首页> 外文期刊>Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry >Reply to the comment by Zhang et al.on:'First finding of A-type and adakitic magmatism association in Songpan-Garze fold belt,eastern Tibetan Plateau:Implication for lithospheric delamination'
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Reply to the comment by Zhang et al.on:'First finding of A-type and adakitic magmatism association in Songpan-Garze fold belt,eastern Tibetan Plateau:Implication for lithospheric delamination'

机译:回应张等人的评论:“青藏高原东部松潘-甘孜褶皱带的A型和埃达克岩浆作用的首次发现:对岩石圈分层的影响”

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摘要

We greatly thank Zhang et al.(2008-this issue)for their comments on our recent paper(Zhang et al.,2007)regarding the tectonic setting of the Indosinian granitoids in the Songpan-Garze fold belt,as it gives us an opportunity to further clarify our viewpoints.The discrepancy between Zhang et al.(2008-this issue)and Zhang et al.(2007)is focused on the interpretation of the tectonic setting of the Indosinian A-type granite(211±1 Ma)and adakitic magmatism(216-221 Ma)in the Songpan-Garze fold belt.
机译:非常感谢Zhang等人(2008年本期)对我们最近发表的论文(Zhang等人,2007年)关于松潘-甘孜褶皱带中印支期花岗岩构造背景的评论,为我们提供了机会为了进一步阐明我们的观点,Zhang等人(2008年,本期)与Zhang等人(2007年)之间的差异主要在于对印度支那A型花岗岩(211±1 Ma)和松潘-甘孜褶皱带的岩石成岩作用(216-221 Ma)。

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