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青藏高原东南缘哀牢山构造带泥质高压麻粒岩的发现及其构造意义
引用本文:戚学祥,赵宇浩,朱路华,李志群.青藏高原东南缘哀牢山构造带泥质高压麻粒岩的发现及其构造意义[J].岩石学报,2012,28(6):1846-1856.
作者姓名:戚学祥  赵宇浩  朱路华  李志群
作者单位:1. 大陆构造与动力学国家重点实验室,中国地质科学院院地质研究所,北京100037
2. 广东省有色地质勘察局地质勘察研究院,广州,510080
3. 云南有色地质局,昆明,650051
基金项目:本文受中国地质调查局项目(1212011121266)和科技部深部探测技术与实验研究专项(SinoProbe-05-03)联合资助.
摘    要:哀牢山构造带泥质高压麻粒岩主要由石榴石、夕线石、钾长石和斜长石变斑晶及尖晶石、铁假蓝宝石、蓝晶石、石英、金红石和钛铁矿包裹体组成,为确定印支地块和华南地块的边界提供了关键性标志。石榴石-黑云母-斜长石-石英地质温压计(GBPQ)计算结果及标志性高温矿物组合(Spl+Qz)表明泥质高压麻粒岩的形成和演化经历了高压/高温进变质到中温/低压退变质的顺时针P-T演化过程。其中:1)高压/高温进变质阶段的矿物组合为Ky+Sil+Grt1+Kf1+Pl1+Spr+Ter(Kf+Pl)+Bt1+Spl+Qtz+Ilm1+Rut1,形成于850~919℃,≥10.4kbar;2)中温/低压退变质阶段的矿物组合为Grt2+Bt2+Pl2+Ms+Qtz+Ilm2+Rut2,早期和晚期的温压条件分别为664~754℃,4.9~6.5kbar和572~576℃,3.5~3.9kbar。反映陆壳物质在碰撞过程中俯冲到地下深处(≥30km)经高压高温变质后快速折返到中上地壳的动力学演变轨迹。

关 键 词:泥质高压麻粒岩  高压/高温变质作用  大陆碰撞  哀牢山构造带
收稿时间:1/5/2012 12:00:00 AM
修稿时间:2012/4/27 0:00:00

Discovery of high-pressure pelitic granulite in Ailaoshan orogenic belt, southeastern Tibet, and its tectonic implications
QI XueXiang,ZHAO YuHao,ZHU LuHua and LI ZhiQun.Discovery of high-pressure pelitic granulite in Ailaoshan orogenic belt, southeastern Tibet, and its tectonic implications[J].Acta Petrologica Sinica,2012,28(6):1846-1856.
Authors:QI XueXiang  ZHAO YuHao  ZHU LuHua and LI ZhiQun
Institution:State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;State Key Laboratory of Continental Tectonics and Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;Geological Survey Institute of Guangzhou Bureau of Nonferrous Geology, Guangzhou 510080, China;Yunnan Bureau of Nonferrous Geology, Kunming 650051, China
Abstract:High-pressure pelitic granulite containing porphyroblasts of garnet(Grt),sillimanite(Sil),K-feldspar(Kf) and plagioclase(Pl),and inclusions of spinel(Spl),kyanite(Ky),sapphirine(Spr) and rutile(Rut) have been found from the Ailaoshan orogenic belt,southeastern Tibet,regarded as a key indicator for identification of the boundary between the Indochina and South China blocks.The temperatures and pressures calculated by garnet-biotite-plagioclase-quartz geothermobarometery and hightemperature equilibrium spinel + quartz assemblage show the formation and evolution of the graunlite had experienced clockwise P-T path from high-pressure/-temperature to mid-temperature and low-pressure metamorphism.That are:1) the high-pressure/-temperature metamorphism(HP/HT) is characterized by an assemblage of Ky + Sil + Grt1 + Kf1 + Pl1 + Spr + Ter(Kf + Pl) + Bt1 + Spl + Qtz + Ilm1 + Rut1,and the peak P-T conditions of ≥ 10.4kbar at 850 ~ 919℃;2) the mid-temperature and low-pressure retrogressive metamorphism characterized by an assemblage of Grt2 + Bt2 + Pl2 + Ms + Qtz + Ilm2 + Rut2,and two stage P-T conditions of 4.9 ~ 6.5kbar at 664 ~ 754℃ and 3.5 ~ 3.9kbar at 572 ~ 576℃ respectively.The dynamic metamorphic path was that the metapelitic rock experienced high-pressure/-temperature granulite-facies metamorphism in lower continental crust(≥30km) exhumated to mid-upper crust rapidly,it might be related to the continental collision and underthrusting between the Indochina and South China blocks,and exhumation and slip shearing lately.
Keywords:High-pressure pelitic granulite  High-pressure/-temperature metamorphism  Continental collision  Ailaoshan orogenic belt
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