从潘拥枕状玄武岩的40Ar/39Ar年龄论金沙江缝合带和甘孜—理塘缝合带的演化关系
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40Ar/39Ar Age of the Panyong Pillow Basalt: Implication for the Evolution Relationship between the Jinshajiang and GarzeLitang Suture Zones
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  • 中国地质科学院矿产资源研究所,北京,100037    
  • 中国地质科学院矿产资源研究所,北京,100038    
  • Institute of Mineral Resource,Chinese Academy of Geological Sciences,Beijing, 100037    
  • Institute of Mineral Resource,Chinese Academy of Geological Sciences,Beijing, 100037    
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    摘要:

    金沙江缝合带东侧白松至潘拥一带沿NNE向断续分布着若干基性火山岩。本文对潘拥枕状玄武岩开展了岩石地球化学研究和40Ar/39Ar定年,发现这些基性火山岩是由弱富集的MORB型地幔经过约15%的部分熔融形成的。用逐级加热法测得斜长石斑晶的40Ar/39Ar坪年龄为231.6±6.7 Ma,它们代表了晚三叠世早期中咱微陆块内的一个局限性洋盆。该洋盆的形成既是金沙江洋盆向西持续俯冲的结果,同时又是甘孜—理塘洋盆向西俯冲形成义敦古岛弧的原因。

    Abstract:

    A lot of basic volcanic rocks occur discontinuously in a NNEstriking zone from Baisong to Panyong to the east of the Jinshajiang suture zone. Based on petrogeo chemical study and 40Ar/39Ar dating of the Panyong pillow basalts,the paper points out that these basic volcanic rocks formed from about 15% partial melting of a weakly enriched MORBtype mantle.Using a stepbystep evaporation technique the authors obtained an 40Ar/39Ar plateau age of 231.6±6.7Ma from plagioclase porphyrocrysts. The pillow basalts represented a local ocean basin within the Zhongza micro continental block during the early stage of the Late Triassic.Its formation was both the result of the lasting subduction toward the west of the Jinshajiang ocean basin and the westward subduction of the GarzeLitang ocean basin, which led to formation of the Yidun arc belt.

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曲晓明,侯增谦.从潘拥枕状玄武岩的40Ar/39Ar年龄论金沙江缝合带和甘孜—理塘缝合带的演化关系[J].地质论评,():115-121,[DOI].
QU Xiaoming, HOU Zengqian.40Ar/39Ar Age of the Panyong Pillow Basalt: Implication for the Evolution Relationship between the Jinshajiang and GarzeLitang Suture Zones[J]. Geological Review,():115-121.

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