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": "99dc5369-ab75-413c-8f20-be501eecb822"}, "_deposit": {"id": "4233", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4233"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004233", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2012-08"}, "bibliographicPageEnd": "139", "bibliographicPageStart": "128", "bibliographicVolumeNumber": "320", "bibliographic_titles": [{"bibliographic_title": "CHEMICAL GEOLOGY", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Helium (He-3/He-4), argon (Ar-40/Ar-36) and oxygen (O-18/O-16) isotopic ratios in fluid inclusions trapped in quartz and pyrite from the Sunshin epithermal gold-silver ore deposits in South Korea were analyzed to investigate the magmatic contribution to ore forming fluids. Mantle helium with high He-3/He-4 ratios (up to He-3/He-4 similar to 9R(A), where R-A = 1.4 x 10(-6) for air) were identified from fluid inclusions in auriferous quartz veins, which are characterized as low sulfidation (adularia-sericite) type. The ratios provide direct evidence of links between low sulfidation ore fluids in epithermal gold deposits and magma from a mantle source. Interestingly, the oxygen and hydrogen isotopic compositions of the ore fluids (delta O-18= - 1.9 to - 6.6%., delta D = - 82 to - 100%.), calculated from ore quartz, indicate that meteoric waters were predominant during precipitation of the Au-Ag ore. Microthermometric measurements for fluid inclusions indicate relatively low temperatures (\u0026lt;= 300 degrees C) for the formation of the low sulfidation epithermal ore deposits. (C) 2012 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.chemgeo.2012.05.027"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0009-2541", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Kyu Han Kim", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Seungyeol Lee", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Keisuke Nagao", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Hirochika Sumino", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Kyounghee Yang", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Jong Ik Lee", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4233", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4233", "relation": {}, "relation_version_is_last": true, "title": ["He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea"], "weko_shared_id": -1}
  1. 防災科研関係論文

He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea

https://nied-repo.bosai.go.jp/records/4233
https://nied-repo.bosai.go.jp/records/4233
d109b1b7-6fd8-499b-856c-6fa2a9c83213
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea
言語
言語 eng
著者 Kyu Han Kim

× Kyu Han Kim

en Kyu Han Kim

Search repository
Seungyeol Lee

× Seungyeol Lee

en Seungyeol Lee

Search repository
Keisuke Nagao

× Keisuke Nagao

en Keisuke Nagao

Search repository
Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

Search repository
Kyounghee Yang

× Kyounghee Yang

en Kyounghee Yang

Search repository
Jong Ik Lee

× Jong Ik Lee

en Jong Ik Lee

Search repository
抄録
内容記述タイプ Other
内容記述 Helium (He-3/He-4), argon (Ar-40/Ar-36) and oxygen (O-18/O-16) isotopic ratios in fluid inclusions trapped in quartz and pyrite from the Sunshin epithermal gold-silver ore deposits in South Korea were analyzed to investigate the magmatic contribution to ore forming fluids. Mantle helium with high He-3/He-4 ratios (up to He-3/He-4 similar to 9R(A), where R-A = 1.4 x 10(-6) for air) were identified from fluid inclusions in auriferous quartz veins, which are characterized as low sulfidation (adularia-sericite) type. The ratios provide direct evidence of links between low sulfidation ore fluids in epithermal gold deposits and magma from a mantle source. Interestingly, the oxygen and hydrogen isotopic compositions of the ore fluids (delta O-18= - 1.9 to - 6.6%., delta D = - 82 to - 100%.), calculated from ore quartz, indicate that meteoric waters were predominant during precipitation of the Au-Ag ore. Microthermometric measurements for fluid inclusions indicate relatively low temperatures (<= 300 degrees C) for the formation of the low sulfidation epithermal ore deposits. (C) 2012 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : CHEMICAL GEOLOGY

巻 320, p. 128-139
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 0009-2541
DOI
関連識別子 10.1016/j.chemgeo.2012.05.027
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:48:12.739052
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