中天山卡瓦布拉克地区彩霞山花岗岩体年龄及成因
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摘要
彩霞山花岗岩体位于中天山南缘的卡瓦布拉克地区,由糜棱岩化二长花岗岩和斑状钾长花岗岩组成,其LA-ICP-MS锆石U-Pb年龄分别为(330. 0±3. 6) Ma、(333. 3±3. 6) Ma;其锆石εHf(t)分别为5. 23～0. 87和10. 85～-5. 81,tDM2分别为1. 28～1. 00 Ga和1. 7～0. 65 Ga。地球化学分析结果显示,二长花岗岩和斑状钾长花岗岩的A/CNK、Na2O+K2O值分别为6. 40、45. 91和4. 17、33. 19,均属于高钾钙碱性过铝质I型花岗岩。富集轻稀土元素,具有强烈的铕负异常(δEu=2. 76～4. 14)。糜棱岩化二长花岗岩同构造侵位的显微构造特征揭示卡瓦布拉克韧性剪切带至少在早石炭世晚期处于活动状态。结合区域地质资料,认为彩霞山花岗岩体形成于南天山洋向北俯冲的活动大陆边缘环境,代表中天山南缘晚古生代岩浆弧的一部分。
The Caixiashan granitic pluton,which consists of mylonitized monzonitic granite and porphyritic moyite,is located in the Kawabulake area of the southern Central Tianshan. The LA-ICP-MS zircon U-Pb dating results show that those granitoids were formed at( 330. 0±3. 6) Ma and( 333. 3 ± 3. 6) Ma respectively. The εHf( t) values of mylonitized monzonitic granite vary from 5. 23 to 0. 87 with the tDM2 values of 1. 28-1. 00 Ga,while the εHf( t) values of porphyritic moyite vary from 10. 85 to-5. 81 with tDM2 values of 1. 7-0. 65 Ga. Geochemical analyses indicate that the A/CNK,Na2 O+K2 O ratios are 6. 40 and 45. 91 for the mylonitized monzonitic granite and 4. 17 and 33. 19 for the porphyritic moyite,and respectively. Both of them belong to the high-K calc-alkaline peraluminous I-type granite. They have relatively enriched in LREE with obviously negative Eu anomalies( δEu = 2. 76-4. 14). Microstructural features of syntectonic emplacement for themylonitized monzonitic granite indicate that the Kawabulake ductile shear zone was in an active state at least during the late agee of Early Carboniferous. Integrating with the regional geological data,It is believed that the Caixiashan pluton was formed in an active continental margin arc setting caused by the norward subduction of the South Tianshan Ocean and it represents a part of the Late Paleozoic magmatic arc in southern margin of the Central Tianshan.
The Caixiashan granitic pluton,which consists of mylonitized monzonitic granite and porphyritic moyite,is located in the Kawabulake area of the southern Central Tianshan. The LA-ICP-MS zircon U-Pb dating results show that those granitoids were formed at( 330. 0±3. 6) Ma and( 333. 3 ± 3. 6) Ma respectively. The εHf( t) values of mylonitized monzonitic granite vary from 5. 23 to 0. 87 with the tDM2 values of 1. 28-1. 00 Ga,while the εHf( t) values of porphyritic moyite vary from 10. 85 to-5. 81 with tDM2 values of 1. 7-0. 65 Ga. Geochemical analyses indicate that the A/CNK,Na2 O+K2 O ratios are 6. 40 and 45. 91 for the mylonitized monzonitic granite and 4. 17 and 33. 19 for the porphyritic moyite,and respectively. Both of them belong to the high-K calc-alkaline peraluminous I-type granite. They have relatively enriched in LREE with obviously negative Eu anomalies( δEu = 2. 76-4. 14). Microstructural features of syntectonic emplacement for themylonitized monzonitic granite indicate that the Kawabulake ductile shear zone was in an active state at least during the late agee of Early Carboniferous. Integrating with the regional geological data,It is believed that the Caixiashan pluton was formed in an active continental margin arc setting caused by the norward subduction of the South Tianshan Ocean and it represents a part of the Late Paleozoic magmatic arc in southern margin of the Central Tianshan.
引文
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report204Pb.Chemical Geology,23(10):2595-2604
Barbarin B.1996.Genesis of the two main types of peraluminous granitoids.Geology,24(1-2):295-298
Chen C M,Lu H F,Jia D,Cai D S,Wu S M.1999.Closing history of the southern Tianshan oceanic basin,western China:An oblique collisional orogeny.Tectonophysics,302(1-2):23-40
Chen X J,Shu L S,Santosh M.2011.Late Paleozoic post-collisional magmatism in the Eastern Tianshan Belt,Northwest China:New insights from geochemistry,geochronology and petrology of bimodal volcanic rocks.Lithos,127(3-4):581-598
Gelman S E,Deering C D,Bachmann O,Huber C,Gutiérrez F J.2014.Identifying the crystal graveyards remaining after large silicic eruptions.Earth and Planetary Science Letters,403:299-306
Green T H.1995.Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system.Chemical Geology,120(3-4):347-359
He Z Y,Klemd R,Zhang Z M,Zong K Q,Sun L X,Tian Z L,Huang B T.2015.Mesoproterozoic continental arc magmatism and crustal growth in the eastern Central Tianshan Arc Terrane of the southern central Asian orogenic belt:Geochronological and geochemical evidence.Lithos,236-237:74-89
Kemp A I S,Hawkesworth C J,Foster G L,Paterson B A,Woodhead JD,Hergt J M,Gray C M,Whitehouse M J.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon.Science,315(5814):980-983
Klemd R,Gao J,Li J L,Meyer M.2015.Metamorphic evolution of(ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen(Central Asian Orogenic Belt):Geodynamic implications.Gondwana Research,28(1):1-25
Lei R X,Wu C Z,Gu L X,Zhang Z Z,Chi G X,Jiang Y H.2011.Zircon U-Pb chronology and Hf isotope of the Xingxingxia granodiorite from the Central Tianshan zone(NW China):Implications for the tectonic evolution of the southern Altaids.Gondwana Research,20(2-3):582-593
Liu Y S,Hu Z C,Gao S,Günther D,Xu J,Gao C G,Chen H H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Ma X X,Shu L S,Meert J G,Li J Y.2014.The Paleozoic evolution of Central Tianshan:Geochemical and geochronological evidence.Gondwana Research,25(2):797-819
Middlemost E A K.1994.Naming materials in the magma/igneous rock system.Earth-Science Reviews,37(3-4):215-224
Pearce J A,Peate D W.1995.Tectonic implications of the composition of volcanic Are magmas.Annual Review of Earth and Planetary Sciences,23:251-285
Pitcher W S,Atherton M P,Cobbing E J,Beckinsale R D.1985.Magmatism at a plate edge:The Peruvian Andes.New York:Springer,1-328
Rickwood P C.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263
Scherer E E,Cameron K L,Blichert-Toft J.2000.Lu-f garnet geochronology:Closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions.Geochimica et Cosmochimica Acta,64(19):3413-3432
Sun S S,Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.Geological Society,London,Special Publications,42(1):313-345
Wang B,Shu L S,Faure M,Jahn B M,Cluzel D,Charvet J,Chung SL,Meffre S.2010.Paleozoic tectonics of the southern Chinese Tianshan:Insights from structural,chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China).Tectonophysics,497(1-4):85-104
Wu F Y,Yang Y H,Xie L W,Yang J H,Xu P.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1-2):105-126
Xiao W J,Windley B F,Allen M B,Han C M.2013.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage.Gondwana Research,23(4):1316-1341
陈博,秦克章,唐冬梅,毛亚晶,冯宏业,薛胜超,姚卓森.2015.新疆磁海铁矿区镁铁质岩及正长岩锆石U-Pb年代学、岩石地球化学特征:对成岩、成矿作用的制约.岩石学报,31(8):2156-2174
顾连兴,胡受奚,于春水,吴昌志,严正富.2011.论博格达俯冲撕裂型裂谷的形成与演化.岩石学报,17(4):585-597
郭瑞清,尼加提·阿布都逊,秦切,贾晓亮,朱志新,王克卓,李亚萍.2013.新疆塔里木北缘志留纪花岗岩类侵入岩的地质特征及构造意义.地质通报,32(2-3):220-238
贺振宇,张泽明,宗克清,王伟,于飞.2012.星星峡石英闪长质片麻岩的锆石年代学:对天山造山带构造演化及基底归属的意义.岩石学报,28(6):1857-1874
侯可军,李延河,邹天人,曲晓明,石玉若,谢桂青.2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报,23(10):2595-2604
黄河,王涛,秦切,侯继尧,童英,郭磊,张磊,王静,梁昭元.2015.中天山巴仑台地区花岗质岩石的Hf同位素研究:对构造演化及大陆生长的约束.地质学报,89(12):2286-2313
李锦轶.2004.新疆东部新元古代晚期和古生代构造格局及其演变.地质论评,50(3):304-322
李锦轶,何国琦,徐新,李华芹,孙桂华,杨天南,高立明,朱志新.2006.新疆北部及邻区地壳构造格架及其形成过程的初步探讨.地质学报,80(1):148-168
李锦轶.2009.中国大陆地质历史的旋回与阶段.中国地质,36(3):504-527,748
李鹏,吕新彪,陈超,曹晓峰,玛依拉,苏怡芸.2011.新疆东天山小白石头黑云母花岗岩年代学、地球化学特征及其地质意义.地质与勘探,47(4):543-554
李伍平,王涛,李金宝,康旭,于福生,韩庆军,马忠平.2001.东天山红柳河地区晚加里东期花岗岩类岩石锆石U-Pb年龄及其地质意义.地球学报,22(3):231-235
李小伟,莫宣学,赵志丹,朱弟成.2010.关于A型花岗岩判别过程中若干问题的讨论.地质通报,29(2-3):278-285
林涛,邓宇峰,屈文俊,周涛发,袁峰,邓刚.2017.新疆东天山地区三岔口铜矿床的成因:岩石学、年代学和地球化学证据.矿物岩石,37(4):47-61
南云,柳益群,周鼎武,周小虎,焦鑫,李哲萱.2018.新疆哈尔里克山石城子地区钠铁闪石花岗斑岩岩墙的发现及构造背景示踪.地质学报,92(6):1240-1263
尼加提·阿布都逊,木合塔尔·扎日,吴兆宁.2015.中天山卡瓦布拉克杂岩带中闪长岩的锆石U-Pb年龄及Hf同位素特征.吉林大学学报(地球科学版),45(6):1702-1712
尼加提·阿布都逊,木合塔尔·扎日,贾晓亮.2016.新疆南天山东段早石炭世---早二叠世花岗岩类及其对南天山洋盆闭合时间的约束.现代地质,30(2):263-273
庞迎春,程顺波.2009.花岗岩分类问题研究现状.资源环境与工程,23(2):119-122,137
彭明兴,钟春根,左琼华,朱婉明,杨世文,黄迅.2012.东天山卡瓦布拉克地区片麻状花岗岩形成时代及地质意义.新疆地质,30(1):12-18
邱检生,王睿强,赵姣龙,喻思斌.2015.冈底斯中段早侏罗世辉长岩-花岗岩杂岩体成因及其对新特提斯构造演化的启示:以日喀则东嘎岩体为例.岩石学报,31(12):3569-3580
舒良树,马瑞士,郭令智,孙家齐.1997.天山东段推覆构造研究.地质科学,32(3):337-350
舒良树,朱文斌,王博,吴昌志,马东升,马绪宣,丁海峰.2013.新疆古块体的形成与演化.中国地质,40(1):43-60
宋述光,王梦珏,王潮,牛耀龄.2015.大陆造山带碰撞-俯冲-折返-垮塌过程的岩浆作用及大陆地壳净生长.中国科学:地球科学,45(7):916-940
孙桂华,李锦轶,王德贵,高立明,宋安江.2006.东天山阿其克库都克断裂南侧花岗岩和花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义.地质通报,25(8):945-952
唐俊华,顾连兴,张遵忠,吴昌志,三金柱,汪传胜,刘四海,张光辉.2007.东天山咸水泉片麻状花岗岩特征、年龄及成因.岩石学报,23(8):1803-1820
田亚洲,杨经绥,刘飞,赵一珏,冯光英,牛晓露,张岚,高健.2014.新疆布鲁斯台辉长岩岩石学特征及对南天山洋俯冲时限的制约.岩石学报,30(8):2363-2380
王登红,李纯杰,陈郑辉,陈世平,肖克炎,李华芹,梁婷.2006.东天山成矿规律与找矿方向的初步研究.地质通报,25(8):910-915
吴福元,李献华,郑永飞,高山.2007.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220
吴福元,刘小驰,纪伟强,王佳敏,杨雷.2017.高分异花岗岩的识别与研究.中国科学:地球科学,47(7):745-765
吴浩若,李忠.2013.南天山洋古地理及构造演化:西南天山放射虫硅质岩与地层记录的再认识.古地理学报,15(3):293-304
夏林圻,张国伟,夏祖春,徐学义,董云鹏,李向民.2002.天山古生代洋盆开启、闭合时限的岩石学约束---来自震旦纪、石炭纪火山岩的证据.地质通报,21(2):55-62
谢才富.2002.同构造花岗岩的一种显微构造标记.岩石矿物学杂志,21(2):179-185
杨经绥,徐向珍,李天福,陈松永,任玉峰,李金阳,刘钊.2011.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年:早古生代洋盆的证据.岩石学报,27(1):77-95
张斌,陈文,喻顺,尹继元,李洁,孙敬博,杨莉,杨静.2014.南天山洋古生代期间俯冲作用过程探讨.岩石学报,30(8):2351-2362
张立飞,艾永亮,李强,李旭平,宋述光,魏春景.2005.新疆西南天山超高压变质带的形成与演化.岩石学报,21(4):1029-1038
张元元,郭召杰.2008.甘新交界红柳河蛇绿岩形成和侵位年龄的准确限定及大地构造意义.岩石学报,24(4):803-809
Barbarin B.1996.Genesis of the two main types of peraluminous granitoids.Geology,24(1-2):295-298
Chen C M,Lu H F,Jia D,Cai D S,Wu S M.1999.Closing history of the southern Tianshan oceanic basin,western China:An oblique collisional orogeny.Tectonophysics,302(1-2):23-40
Chen X J,Shu L S,Santosh M.2011.Late Paleozoic post-collisional magmatism in the Eastern Tianshan Belt,Northwest China:New insights from geochemistry,geochronology and petrology of bimodal volcanic rocks.Lithos,127(3-4):581-598
Gelman S E,Deering C D,Bachmann O,Huber C,Gutiérrez F J.2014.Identifying the crystal graveyards remaining after large silicic eruptions.Earth and Planetary Science Letters,403:299-306
Green T H.1995.Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system.Chemical Geology,120(3-4):347-359
He Z Y,Klemd R,Zhang Z M,Zong K Q,Sun L X,Tian Z L,Huang B T.2015.Mesoproterozoic continental arc magmatism and crustal growth in the eastern Central Tianshan Arc Terrane of the southern central Asian orogenic belt:Geochronological and geochemical evidence.Lithos,236-237:74-89
Kemp A I S,Hawkesworth C J,Foster G L,Paterson B A,Woodhead JD,Hergt J M,Gray C M,Whitehouse M J.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon.Science,315(5814):980-983
Klemd R,Gao J,Li J L,Meyer M.2015.Metamorphic evolution of(ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen(Central Asian Orogenic Belt):Geodynamic implications.Gondwana Research,28(1):1-25
Lei R X,Wu C Z,Gu L X,Zhang Z Z,Chi G X,Jiang Y H.2011.Zircon U-Pb chronology and Hf isotope of the Xingxingxia granodiorite from the Central Tianshan zone(NW China):Implications for the tectonic evolution of the southern Altaids.Gondwana Research,20(2-3):582-593
Liu Y S,Hu Z C,Gao S,Günther D,Xu J,Gao C G,Chen H H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Ma X X,Shu L S,Meert J G,Li J Y.2014.The Paleozoic evolution of Central Tianshan:Geochemical and geochronological evidence.Gondwana Research,25(2):797-819
Middlemost E A K.1994.Naming materials in the magma/igneous rock system.Earth-Science Reviews,37(3-4):215-224
Pearce J A,Peate D W.1995.Tectonic implications of the composition of volcanic Are magmas.Annual Review of Earth and Planetary Sciences,23:251-285
Pitcher W S,Atherton M P,Cobbing E J,Beckinsale R D.1985.Magmatism at a plate edge:The Peruvian Andes.New York:Springer,1-328
Rickwood P C.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263
Scherer E E,Cameron K L,Blichert-Toft J.2000.Lu-f garnet geochronology:Closure temperature relative to the Sm-Nd system and the effects of trace mineral inclusions.Geochimica et Cosmochimica Acta,64(19):3413-3432
Sun S S,Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.Geological Society,London,Special Publications,42(1):313-345
Wang B,Shu L S,Faure M,Jahn B M,Cluzel D,Charvet J,Chung SL,Meffre S.2010.Paleozoic tectonics of the southern Chinese Tianshan:Insights from structural,chronological and geochemical studies of the Heiyingshan ophiolitic mélange(NW China).Tectonophysics,497(1-4):85-104
Wu F Y,Yang Y H,Xie L W,Yang J H,Xu P.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1-2):105-126
Xiao W J,Windley B F,Allen M B,Han C M.2013.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage.Gondwana Research,23(4):1316-1341
陈博,秦克章,唐冬梅,毛亚晶,冯宏业,薛胜超,姚卓森.2015.新疆磁海铁矿区镁铁质岩及正长岩锆石U-Pb年代学、岩石地球化学特征:对成岩、成矿作用的制约.岩石学报,31(8):2156-2174
顾连兴,胡受奚,于春水,吴昌志,严正富.2011.论博格达俯冲撕裂型裂谷的形成与演化.岩石学报,17(4):585-597
郭瑞清,尼加提·阿布都逊,秦切,贾晓亮,朱志新,王克卓,李亚萍.2013.新疆塔里木北缘志留纪花岗岩类侵入岩的地质特征及构造意义.地质通报,32(2-3):220-238
贺振宇,张泽明,宗克清,王伟,于飞.2012.星星峡石英闪长质片麻岩的锆石年代学:对天山造山带构造演化及基底归属的意义.岩石学报,28(6):1857-1874
侯可军,李延河,邹天人,曲晓明,石玉若,谢桂青.2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报,23(10):2595-2604
黄河,王涛,秦切,侯继尧,童英,郭磊,张磊,王静,梁昭元.2015.中天山巴仑台地区花岗质岩石的Hf同位素研究:对构造演化及大陆生长的约束.地质学报,89(12):2286-2313
李锦轶.2004.新疆东部新元古代晚期和古生代构造格局及其演变.地质论评,50(3):304-322
李锦轶,何国琦,徐新,李华芹,孙桂华,杨天南,高立明,朱志新.2006.新疆北部及邻区地壳构造格架及其形成过程的初步探讨.地质学报,80(1):148-168
李锦轶.2009.中国大陆地质历史的旋回与阶段.中国地质,36(3):504-527,748
李鹏,吕新彪,陈超,曹晓峰,玛依拉,苏怡芸.2011.新疆东天山小白石头黑云母花岗岩年代学、地球化学特征及其地质意义.地质与勘探,47(4):543-554
李伍平,王涛,李金宝,康旭,于福生,韩庆军,马忠平.2001.东天山红柳河地区晚加里东期花岗岩类岩石锆石U-Pb年龄及其地质意义.地球学报,22(3):231-235
李小伟,莫宣学,赵志丹,朱弟成.2010.关于A型花岗岩判别过程中若干问题的讨论.地质通报,29(2-3):278-285
林涛,邓宇峰,屈文俊,周涛发,袁峰,邓刚.2017.新疆东天山地区三岔口铜矿床的成因:岩石学、年代学和地球化学证据.矿物岩石,37(4):47-61
南云,柳益群,周鼎武,周小虎,焦鑫,李哲萱.2018.新疆哈尔里克山石城子地区钠铁闪石花岗斑岩岩墙的发现及构造背景示踪.地质学报,92(6):1240-1263
尼加提·阿布都逊,木合塔尔·扎日,吴兆宁.2015.中天山卡瓦布拉克杂岩带中闪长岩的锆石U-Pb年龄及Hf同位素特征.吉林大学学报(地球科学版),45(6):1702-1712
尼加提·阿布都逊,木合塔尔·扎日,贾晓亮.2016.新疆南天山东段早石炭世---早二叠世花岗岩类及其对南天山洋盆闭合时间的约束.现代地质,30(2):263-273
庞迎春,程顺波.2009.花岗岩分类问题研究现状.资源环境与工程,23(2):119-122,137
彭明兴,钟春根,左琼华,朱婉明,杨世文,黄迅.2012.东天山卡瓦布拉克地区片麻状花岗岩形成时代及地质意义.新疆地质,30(1):12-18
邱检生,王睿强,赵姣龙,喻思斌.2015.冈底斯中段早侏罗世辉长岩-花岗岩杂岩体成因及其对新特提斯构造演化的启示:以日喀则东嘎岩体为例.岩石学报,31(12):3569-3580
舒良树,马瑞士,郭令智,孙家齐.1997.天山东段推覆构造研究.地质科学,32(3):337-350
舒良树,朱文斌,王博,吴昌志,马东升,马绪宣,丁海峰.2013.新疆古块体的形成与演化.中国地质,40(1):43-60
宋述光,王梦珏,王潮,牛耀龄.2015.大陆造山带碰撞-俯冲-折返-垮塌过程的岩浆作用及大陆地壳净生长.中国科学:地球科学,45(7):916-940
孙桂华,李锦轶,王德贵,高立明,宋安江.2006.东天山阿其克库都克断裂南侧花岗岩和花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义.地质通报,25(8):945-952
唐俊华,顾连兴,张遵忠,吴昌志,三金柱,汪传胜,刘四海,张光辉.2007.东天山咸水泉片麻状花岗岩特征、年龄及成因.岩石学报,23(8):1803-1820
田亚洲,杨经绥,刘飞,赵一珏,冯光英,牛晓露,张岚,高健.2014.新疆布鲁斯台辉长岩岩石学特征及对南天山洋俯冲时限的制约.岩石学报,30(8):2363-2380
王登红,李纯杰,陈郑辉,陈世平,肖克炎,李华芹,梁婷.2006.东天山成矿规律与找矿方向的初步研究.地质通报,25(8):910-915
吴福元,李献华,郑永飞,高山.2007.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220
吴福元,刘小驰,纪伟强,王佳敏,杨雷.2017.高分异花岗岩的识别与研究.中国科学:地球科学,47(7):745-765
吴浩若,李忠.2013.南天山洋古地理及构造演化:西南天山放射虫硅质岩与地层记录的再认识.古地理学报,15(3):293-304
夏林圻,张国伟,夏祖春,徐学义,董云鹏,李向民.2002.天山古生代洋盆开启、闭合时限的岩石学约束---来自震旦纪、石炭纪火山岩的证据.地质通报,21(2):55-62
谢才富.2002.同构造花岗岩的一种显微构造标记.岩石矿物学杂志,21(2):179-185
杨经绥,徐向珍,李天福,陈松永,任玉峰,李金阳,刘钊.2011.新疆中天山南缘库米什地区蛇绿岩的锆石U-Pb同位素定年:早古生代洋盆的证据.岩石学报,27(1):77-95
张斌,陈文,喻顺,尹继元,李洁,孙敬博,杨莉,杨静.2014.南天山洋古生代期间俯冲作用过程探讨.岩石学报,30(8):2351-2362
张立飞,艾永亮,李强,李旭平,宋述光,魏春景.2005.新疆西南天山超高压变质带的形成与演化.岩石学报,21(4):1029-1038
张元元,郭召杰.2008.甘新交界红柳河蛇绿岩形成和侵位年龄的准确限定及大地构造意义.岩石学报,24(4):803-809