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  1. B100 理学部/理学研究科
  2. B100b 紀要
  3. The Journal of earth and planetary sciences
  4. 49

Autoclastic subvolcanic rocks in the Tonglu basin, Zhejiang Province, China : a description of "pearlitic border" textures in an adamellite porphyry

https://doi.org/10.18999/joueps.49.31
https://doi.org/10.18999/joueps.49.31
fb3527fa-99c8-473c-b231-a8b31371fb4e
名前 / ファイル ライセンス アクション
KJ00000703141.pdf KJ00000703141.pdf (2.2 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2006-01-05
タイトル
タイトル Autoclastic subvolcanic rocks in the Tonglu basin, Zhejiang Province, China : a description of "pearlitic border" textures in an adamellite porphyry
言語 en
著者 ZEN, Ja Hu

× ZEN, Ja Hu

WEKO 3374

en ZEN, Ja Hu

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SUWA, Kanenori

× SUWA, Kanenori

WEKO 3375

en SUWA, Kanenori

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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
抄録
内容記述 Autoclastic rocks are produced in a shallow-level subvolcanic setting by cryptoexplosive activity. In many localities around southeastern China, autoclastic subvolcanic rocks were formed between the late Jurassic and the early Cretaceous. In the Tonglu volcanic basin, three comagmatic stages of volcanic rock have been exposed by deep denudation. First stage rocks consist of rhyolites and rhyodacites and are distributed along the margins of the basin. Third stage hypabyssal intrusions consist of aegirine-riebeckite bearing quartz monzonitic porphyry, and occupy the central basin. Between these stages, autoclastic adamellite porphyry occurs, a subvolcanic rock with porphyritic texture. Autoclastic adamellite porphyry contains "pearlitic" overgrowths around orthoclase phenocryst. The overgrowths contain quartz intergrown with orthoclase that is optically continuous with the host phenocrysts. Pearlitic overgrowths also occur around porphyritic plagioclase, quartz and hornblende. Overgrowths around plagioclase contain mostly plagioclase or orthoclase, with lesser quartz. Overgrowths around quartz phenocrysts are predominantly quartz, with lesser amounts of orthoclase. Overgrowths around hornblende phenocrysts are mostly composed of hornblende with lesser quartz and orthoclase. In general, the pearlitic overgrowths have compositions that are intermediate between the phenocrysts and the groundmass. The overgrowths may therefore represent reaction textures that developed in an autoclastic environment.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 国立情報学研究所で電子化したコンテンツを使用している。
言語 ja
内容記述タイプ Other
出版者
言語 en
出版者 Dept. of Earth and Planetary Sciences, Nagoya University
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.18999/joueps.49.31
ID登録タイプ JaLC
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0919875X
書誌情報 en : The Journal of earth and planetary sciences, Nagoya University

巻 49, p. 31-43, 発行日 2002
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/2855
識別子タイプ HDL
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