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对《拉克希米盆地简单火山裂谷而非复杂俯冲起始的证据》的回复

Reply to 'Evidence for simple volcanic rifting not complex subduction initiation in the Laxmi Basin'.

作者信息

Pandey Dhananjai K, Pandey Anju, Whattam Scott A

机构信息

National Centre for Polar & Ocean Research, Ministry of Earth Sciences, Vasco da Gama, Goa, 403804, India.

H-V-3, NCPOR Campus, Vasco da Gama, Goa, 403804, India.

出版信息

Nat Commun. 2020 Jun 1;11(1):2734. doi: 10.1038/s41467-020-16570-5.

Abstract

Recently, Pandey et al. proposed relict subduction initiation occurred along a passive margin in the northwest Indian Ocean, however, Clift et al. questioned their evidence for subduction initiation, suggesting that simpler rifting-related processes could more simply explain the available data. Here, Pandey et al. reply to Clift et al.’s comment, and argue that geochemical and isotope data for Laxmi basin lavas distinctly imply relict subduction initiation.

摘要

最近,潘迪等人提出,残留俯冲作用起始于印度洋西北部的被动大陆边缘,然而,克利夫特等人对他们关于俯冲作用起始的证据提出质疑,认为更简单的与裂谷作用相关的过程能更简洁地解释现有数据。在此,潘迪等人回应了克利夫特等人的评论,并认为拉克希米盆地熔岩的地球化学和同位素数据明显暗示了残留俯冲作用的起始。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e90e/7264283/ee02e25a7de0/41467_2020_16570_Fig1_HTML.jpg

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