当サイトでは、より良いサービスを提供するため、クッキーを利用しています。クッキーの使用に同意いただける場合は「同意」ボタンをクリックし、クッキーポリシーについては「詳細を見る」をクリックしてください。詳しくは当サイトの サイトポリシー をご確認ください。

詳細を見る...
ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To

Field does not validate



インデックスリンク

インデックスツリー

  • RootNode

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "ce22d1a2-bdfc-4c9d-8821-5a25a7fe5a50"}, "_deposit": {"id": "4263", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4263"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004263", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2010-05"}, "bibliographicIssueNumber": "1-2", "bibliographicPageEnd": "172", "bibliographicPageStart": "163", "bibliographicVolumeNumber": "294", "bibliographic_titles": [{"bibliographic_title": "EARTH AND PLANETARY SCIENCE LETTERS", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Here we show how the Higashi-akaishi peridotite body in the Sanbagawa metamorphic belt, a sliver of the former mantle wedge of the eastern Eurasian plate margin, has exhumed subduction fluid noble gases and halogens with a marine pore-fluid signature from a depth of 100 km. Previous work has only considered that water subduction into the mantle wedge occurs via decomposition of hydrated minerals in altered oceanic crust and sediment. The striking similarities of the observed noble gas and halogen compositions with marine pore fluids require subduction and closed system retention of marine pore fluid to at least 100 km. The Higashi-akaishi peridotites appear to have frozen-in and preserved a previously unseen part of the deep water recycling process, requiring a reassessment of the dominant transport mechanism and source of water in subduction zones. Indeed, a small proportion of marine pore fluid, preserved in the downgoing hydrous peridotite, can account for the dominant heavy noble gas isotopic and elemental composition observed in the convecting mantle. (C) 2010 Elsevier B.V. All rights reserved.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "ELSEVIER SCIENCE BV", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1016/j.epsl.2010.03.029"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0012-821X", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Hirochika Sumino", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Ray Burgess", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tomoyuki Mizukami", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Simon R. Wallis", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Greg Holland", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Chris J. Ballentine", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4263", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4263", "relation": {}, "relation_version_is_last": true, "title": ["Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite"], "weko_shared_id": -1}
  1. 防災科研関係論文

Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite

https://nied-repo.bosai.go.jp/records/4263
https://nied-repo.bosai.go.jp/records/4263
227e415f-e429-4912-b1ef-6d1c0bfab3f6
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Seawater-derived noble gases and halogens preserved in exhumed mantle wedge peridotite
言語
言語 eng
著者 Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

Search repository
Ray Burgess

× Ray Burgess

en Ray Burgess

Search repository
Tomoyuki Mizukami

× Tomoyuki Mizukami

en Tomoyuki Mizukami

Search repository
Simon R. Wallis

× Simon R. Wallis

en Simon R. Wallis

Search repository
Greg Holland

× Greg Holland

en Greg Holland

Search repository
Chris J. Ballentine

× Chris J. Ballentine

en Chris J. Ballentine

Search repository
抄録
内容記述タイプ Other
内容記述 Here we show how the Higashi-akaishi peridotite body in the Sanbagawa metamorphic belt, a sliver of the former mantle wedge of the eastern Eurasian plate margin, has exhumed subduction fluid noble gases and halogens with a marine pore-fluid signature from a depth of 100 km. Previous work has only considered that water subduction into the mantle wedge occurs via decomposition of hydrated minerals in altered oceanic crust and sediment. The striking similarities of the observed noble gas and halogen compositions with marine pore fluids require subduction and closed system retention of marine pore fluid to at least 100 km. The Higashi-akaishi peridotites appear to have frozen-in and preserved a previously unseen part of the deep water recycling process, requiring a reassessment of the dominant transport mechanism and source of water in subduction zones. Indeed, a small proportion of marine pore fluid, preserved in the downgoing hydrous peridotite, can account for the dominant heavy noble gas isotopic and elemental composition observed in the convecting mantle. (C) 2010 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : EARTH AND PLANETARY SCIENCE LETTERS

巻 294, 号 1-2, p. 163-172
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ ISSN
収録物識別子 0012-821X
DOI
関連識別子 10.1016/j.epsl.2010.03.029
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:49:01.530956
Show All versions

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3

Change consent settings


Powered by WEKO3

Change consent settings