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西藏改则洞错地区白垩纪火山岩锆石U-Pb年代学、Hf同位素组成及对班公-怒江洋俯冲闭合的制约
付佳俊; 丁林; 许强; 蔡福龙; 岳雅慧; 郭钰
Source Publication地质科学
2015
Pages182-202
Abstract班公湖—怒江缝合带是青藏高原内一条重要的缝合带,其俯冲极性和闭合时限一直存在着争议,这无疑限制了我们对青藏高原演化历史的认识。本文对仲岗安山玄武岩和一套新发现的晚白垩世安山岩进行研究,获得了其锆石U-Pb年龄分别为123.75±0.92 Ma和74.23±0.76 Ma。仲岗安山玄武岩锆石的ε_(Hf)(t)值为-7.3~+4.4,具有岛弧玄武岩特征,指示班公湖—怒江洋盆在该地区仍然继续向北俯冲;晚白垩世安山岩锆石的ε_(Hf)(t)值为+3.1~+11.1,其可能是亏损地幔混熔了部分的陆壳物质而形成的,且不整合在蛇绿岩之上。结合区域资料本文认为班公湖—怒江洋盆在改则地区的闭合时限在100~7...
Keyword班公湖—怒江缝合带 西藏改则 白垩纪火山岩 U-pb年代学 Hf同位素
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7104
Collection图书馆
Recommended Citation
GB/T 7714
付佳俊,丁林,许强,等. 西藏改则洞错地区白垩纪火山岩锆石U-Pb年代学、Hf同位素组成及对班公-怒江洋俯冲闭合的制约[J]. 地质科学,2015:182-202.
APA 付佳俊,丁林,许强,蔡福龙,岳雅慧,&郭钰.(2015).西藏改则洞错地区白垩纪火山岩锆石U-Pb年代学、Hf同位素组成及对班公-怒江洋俯冲闭合的制约.地质科学,182-202.
MLA 付佳俊,et al."西藏改则洞错地区白垩纪火山岩锆石U-Pb年代学、Hf同位素组成及对班公-怒江洋俯冲闭合的制约".地质科学 (2015):182-202.
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