First report of (U–Th)/He thermochronometric data across Northeast Japan Arc : implications for the long-term inelastic deformation
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- 資料種別
- 記事
- 著者・編者
- Shigeru SueokaTakahiro TagamiBarry P. Kohn
- 出版年月日等
- 2017-06-13
- 出版年（W3CDTF）
- 2017-06-13
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 69(79)
- 掲載巻
- 69(79)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-017-0661-z
- 国立国会図書館永続的識別子
- info:ndljp/pid/10369106
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2017-06-22T22:40:19+09:00
- 保存日（W3CDTF）
- 2017-06-22
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
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- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/10319651
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- (U–Th)/He thermochronometric analyses were performed across the southern part of the Northeast Japan Arc for reconstructing the long-term uplift and denudation history in the region. Apatite (U–Th–Sm)/He ages ranged from 64.3 to 1.5 Ma, while zircon (U–Th)/He ages ranged between 39.6 and 11.0 Ma. Apatite (U–Th–Sm)/He ages showed obvious contrast among the morphostructural provinces; older ages of 64.3–49.6 Ma were obtained in the Abukuma Mountains on the fore-arc side, whereas younger ages of 11.4–1.5 Ma were determined in the Ou Backbone Range (OBR) along the volcanic front and the Asahi Mountains on the back-arc side. The age contrasts are basically interpreted to reflect the differences in the uplift and the denudation histories of the provinces considering the thermal effects of magmatism and timing of the known uplift episodes. Denudation rates were calculated to be <0.1 mm/year in the Abukuma Mountains, ~0.1 to 1 mm/year in the Ou Backbone Range, and ~0.1 to 0.3 mm/year in the Asahi Mountains. The denudation rates tend to increase from the mountain base to the ridges in the OBR (and the Asahi Mountains). This relationship shows a contrast with the previous findings in fault-block mountains in the Southwest (SW) Japan Arc, where the highest denudation rates were estimated near fault(s) along the base(s). This observation might reflect a difference in mountain uplift mechanisms between the NE and the SW Japan Arcs and imply that thermochronometric approaches are useful for constraining uplift and denudation histories at the scale of an island arc, as well as continental orogens. However, careful discussion of magmatic thermal effects is required.
- DOI
- 10.1186/s40623-017-0661-z
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © The Author(s) 2017. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
- 関連情報（URI）
- 参照
- Crustal dynamics: unified understanding of geodynamic processes at different time and length scalesRapid Exhumation of Earth's Youngest Exposed Granites Driven by Subduction of an Oceanic Arc87Sr/86Sr Isotopic Ratio of Ferromanganese Crusts as a Record of Detrital Influx to the Western North Pacific OceanLow‐temperature thermochronological database of bedrock in the Japanese IslandsFirst report of geo- and thermochronological results from the Cordillera Central, Luzon, Philippines不均質レオロジー構造を考慮した島弧地殻における変形と応力場のモデル化フィッション・トラック法を利用した島弧山地の熱年代学低温領域の熱年代学の原理と地殻浅部のテクトニクスへの応用(U–Th)/He thermochronometric mapping across the northeast Japan Arc : towards understanding mountain building in an island-arc setting
- 参照
- Free software helps map and display dataNatural age dispersion arising from the analysis of broken crystals: Part II. Practical application to apatite (U–Th)/He thermochronometryThe influence of eroding topography on steady-state isotherms. Application to fission track analysisRifting and basin inversion in the eastern margin of the Japan SeaJapan Sea, opening history and mechanism: A synthesisDenudation history of the Kiso Range, central Japan, and its tectonic implications: Constraints from low‐temperature thermochronologyEvolution of late Cenozoic magmatism and the crust–mantle structure in the NE Japan ArcThe Fish Canyon Tuff: A new look at an old low-temperature thermochronology standardThe effects of long alpha-stopping distances on (U‐Th)/He agesQuantifying crustal extension and shortening in the back‐arc region of Northeast JapanHeterogeneous stress state of island arc crust in northeastern Japan affected by hot mantle fingersNew approach to resolve the amount of Quaternary uplift and associated denudation of the mountain ranges in the Japanese IslandsThe influence of natural radiation damage on helium diffusion kinetics in apatiteHot fingers in the mantle wedge: new insights into magma genesis in subduction zonesUSING THERMOCHRONOLOGY TO UNDERSTAND OROGENIC EROSIONHelium diffusion in natural zircon: Radiation damage, anisotropy, and the interpretation of zircon (U-Th)/He thermochronologyChemical influence on α-recoil damage annealing in apatite: Implications for (U–Th)/He datingUltra-high precision 40Ar/39Ar ages for Fish Canyon Tuff and Alder Creek Rhyolite sanidine: New dating standards required?Crustal Thermal Processes and the Interpretation of Thermochronometer DataNatural age dispersion arising from the analysis of broken crystals. Part I: Theoretical basis and implications for the apatite (U–Th)/He thermochronometerApatite (U–Th)/He thermochronometry using a radiation damage accumulation and annealing modelUplift of the Ou Backbone Range in Northeast Japan at around 10 Ma and its implication for the tectonic evolution of the eastern margin of AsiaVariability of apatite fission-track annealing kinetics; III, Extrapolation to geological time scalesCoseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquakeApatite (U–Th–Sm)/He thermochronology of rapidly cooled samples: The effect of He implantationFission-Track DatingQuantitative Constraints on the Rate of Landform Evolution Derived from Low-Temperature ThermochronologyThe relationship between Late Cenozoic tectonic events and stress field and basin development in northeast JapanHelium diffusion from apatite: General behavior as illustrated by Durango fluorapatiteSeeing is believing: Visualization of He distribution in zircon and implications for thermal history reconstruction on single crystalsFormation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central JapanClosure temperature in cooling geochronological and petrological systemsLate Cenozoic Tectonic Events and Intra-Arc Basin Development in Northeast JapanEffect of alpha-damage annealing on apatite (U–Th)/He thermochronologyQuantifying the effect of recent relief changes on age–elevation relationshipsApatite (U–Th)/He thermochronometry: methods and applications to problems in tectonic and surface processesPast, Present, and Future of ThermochronologyStrain buildup in the Northeast Japan orogen with implications for gigantic subduction earthquakesTime-dependent effects of heat advection and topography on cooling histories during erosionPaleomagnetic evidence for the Miocene counter-clockwise rotation of Northeast Japan—rifting process of the Japan arcU-Th zonation-dependent alpha-ejection in (U-Th)/He chronometryA precise 40Ar–39Ar reference age for the Durango apatite (U–Th)/He and fission-track dating standardActive forearc shortening in Tohoku, Japan: Constraints on fault geometry from erosion rates and fluvial longitudinal profilesCrustal structure and origin of the northeast Japan arcHelium chronometry of apatite and titanite using Nd-YAG laser heatingα-Emitting mineral inclusions in apatite, their effect on (U–Th)/He ages, and how to reduce it日本海の拡大と構造線朝日山地西縁の完新世海成段丘と地殻変動低温領域の熱年代学的手法に基づいた赤石山脈の隆起・削剥史の解明仙台平野南西部に露出する中部中新統‐鮮新統の年代データ：奥羽脊梁山地の隆起と関連して東北日本背弧側に産する鮮新統明神岩層の安山岩類の成因-AFCプロセス- : 主要・微量元素組成およびSr・Nd同位体組成からの制約北部本州背弧域の地殻構造と震源断層東北日本島弧−海溝系における長期的歪み蓄積過程と超巨大歪み解放イベントQuantitative determination of long-term erosion rates of weathered granitic soil surfaces in western Abukuma, Japan using cosmogenic 10Be and 26Al depth profile湿潤変動帯の地形学山形県新庄盆地西縁部の鮮新世古地理の変遷－出羽丘陵の隆起時期と隆起過程－Geochronological constraint on the brittle-plastic deformation along the Hatagawa Fault Zone, NE Japan
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 10369106
- NII論文ID
- 120006368167