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  1. F300 宇宙地球環境研究所
  2. F300a 雑誌掲載論文
  3. 学術雑誌

Significance of an amorphous SiO2 phase in a pseudomorph after coesite enclosed in garnet from ultrahigh-pressure eclogite, Su-Lu Belt, eastern China

http://hdl.handle.net/2237/00029105
http://hdl.handle.net/2237/00029105
b99fada6-9b9b-4dad-8058-ceddf04201e0
名前 / ファイル ライセンス アクション
Taguchi_et_al_2018JMG.pdf Taguchi_et_al_2018JMG (5.3 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2018-12-12
タイトル
タイトル Significance of an amorphous SiO2 phase in a pseudomorph after coesite enclosed in garnet from ultrahigh-pressure eclogite, Su-Lu Belt, eastern China
言語 en
著者 Taguchi, Tomoki

× Taguchi, Tomoki

WEKO 88154

en Taguchi, Tomoki

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Miyake, Akira

× Miyake, Akira

WEKO 88155

en Miyake, Akira

Search repository
Enami, Masaki

× Enami, Masaki

WEKO 88156

en Enami, Masaki

Search repository
Igami, Yohei

× Igami, Yohei

WEKO 88157

en Igami, Yohei

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
言語 en
権利情報 This is the peer reviewed version of the following article: [Taguchi T, Miyake A, Enami M, Igami Y. Significance of an amorphous SiO2 phase in a pseudomorph after coesite enclosed in garnet from ultrahigh‐pressure eclogite, Su–Lu Belt, eastern China. J Metamorph Geol. 2018;36:843–854. https://doi.org/10.1111/jmg.12315], which has been published in final form at [https://doi.org/10.1111/jmg.12315]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions.
キーワード
主題Scheme Other
主題 amorphous SiO2 phase
キーワード
主題Scheme Other
主題 metamorphic fluid
キーワード
主題Scheme Other
主題 pseudomorph after coesite
キーワード
主題Scheme Other
主題 Su–Lu Belt
キーワード
主題Scheme Other
主題 TEM observation
抄録
内容記述 Here, we report the first discovery of an amorphous SiO2 phase (APSI phase) in a pseudomorph after coesite included in garnet from an ultrahigh‐pressure (UHP) eclogite from the Su–Lu metamorphic belt, eastern China. Using transmission electron microscopy, Raman spectroscopy and selected area electron diffraction, we show that the internal structure of the pseudomorph consists of an APSI phase with nano/submicrocrystalline particles of quartz and a polycrystalline K‐bearing fibrous sheet‐silicate phase (KFSS phase). The APSI phase‐bearing aggregates included in the garnet might have formed by reactions involving a supercritical fluid during exhumation by the following processes: (1) the development of radial cracks within the host garnet by the phase transition of coesite to quartz; (2) the decomposition of a part of the pseudomorph following infiltration of supercritical fluid; (3) the precipitation of the KFSS phase from the fluid phase during subsequent exhumation and cooling, which was likely promoted by a change in the metamorphic fluid from supercritical and/or subcritical to aqueous fluid; and (4) the rapid precipitation of the APSI phase under a metastable (non‐equilibrium) state, such as quenching, during a later stage of the exhumation. Whether the APSI phase generally formed during exhumation and survived widely throughout the Su‐Lu terrane is unknown. However, the presence of the APSI phase in a UHP eclogite provides new insight into the geodynamic phenomena occurring at continental collision zones.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 ファイル公開:2019-09-01
言語 ja
内容記述タイプ Other
出版者
言語 en
出版者 Wiley
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1111/jmg.12315
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0263-4929
ISSN(Online)
収録物識別子タイプ EISSN
収録物識別子 1525-1314
書誌情報 en : Journal of Metamorphic Geology

巻 36, 号 7, p. 843-854, 発行日 2018-09
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