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中阿尔金南缘志留纪高压泥质片麻岩的发现及其构造地质意义
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  • 英文篇名:Discovery of the Silurian high-pressure pelitic gneiss in southern margin of middle Altyn and its tectonic geological significance
  • 作者:马拓 ; 刘良 ; 盖永升 ; 杨文强 ; 王超 ; 康磊 ; 廖小莹 ; PAK ; SangWan
  • 英文作者:MA Tuo;LIU Liang;GAI Yong Sheng;YANG Wen Qiang;WANG Chao;KANG Lei;LIAO Xiao Ying;PAK SangWan;State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University;
  • 关键词:高压泥质片麻岩 ; 志留纪变质时代 ; P-T-t演化轨迹 ; 中阿尔金南缘
  • 英文关键词:High-pressure pelitic gneiss;;Silurian metamorphism;;P-T-t path;;Southern margin of middle Altyn
  • 中文刊名:YSXB
  • 英文刊名:Acta Petrologica Sinica
  • 机构:大陆动力学国家重点实验室西北大学地质学系;
  • 出版日期:2019-06-15
  • 出版单位:岩石学报
  • 年:2019
  • 期:v.35
  • 基金:国家自然科学重点基金项目(41430209);; 国家重点基础研究发展计划项目(2015CB856103);; 国家自然科学群体和面上基金项目(41421002、41602052、41672187、41502051);; 陕西省教育厅自然科学基金项目(15JK1752);; 西北大学大陆动力学国家重点实验室自主研究重点课题联合资助
  • 语种:中文;
  • 页:YSXB201906010
  • 页数:19
  • CN:06
  • ISSN:11-1922/P
  • 分类号:204-222
摘要
在中阿尔金南缘西段尤努斯萨依北部原划长城系巴什库尔干岩群中首次发现一套高压泥质片麻岩。根据岩相学观察和矿物化学成分可识别出其四期矿物共生组合:早期为石榴子石+多硅白云母+单斜辉石(?)+斜长石+黑云母+石英+金红石+钛铁矿;第二期为石榴子石+蓝晶石+钾长石+斜长石+黑云母+石英+金红石+钛铁矿;第三期为石榴子石+夕线石+钾长石+斜长石+黑云母+石英+金红石+钛铁矿;晚期为石榴子石+夕线石+斜长石+黑云母+石英+钛铁矿。依据矿物内部一致性热力学数据,基于THERMOCALC 3. 40程序平台,计算出P-T视剖面图,并结合矿物等值线、矿物对温压计等计算,依次确定四期变质温压条件为15. 8~18. 3kbar/646~729℃、10. 30~12. 30kbar/781~821℃、8. 50~9. 60kbar/812~838℃和4. 65~5. 70kbar/698~725℃。上述四期变质阶段共同构成一个早期降压升温后降压降温的顺时针型演化的P-T轨迹,指示出与陆壳俯冲-折返相关的变质地质事件。利用LA-ICP-MS进行的锆石原位微区U-Pb定年和微量元素分析结果表明,该岩石记录了432. 0±2. 7Ma、401. 4±2. 5Ma和381. 1±2. 4Ma三期变质年龄,可能分别代表了该岩石早期高压、中期高压麻粒岩相-麻粒岩相和后期角闪岩相变质阶段的时代。该高压岩石出露于中阿尔金地块西段南缘长城系巴什库尔干岩群之中,与南侧以断裂带分隔的赋存于阿尔金岩群之中的南阿尔金高压-超高压岩石出露的构造位置明显不同,其峰期变质时代(~432Ma)亦明显不同于南阿尔金高压-超高压岩石的峰期变质时代(~500Ma)。因此,该高压岩石与南阿尔金高压-超高压岩石显然不能构成同一条变质岩带。结合区域地质背景和前人关于柴北缘陆壳属性高压-超高压岩石峰期变质时代(~430Ma)的研究成果综合分析,本文初步认为该高压岩石可能是柴北缘高压-超高压变质岩带的西延或是被中新生代以来阿尔金复杂多期次走滑断裂系迁移而就位于中阿尔金南缘的部分柴北缘高压-超高压变质岩片/岩块。
        The high-pressure pelitic gneiss is first discovered in the Bashikuergan Group at the northern part of Younusisayi,which located at the southern margin of the middle Altyn Tagh. Four stages of mineral assemblage were identified by petrographic observation and mineral composition,which are Grt + Cpx + Ph + Pl + Bi + Q + Ru + Ilm,Grt + Ky + Ksp + Pl + Bi + Q + Ru + Ilm,Grt + Sill + Ksp+ Pl + Bi + Q + Ru + Ilm and Grt + Sill + Ksp + Pl + Bi + Q + Ilm. The metamorphic conditions of these four stages were constrainted as15. 8 ~ 18. 3 kbar/646 ~ 729℃,10. 30 ~ 12. 30 kbar/781 ~ 821℃,8. 50 ~ 9. 60 kbar/812 ~ 838℃ and 4. 65 ~ 5. 70 kbar/698 ~ 725℃by equilibrium modeling accroding to the THERMOCALC 3. 40,indicated a clockwise P-T path. This character suggests a continental deep subduction-exhumation associated tectonic event. LA-ICP-MS U-Pb dating yelds the peak age of 432. 0 ± 2. 7 Ma,the HP granulite-granulite facies age of 401. 4 ± 2. 5 Ma,and the amphibolite facies age of 381. 1 ± 2. 4 Ma. The tectonic position of the highpressure politic gneiss exposed in the Bashikuergan Group at the southern margin of middle Altyn is obviously different from those HPUHP rocks occurring in the Altyn Group in South Altyn. And peak metamorphic age( ~ 432 Ma) was also significantly different from the HP-UHP rocks in South Altyn Tagh( ~ 500 Ma). Therefore,the high-pressure pelitic gneiss in this study should obviously not belong to the same metamorphic rocks belt with the South Altyn HP-UHP rocks. Combined with regional geological background and previous studies on peak metamorphic ages( ~ 430 Ma) of HP-UHP rocks with continental crust properties in the northern margin of Qaidam basin,we preliminarily suggest that the high-pressure rocks may be the western extension of the HP-UHP metamorphic belt in the northern margin of Qaidam basin,or a part of the HP-UHP rock blocks in the southern margin of Qaidam basin,migrated by the complex multi-stage strike-slip fault system since Meso-Cenozoic.
引文
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