吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (2): 455-472.doi: 10.13278/j.cnki.jjuese.20200009

• 地质与资源 • 上一篇    

东准噶尔奥依托浪格地区石炭纪双峰式火山岩地球化学特征及其构造意义

邹国庆1, 余牛奔1, 孙国庆1, 黄修保2, 尼加提·阿布都逊3,4, 卢观送1   

  1. 1. 江西省地质矿产勘查开发局赣西北大队, 江西 九江 332000;
    2. 江西省地质矿产勘查开发局, 南昌 330002;
    3. 新疆大学地质与矿业工程学院, 乌鲁木齐 830047;
    4. 新疆中亚造山带大陆动力学与成矿预测自治区重点实验室, 乌鲁木齐 830047
  • 收稿日期:2020-01-08 发布日期:2021-04-06
  • 通讯作者: 余牛奔(1990-),男,工程师,硕士,主要从事区域地质调查及矿产勘查方面的研究,E-mail:820707631@qq.com E-mail:820707631@qq.com
  • 作者简介:邹国庆(1964-),男,高级工程师,主要从事区域地质调查及矿产勘查方面的研究,E-mail:694578360@qq.com
  • 基金资助:
    中国地质调查局项目（DD20190368）

Geochemical Characteristics and Tectonic Significance of Carboniferous Bimodal Volcanic Rocks in Aoyituolangge Area, Eastern Junggar

Zou Guoqing1, Yu Niuben1, Sun Guoqing1, Huang Xiubao2, Nijiati·Abuduxun3,4, Lu Guansong1   

  1. 1. Northwestern Jiangxi Geological Party, Bureau of Geology and Exploration and Development of Mineral Researches of Jiangxi Province, Jiujiang 332000, Jiangxi, China;
    2. Bureau of Geology and Exploration and Development of Mineral Researches of Jiangxi Province, Nanchang 330002, China;
    3. College of Geology and Mining Engineering, Xinjiang University, Urumqi 830047, China;
    4. Key Laborary of Orogenic Belts Continental Dynamics and Metallogenic Prediction, Xinjiang Autonomous Region, Urumqi 830047, China
  • Received:2020-01-08 Published:2021-04-06
  • Supported by:
    Supported by the Project of China Geological Survey (DD20190368)

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摘要： 本文对东准噶尔造山带三塘湖盆地西北缘奥依托浪格地区石炭纪巴塔玛依内山组进行了火山岩地质、岩相学、地球化学特征研究，并结合相关年代学成果，探讨了火山岩成因、形成环境与东准噶尔造山带构造演化。研究认为：该区石炭纪巴塔玛依内山组火山岩具明显的陆相火山岩、双峰式火山岩特征，岩石组合基性端元以玄武岩为主，酸性端元为珍珠岩、英安岩；主量元素特征显示基性端元为钙碱—碱性性质，酸性端元珍珠岩、英安岩分别属于碱性、拉斑性质；微量元素特征显示基性端元相对富集Ba、K、Sr等大离子亲石元素（LILE），亏损Th、Nb、Nd等高场强元素（HFSE），酸性端元强烈亏损Ba、Nb、Sr、Sm、Ti等元素，富集K元素；稀土元素显示两端元均为轻稀土元素（LREE）相对富集、重稀土元素（HREE）相对亏损特征；珍珠岩主、微量元素特征与整体具有明显差异。综合研究表明：该双峰式火山岩基性端元来源于地幔岩的部分熔融，酸性端元英安岩来源于基性端元的分离结晶作用，珍珠岩则来源于下地壳的部分熔融；地球动力学背景为俯冲洋壳的拆沉作用，造成软流圈热源上涌，引发地幔岩的部分熔融与岩石圈的伸展减薄，进而诱发下地壳镁铁质岩的减压熔融；构造环境为后碰撞伸展阶段晚期，并指示了板块链式缝合的特点。

关键词: 东准噶尔造山带, 石炭纪, 双峰式火山岩, 地球化学, 构造意义

Abstract: In this paper, the geological,petrological, and geochemical characteristics of volcanic rocks of the Batamayineishan formation are studied in the Aoyituolangge area at the northwestern margin of Santanghu basin of the eastern Junggar orogenic belt, and the genesis, formation environment, and tectonic evolution of the eastern Junggar orogenic belt are discussed in combination with the relevant chronological results. It is concluded that the Carboniferous volcanic rocks in this area have obvious characteristics of continental volcanic rocks and bimodal volcanic rocks. The basic end member of the rock combination is mainly basalt, and the acid end members are perlite and dacite. The characteristics of the major elements show that the basic endmembers have calc-alkaline-alkaline properties; While the acidic endmembers of perlite and dacite have alkaline and freckling properties respectively. The characteristics of trace elements show that the fundamental end elements are relatively rich in LILE, such as Ba, K, Sr, etc., while Th, Nb, Nd, and other high-field strength elements (HFSE) are poor. Among the acidic end elements, Ba, Nb, Sr, Sm, Ti and other elements are strongly depleted, while K is more enriched. The analysis of rare earth elements show that LREE at both ends are relatively enriched, while HREE are relatively depleted. The main and trace elements characteristics of perlite are obviously different from the whole. The geochemical characteristics indicate that the basic end members of the bimodal volcanic rocks came from the partial melting of mantle rocks, the acidic end member of dacite came from the separation and crystallization of the basic end members, and the perlite came from the partial melting of the lower crust. The geodynamic background was the subduction of oceanic crust, which caused the upwelling of asthenosphere heat source, the partial melting of mantle rocks, the extensional thinning of lithosphere, and the decompression and melting of the mafic rocks in the lower crust. The tectonic environment was late in the post-collision extension stage, showing the characteristics of plate chain suture.

Key words: Eastern Junggar orogenic belt, Carboniferous, bimodal volcanic rocks, geochemistry, tectonic significance

中图分类号: 

  • P588.14
[1] 肖序常,汤耀庆,冯益民.新疆北部以及其邻区大地构造[M].北京:地质出版社,1992:1-169. Xiao Xuchang, Tang Yaoqing, Feng Yimin. Tectonics in Northern Xinjiang and Adjacent Areas[M]. Beijing:Geological Publishing House, 1992:1-169.
[2] 何国琦,李茂松,刘德权,等.中国新疆古生代地壳演化以及成矿[M].乌鲁木齐:新疆人民出版社,1994:1-437. He Guoqi, Li Maosong, Liu Dequan, et al. Paleozoic Crustal Evolution and Mineralization in Xinjiang, China[M]. Urumqi:Xinjiang People's Publishing House, 1994:1-437.
[3] 李锦轶,肖序常,陈文.准噶尔盆地东部的前晚奥陶世陆壳基底:来自盆地东北缘老君庙变质岩的证据[J].中国区域地质,2000,19(3):297-302. Li Jinyi, Xiao Xuchang, Chen Wen. Late Ordovician Continental Basement of the Eastern Junggar Basin in Xinjiang, NW China:Evidence from the Laojunmiao Metamorphic Complex on the Northeast Basin Margim[J]. Regional Geology of China, 2000:19(3):297-302.
[4] 张峰,陈建平,徐涛,等.东准噶尔晚古生代依旧存在俯冲消减作用:来自石炭纪火山岩岩石学、地球化学及年代学证据[J].大地构造与成矿学,2014,38(1):140-156. Zhang Feng, Chen Jianping, Xu Tao, et al. Late Paleozoic Subduction in the Eastern Junggar:Evidence from the Petrology, Geochemistry and Geochronology of Carboniferous Volcanic Rocks[J]. Geotectonica et Metallogenia, 2014, 38(1):140-156.
[5] 王道永,邓江红.东准噶尔地区板块构造特征及演化[J].成都理工学院学报,1995,22(4):38-45. Wang Daoyong, Deng Jianghong. Charcteristics and Evolution of the Plate Tectonics in Eastern Junggar, Xinjiang[J]. Journal of Chengdu Institute of Technology, 1995,22(4):38-45.
[6] 肖序常,冯益民.试论新疆北部大地构造演化[J].新疆地质科学,1990,7(1):47-68. Xiao Xuchang, Feng Yimin. On the Tectonic Evolution of Northern Xinjiang[J]. Xinjiang Geological Science, 1990, 7(1):47-68.
[7] 成守德,王元龙.新疆大地构造演化基本特征[J].新疆地质,1998,16(2):97-107. Cheng Shoude, Wang Yuanlong. Basic Charcteristics of Geotectonic Evolution of Xinjiang[J]. Xinjiang Geology, 1998, 16(2):97-107.
[8] 韩宝福,季建清,宋彪,等.新疆准噶尔晚古生代陆壳垂向生长(Ⅰ):后碰撞深成岩浆活动的时限[J].岩石学报,2006,22(5):1077-1086. Han Baofu, Ji Jianqing, Song Biao,et al. Late Paleozoic Vertical Growth of Continental Crust Around the Junggar Basin, Xinjiang, China (Part I):Timing of Post-Collisional Plutonism[J]. Acta Petrologica Sinica, 2006, 22(5):1077-1086.
[9] 龙晓平,孙敏,袁超,等.东准噶尔石炭系火山岩的形成机制及其对准噶尔洋盆闭合时限的制约[J].岩石学报,2006,22(1):31-40. Long Xiaoping, Sun Min, Yuan Chao,et al. Genesis of Carboniferous Volcanic Rocks in the Eastern Junggar:Constraints on the Closure of the Junggar Ocean[J]. Acta Petrologica Sinica, 2006, 22(1):31-40.
[10] 吴小奇,刘德良,魏国齐,等.准噶尔盆地陆东-五彩湾地区石炭系火山岩地球化学特征及其构造背景[J].岩石学报,2009,25(1):55-66. Wu Xiaoqi, Liu Deliang, Wei Guoqi.et al. Geochemical Characteristics and Tectonic Settings of Carboniferous Volcanic Rocks from Ludong-Wucaiwan Area, Junggar Basin[J]. Acta Petrologica Sinica, 2009, 25(1):55-66.
[11] 李涤,何登发,樊春,等.东准噶尔早二叠世后碰撞岩浆活动:蕴都卡拉流纹岩SHRIMP U-Pb年代学、地球化学和Hf同位素的制约[J].岩石学报, 2013,29(1):317-337. Li Di. He Dengfa, Fan Chun,et al. Early Permian Post-Collisional Magmatic Events, East Junggar:Constraints from Zircon SHRIMP U-Pb Age, Geochemistry and Hf Isotope of Rhyolite in the Yundukala Area[J]. Acta Petrologica Sinica,2013, 29(1):317-337.
[12] 汤贺军,孟贵祥,杨岳清,等.新疆东准噶尔恰库尔图地区二叠纪双峰式火山岩地质地球化学特征及构造意义[J].地质论评,2018,64(6):1393-1412. Tang Hejun, Meng Guixiang, Yang Yueqing,et al. Geological and Geochemical Features of the Permian Bimodal Volcanic Rocks in the Qiakurtu Area, Eastern Junggar Basin, Xinjiang, and Their Tectonic Significance[J]. Geological Review, 2018. 64(6):1393-1412.
[13] 李锦轶,肖序常,汤耀庆,等.新疆东准噶尔卡拉麦里地区晚古生代板块构造的基本特征[J].地质论评,1990,36(4):305-316. Li Jinyi, Xiao Xuchang, Tang Yaoqing,et al. Main Characteristics of Late Paleozoic Plate Tectonics in the Southern Part of East Junggar, Xinjiang[J]. Geological Review, 1990,36(4):305-316.
[14] 朱志新,李少贞,李嵩龄.东准噶尔纸房地区晚石炭世巴塔玛依内山组陆相火山-沉积体系特征[J].新疆地质,2005,23(1):14-18. Zhu Zhixin, Li Shaozhen, Li Songling. The Characteristics of Sedimentary System-Continental Facies Volcano in Later Carboniferous Batamayi Group, Zhifang Region, East Junggar[J]. Xinjiang Geology, 2005, 23(1):14-18.
[15] 夏林圻,李向民,夏祖春,等.天山石炭-二叠纪大火成岩省裂谷火山作用与地幔柱[J].西北地质,2006,39(1):1-49. Xia Linqi, Li Xiangmin, Xia Zuchun, et al. Carboniferous-Permian Rift-Related Volcanism and Mantle Plume in the Tianshan, Northwestern China[J]. Northwest Geology, 2006, 39(1):1-49.
[16] 张招崇,周刚,闫升好,等.阿尔泰山南缘晚古生代火山岩的地质地球化学特征及其对构造演化的启示[J].地质学报,2007,81(3):344-358. Zhang Zhaochong, Zhou Gang, Yan Shenghao,et al. Geology and Geochemistry of the Late Paleozoic Volcanic Rocks of the South Margin of the Altai Mountains and Implications for Tectonic Evolution[J]. Acta Geologica Sinica, 2007, 81(3):344-358.
[17] 王晓伟,杨春霞,王启航,等.北山石板泉一带石炭纪双峰式火山岩地球化学特征及构造意义[J].西北地质,2016,49(2):25-33. Wang Xiaowei, Yang Chunxia, Wang Qihang,et al. Geochemical Characteristics of Carboniferous Bimodal Volcanic Rocks in Shibanquan, Beishan and Its Tectonic Significance[J]. Northwest Geology, 2016, 49(2):25-33.
[18] 罗静兰,侯连华,蒋宜勤,等.陆东地区火成岩形成时代与构造背景及火山岩储层成因[J].石油学报,2012,33(3):351-360. Luo Jinglan, Hou Lianhua, Jiang Yiqin,et al. Chronology and Tectonic Settings of Igneous Rocks and Origin of Volcanic Reservoirs in Ludong Area, Eastern Junggar Basin[J]. Acta Petrolei Sinica, 2012, 33(3):351-360.
[19] 张元元,陈石,郭召杰,等.东准噶尔扎河坝地区古生代晚期火山岩的锆石SHRIMP U-Pb定年及其地质意义[J].岩石学报,2009,25(3):506-514. Zhang Yuanyuan, Chen Shi, Guo Zhaojie, et al. Zircon SHRIMP U-Pb Dating of the Latest Paleozoic Volcanic Rocks in Zhaheba Area, Eastern Junggar and Its Geological Implications[J]. Acta Petrologica Sinica, 2009, 25(3):506-514.
[20] 谭佳奕,吴润江,张元元,等.东准噶尔卡拉麦里地区巴塔玛依内山组火山岩特征和年代确定[J].岩石学报,2009,25(3):539-546. Tan Jiayi, Wu Runjiang, Zhang Yuanyuan,et al. Characteristics and Geochronology of Volcanic Rocks of Batamayineishan Formation in Kalamaily,Eastern Junggar, Xinjiang[J]. Acta Petrologica Sinica, 2009, 25(3):539-546.
[21] 李涤,何登发,樊春,等.准噶尔盆地克拉美丽气田石炭系玄武岩的地球化学特征及构造意义[J].岩石学报,2012,28(3):981-992. Li Di, He Dengfa, Fan Chun,et al. Geochemical Characteristics and Tectonic Significance of Carboniferous Basalt in the Karamaili Gas Field of Junggar Basin[J]. Acta Petrologica Sinica, 2012, 28(3):981-992.
[22] Xiao Yan, Zhang Hongfu, Shi Ji'an, et al. Late Paleozoic Magmatic Record of East Junggar, NW China and Its Significance:Implication from Zircon U-Pb Dating and Hf Isotope[J]. Gondwana Research, 2010, 20(2):532-542.
[23] Su Yuping, Zheng Jiangping, Griffin W L, et al. Geochemistry and Geochronology of Carboniferous Volcanic Rocks in the Eastern Junggar Terrane, NW China:Implication for a Tectonic Transition[J]. Gondwana Research, 2012, 22(3):1009-1029.
[24] Su Yuping, Zheng Jianping, Griffin W L. Zircon U-Pb and HfIsotopes of Volcanic Rocks from the Batamayineishan Formation in the Eastern Junggar Basin[J]. Chinese Science Bulletin, 2010, 55(36):2933-2945.
[25] Yang Xiaofa, He Dengfa, Wang Qingchen,et al. Tectonostratigraphic Evolution of the Carboniferous Arc-Related Basin in the East Junggar Basin, Northwest China:Insights into Its Link with the Subduction Process[J]. Gondwana Research, 2012, 22(3):1030-1046.
[26] Li Di, He Dengfa, Santosh M, et al. Petrogenesis of Late Paleozoic Volcanics from the Zhaheba Depression, East Junggar:Insights into Collisional Event in an Accretionary Orogeny of Central Asia[J]. Lithos, 2014, 184/185/186/187(1):167-193.
[27] 罗婷,陈帅,廖群安,等.东准噶尔晚石炭世双峰式火山岩年代学、地球化学及其构造意义[J].地球科学,2016,41(11):1845-1862. Luo Ting, Chen Shuai, Liao Qun'an, et al. Geochronology, Geochemistry and Geological Significance of the Late Carboniferous Bimodal Volcanic Rocks in the Eastern Junggar[J]. Earth Science, 2016, 41(11):1845-1862.
[28] 孙巧缡.新命名地层单位:三塘湖组[J].新疆地质,1995,13(3):214-223. Sun Qiaoli. Newly Named Stratigraphic Unit Santanghu Formation[J]. Xinjiang Geology, 1995, 13(3):214-223.
[29] 毕承彬,余牛奔,卢观送,等. 东准噶尔奥依托浪格地区原三塘湖组陆相火山岩地层的重新厘定与解体[J]. 中国地质, 2019, 46(6):1384-1395. Bi Chengbin, Yu Niuben, Lu Guansong,et al. Redetermination and Disintegration of the Continental Volcanic Strata of the Former Santanghu Formation in Oetonggar Area, Eastern Junggar Basin[J]. Geology in China, 2019, 46(6):1384-1395.
[30] 木合塔尔·扎日,尼加提·阿布都逊,吴兆宁.觉罗塔格南缘石炭系火山岩地球化学特征及其对古亚洲洋南缘构造演化的指示意义[J].地学前缘,2015,22(1):238-250. Muhetaer Zari, Nijati Abdursul, Wu Zhaoning. Geochemical Characteristics of the Volcanics from the Southern Jueluotage Area and Their Constraints on the Tectonic Evolution of Paleo-Asian Ocean[J]. Earth Science Frontiers, 2015, 22(1):238-250.
[31] 徐学义,李荣社,陈隽璐,等.新疆北部古生代构造演化的几点认识[J].岩石学报,2014,30(6):1521-1534. Xu Xueyi, Li Rongshe, Chen Juanlu,et al. New Constrains on the Paleozoic Tectonic Evolution of the Northern Xinjiang Area[J]. Acta Petrologica Sinica, 2014, 30(6):1521-1534.
[32] 赵霞,贾承造,张光亚,等.准噶尔盆地陆东-五彩湾地区石炭系中、基性火山岩地球化学及其形成环境[J].地学前缘,2008,15(2):272-279. Zhao Xia, Jia Chengzao, Zhang Guangya, et al. Geochemistry and Tectonic Settings of Carbonif Erous Intermediate Basic Bolcanic Rocks in Ludong-Wucaiwan, Junggar Basin[J]. Earth Science Frontiers, 2008, 15(2):272-279.
[33] Chen B, Jahn B M. Genesis of Post-Collisional Granitoids and Basement Nature of the Junggar Terrane, NW China:Nd-Sr Isotope and Trace Element Evidence[J]. Journal of Asian Earth Sciences, 2004, 23(5):691-703.
[34] Su Y P, Tang H F, Sylvester P J, et al, Petrogene-Sis of Karamaili Alkaline A-Type Granites from East Junggar, Xinjiang (NW China) and Their Relationship with Tin Mineralization[J]. Geochemical Joural, 2007, 41(5):341-357.
[35] 樊婷婷,周小虎,柳益群,等.新疆大黑山东部姜巴斯套组下段的凝灰岩锆石LA-ICP-MS U-Pb年龄及其地质意义[J].沉积学报,2011,29(2):312-320. Fan Tingting, Zhou Xiaohu, Liu Yiqun,et al. Crystal Tuff Zircon LA-ICP-MS U-Pb Ages from the Lower Jiangbasitao Formation in the East Daheishan Area, Xinjiang and Their Geological Implications[J]. Acta Sedimentologica Sinica, 2011, 29(2):312-320.
[36] 王富明,廖群安,樊光明,等.新疆卡拉麦里上-中泥盆统间角度不整合和346.8 Ma后碰撞火山岩的意义[J].地球科学:中国地质大学学报,2014,39(9):1243-1257. Wang Fuming, Liao Qun'an, Fan Guangming, et al. Geological Implications of Unconformity between Upper and Middle Devonian, and 346.8 Ma Post-Collision Volcanic Rocks in Karamaili, Xinjiang[J]. Earth Science:Journal of China University of Geosciences, 2014, 39(9):1243-1257.
[37] 黄小文,漆亮,高剑峰,等.东天山觉罗塔格地区底坎儿组火山岩地球化学特征及构造环境探讨[J].岩石矿物学杂志,2012,31(6):799-817. Huang Xiaowen, Qi Liang, Gao Jianfeng,et al. Geochemistry of Volcanic Rocks in the Dikan,er Formation of Jueluotage Region, Eastern Tianshan Mountains and Its Tectonic Implications[J]. Acta Petrologica et Mineralogica, 2012, 31(6):799-817.
[38] 田陟贤,李永军,田猛,等.西准噶尔恰达地区哈尔加乌组火山岩锆石U-Pb年代学、地球化学及地质意义[J].吉林大学学报(地球科学版),2016,46(1):135-145. Tian Zhixian, Li Yongjun, Tian Meng,et al. Zircon U-Pb Geochronology, Geochemical Characteristics and Geological Significance of Volcanic Rocks of Haerjiawu Formation in Qiada, West Junggar[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1):135-145.
[39] 柳成志, 孙玉凯, 于海山,等. 三塘湖盆地石炭系火山岩油气储层特征及碱性成岩作用[J]. 吉林大学学报(地球科学版), 2010, 40(6):1221-1231. Liu Chengzhi, Sun Yukai, Yu Haishan, et al. Study on Characteristic of Carboniferous Volcanic Oil and Gas Reservoirs and Alkaline Diagenesis in the Santanghu Basin,NW China[J]. Journal of Jilin University(Earth Science Edition), 2010, 40(6):1221-1231.
[40] 王焰,钱青,刘良,等.不同构造环境中双峰式火山岩的主要特征[J].岩石学报,2000,16(2):169-173. Wang Yan, Qian Qing, Liu Liang, et al. Major Geochmical Characteistics of Bimodal Volcanic Rocks in Different Geochmical Environments[J]. Acta Petrologica Sinica, 2000, 16(2):169-173.
[41] Tian J, Liao Q A, Fan G M, et al. The Discovery and Tectonic Implication of Early Carboniferous Post-Collisional I-Type Granites from the South of Karamaili in Eastern Junngar[J]. Acta Petrologica Sinica, 2015, 31(5):1471-1484.
[42] MacDonald R, Sparks R S J. The 1875 Eruption of Askja Volcano Lceland:Combined Fractional Crystallization and Selective Contamination in the Generation of Rhyolitic Magma[J]. Mineralogical Magazine, 1987, 51:183-202.
[43] Frisch W, Dunkl I, Kuhlemann J. Post-Collisional Orogen-Parallel Large-Scale Extension in the Eastern Alps[J]. Tectonophysics, 2000, 327(3/4):239-265.
[44] 于介禄,于介江,杨万志,等. 东天山觉罗塔格带东段早志留世中酸性侵入岩的年代学、地球化学及构造意义[J].吉林大学学报(地球科学版),2019,49(3):690-708. doi:10.13278/j.cnki. jjuese.20180240. Yu Jielu,Yu Jiejiang,Yang Wanzhi,et al. Geochronology, Geochemistry and Tectonic Implications of Early Silurian Intermediate-Acid Intrusive Rocks in East of Jueluotage Belt, Eastern Tianshan[J]. Journal of Jilin University (Earth Science Edition),2019, 49(3):690-708. doi:10.13278/j.cnki. jjuese.20180240.
[45] Pearce J A, Peate D W. Tectonic Implications of the Composition of Volcanic Arc Magmas[J]. Annual Review of Earth and Planetary Sciences, 1995, 23(1):251-286.
[46] 路彦明,张玉杰,潘懋,等.东准噶尔黄羊山西金矿区含矿花岗斑岩锆石U-Pb定年及地质意义[J].吉林大学学报(地球科学版),2010,40(4):852-858. Lu Yanming, Zhang Yujie, Pan Mao, et al. Zircon U-Pb Dating of Ore-Bearing Granite-Porphyry Vein in Western Huangyangshan Gold Deposit, Eastern Junggar and Its Geological Significance[J]. Journal of Jilin University(Earth Science Edition), 2010, 40(4):852-858.
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