新疆阿克塔斯金矿床黑云母花岗岩锆石U-Pb和绢云母~(39)Ar/~(40)Ar测年及地质意义
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摘要
阿克塔斯金矿床位于新疆阿尔泰造山带南缘,矿体赋存于黑云母花岗岩与中泥盆统北塔山组中性火山岩接触带,矿石类型主要为石英脉型和蚀变岩型。矿区中酸性侵入岩体的岩石类型为二长花岗岩、黑云母花岗岩。近矿的黑云母花岗岩LA-ICP-MS锆石U-Pb年龄为(329.5±1.8)Ma,成岩时代为早石炭世;主成矿期的金-黄铁矿-石英细脉中的绢云母~(40)Ar/~(39)Ar坪年龄为(247.7±1.3) Ma、等时线年龄为(245.1±1.4)Ma,成矿时代为早三叠世。研究表明,阿克塔斯金矿成岩与成矿时代相距80 Ma,为碰撞造山和后碰撞造山不同地质作用的产物。该矿床具有造山型金矿的特点,额尔齐斯断裂带的右形剪切走滑作用控制金矿成矿过程。
The Aketasi gold deposit is located on the southern margin of the Altay orogenic belt. Gold orebodies are mainly hosted in the contact zone between the biotite granite and the middle Devonian Beitashan Formation volcanic rock. The main ore types are quartz vein type and altered rock type. The lithology of the Aketasi rocks is mainly composed of monzonitic granite and biotite granite. The age of U-Pb dating of zircon from the biotite granite is(329.5±1.8)Ma, demonstrating that the petrogenetic age is early Carboniferous. The ~(39)Ar/~(40)Ar age of sericite which is coexistent with that of gold, pyrite and quartz veinlets at the main metallogenic stage shows the plateau age of(247.7±1.3)Ma, and isochronal age of(245.1±1.4)Ma, implying that the metallogenic age is Early Triassic. Studies show that the difference between petrogenesis age and mineralization age of the Aktas gold deposit is 80 Ma, suggesting products of different geological processes of collision orogeny and post-collision orogeny. The deposit has the characteristics of orogenic gold deposit and the ore-forming process was controlled by the right-shaped shear strike-slip of the Irtysh fault zone
The Aketasi gold deposit is located on the southern margin of the Altay orogenic belt. Gold orebodies are mainly hosted in the contact zone between the biotite granite and the middle Devonian Beitashan Formation volcanic rock. The main ore types are quartz vein type and altered rock type. The lithology of the Aketasi rocks is mainly composed of monzonitic granite and biotite granite. The age of U-Pb dating of zircon from the biotite granite is(329.5±1.8)Ma, demonstrating that the petrogenetic age is early Carboniferous. The ~(39)Ar/~(40)Ar age of sericite which is coexistent with that of gold, pyrite and quartz veinlets at the main metallogenic stage shows the plateau age of(247.7±1.3)Ma, and isochronal age of(245.1±1.4)Ma, implying that the metallogenic age is Early Triassic. Studies show that the difference between petrogenesis age and mineralization age of the Aktas gold deposit is 80 Ma, suggesting products of different geological processes of collision orogeny and post-collision orogeny. The deposit has the characteristics of orogenic gold deposit and the ore-forming process was controlled by the right-shaped shear strike-slip of the Irtysh fault zone
引文
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,192(1-2):59-79.
Belousova E A,Griffin W L,O Reilly S Y and Fisher N I.2002.Igneous zircon:Trace elementcomposition as an indicator of source rock type[J].Contributions to Mineralogy and Petrology,143:602-622.
Buslov M M,Watanabe T,Fujiwara Y,Iwata K,Smirnova L V,Yu S,Semakov N N and Kiryanova A P.2004.Late Paleozoic faults of the Altai region,Central Asia:Tectonic pattern and model of formation[J].Journal of Asian Earth Sciences,23:655-671.
Cai K,Sun M,Yuan C,Long X and Xiao W.2011.Geological framework and Paleozoic tectonic history of the Chinese Altai[J].NWChina:A review.Russian Geology and Geophysics,52:1619-1633.
Filippova I B,Bush V A and Didenko A N.2001.Middle Paleozoic subduction belts:The leading factor in the formation of the Central Asian fold-and-thrust belt[J].Russian Journal of Earth Sciences,3:405-426.
Hong T,Xiang P,You J,Zhang L C,Wu C,Wu Q and Xu X W.2015.Texture and formation age of the eastern Irtysh collision belt[J].Acta Petrologica Sinica,31(2):571-593(in Chinese with English abstract).
Huang X L,Xu Y G,Luo C H,Wang R C and Lin G Y.2007.Exsolution lamellae in a chlinopyroxene megacryst aggregate from cenozoic basalt leizhou Peninsula,South China:Petrography and chemical evolution[J].Contribtions to Mineralogy and Petrology,154(6):691-705.
Ji S S,Ding R F,Zhao Z X and Liu M.2012.Fuyun County Aketas copper-gold depositsvolcanic,rocks geochemistry[J].Guanzhou Chemistry,37(3):39-49(in Chinese with English abstract).
Laurent-Charvet S,Charvet J,Monie P and Shu L S.2003.Late Palezoic strike-slip shear zones in eastern Central Asia(NW China):New strucural and geochronological data[J].Tectonics,22(2):1-24.
Li C M.2009.A review on the minerageny and situmicroanalytical dating techniques of zircons[J].Geological Survey and Reasearch,33(3):161-174(in Chinese with English abstract).
Li W Y,Dong F C,Zhang Z W,Tan W J,Jiang H B and Xiao C Y.2015.Major progress and Achievements in study of the Metallogenic prospect and prospecting deloyment of mineral resources in northwest China[J].Geologicial Survey of China,2(1):19-24(in Chinese with English abstract).
Liang W,Yang Z S and Zheng Y C.2015.The Zhaxikang Pb-Zn polymetallic deposit:Ar-Ar age of sericite and its metaooogenic significance[J].Acta Geologica Sinca,89(3):560-568(in Chinese with English abstract).
Liu F,Wang Z Y,Lin W,Chen K,Jiang L and Wang Q C.2013.Structure deformation and tectonic significance of Erqis fault zone in the southern margin of Chinese Altay[J].Acta Petrologica Sinica,29(5):1811-1824(in Chinese with English abstract).
Seng?r A M C,Natalin B A and Burtman V S.1993.Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J].Nature,364:299-307.
Pan D,Ding R F,Zhang H and You J.2012.Main charactersitics and prospecting perspective of Aketasi gold field prospecting target area in Funyun Country,Xinjiang[J].Science Technology and Engineering,12(5):1007-1013(in Chinese with English abstract).
Wang F S,Wen B and Zhu R X.2014.Problems of modern40Ar/39Ar geochronology[J].Acta Petrologica Sinica,30(2):326-340(in Chinese with English abstract).
Wang J B and Xu X.2006.Post-collisional tectonic evolution and metallogenesis in northern Xinjiang,China[J].Acta Geologica Sinica,80(1):23-31(in Chinese with English abstract).
Wang Y W,Wang J B,Long L L,Ding R F,Shi Y and Zhao L T.2015.The Early Carboniferous gold-copper-molybdenum mineralization events in the northern margin of Junggar Basin,Xinjiang:Geochronological evidence[J].Acta Petrologica Sinica,31(5):1448-1460(in Chinese with English abstract).
Wei X F,Yin Y J,Huang X K,Ding R F,Liao Z and Jiang J P.2016.40Ar/39Ar dating of the gold-bearing quartz veins in Aktas gold deposite and its geological implications Xinjiang[J].Mineral Exploration,7(1):65-71(in Chinese with English abstract).
Windley B F,Alexeiev D,Xiao W,Kroner A and Badarch G.2007.Tectonic models for accretion of the Central Asian Orogenic Belt[J].Journal of Geological Society London,164:31-47.
Wu Y F,Yang F Q,Liu F,Zhou M and Chen H Q.2015.40Ar/39Ar dating of sericite from the Brittle Ductile Shear Zone in the Ashele Cu-Zn ore district,Xinjiang[J].Acta Geoscientica Sinica,(36)1:121-126(in Chinese with English abstract).
Xiao W J and Santosh M.2014.The western Central Asian Orogenic Belt:A window to accretionary orogenesis and continental growth[J].Gondwana Research,25(4):1429-1444.
Xu X Y,Li R S,Chen J L,Ma Z P,Li Z P,Wang H L,Bai J K and Tang Z.2014.New constrains on the Paleozoic tectonic evolution of the northern Xinjiang area[J].Acta Petrologica Sinica,30(6):1521-1534(in Chinese with English abstract).
Yan S H,Teng R L,Wang Y T,Chen W,Zhang Z C and Chen B L.2006a.40Ar/39Ar dating of the Burgen gold-bearing shear zone on the southern margin of the Altay Mountains,Xinjiang,and its significance[J].Geology in China,33(33):648-653(in Chinese with English abstract).
Yan S H,Wang Y T,Zhang Z C,Chen B L and Chen W.2006b.Metallogenic type,tectonic setting,and resource potential of Ertix gold ore belt in northern Xinjiang[J].Mineral Deposits,25(6):693-702(in Chinese with English abstract).
Yang F Q,Yan S H,Liu G R,Zhou G,Zhang Z X,Liu F,Geng X Xand Guo C L.2010.Geological characteristics and metallogenesis of porphyry copper deposits in Junggar,Xinjiang[J].Mineral Deposits,29(6):956-971(in Chinese with English abstract).
Yuan H L,Wu F Y,Gao S,Liu X M,Xu P and Sun D Y.2003.Precise determinations of U-Pb age and rare earth element concetraions of zircons from Cenozoic instrusions in northern China by laser ablation ICP-Ms[J].Chinese Science Bulletin,48(22):4211-2421(in Chinese with English abstract).
Zhang H Y,Niu H C,Shen X M,Ma L and Yu X Y.2008.Late Paleozoic tectonic evolution and polymetallic ore-forming processes in southern Altay and northern Junggar[J].Mineral Deposits,27(5):596-603(in Chinese with English abstract).
Zhang Z C,Yan S H,Chen B L,Zhou G,He Y K,Chai F M,He L Xand Wan Y S.2006.SHRIMP zicron U-Pb dating for subductingrelated granitic rocks in the northern part of East Junggar,Xinjiang[J].Chinese Science Bulletion,51(13):1565-1574(in Chinese with English abstract).
Zheng Y,Zhang L and Guo Z L.2013.Zircon LA-ICP-MS U-Pb and biotite 40Ar/39Ar geochronology of the tiemuert Pb-Zn-Cu deposit,Xinjiang:Implications for ore gendsis[J].Acta Petrologica Sinica,29(1):191-204(in Chinese with English abstract).
Zheng Y,Li D F,Zhang L and Chen H Y.2014.Biotite40Ar/39Ar geochronology constraint on the genesis of the Sarekuobu gold deposit,Xinjiang[J].Acta Scientiarum Naturalium Universitatis Sunyatseni,6(53):10-19(in Chinese with English abstract).
Zhou G,Zhang Z C,Wang X K,Luo S B,He B and Zhang X L.2007.Zircon U-Pb SHRIMP and 40Ar/39Ar dating of the granitic mylonite in the Mayinebo fault belt of North Xinjiang and its geological significance[J].Acta Geoscientica Sinica,81(3):358-369(in Chinese with English abstract).
Zhou W K.1991.Geological features and prospect of Aketasi gold deposit,Xinjiang[J].Volcanology&Mineral Resources,12(4):87-95(in Chinese with English abstract).
洪涛,相鹏,游军,张连昌,吴楚,吴琪,徐兴旺.2015.额尔齐斯碰撞带东段结构与形成时代[J].岩石学报.31(2):571-593.
纪珊珊,丁汝福,赵智贤,刘猛.2012.富蕴县阿克塔斯铜金矿床火山岩地球化学[J].广州化学,37(3):39-49.
李长民.2009.锆石成因矿物学与锆石微区定年综述[J].地质调查与研究,33(3):161-174.
李文渊,董福辰,张照伟,谭文娟,姜寒冰,肖朝阳.2015.西北地区矿产资源成矿远景与召开部署研究主要进展及成果[J].中国地质调查局,2(1):19-24.
梁维,杨竹森,郑远川.2015.藏南扎西康铅锌多金属矿绢云母Ar-Ar年龄及其成矿意义[J].地质学报,89(3):560-568.
刘飞,王镇远,林伟,陈科,姜琳,王清晨.2013.中国阿尔泰造山带南缘额尔齐斯断裂带的构造变形及意义[J].岩石学报,29(5):1811-1824.
潘东,丁汝福,张华,游军.2012.新疆富蕴县阿克塔斯金矿找矿靶区主要特征及找矿远景[J].科学技术与工程,12(5):1007-1013.
王非,师文贝,朱日祥.2014.40Ar/39Ar年代学中几个重要问题讨论[J].岩石学报,30(2):326-340.
王京彬,徐新.2006.新疆北部后碰撞构造演化与成矿[J].地质学报,80(1):23-31.
王玉往,王京彬,龙灵利,丁汝福,石煜,赵路通.2015.新疆准噶尔北缘早石炭世金-铜-钼成矿事件:年代学证据[J].岩石学报,31(5):1448-1460.
卫晓锋,阴元军,黄兴凯,丁汝福,廖震,姜建平.2016.阿克塔斯含金石英脉40Ar/39Ar年代学及地质意义[J].矿产勘查,7(1):65-71.
吴玉峰,杨富全,刘锋,周明,陈红琦.2015.新疆阿舍勒铜锌矿区脆韧性剪切带中绢云母40Ar/39Ar年代学及其地质意义[J].地球学报,36(1):121-126.
徐学义,李荣社,陈隽璐,马中平,李智佩,王洪亮,白建科,唐卓.2014.新疆北部古生代构造演化的几点认识[J].岩石学报,30(6):1521-1534.
闫升好,滕荣丽,王义天,陈文,张招崇,陈柏林.2006a.新疆布尔根含金剪切带的40Ar/39Ar年龄及其地质意义[J].中国地质,33(3):648-655.
闫升好,王义天,张招崇,陈柏林,陈文.2006b.新疆额尔齐斯金矿带的成矿类型、地球化学动力学背景及资源潜力[J].矿床地质,29(6):956-971.
杨富全,闫升好,刘国仁,周刚,张志欣,刘锋,耿新霞,郭春丽.2010.新疆准噶尔斑岩铜矿地质特征及成矿作用[J].矿床地质,29(6):956-971.
袁洪林,吴福元,高山,柳小明,徐平,孙德有.2003.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,48(14):1511-1520.
张海洋,牛贺才,沈晓明,马林,于学元.2008.阿尔泰造山带南缘和准噶尔板块北缘晚古生代构造演化及多金属成矿作用[J].矿床地质,27(5):596-603.
张招崇,闫升好,陈柏林,周刚,贺永康,柴凤梅,何立新,万渝生.2006.新疆东准噶尔北部俯冲花岗岩的SHRIMP U-Pb锆石定年[J].科学通报,51(13):1565-1574.
郑义,张莉,郭正林.2013.新疆铁木尔特铅锌铜矿床锆石U-Pb和黑云母40Ar/39Ar年代学及其矿床成因意义[J].岩石学报,29(1):191-204.
郑义,李登峰,张莉,陈华勇.2014.新疆萨热阔布金矿黑云母40Ar/39Ar年龄及矿床成因启示[J].中山大学学报(自然科学版),6(53):10-19.
周刚,张招崇,王新昆,王祥昆,罗世宾,何斌,张小林.2007.新疆玛因鄂博断裂带中花岗质糜棱岩锆石U-Pb SHRIMP和黑云母40Ar/39Ar年龄及意义[J].地质学报,81(3):358-369.
周维康.1991.阿克塔斯金矿地质特征及找矿前景[J].火山地质与矿产,12(4):87-95.
Belousova E A,Griffin W L,O Reilly S Y and Fisher N I.2002.Igneous zircon:Trace elementcomposition as an indicator of source rock type[J].Contributions to Mineralogy and Petrology,143:602-622.
Buslov M M,Watanabe T,Fujiwara Y,Iwata K,Smirnova L V,Yu S,Semakov N N and Kiryanova A P.2004.Late Paleozoic faults of the Altai region,Central Asia:Tectonic pattern and model of formation[J].Journal of Asian Earth Sciences,23:655-671.
Cai K,Sun M,Yuan C,Long X and Xiao W.2011.Geological framework and Paleozoic tectonic history of the Chinese Altai[J].NWChina:A review.Russian Geology and Geophysics,52:1619-1633.
Filippova I B,Bush V A and Didenko A N.2001.Middle Paleozoic subduction belts:The leading factor in the formation of the Central Asian fold-and-thrust belt[J].Russian Journal of Earth Sciences,3:405-426.
Hong T,Xiang P,You J,Zhang L C,Wu C,Wu Q and Xu X W.2015.Texture and formation age of the eastern Irtysh collision belt[J].Acta Petrologica Sinica,31(2):571-593(in Chinese with English abstract).
Huang X L,Xu Y G,Luo C H,Wang R C and Lin G Y.2007.Exsolution lamellae in a chlinopyroxene megacryst aggregate from cenozoic basalt leizhou Peninsula,South China:Petrography and chemical evolution[J].Contribtions to Mineralogy and Petrology,154(6):691-705.
Ji S S,Ding R F,Zhao Z X and Liu M.2012.Fuyun County Aketas copper-gold depositsvolcanic,rocks geochemistry[J].Guanzhou Chemistry,37(3):39-49(in Chinese with English abstract).
Laurent-Charvet S,Charvet J,Monie P and Shu L S.2003.Late Palezoic strike-slip shear zones in eastern Central Asia(NW China):New strucural and geochronological data[J].Tectonics,22(2):1-24.
Li C M.2009.A review on the minerageny and situmicroanalytical dating techniques of zircons[J].Geological Survey and Reasearch,33(3):161-174(in Chinese with English abstract).
Li W Y,Dong F C,Zhang Z W,Tan W J,Jiang H B and Xiao C Y.2015.Major progress and Achievements in study of the Metallogenic prospect and prospecting deloyment of mineral resources in northwest China[J].Geologicial Survey of China,2(1):19-24(in Chinese with English abstract).
Liang W,Yang Z S and Zheng Y C.2015.The Zhaxikang Pb-Zn polymetallic deposit:Ar-Ar age of sericite and its metaooogenic significance[J].Acta Geologica Sinca,89(3):560-568(in Chinese with English abstract).
Liu F,Wang Z Y,Lin W,Chen K,Jiang L and Wang Q C.2013.Structure deformation and tectonic significance of Erqis fault zone in the southern margin of Chinese Altay[J].Acta Petrologica Sinica,29(5):1811-1824(in Chinese with English abstract).
Seng?r A M C,Natalin B A and Burtman V S.1993.Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J].Nature,364:299-307.
Pan D,Ding R F,Zhang H and You J.2012.Main charactersitics and prospecting perspective of Aketasi gold field prospecting target area in Funyun Country,Xinjiang[J].Science Technology and Engineering,12(5):1007-1013(in Chinese with English abstract).
Wang F S,Wen B and Zhu R X.2014.Problems of modern40Ar/39Ar geochronology[J].Acta Petrologica Sinica,30(2):326-340(in Chinese with English abstract).
Wang J B and Xu X.2006.Post-collisional tectonic evolution and metallogenesis in northern Xinjiang,China[J].Acta Geologica Sinica,80(1):23-31(in Chinese with English abstract).
Wang Y W,Wang J B,Long L L,Ding R F,Shi Y and Zhao L T.2015.The Early Carboniferous gold-copper-molybdenum mineralization events in the northern margin of Junggar Basin,Xinjiang:Geochronological evidence[J].Acta Petrologica Sinica,31(5):1448-1460(in Chinese with English abstract).
Wei X F,Yin Y J,Huang X K,Ding R F,Liao Z and Jiang J P.2016.40Ar/39Ar dating of the gold-bearing quartz veins in Aktas gold deposite and its geological implications Xinjiang[J].Mineral Exploration,7(1):65-71(in Chinese with English abstract).
Windley B F,Alexeiev D,Xiao W,Kroner A and Badarch G.2007.Tectonic models for accretion of the Central Asian Orogenic Belt[J].Journal of Geological Society London,164:31-47.
Wu Y F,Yang F Q,Liu F,Zhou M and Chen H Q.2015.40Ar/39Ar dating of sericite from the Brittle Ductile Shear Zone in the Ashele Cu-Zn ore district,Xinjiang[J].Acta Geoscientica Sinica,(36)1:121-126(in Chinese with English abstract).
Xiao W J and Santosh M.2014.The western Central Asian Orogenic Belt:A window to accretionary orogenesis and continental growth[J].Gondwana Research,25(4):1429-1444.
Xu X Y,Li R S,Chen J L,Ma Z P,Li Z P,Wang H L,Bai J K and Tang Z.2014.New constrains on the Paleozoic tectonic evolution of the northern Xinjiang area[J].Acta Petrologica Sinica,30(6):1521-1534(in Chinese with English abstract).
Yan S H,Teng R L,Wang Y T,Chen W,Zhang Z C and Chen B L.2006a.40Ar/39Ar dating of the Burgen gold-bearing shear zone on the southern margin of the Altay Mountains,Xinjiang,and its significance[J].Geology in China,33(33):648-653(in Chinese with English abstract).
Yan S H,Wang Y T,Zhang Z C,Chen B L and Chen W.2006b.Metallogenic type,tectonic setting,and resource potential of Ertix gold ore belt in northern Xinjiang[J].Mineral Deposits,25(6):693-702(in Chinese with English abstract).
Yang F Q,Yan S H,Liu G R,Zhou G,Zhang Z X,Liu F,Geng X Xand Guo C L.2010.Geological characteristics and metallogenesis of porphyry copper deposits in Junggar,Xinjiang[J].Mineral Deposits,29(6):956-971(in Chinese with English abstract).
Yuan H L,Wu F Y,Gao S,Liu X M,Xu P and Sun D Y.2003.Precise determinations of U-Pb age and rare earth element concetraions of zircons from Cenozoic instrusions in northern China by laser ablation ICP-Ms[J].Chinese Science Bulletin,48(22):4211-2421(in Chinese with English abstract).
Zhang H Y,Niu H C,Shen X M,Ma L and Yu X Y.2008.Late Paleozoic tectonic evolution and polymetallic ore-forming processes in southern Altay and northern Junggar[J].Mineral Deposits,27(5):596-603(in Chinese with English abstract).
Zhang Z C,Yan S H,Chen B L,Zhou G,He Y K,Chai F M,He L Xand Wan Y S.2006.SHRIMP zicron U-Pb dating for subductingrelated granitic rocks in the northern part of East Junggar,Xinjiang[J].Chinese Science Bulletion,51(13):1565-1574(in Chinese with English abstract).
Zheng Y,Zhang L and Guo Z L.2013.Zircon LA-ICP-MS U-Pb and biotite 40Ar/39Ar geochronology of the tiemuert Pb-Zn-Cu deposit,Xinjiang:Implications for ore gendsis[J].Acta Petrologica Sinica,29(1):191-204(in Chinese with English abstract).
Zheng Y,Li D F,Zhang L and Chen H Y.2014.Biotite40Ar/39Ar geochronology constraint on the genesis of the Sarekuobu gold deposit,Xinjiang[J].Acta Scientiarum Naturalium Universitatis Sunyatseni,6(53):10-19(in Chinese with English abstract).
Zhou G,Zhang Z C,Wang X K,Luo S B,He B and Zhang X L.2007.Zircon U-Pb SHRIMP and 40Ar/39Ar dating of the granitic mylonite in the Mayinebo fault belt of North Xinjiang and its geological significance[J].Acta Geoscientica Sinica,81(3):358-369(in Chinese with English abstract).
Zhou W K.1991.Geological features and prospect of Aketasi gold deposit,Xinjiang[J].Volcanology&Mineral Resources,12(4):87-95(in Chinese with English abstract).
洪涛,相鹏,游军,张连昌,吴楚,吴琪,徐兴旺.2015.额尔齐斯碰撞带东段结构与形成时代[J].岩石学报.31(2):571-593.
纪珊珊,丁汝福,赵智贤,刘猛.2012.富蕴县阿克塔斯铜金矿床火山岩地球化学[J].广州化学,37(3):39-49.
李长民.2009.锆石成因矿物学与锆石微区定年综述[J].地质调查与研究,33(3):161-174.
李文渊,董福辰,张照伟,谭文娟,姜寒冰,肖朝阳.2015.西北地区矿产资源成矿远景与召开部署研究主要进展及成果[J].中国地质调查局,2(1):19-24.
梁维,杨竹森,郑远川.2015.藏南扎西康铅锌多金属矿绢云母Ar-Ar年龄及其成矿意义[J].地质学报,89(3):560-568.
刘飞,王镇远,林伟,陈科,姜琳,王清晨.2013.中国阿尔泰造山带南缘额尔齐斯断裂带的构造变形及意义[J].岩石学报,29(5):1811-1824.
潘东,丁汝福,张华,游军.2012.新疆富蕴县阿克塔斯金矿找矿靶区主要特征及找矿远景[J].科学技术与工程,12(5):1007-1013.
王非,师文贝,朱日祥.2014.40Ar/39Ar年代学中几个重要问题讨论[J].岩石学报,30(2):326-340.
王京彬,徐新.2006.新疆北部后碰撞构造演化与成矿[J].地质学报,80(1):23-31.
王玉往,王京彬,龙灵利,丁汝福,石煜,赵路通.2015.新疆准噶尔北缘早石炭世金-铜-钼成矿事件:年代学证据[J].岩石学报,31(5):1448-1460.
卫晓锋,阴元军,黄兴凯,丁汝福,廖震,姜建平.2016.阿克塔斯含金石英脉40Ar/39Ar年代学及地质意义[J].矿产勘查,7(1):65-71.
吴玉峰,杨富全,刘锋,周明,陈红琦.2015.新疆阿舍勒铜锌矿区脆韧性剪切带中绢云母40Ar/39Ar年代学及其地质意义[J].地球学报,36(1):121-126.
徐学义,李荣社,陈隽璐,马中平,李智佩,王洪亮,白建科,唐卓.2014.新疆北部古生代构造演化的几点认识[J].岩石学报,30(6):1521-1534.
闫升好,滕荣丽,王义天,陈文,张招崇,陈柏林.2006a.新疆布尔根含金剪切带的40Ar/39Ar年龄及其地质意义[J].中国地质,33(3):648-655.
闫升好,王义天,张招崇,陈柏林,陈文.2006b.新疆额尔齐斯金矿带的成矿类型、地球化学动力学背景及资源潜力[J].矿床地质,29(6):956-971.
杨富全,闫升好,刘国仁,周刚,张志欣,刘锋,耿新霞,郭春丽.2010.新疆准噶尔斑岩铜矿地质特征及成矿作用[J].矿床地质,29(6):956-971.
袁洪林,吴福元,高山,柳小明,徐平,孙德有.2003.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,48(14):1511-1520.
张海洋,牛贺才,沈晓明,马林,于学元.2008.阿尔泰造山带南缘和准噶尔板块北缘晚古生代构造演化及多金属成矿作用[J].矿床地质,27(5):596-603.
张招崇,闫升好,陈柏林,周刚,贺永康,柴凤梅,何立新,万渝生.2006.新疆东准噶尔北部俯冲花岗岩的SHRIMP U-Pb锆石定年[J].科学通报,51(13):1565-1574.
郑义,张莉,郭正林.2013.新疆铁木尔特铅锌铜矿床锆石U-Pb和黑云母40Ar/39Ar年代学及其矿床成因意义[J].岩石学报,29(1):191-204.
郑义,李登峰,张莉,陈华勇.2014.新疆萨热阔布金矿黑云母40Ar/39Ar年龄及矿床成因启示[J].中山大学学报(自然科学版),6(53):10-19.
周刚,张招崇,王新昆,王祥昆,罗世宾,何斌,张小林.2007.新疆玛因鄂博断裂带中花岗质糜棱岩锆石U-Pb SHRIMP和黑云母40Ar/39Ar年龄及意义[J].地质学报,81(3):358-369.
周维康.1991.阿克塔斯金矿地质特征及找矿前景[J].火山地质与矿产,12(4):87-95.
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