, PEI Fu-ping, et al. Mesozoic tectonic regimes and regional ore-forming background in NE China: constraints from spatial and temporal variations of Mesozoic volcanic rock associations [J]. Acta Petrologica Sinica, 2013, 29(2): 339-353.
[12] 佘宏全,李进文,向安平,等.大兴安岭中北段原岩锆石U-Pb 测年及其与区域构造演化关系[J]. 岩石学报,2012,28(2): 571-594. SHE Hong-quan, LI Jin-wen, XIANG An-ping, et al. U-Pb ages of the zircons from primary rocks in middle-northern Daxing'anling and its implications to geotectonic evolution [J]. Acta Petrologica Sinica, 2012, 28(2): 571-594.
[13] GUO Zhi-jun, LI Jin-wen, XU Xin-ying, et al. Sm-Nd dating and REE composition of scheelite for the Honghuaerji scheelite deposit, Inner Mongolia, Northeast China [J]. Lithos, 2016, 261: 307-321.
[14] 黑龙江省地质调查研究总院齐齐哈尔分院. 黑龙江省大兴安岭地区松岭区古中公路13公里钼多金属矿普查续作评估报告[R]. 齐齐哈尔:黑龙江省地质调查研究总院齐齐哈尔分院,2013. Qiqihaer Branch of Heilongjiang Institute of Geological Survey. Guzhonggonglu 13 kilometers molybdenum deposit continued survey report [R]. Qiqihaer: Qiqihaer Branch of Heilongjiang Institute of Geological Survey. 2013.
[15] 杜安道,何红蓼,殷宁万,等. 辉钼矿的铼-锇同位素地质年龄测定方法研究[J]. 地质学报,1994,68(4): 339-347. DU An-dao, HE Hong-liao, YIN Ning-wan, et al. A study on the rhenium-osmium geochronometry of molybdenites [J]. Acta Geologica Sinica, 1994, 68(4): 339-347.
[16] 贾志业,薛春纪,屈文俊,等. 新疆肯凳登高尔铜钼矿地质和S、Pb、O、H同位素组成及Re-Os测年[J]. 矿床地质,2011,30(1): 74-86. JIA Zhi-ye, XUE Chun-ji, QU Wen-jun, et al. Geology, S, Pb, O and H isotopic compositions and Re-Os chronology of Kendenggaoer Cu-Mo deposit in Xinjiang [J]. Mineral Deposits, 2011, 30(1): 74-86.
[17] 杜安道,赵敦敏,王淑贤,等. Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄[J].岩矿测试,2001,20(4): 247-252. DU An-dao, ZHAO Dun-min, WANG Shu-xian, et al. Precise Re-Os dating for molybdenite by ID-NTIMS with carius tube sample preparation [J]. Rock and Mineral Analysis, 2001, 20(4): 247-252.
[18] Shirey S B, Walker R J. Carius tube digestion for low-blank rhenium-osmium analysis, Anal [J]. Chemistry, 1995, 67: 2136-2141.
[19] Smoliar M L, Walker R J, Morgan J W. Re-Os ages of group ⅠA, ⅡA, ⅣA and ⅣB iron meteorites[J]. Science, 1996, 271: 1099-1102.
[20] 王可勇,王力,刘正宏,等. 辽宁高家堡子大型银矿床流体包裹体特征及矿床成因[J]. 岩石学报,2008,24 (9): 2085-2093. WANG Ke-yong, WANG Li, LIU Zheng-hong, et al. Characteristics of fluid inclusions and origin of Gaojiapuzi silver deposit, Liaoning Province[J].Acta Petrologica Sinica, 2008, 24(9): 2085-2093.
[21] 卢焕章,范宏瑞,倪培,等. 流体包裹体[M]. 北京: 科学出版社,2004:1-485. LU Huan-zhang, FAN Hong-rui, NI Pei, et al. Fluid inclusions [M]. Beijing: Science Press, 2004:1-485.
[22] Bodnar R J. Reviced equation and table for determining the freezing point depression of H2O-NaCl solutions [J]. Geochimca et Cosmochimica Acta, 1993, 57: 683-684.
[23] Hall D L,Sterner S M,Bodnar R J.Freezing point of NaCl-KCl-H2O solutions[J]. Economic Geology, 1988, 83: 197-202.
[24] Collins P L. Gas hydrates in CO2-bearing fluid inclusions and the use of freezing data for estimation of salinity [J]. Economic Geology, 1979, 74: 1435-1444.
[25] McCandless T E, Ruiz J R, Campbell A R. Rhenium behavior in molybdenite in hypogene and near-surface environments: implications for Re-Os geochronometry[J]. Geochimica et Cosmochimica Acta, 1993, 57: 889-905.
[26] Rollison H R. Using geochemical data: evaluation, presentation, interptrtation[M]. London: Longman, 1993: 1-384.
[27] Stein H J, Markey R J, Morgan J W, et al. The remarkable Re-Os chronometer in molybdenite: how and why it works[J]. Terra Nova, 2001, 13: 479-486.
[28] 刘翠,邓晋福,许立权,等. 大兴安岭—小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架[J]. 地学前缘,2011,18(3): 166-178. LIU Cui, DENG Jin-fu, XU Li-quan, et al. A preliminary frame of magma-tectonic-Mo metallogenic events of Mesozoic era in Da Hinggan Mountains and Xiao Hinggan Mountains areas[J]. Earth Science Frontiers, 2011, 18(3): 166-178.
[29] 刘军,武广,王峰,等. 大兴安岭北段岔路口斑岩钼矿床成矿年代学、岩石地球化学及其地质意义[J]. 矿床地质,2013,32(6): 1093-1116. LIU Jun, WU Guang, WANG Feng, et al. Geochronology and petrogeochemistry of Chalukou porphyry Mo depositin northern Da Hinggan Mountains [J]. Mineral Deposits, 2013, 32(6): 1093-1116.
[30] 朱怀亮,陈跃军,吴国学,等. 黑河新生地区早白垩世花岗岩质岩石的锆石U-Pb年龄、地球化学特征及地质意义[J]. 世界地质,2013,32(4): 665-680. ZHU Huai-liang, CHEN Yue-jun, WU Guo-xue, et al. Zircon U-Pb ages, geochemistry features and its geological implication of Early Cretaceous granites in Xinsheng area of Heihe City [J]. Global Geology, 2013, 32(4): 665-680.
[31] 聂凤军,孙振江,刘翼飞,等. 大兴安岭岔路口矿区中生代多期岩浆活动与钼成矿作用[J]. 中国地质,2013,40(1): 273-286. NIE Feng-jun, SUN Zhen-jiang, LIU Yi-fei, et al. Mesozoic multiple magmatic activities and molybdenum mineralization in the Chalukou ore district, Da Hinggan Mountains [J]. Geology in China, 2013, 40(1): 273-286.
[32] 翟德高,刘家军,王建平,等. 内蒙古太平沟斑岩型钼矿床Re-Os等时线年龄及其地质意义[J]. 现代地质,2009,23(2): 262-268. ZHAI De-gao, LIU Jia-jun, WANG Jian-ping, et al. Re-Os isotopic chronology of molybdenite from the Taipinggou porphyry-type molybdenum deposit in Inner Mongolia and its geological significance [J]. Geoscience, 2009, 23(2): 262-268.
[33] 张成,李诺,陈衍景,等. 内蒙古兴阿钼铜矿区侵入岩锆石U-Pb年龄及Hf同位素组成[J]. 岩石学报,2013,29(1): 217-230. ZHANG Cheng, LI Nuo, CHEN Yan-jing, et al. Zircon U-Pb ages and Hf isotopic compositions of the intrusive rocks in the Xing'a Mo-Cu deposit, Inner Mongolia [J]. Acta Petrologica Sinica, 2013, 29(1): 217-230.
[34] ZHAO Xi-xi, Coe R S, ZHOU Yao-xiu, et al. New paleomagnetic results from northern China: collision and suturing with Siberia and Kazakhstan [J]. Tectonophysics, 1990, 181(1/4): 43-81.
[35] Zorin Y A. Geodynamics of the western part of the Mongolia-Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia[J]. Tectonophysics, 1999, 306(1): 33-56.
[36] 李锦轶,莫申国,和政军,等. 大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J]. 地学前缘,2004,11(3): 157-167. LI Jin-yi, MO Shen-guo, HE Zheng-jun, et al. The timing of crustal sinistral strike-slip movement in the northern Great Hing'an Ranges and its constraint on reconstruction of the crustal tectonic evolution of NE China and adjacent areas since the Mesozoic [J]. Earth Science Frontiers, 2004, 11(3): 157-167.
[37] 赵越,徐刚,张拴宏,等. 燕山运动与东亚构造体制的转变[J]. 地学前缘,2004,11(3): 319-328. ZHAO Yue, XU Gang, ZHANG Shuan-hong, et al. Yanshanian Movement and conversion of tectonic regimes in East Asia [J]. Earth Science Frontiers, 2004, 11(3): 319-328.
[38] WANG Fei, ZHOU Xin-hua, ZHANG Lian-chang, et al. Late Mesozoic volcanism in the Great Xing'an Range (NE China): timing and implications for the dynamic setting of NE Asia [J]. Earth and Planetary Science Letters, 2006, 251(1/2): 179-198.
[39] 陈志广,张连昌,周新华,等. 满洲里新右旗火山岩剖面年代学和地球化学特征[J]. 岩石学报,2006,22(12): 2971-2986. CHEN Zhi-guang, ZHANG Lian-chang, ZHOU Xin-hua, et al. Geochronology and geochemical characteristics of volcanic rocks section in Manzhouli Xinyouqi, Inner Mongolia [J]. Acta Petrologica Sinica, 2006, 22(12): 2971-2986.
[40] Walker R J, Carlson R W, Shirey S B, et al. Os, Sr, Nd and Pb isotope systematics of southern African peridotite xenoliths: implications for the chemical evolution of subcontinental mantle[J]. Geochimica et Cosmochimica Acta, 1989, 53(7): 1583-1595.
[41] Walker R J, Morgan J W, Horan M F. Re-Os isotopic evidence for an enriched-mantle source for the Noril'sk-type, ore-bearing inclusions, Siberia[J]. Geochimica et Cosmochimica Acta, 1994, 58:4179-4197.
[42] Foster J G, Lambert D D, Frick L R, et al. Re-Os isotopic evidence for genesis of Archaen nickel ores from uncontaminated komatiites[J]. Nature, 1996, 382(6593): 703-706.
[43] 吴福元,孙德有. Re-Os同位素体系理论及其应用[J]. 地质科技情报,1999,18(3):43-46. WU Fu-yuan, SUN De-you. Theory and applications of Re-Os isotopic system [J]. Geological Science and Technology Information, 1999, 18(3):43-46.
[44] Lambert D D, Foster J G, Frick L R, et al. Re-Os isotopic systematics of the Voisey's bay Ni-Cu-Co magmatic ore system, Labrador, Canada [J]. Lithos, 1999, 47: 69-88.
[45] MAO Jing-wen, ZHANG Zhao-chong, ZHANG Zuo-heng, et al. Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit in the northern Qilian Mountains and its geological significance[J]. Geochimica et Cosmochimica Acta, 1999, 63(11/12): 1815-1818.
[46] 张振亮,吕新彪,饶冰. 均匀流体和不均匀流体的形成机制:来自合成流体包裹体的证据[J]. 地球科学,2008,33(2): 259-265. ZHANG Zhen-liang, LV Xin-biao, RAO Bing. Formational mechanisms of homogeneous fluid and boiling fluid: evidence from synthetic fluid inclusions [J]. Earth Science, 2008, 33(2): 259-265.
[47] 印贤波,张德会,王晨昇,等. 中国典型脉型钨、锡矿床和斑岩钼矿流体包裹体特征[J]. 桂林理工大学学报,2011,31(4): 524-532. YIN Xian-bo, ZHANG De-hui, WANG Chen-sheng, et al. Characteristics of fluid inclusion for typical tungsten, stannary vein deposit and porphyry molybdenum deposit in China [J]. Journal of Guilin University of Technology, 2011, 31(4): 524-532.
[48] 刘军,武广,王峰,等. 黑龙江省岔路口斑岩钼矿床流体包裹体和稳定同位素特征[J]. 中国地质,2013,40(4): 1231-1251. LIU Jun, WU Guang, WANG Feng, et al. Fluid inclusions and stable isotope characteristics of the Chalukou porphyry Mo deposit in Heilongjiang Province [J]. Geology in China, 2013, 40(4): 1231-1251.
[49] 黄凡、刘翠辉,谢有炜,等. 内蒙古宜里钼矿流体包裹体特征及其地质意义[J]. 地质与勘探,2014,50(3): 445-453. HUANG Fan, LIU Cui-hui, XIE You-wei, et al. Characteristics of fluid inclusions of the Yili Mo deposit in Inner Mongolia and their geological significance [J]. Geology and Exploration, 2014,50(3): 445-453.
[50] 王建国,张静,王圣文,等. 内蒙古太平沟钼矿床流体包裹体特征及成矿动力学背景[J]. 岩石学报,2009,25(10): 2621-2630. WANG Jian-guo, ZHANG Jing, WANG Sheng-wen, et al. Characteristics of fluid inclusions and metallogenetic geodynamical setting of the Taipinggou Mo deposit in Inner Mongolia, China [J]. Acta Petrologica Sinica, 2009, 25(10): 2621-2630.

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