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[1]杨高学,李永军,郭文杰,等.西天山阿吾拉勒阔尔库岩基解体的岩石化学证据[J].地球科学与环境学报,2008,30(02):125.
　YANG Gao-xue,LI Yong-jun,GUO Wen-jie,et al.Petrochemical Evidence and Its Significance of Disintegration of Kuoerku Granite Batholith in Awulale , Western Tianshan[J].Journal of Earth Sciences and Environment,2008,30(02):125.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:: 第30卷
期数:: 2008年第02期

页码:: 125

栏目:: 基础地质与矿产地质

出版日期:: 2008-06-20

文章信息/Info

Title:: Petrochemical Evidence and Its Significance of Disintegration of Kuoerku Granite Batholith in Awulale , Western Tianshan

作者:: 杨高学¹; 李永军¹; 郭文杰²; 毕明波¹; 栾新东²; 李注苍¹; 李宏²; 佟黎明²; 1.长安大学地球科学与资源学院,陕西西安710054;2.新疆地质矿产勘查开发局第九地质大队,新疆乌鲁木齐830000

Author(s):: YANG Gao-xue¹; LI Yong-jun¹; GUO Wen-jie²; BI Ming-bo¹; LUAN Xin-dong ²; LI Zhu-cang¹; LI Hong²; TONG Li-ming²; 1. School o f Earth Sciences and Resources, Chang︐an University, Xi︐an 710054, Shaanxi, China; 2. No.9 Geological Party, Xinjiang Bureau o f Geology and Mineral Exploration and Development, Urumqi 830000, Xinjiang, China)

关键词:: 花岗岩; 岩石化学; 阔尔库岩基; 阿吾拉勒; 西天山

Keywords:: granite; petrochemistry; Kuoerku batholith; Awulale; Western Tianshan

分类号:: P584

DOI:: -

文献标志码:: A

摘要:: 西天山阿吾拉勒阔尔库岩基被解体为早石炭世赛肯都鲁序列和早二叠世阔尔库序列。岩石化学研究表明,赛肯都鲁序列中SiO2质量分数平均62.81%,富CaO贫Na2O和K2O,K2O小于Na2O,属钙碱性次铝质,为壳幔混源岛弧花岗岩,与研究区的早石炭世大哈拉军山组钙碱性岛弧火山岩共同构成了岛弧火成岩组合;而阔尔库序列SiO2质量分数平均为70.99%,贫CaO而富Na2O和K2O,碱值明显高于赛肯都鲁序列,K2O大于 Na2O,属碱性弱过铝质,为壳源后造山花岗岩,与晚石炭世—早二叠世大陆裂谷碱性双峰式火山岩共同构成了板内裂谷火成岩组合。岩石化学特征为这一岩基的解体提供了有力的证据。

Abstract:: The Kuoerku batholith in the Awulale of western Tianshan is disintegrated into two intrusive series, that is, the early Carboniferous Saikendulu series and the early Permian Kuoerku series. Petrochemistry study indicates that in Saikendulu series,the average SiO2content is 62. 81%,it is rich in CaO but poor in Na2O and K2O, the contents of K2O is less than the one of Na2O, showing the characters of calc-alkline, sub-aluminum derived from the mixing of mantle and crustal materials, and it constitutes island-arc igneous association together with the calc-alkline island-arc igneous rock of the early Carboniferous Dahalajunshan Formation. However, in the Kuoerku series,the average SiO2content is 70. 99%, it is poor in CaO but rich in Na2O and K2O, the contents of Na2O and K2O are distinctly higher than those in the Saikendulu series, the contents of K2O is more than the one of Na2O, showing the characters of alkaline and over-aluminum and post-orogenic granite derived from crust, and it constitutes intraplate rift igneous association together with alkline bimodal igneous rock of the later Carboniferous to early Permian in terrestrial rift. The characteristics of petrochemistry provides evidence for the disintegration of the Kuoerku batholith.

参考文献/References:

[1] 李锦轶 , 王克卓 , 李亚萍 , 等 .天山山脉地貌特征、地壳组成与地质演化[J] .地质通报 , 2006 , 25(8):895-909 .
[2] 张国伟 , 李三忠 , 刘俊霞 , 等 .新疆伊犁盆地的构造特征与形成演化[J] .地学前缘 , 1999 , 6(4):203-214 .
[3] 张良臣 , 吴乃元 .天山地质构造及演化史[J] .新疆地质 , 1985 , 3(3):1-14 .
[4] 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 .
[5] 成守德 , 王广瑞 , 杨树德 , 等 .新疆古板块构造[J] .新疆地质 , 1986 , 4(2):1-26 .
[6] 陈哲夫 , 梁云海 .新疆多旋回构造与板块运动[J] .新疆地质 , 1991 , 9(2):95-107 .
[7] 邵铁全 , 石莹 , 靳红 , 等 .新疆西天山大哈拉军山组火山岩岩石化学特征及地质意义[J] .新疆地质 , 2006 , 24(3): 218-222 .
[8] 李注苍 , 李永军 , 李景宏 , 等 .西天山阿吾拉勒一带大哈拉军山组火山岩地球化学特征及构造环境分析[J] .新疆地质 , 2006 , 24(2):120-124 .
[9] 朱永峰 , 周晶 , 宋彪 , 等 .新疆大哈拉军山组火山岩的形成时代问题及其解体方案[J] .中国地质 , 2006 , 33(3): 487-497 .
[10] 崔尚森, 吴文奎, 姜常义, 等 .阿吾拉勒山区中石炭统含矿地层的沉积环境分析[J] .西安地质学院学报 ,1997 ,19(1):1-6 .
[11] 高永利 , 李永军 , 孔德义 , 等 .西天山阿吾拉勒一带阿克沙克组的厘定[J] .新疆地质 , 2006 , 24(3):215-218 .
[12] 姜常义 , 吴文奎 , 张学仁 , 等 .从岛弧向裂谷的变迁 ———来自阿吾拉勒地区火山岩的证据[J] .岩石矿物学杂志 , 1995 , 14 (4):294-295 .
[13] 刘静 , 李永军 , 王小刚 , 等 .西天山阿吾拉勒一带伊什基里克组火山岩地球化学特征及其构造环境[J] .新疆地质 , 2006 , 24(2):105-108 .
[14] 李永军 , 杨高学 , 郭文杰 , 等 .西天山阿吾拉勒阔尔库岩基的解体及地质意义[J] .新疆地质 , 2007, 25(3):233-236 .
[15] 新疆地质矿产局区调队 .天山花岗岩地质[M] .北京 :地质出版社 , 1985 .
[16] 中国科学院贵阳地球化学研究所 .华南花岗岩的地球化学 [M] .北京 :科学出版社 , 1979 .
[17] De La Roche, Leteeei er H , Grande Claude J P , et al.A Classi ficat ion of Volcanic and Plut onic Rock s Using R1-R 2 Di agrams and Major El ement Analyses :It s Relation ships and C urrent Nomem clature[J] .Chem Geol , 1980 , 29 :183- 210 .
[18] 肖庆辉 , 邓晋福 , 马大铨 , 等 .花岗岩研究思维与方法[M] .北京 :地质出版社 , 2002 .
[19] 高秉章 , 洪大为 , 郑基俭 , 等 .花岗岩类区 1 ∶5 万区域地质填图方法指南[M] .武汉 :中国地质大学出版社 , 1991 .
[20] M aniar P D , Piccoli P M .Tect onic Discriminati on of Grani toids[ J] .Geol S oc Am Bull , 1989 , 101 :635-643 .
[21] 李锁成 , 李永军 , 李金宝 , 等 .天水坪道花岗岩体的地球化学特征及构造环境[J] .地球科学与环境学报 , 2005 , 27(5):33- 37 .
[22] 李永军 , 杨高学 , 庞振甲 , 等 .天水渭北地区变质花岗岩类岩石学特征及其地质时代[J] .地球科学与环境学报 , 2007 , 29(1):6-10 .
[23] 李注苍 , 李永军 , 曾俊杰 .西秦岭糜署岭岩浆混合花岗岩的地球化学特征及构造意义[J] .地球科学与环境学报 , 2005 , 27 (2):12-16 .
[24] 李永军 , 李注苍 , 丁仨平 , 等 .西秦岭温泉花岗岩体岩石学特征岩浆混合标志[J] .地球科学与环境学报 , 2004 , 26(3): 7-12 .

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备注/Memo

备注/Memo:: 收稿日期:2007-10-20
基金项目:新疆维吾尔自治区区域地质矿产调查项目(XJQDW-2003-07)
作者简介:杨高学(1980-),男,宁夏固原人,从事构造地质学研究。E-mail:mllllmygxxgy@126.com

更新日期/Last Update: 2008-06-20

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