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首页> 外文期刊>Journal of the Geological Society >Understanding K-feldspar 40Ar/39Ar data: reconciling models, methods and microtextures
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Understanding K-feldspar 40Ar/39Ar data: reconciling models, methods and microtextures

机译:了解钾长石40Ar / 39Ar数据:协调模型,方法和微观纹理

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摘要

Several descriptions of argon diffusion in K-feldspar have been developed, including the quantitative multiple-diffusion-domain (MDD) and multipath models and the qualitative ‘recrystallization’ model. These models remain contentious and the natural range in behaviour remains poorly understood. Feldspars from the Klokken syenite intrusion show a systematic relationship between 40Ar/39Ar age and microtexture suggesting that the loss of argon from different feldspars operates via different mechanisms such that the existing models represent only end-member scenarios. The MDD model can yield reliable thermal history information only for feldspars with pristine microtexture, with this model best viewed as a cipher for the real (but unknown) domain structure in such samples.
机译:已经开发了对氩在长石中扩散的几种描述,包括定量多扩散域 (MDD)模型和多径模型以及定性的“重结晶” 模型。这些模型仍然存在争议,行为的自然范围 仍然知之甚少。 Klokken 堇青石侵入岩的长石表明 40 Ar / 39 Ar 年龄与微观纹理之间的系统关系表明来自不同长石的 损失氩气的机制不同,因此现有模型 仅代表最终成员场景。对于具有原始微纹理的长石, MDD模型只能产生可靠的热历史信息, 该模型最好将 视为真实的密码(但未知)域结构 (在此类示例中。

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  • 来源
    《Journal of the Geological Society》 |2007年第5期|941-944|共4页
  • 作者单位

    Research School of Earth Sciences, Australian National University, Acton, ACT 0200, Australia|School of Earth Sciences, University of Melbourne, Melbourne, Vic. 3010, Australia (e-mail: mclarens@unimelb.edu.au);

    Research School of Earth Sciences, Australian National University, Acton, ACT 0200, Australia;

    School of Earth Sciences, University of Melbourne, Melbourne, Vic. 3010, Australia (e-mail: mclarens@unimelb.edu.au);

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