GEOCHRONOOGICAL AND GEOCHEMICAL STUDY OF THE LATE TRIASSIC LAYERED MAFIC-ULTRAMFIC INTRUSIONS IN BEISHAN AREA OF WUSHI COUNTY, SOUTHWEST TIANSHAN

HU Chao-bin; LI Pei-qing; GU Ping-yang; CHEN Rui-ming; ZHA Xian-feng; ZHUANG Yu-jun

2016 Vol. 22, No. 4

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Article navigation > Journal of Geomechanics > 2016 > 22(4): 1015-1031

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HU Chao-bin, LI Pei-qing, GU Ping-yang, CHEN Rui-ming, ZHA Xian-feng, ZHUANG Yu-jun. GEOCHRONOOGICAL AND GEOCHEMICAL STUDY OF THE LATE TRIASSIC LAYERED MAFIC-ULTRAMFIC INTRUSIONS IN BEISHAN AREA OF WUSHI COUNTY, SOUTHWEST TIANSHAN[J]. Journal of Geomechanics, 2016, 22(4): 1015-1031.

Citation:

GEOCHRONOOGICAL AND GEOCHEMICAL STUDY OF THE LATE TRIASSIC LAYERED MAFIC-ULTRAMFIC INTRUSIONS IN BEISHAN AREA OF WUSHI COUNTY, SOUTHWEST TIANSHAN

1.
Xi'an Center of Geological Survey, Xi'an 710054, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 12 September 2016

Publish Date: 25 December 2016

Abstract

Abstract

Layered Mafic-ultramafic intrusions, which carry abundant information of mantle and provide an excellent approach to probe the mantle material composition, plate tectonic and deep geological process, are generally considered to be an important symbol of lithosphere extension, We discovered a suit of layered Mafic-ultramafic intrusions in Southwest Tianshan area, and obtained the zircon U-Pb age of gabbros of 224±4 Ma. These rocks are characterized by the enrichment of LREE, H₂O, Na₂O+K₂O and incompatible elements such as Th, U, Nb, Ta, etc., and depleted in HREE. They might be derived from enriched mantle, which is formed by low degree partial melting of garnet lherzolite. The primary magma may be high Mg basaltic magma which was rich in iron and titanium and mainly controlled by the fractional crystallization. This magam in the continental orogenic stage was actived in the environment of intracontinent orogen after the closure of the South Tianshan ocean and post collisional orogeny, which derived from mantle in the envirnment of extensional environment. We can concluded that the Southwest Tianshan area was under an extensional tectonic seting during late Triassic.
- Southwest Tianshan area /
- mafic-ultramafic /
- layered intrusions

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References

[1]	Day J M D, Pearson D G, Hulbert L J. Rhenium-Osmium isotope and platinum-group element constrains on the origin and evolution of the 1.27Ga Muskox layered intrusion[J]. Journal of Petrology, 2008, 49(7):1255~1295. doi: 10.1093/petrology/egn024 CrossRef Google Scholar
[2]	Niu Y L, Wilson M, Humphreys E R, et al. The origin of intra-plate ocean island basalts (OIB):The lid effect and its geodynamic implications[J]. Journal of Petrology, 2011, 52(7/8):1443~1468. Google Scholar
[3]	Spandler C, Mavrogenes J, Arculus R. Orign of chromitiel in layered instrusions:Evidence from hromite-hosted meit inclusion from the still water complex[J]. Geology, 2005, 33:893~896. doi: 10.1130/G21912.1 CrossRef Google Scholar
[4]	Maier W D, Barnes S J, Bandyayera D, et al. Early Kibaran rift-related mafic-ultramafic magmatism in western Tanzania and Burundi:Petrogenesis and ore potential of the Kapalagulu and Musongati layered intrusions[J]. Lithos, 2008, 101(1/2):24~53. Google Scholar
[5]	White R S, Smith L K, Roberts A W. Lower-crustal intrusion on the North Atlantic continental margin[J]. Nature, 2008, 452:460~464. doi: 10.1038/nature06687 CrossRef Google Scholar
[6]	宋谢炎, 张成江, 胡瑞忠, 等.峨眉火成岩省岩浆矿床成矿作用与地幔柱动力学过程的耦合关系[J].矿物岩石, 2005, 25(4):35~44. Google Scholar SONG Xie-yan, ZHANG Cheng-jiang, HU Rui-zhong, et al. Genetic links of magmatic deposits in the Emeishan Large Igneous Province with dynamics of mantle plume[J]. Journal of Mineralogy and Petrology, 2005, 25(4):35~44. Google Scholar
[7]	徐义刚, 何斌, 罗震宇, 等.我国大火成岩省和地幔柱研究进展与展望[J].矿物岩石地球化学通报, 2013, 32(1):25~39. Google Scholar XU Yi-gang, HE Bin, LUO Zhen-yu, et al. Study on mantle plume and large igneous provinces in chine:An overview and perspectives[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2013, 32(1):25~39. Google Scholar
[8]	Mao J W, Pirajno F, Zhang Z H, et al. A review of the Cu-Ni sulphide deposits in the Chinese Tianshan and Altay orogens (Xinjiang Autonomous Region, NW China):Principal characteristics and ore-forming processes[J]. Journal of Asian Earth Sciences, 2008, 32(2/4):184~203. Google Scholar
[9]	Schilling J G. Upper mantle heterogeneiries and dynamics[J]. Nature, 1985, 314:62~67. doi: 10.1038/314062a0 CrossRef Google Scholar
[10]	Hofmann A W. Mantle geochemistry:The message from oceanic volcanism[J]. Nature, 1997, 385:219~229. doi: 10.1038/385219a0 CrossRef Google Scholar
[11]	汤耀庆, 肖序常, 赵民.古中亚复合巨型缝合带南缘构造演化[M].北京:科学技术出版社, 1991:109~124. Google Scholar TANG Yao-qing, XIAO Xu-chang, ZHAO Min. The tectonic evolution of southern margin of the paleo Asia giant composite suture[M]. Beijing:Science and Technology Press, 1991:109~124. Google Scholar
[12]	肖序常, 汤耀庆, 李锦轶, 等.新疆北部及邻区大地构造[M].北京:地质出版社, 1992:1~169. Google Scholar XIAO Xu-chang, TANG Yao-qing, LI Jin-yi, et al, Tectonics of northern Xinjiang and its adjacent area[M]. Beijing:Geological Publishing House, 1992:1~169. Google Scholar
[13]	夏林圻, 夏祖春, 徐学义, 等.天山及邻区石炭纪-早二叠世裂谷火山岩岩石成因[J].西北地质, 2008, 04:1~68. doi: 10.3969/j.issn.1009-6248.2008.01.001 CrossRef Google Scholar XIA Lin-qi, XIA Zu-chun, XU Xue-yi, et al. Petrogenesis of Caboniferous-Early Permian rift-related volcanic rocks in the Tianshan and its neighboring areas, Northwestern China[J]. Northwestern Geology, 2008, 4:1~68. doi: 10.3969/j.issn.1009-6248.2008.01.001 CrossRef Google Scholar
[14]	肖序常, 汤耀庆, 王军, 等.中国南天山造山带蓝片岩及其构造意义[J].地球学报, 1994, Z2:54~64. Google Scholar XIAO Xu-chang, TANG Yao-qing, WANG Jun, et al. Blue schist belts and their tectonic implications of the South Tianshan Mts., NW China[J]. Acta Geologica Sinica, 1994, Z2:54~64. Google Scholar
[15]	蔡东升, 卢华复, 贾东, 等.南天山古生代板块构造演化[J].地质论评, 1995, 05:432~443. doi: 10.3321/j.issn:0371-5736.1995.05.006 CrossRef Google Scholar CAI Dong-sheng, LU Hua-fu, JIA Dong, et al. Paleozoic plate tectonic evolution of southern Tianshan[J]. Geological Review, 1995, 05:432~443. doi: 10.3321/j.issn:0371-5736.1995.05.006 CrossRef Google Scholar
[16]	夏林圻, 张国伟, 夏祖春.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[J].地质通报, 2002, 21(2):55~62. Google Scholar XIA Lin-qi, ZHANG Guo-wei, XIA Zi-chun. Constrain on the timing of opening and closing of the Tianshan Paleozoic basin:Evidence from Sinian and Carbonifercous volcanic rocks[J]. Geological Bulletin of China, 2002, 21(2):55~62. Google Scholar
[17]	Xiao W J, Zhang L C, Qin K Z, et al. Paleozoic accretionary and collisional tectonics of the eastern Tianshan (China):Implications for the continental growth of Central Asia[J]. American Journal of Science, 2004, 304:370~395. doi: 10.2475/ajs.304.4.370 CrossRef Google Scholar
[18]	李永军, 李注苍, 佟丽莉, 等.论天山古洋盆关闭的地质时限——来自伊宁地块石炭系的新证据[J].岩石学报, 2010, 10:2905~2912. Google Scholar LI Yong-jun, LI Zhu-cang, TONG Li-li, et al. Revisit the constraints on the closure of the Tianshan ancient oceanic basin:New evidence from Yining block of the Carboniferous[J]. Acta Petrologica Sinica, 2010, 10:2905~2912. Google Scholar
[19]	李文明, 任秉琛, 杨兴科, 等.东天山中酸性侵入岩浆作用及其地球动力学意义[J].西北地质, 2002, 04:41~64. doi: 10.3969/j.issn.1009-6248.2002.01.005 CrossRef Google Scholar LI Wen-ming, REN Bing-chen, YANG Xing-ke, et al. The intermediate-acid intrusive magmatism and its geodynamic significance in Eastern Tianshan region[J]. Northwestern Geology, 2002, 04:41~64. doi: 10.3969/j.issn.1009-6248.2002.01.005 CrossRef Google Scholar
[20]	江思宏, 聂凤军.北山地区花岗岩类的⁴⁰Ar/³⁹Ar同位素年代学研究[J].岩石学报, 2006, 11:2719~2732. doi: 10.3969/j.issn.1000-0569.2006.11.010 CrossRef Google Scholar JIANG Si-hong, NIE Feng-jun, ⁴⁰Ar/³⁹Ar geochronology of the granitoids in Beishan Moutain, NW China[J]. Acta Petrologica Sinica, 2006, 11:2719~2732. doi: 10.3969/j.issn.1000-0569.2006.11.010 CrossRef Google Scholar
[21]	郭瑞清, 秦切, 张晓帆, 等.新疆库鲁克塔格阔克塔格西碱性岩年代学、岩石地球化学特征及其地质意义[J].吉林大学学报:地球科学版, 2013, 02:457~468. Google Scholar GUO Rui-qing, QIN Qie, ZHANG Xiao-fan, et al. Geochronology, petrogeochemistry of western Kuoktagh alkaline rocks in Quruqtagh area in Xinjiang and its geolohical implications[J]. Journal of Jilin University:Earth Science Edition, 2013, 02:457~468. Google Scholar
[22]	刘畅, 赵泽辉, 郭召杰.甘肃北山地区煌斑岩的年代学和地球化学及其壳幔作用过程讨论[J].岩石学报, 2006, 05:1294~1306. doi: 10.3321/j.issn:1000-0569.2006.05.019 CrossRef Google Scholar LIU Chang, ZHAO Ze-hui, GUO Zhao-jie. Chronology and geochemistry of lamprophyre dykes from Beishan area, Gansu province and implications for the crust-mantle interaction[J]. Acta Petrologica Sinica, 2006, 05:1294~1306. doi: 10.3321/j.issn:1000-0569.2006.05.019 CrossRef Google Scholar
[23]	张遵忠, 顾连兴, 吴昌志, 等.东天山印支早期尾亚石英正长岩:成岩作用及成岩意义[J].岩石学报, 2006, 05:1135~1149. doi: 10.3321/j.issn:1000-0569.2006.05.007 CrossRef Google Scholar ZHANG Zun-zhong, GU Lian-xing, WU Chang-zhi, et al. Weiya quartz syenite in early Indosinina from eastern Tianshan Moutains:Petrogenesis and tectonic implications[J]. Acta Petrologica Sinica, 2006, 05:1135~1149. doi: 10.3321/j.issn:1000-0569.2006.05.007 CrossRef Google Scholar
[24]	张遵忠, 顾连兴, 吴昌志, 等.中天山东段尾亚印支早-中期石英闪长岩-陆内俯冲与原生下陆壳部分熔融[J].地质学报, 2011, 09:1420~1434. Google Scholar ZHANG Zun-zhong, GU Lian-xing, WU Chang-zhi, et al. Early-Middle Indosinian Weiya quartz diorite, eastern segment of the Middle Tianshan Mountains, NW China:Implications for intra-continent subduction and partial melting of juvenile lower crust[J]. Acta Geologica Sinica, 2011, 09:1420~1434. Google Scholar
[25]	朱志新, 董连慧, 王克卓, 等.西天山造山带构造单元划分与构造演化[J].地质通报, 2013, Z1:297~306. doi: 10.3969/j.issn.1671-2552.2013.02.009 CrossRef Google Scholar ZHU Zhi-xin, DONG Lian-hui, WANG Ke-zhuo, et al. Tectonic division and regional tectonic evolution of West Tianshan organic belt[J]. Geological Bulletin of China, 2013, Z1:297~306. doi: 10.3969/j.issn.1671-2552.2013.02.009 CrossRef Google Scholar
[26]	邹亚锐, 塔吉古丽, 邢作云, 等.塔里木新元古代-古生代沉积盆地演化[J].地球科学:中国地质大学学报, 2014, 08:1200~1216. Google Scholar ZOU Ya-rui, TAJI Gu-li, XING Zuo-yun, et al. Evolution of sedimentary basins in Tarim during Neoprpterpzoic-Paleozoic[J]. Earth Science:Journal of China University of Geosciences, 2014, 08:1200~1216. Google Scholar
[27]	高小芬, 林晓, 徐亚东, 等.南天山古生代-中生代沉积盆地演化[J].地球科学:中国地质大学学报, 2014, 08:1119~1128. Google Scholar GAO Xiao-fen, LIN Xiao, XU Ya-dong, et al. Evolution of sedimentary basins in South Tianshan during Paleozoic-Mesozoic[J]. Earth Science:Journal of China University of Geosciences, 2014, 08:1119~1128. Google Scholar
[28]	杨树锋, 陈汉林, 厉子龙, 等.塔里木早二叠世大火成岩省[J].中国科学:地球科学, 2014, 02:187~199. Google Scholar YANG Shu-feng, CHEN Han-lin, LI Zi-long, et al. Early Permian Tarim Large Igneous Province in northwest China[J]. Science in China:Earth Sciences, 2014, 02:187~199. Google Scholar
[29]	Andersen T. Correction of common lead in U-Pb analyses that do not report ²⁰⁴Pb[J]. Chemical Geology, 2002, 192:59~79. doi: 10.1016/S0009-2541(02)00195-X CrossRef Google Scholar
[30]	Luddwig KR. Isoplot:A plotting and regression program for radiogenic-isotope data[R]. US Geological Survey Open-File Report, 1991:91~445. Google Scholar
[31]	Rubatto D. Zircon trace element geochemistry:Partitioning with garnet and the link between U-Pb ages and metamorphism[J]. Chemical Geology, 2002, 184:123~138. doi: 10.1016/S0009-2541(01)00355-2 CrossRef Google Scholar
[32]	Winchester J A, Floyd P A. Geochemical discrimination of different magma series and their differentiation products using immobile elements[J]. Chemical Geology, 1977, 20:325~343. doi: 10.1016/0009-2541(77)90057-2 CrossRef Google Scholar
[33]	Sun S, Mcdonough W F. Chemical and isotopic systematics of oceanic Sun 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. doi: 10.1144/GSL.SP.1989.042.01.19 CrossRef Google Scholar
[34]	邓宇峰, 宋谢炎, 陈列锰, 等.东天山黄山西含铜镍矿镁铁-超镁铁岩体岩浆地幔源区特征研究[J].岩石学报, 2011, 27(12):3640~3652. Google Scholar DENG Yu-feng, SONG Xie-yan, CHEN Lie-meng, et al. Features of the mantle source of the Huangshanxi Ni-Cu sulfide-bearing mafic-ultramafic intrusion, eastern Tianshan[J]. Acta Petrologica Sinica, 2011, 27(12):3640~3652. Google Scholar
[35]	Ao S J, Xiao W J, Han C M. Geochronology and geochemistry of early Permian mafic-ultramafic complexes in the Beishan area, Xinjiang, NW China:Implications for late Paleozoic tectonic evolution of the southern Altaids[J]. Gondwana Research, 2010, 1:004. Google Scholar
[36]	姜常义, 贾承造, 李良辰.新疆麻扎尔塔格地区铁富集型高镁岩浆的源区[J].地质学报, 2004, 78(6):770~780. Google Scholar JIANG Chang-yi, JIA Cheng-zao, LI Liang-chen. Source of the Fe-riched-type high-Mg magma in Mazhartag Region, Xinjiang[J]. Acta Geologica Sinica, 2004, 78(6):770~780. Google Scholar
[37]	张传林, 周刚, 王洪燕, 等.塔里木和中亚造山带西段二叠纪大火成岩省的两类地幔源区[J].地质通报, 2010, 29(6):779~794. Google Scholar ZHANG Chuan-lin, ZHOU Gang, WANG Hong-yan, et al. A review on two types of mantle domains of the Permian large igneous province in Tarim and the western section of Central Asian orogenic belt[J]. Geological Bulletin of China, 2010, 29(6):779~794. Google Scholar
[38]	喻学惠, 赵志丹, 莫宣学, 等.甘肃西秦岭新生代钾霞橄黄长岩和碳酸岩的微量、稀土和Sr, Nd, Pb同位素地球化学:地幔柱-岩石圈交换的证据[J].岩石报报, 2004, 3:483~494. Google Scholar YU Xue-hui, ZHAO Zhi-dan, MO Xuan-xue, et al. Trace elements, REE and Sr, Nd, Pb isotopic geochemistry of Cenozoic kamafugite and carbonatite from west Qinling, Gamsu province:Implication of plume-liyhosphere interaction[J]. Acta Petrologica Sinica, 2004, 3:483~494. Google Scholar
[39]	Woodhead J D, Hergt J M, Davidson J P. Hafnium isotope evidence for conservative element mobility during subduction zone processes. Earth and Planetary Science Letters, 2001, 192(3):331~346. doi: 10.1016/S0012-821X(01)00453-8 CrossRef Google Scholar
[40]	Le Roex A O, Dick H J B. Geochemistry, mineralogy and petrogenensis of levaserupted along the southwest Indian Ridge between the Bouvet tripe junction and 11 degrees east[J]. Journal of Petrology, 2003, 24(3):267~318. Google Scholar
[41]	Wang K, Plant T, Walker J D. A mantle melting profile across the basin and range, SW USA[J]. Journal of Geophysical Research, 2002, 107(10):1029. Google Scholar
[42]	Hardarson B S, Fitton J G. Increased mantle melting beneath Snaefellsjokull volcano during Late Pleistocene deglaciation[J]. Nature, 1991, 353:62~64. doi: 10.1038/353062a0 CrossRef Google Scholar
[43]	钟宏, 胡瑞忠, 朱维光.层状岩体的成因及成矿作用[J].地学前缘, 2007, 14(2):159~172. Google Scholar ZHONG Hong, HU Rui-zhong, ZHU Wei-guang. Genesis and mineralization of layered intrusions[J]. Earth Science Frontiers, 2007, 14(2):159~172. Google Scholar
[44]	Green D H. Genesis of archean peridotitic magmas and constraints on archean geothermal gradients and tectonics[J]. Geology, 1975, 3:15~18. doi: 10.1130/0091-7613(1975)3<15:GOAPMA>2.0.CO;2 CrossRef Google Scholar
[45]	Hess P C. Phase equilibria constraints on the origin of ocean floor basalts[C]//Morgan J P, Blackman D K, Sinton J M. Mantle flow and melt generation at mid-ocean ridges.Geophysical Monograph, American Geophysical Union, 1992, 71:67~102. Google Scholar
[46]	Frey F A, Green D H, Roy S D. Integrated models of basalts petrogenesis:A study of quartz tholeiites to olivine melilitites from south eastern Australia utilizing geochemical and experimental petrological data[J]. Journal of Petrolog y, 1978, 19:463~513. doi: 10.1093/petrology/19.3.463 CrossRef Google Scholar
[47]	Macdonald R, Rogers N W, Fitton J G. Plume-lithosphere interactions in the generation of the basalts of the Kenya Rift, East Africa[J]. Journal of Petrology, 2001, 42:877~900. doi: 10.1093/petrology/42.5.877 CrossRef Google Scholar
[48]	Hofmann W. Chemical differentiation of the earth:The realationship between mantle, continental crust and oceanic crust[J]. Earth and Planetary Science Letters, 1986, 90:297~314. Google Scholar
[49]	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. doi: 10.1144/GSL.SP.1989.042.01.19 CrossRef Google Scholar
[50]	韩吟文, 马振东, 张宏飞.地球化学[M].第二版.北京:地质出版社, 2003:227~228. Google Scholar HAN Yin-wen, MA Zhen-dong, ZHANG Hong-fei. Geochemistry[M]. Beijing:Geological Publishing House, 2003:227~228. Google Scholar
[51]	Toplis M J, Carroll M R. An experimental study of the influence of oxygen fugacity on Fe-Ti oxide stability, phase relations, and mineral-melt equilibria in ferrobasaltic systems[J].Journal of Petrology, 1995, 36:1137~1170. doi: 10.1093/petrology/36.5.1137 CrossRef Google Scholar
[52]	杨树锋, 余星, 陈汉林, 等.塔里木盆地巴楚小海子二叠纪超基性脉岩的地球化学特征及其成因探讨[J].岩石学报, 2007, 23(5):1087~1096. Google Scholar YANG Shu-feng, YU Xing, CHEN Han-lin, et al. Geochemical characteristics and petrogenesis of Permian Xiaohaizi ultrabasic dyke in Bachu area, Tarim basin[J]. Acta Petrologica Sinica, 2007, 23(5):1087~1096. Google Scholar
[53]	励音骐, 厉子龙, 孙亚莉励音骐, 厉子龙, 孙亚莉, 等.塔里木瓦吉里塔格超镁铁质隐爆角砾岩铂族元素和微量元素地球化学特征及其岩石成因探讨[J].岩石学报, 2010, 11:3307~3318. Google Scholar LI Yin-qi, LI Zi-long, SUN Ya-li, et al. PGE and geochemistry of Wajilitag ultramafic cryptoexplosive brecciated rocks from Tarim Basin:Implicatons for petrogenesis[J].Acta Petrologica Sinica, 2010, 11:3307~3318. Google Scholar
[54]	陈汉林, 杨树锋, 厉子龙, 等.塔里木盆地二叠纪大火成岩省发育的时空特点[J].新疆石油地质, 2009, 30(2):179~182. Google Scholar CHEN Han-lin, YANG Shu-feng, LI Zi-long, et al. Spatial and temporal characteristics of Permian Large Igneous Province in Tarim Basin[J]. Xinjiang Petroleum Geology, 2009, 30(2):179~182. Google Scholar
[55]	Wei X, Xu Y G, Luo Z Y, et al. Composition of the Tarim mantle plume:Constraints from clinopyroxene antecrysts in the early Permian Xiaohaizi dykes, NW China[J]. Lithos, 2015, 205:69~81. Google Scholar
[56]	Xu Y G, Wei X, Luo Z Y, et al. The Early Permian Tarim Large Igneous Province:Main characteristics and a plume incubation model[J]. Lithos, 2014, 204:20~35. doi: 10.1016/j.lithos.2014.02.015 CrossRef Google Scholar
[57]	Agust Gudmundsson, Ingrid F Loetveit. Dyke emplacement in a layered and faulted rift zone[J]. Journal of Volcanology and Geothermal Research, 2005, 144(1/4):311~327. Google Scholar
[58]	Kiselev A I, Ernst R E, Yarmolyuk V V, et al. Radiating rifts and dyke swarms of the middle Paleozoic Yakutsk plume of eastern Siberian Craton[J]. Journal of Asian Earth Sciences, 2012, 45:1~16. doi: 10.1016/j.jseaes.2011.09.004 CrossRef Google Scholar
[59]	曾广策, 邱家骧.碱性岩的概念及其分类命名综述[J].地质科技情报, 1996, 01:31~37. Google Scholar ZENG Guang-ce, QIU Jia-xiang, Conception of alkaline rocks and their nomenclature[J]. Geological Science and Technology Information, 1996, 01:31~37. Google Scholar
[60]	李曰俊, 孙龙德, 吴浩若, 等.中国南天山西端乌帕塔尔坎群发现石炭纪一二叠纪放射虫化石[J].地质科学, 2005, 40(2):220~226. Google Scholar LI Yue-jun, SUN Long-de, WU Hao-ruo, et al. Permo-Carboniferous radiolaria from the Wupatarkan Group, west terminal of Chinese south Tianshan[J]. Chinese Journal of Geology, 2005, 40(2):220~226. Google Scholar
[61]	李曰俊, 杨海军, 赵岩, 等.南天山区域大地构造与演化[J].大地构造与成矿学, 2009, 33(1):94~104. Google Scholar LI Yue-jun, YANG Hai-jun, ZHAO Yan, et al. Tectonic framework and evolution of south Tianshan, NW China[J]. Geotectonica et Metallogenia, 2009, 33(1):94~104. Google Scholar
[62]	张立飞, 杜瑾雪, 吕增, 等.新疆西南天山超高压变质带的空间分布、峰期变质时代和P-T轨迹特征[J].科学通报, 2013, 22:2107~2112. Google Scholar ZHANG Li-fei, DU Jin-xue, LÜ Zeng, et al. A huge oceanic-type UHP metamorphic belt in southwestern Tianshan, China:Peak metamorphic age and P-T path[J].Chinese Science Bulletin, 2013, 22:2107~2112. Google Scholar
[63]	郑建平, 罗照华, 余淳梅, 等.新疆托云麻粒岩捕虏体地球化学和锆石年代学:岩石成因及西南天山下地壳性质[J].科学通报, 2005, 50(12), 1242~1251. Google Scholar ZHENG Jian-ping, LUO Zhao-hua, YU Chun-mei, et al. Geochemistry and zircon U-Pb ages of granulite xenolith from Tuoyun basalts, Xinjiang:Implications for the petrogenesis and the lower crustal nature beneath the southwestern Tianshan[J].Chinese Science Bulletin, 2005, 50(12), 1242~1251. Google Scholar
[64]	Henderson P. Rare earth element geochemistry[M]. Netherlands:Elsevier Science Publishers B V, 1984:23~28. Google Scholar
[65]	罗金海, 车自成, 周新源, 等.塔里木盆地西部中生代早期伸展作用的辉绿岩证据[J].中国地质, 2006, 33(3):566~571. Google Scholar LUO Jin-hai, CHE Zi-cheng, ZHOU Xin-yuan, et al. Diabase evidence for the early Mesozoic extension in the western Tarim basin, NW China[J]. Geology In China, 2006, 33(3):566~571. Google Scholar