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": "6194867e-cb58-43d7-b380-9489e3bfe0c1"}, "_deposit": {"id": "4748", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4748"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004748", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1986", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "397", "bibliographicPageStart": "371", "bibliographicVolumeNumber": "86", "bibliographic_titles": [{"bibliographic_title": "Geophysical Journal of the Royal Astronomical Society", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Summary. Seismic refraction profiles were shot across the Kurile Trench, south‐east of Hokkaido, Japan. The experiment in a typical island arc‐trench system, where the Pacific Plate subducts beneath Hokkaido, was designed to investigate the transition of crustal structure from oceanic basin to continental slope across the trench. High resolution data were obtained from a 9 litre airgun and multi‐OBS system. They were processed through a series of operations: digitization, filtering, slant stacking, t‐sum inversion, two‐dimensional ray tracing, and comparison with synthetic seismograms. A typical oceanic structure composed of an unconsolidated sedimentary layer (P wavespeed of 1.8?2.2 kms?1, thickness of 0.5?1 km), layer 2 (3.1?5.8 kms?1, 1?2 km) with a large wavespeed gradient, and relatively homogeneous layer 3 (6.0?6.8 kms?1, 5 km) is found on the oceanic side of the trench. Observations of shear waves converted at the boundary between the sedimentary layer and layer 2 gave compressional to shear wavespeed ratios of about 7.0 for the topmost sedimentary layer and 1.73?1.77 for layers 2 and 3. The transition of structure occurs slightly landward of the trench axis and thick low wavespeed materials (P wavespeed of 2.5?4.7 km s?1) persist beneath the continental slope. The density profile derived from our wavespeed structure is consistent with published free‐air gravity anomaly data. The general crustal structure in the southern part of the Kurile Trench is similar to that of the Japan Trench off Sanriku. However, the distribution of the thick low wavespeed materials on the continent side differs between the two trench regions. These materials are more abundant in the Kurile Trench region, as is also inferred from the gravity anomaly pattern. The variability of the gravity anomaly on the continental side along the trench axis suggests that the distribution of these materials changes even within a single trench system. The seismic activity inferred from S?P time distribution at each OBS is high near the trench, and low in the oceanic basin beyond about 30 km from the trench axis as well as on the continental side where thick low wavespeed materials exist. An activity which seems to occur exactly in the narrow transition zone dividing the typical oceanic crust and the thick low wavespeed materials in the continental side structure is found. Copyright c 1986, Wiley Blackwell. All rights reserved", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1111/j.1365-246X.1986.tb03833.x"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1365-246X", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Azusa Nishizawa", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Kiyoshi Suyehiro", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Crustal structure across the Kurile Trench off south‐eastern Hokkaido by airgun‐OBS profiling", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Crustal structure across the Kurile Trench off south‐eastern Hokkaido by airgun‐OBS profiling", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4748", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4748", "relation": {}, "relation_version_is_last": true, "title": ["Crustal structure across the Kurile Trench off south‐eastern Hokkaido by airgun‐OBS profiling"], "weko_shared_id": -1}
  1. 防災科研関係論文

Crustal structure across the Kurile Trench off south‐eastern Hokkaido by airgun‐OBS profiling

https://nied-repo.bosai.go.jp/records/4748
https://nied-repo.bosai.go.jp/records/4748
5be3a26c-fee8-486b-b3c0-07e39de3901d
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Crustal structure across the Kurile Trench off south‐eastern Hokkaido by airgun‐OBS profiling
言語
言語 eng
著者 Azusa Nishizawa

× Azusa Nishizawa

en Azusa Nishizawa

Search repository
Kiyoshi Suyehiro

× Kiyoshi Suyehiro

en Kiyoshi Suyehiro

Search repository
抄録
内容記述タイプ Other
内容記述 Summary. Seismic refraction profiles were shot across the Kurile Trench, south‐east of Hokkaido, Japan. The experiment in a typical island arc‐trench system, where the Pacific Plate subducts beneath Hokkaido, was designed to investigate the transition of crustal structure from oceanic basin to continental slope across the trench. High resolution data were obtained from a 9 litre airgun and multi‐OBS system. They were processed through a series of operations: digitization, filtering, slant stacking, t‐sum inversion, two‐dimensional ray tracing, and comparison with synthetic seismograms. A typical oceanic structure composed of an unconsolidated sedimentary layer (P wavespeed of 1.8?2.2 kms?1, thickness of 0.5?1 km), layer 2 (3.1?5.8 kms?1, 1?2 km) with a large wavespeed gradient, and relatively homogeneous layer 3 (6.0?6.8 kms?1, 5 km) is found on the oceanic side of the trench. Observations of shear waves converted at the boundary between the sedimentary layer and layer 2 gave compressional to shear wavespeed ratios of about 7.0 for the topmost sedimentary layer and 1.73?1.77 for layers 2 and 3. The transition of structure occurs slightly landward of the trench axis and thick low wavespeed materials (P wavespeed of 2.5?4.7 km s?1) persist beneath the continental slope. The density profile derived from our wavespeed structure is consistent with published free‐air gravity anomaly data. The general crustal structure in the southern part of the Kurile Trench is similar to that of the Japan Trench off Sanriku. However, the distribution of the thick low wavespeed materials on the continent side differs between the two trench regions. These materials are more abundant in the Kurile Trench region, as is also inferred from the gravity anomaly pattern. The variability of the gravity anomaly on the continental side along the trench axis suggests that the distribution of these materials changes even within a single trench system. The seismic activity inferred from S?P time distribution at each OBS is high near the trench, and low in the oceanic basin beyond about 30 km from the trench axis as well as on the continental side where thick low wavespeed materials exist. An activity which seems to occur exactly in the narrow transition zone dividing the typical oceanic crust and the thick low wavespeed materials in the continental side structure is found. Copyright c 1986, Wiley Blackwell. All rights reserved
言語 en
書誌情報 en : Geophysical Journal of the Royal Astronomical Society

巻 86, 号 2, p. 371-397, 発行日 1986
ISSN
収録物識別子タイプ ISSN
収録物識別子 1365-246X
DOI
関連識別子 10.1111/j.1365-246X.1986.tb03833.x
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 02:02:24.059050
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