Peridotites with back-arc basin affinity exposed at the southwestern tip of the Mariana forearc
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- 資料種別
- 記事
- 著者・編者
- Shoma OyaKatsuyoshi MichibayashiYasuhiko Ohara
- 出版年月日等
- 2022-03-29
- 出版年（W3CDTF）
- 2022-03-29
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 9(18)
- 掲載巻
- 9(18)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-022-00476-5
- 国立国会図書館永続的識別子
- info:ndljp/pid/12307829
- 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）
- 2022-07-11T20:40:38+09:00
- 保存日（W3CDTF）
- 2022-07-11
- 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
- 図書館・個人送信対象外
- 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/12307811
- 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
- コレクション : 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
- DOI
- 10.1186/s40645-022-00476-5
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報（URI）
- 参照
- Legacy of mantle fabrics preserved within heavily serpentinized peridotites in Hole BA3A cores of the Oman Drilling ProjectStructural evolution of the Horoman peridotite complex in conjunction with the formation of the Hidaka Metamorphic Belt, HokkaidoTextural and chemical variations in peridotite induced by hydrous melt migration in mantle under the back-arc spreadingEffects of mineral mode and textural variation on the seismic anisotropy in lithospheric mantle: an example from Horoman peridotites
- 参照
- The effect of dynamic recrystallization on olivine fabric and seismic anisotropy: Insight from a ductile shear zone, Oman ophioliteShearing within lower crust during progressive retrogression: structural analysis of gabbroic rocks from the Godzilla Megamullion, an oceanic core complex in the Parece Vela backarc basinAmphibolitization within the lower crust in the termination area of the Godzilla Megamullion, Parece Vela backarc basinVariable microstructure of peridotite samples from the southern Mariana Trench: evidence of a complex tectonic evolutionTermination of backarc spreading: Zircon dating of a giant oceanic core complexMelt–fluid infiltration along detachment shear zones in oceanic core complexes: Insights from amphiboles in gabbro mylonites from the Godzilla Megamullion, Parece Vela Basin, the Philippine SeaMelt stagnation in peridotites from the Godzilla Megamullion Oceanic Core Complex, Parece Vela Basin, Philippine SeaDevelopment of shape and lattice preferred orientations: application to the seismic anisotropy of the lower crustOceanic transform fault seismicity and slip mode influenced by seawater infiltrationThe timescales of subduction initiation and subsequent evolution of an oceanic island arcThe Godzilla Megamullion, the largest oceanic core complex on the earth: a historical reviewPetrology and Mineralogy of Mantle Peridotites from the Southern MarianasNatural olivine crystal-fabrics in the western Pacific convergence region: A new method to identify fabric typePeridotites from a ductile shear zone within back‐arc lithospheric mantle, southern Mariana Trench: Results of a <i>Shinkai 6500</i> diveMechanisms of preferred orientations of olivine in tectonite peridotiteCentral role of detachment faults in accretion of slow-spreading oceanic lithospherePeridotites from the southern Mariana forearc: Heterogeneous fluid supply in mantle wedgeGeochemistry and K/Ar ages of volcanics dredged in the Philippine Sea (Mariana, Yap, and Palau trenches and Parece Vela basin)Migrating shoshonitic magmatism tracks Izu–Bonin–Mariana intra-oceanic arc rift propagationRheological properties of the detachment shear zone of an oceanic core complex inferred by plagioclase flow law: Godzilla Megamullion, Parece Vela back-arc basin, Philippine SeaGeodynamic implications of crustal lithologies from the southeast Mariana forearcGlimpses of oceanic lithosphere of the Challenger Deep forearc segment in the southernmost Marianas: The 143°E transect, 5800–4200 mDiffuse spreading, a newly recognized mode of crustal accretion in the southern Mariana Trough backarc basinWhy is the Challenger Deep so deep?Geodynamic evolution of a forearc rift in the southernmost <scp>M</scp>ariana <scp>A</scp>rcCalculating anisotropic physical properties from texture data using the MTEX open-source packageHeterogeneity in texture and crystal fabric of intensely hydrated ultramylonitic peridotites along a transform fault, Southwest Indian RidgeDeformation and hydrothermal metamorphism of gabbroic rocks within the Godzilla Megamullion, Parece Vela Basin, Philippine SeaFore‐arc basalts and subduction initiation in the Izu‐Bonin‐Mariana systemThe effect of a hydrous phase on P‐wave velocity anisotropy within a detachment shear zone in the slow‐spreading oceanic crust: A case study from the Godzilla Megamullion, Philippine SeaRelicts of deformed lithospheric mantle within serpentinites and weathered peridotites from the Godzilla Megamullion, Parece Vela Back‐arc Basin, Philippine SeaWhat Lies Beneath: The Formation and Evolution of Oceanic LithosphereCrustal Accretion in a Slow Spreading Back‐Arc Basin: Insights From the Mado Megamullion Oceanic Core Complex in the Shikoku BasinA New Scenario of the Parece Vela Basin GenesisEffect of water and stress on the lattice-preferred orientation of olivinePeridotites and volcanics from the Yap arc system: implications for tectonics of the southern Philippine Sea PlateFormation of harzburgite by pervasive melt/rock reaction in the upper mantleGeochemistry of peridotites from the Yap Trench, Western Pacific: implications for subduction zone mantle evolutionChemistry and origin of trapped melts in ophioiitic peridotitesThe composition of the EarthOxygen thermobarometry of abyssal spinel peridotites; the redox state and C-O-H volatile composition of the Earth's sub-oceanic upper mantlePeridotites and gabbros from the Parece Vela backarc basin: Unique tectonic window in an extinct backarc spreading ridgeMorphology and origin of the Challenger Deep in the Southern Mariana TrenchStructures of Ophiolites and Dynamics of Oceanic LithospherePeridotites from the Mariana Trough: first look at the mantle beneath an active back-arc basinGabbroic and ultramafic rocks from the Mariana Trench: An island arc ophioliteThe redox state of subduction zones: insights from arc-peridotitesMetamorphic rocks of the Yap arc-trench systemMelt Segregation and Strain Partitioning: Implications for Seismic Anisotropy and Mantle FlowMulti-stage melt–rock interaction in the Mt. Maggiore (Corsica, France) ophiolitic peridotites: microstructural and geochemical evidencePrediction of crystal–melt partition coefficients from elastic moduliGiant Megamullion in the Parece Vela Backarc BasinFeedback between melt percolation and deformation in an exhumed lithosphere–asthenosphere boundaryAbundances of the elements: Meteoritic and solarOrigin and tectonic evolution of the Caroline Ridge and the Sorol Trough, western tropical Pacific, from admittance and a tectonic modeling analysisThe Role of Pre-existing Mechanical Anisotropy on Shear Zone Development within Oceanic Mantle Lithosphere: an Example from the Oman OphioliteDeformation, static recrystallization, and reactive melt transport in shallow subcontinental mantle xenoliths (Tok Cenozoic volcanic field, SE Siberia)Thin crust as evidence for depleted mantle supporting the Marion RiseMechanisms of flow in naturally and experimentally deformed peridotitesChromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavasOrogenic, Ophiolitic, and Abyssal PeridotitesViscoplastic self‐consistent and equilibrium‐based modeling of olivine lattice preferred orientations: Implications for the upper mantle seismic anisotropyHigh pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantleThe geology of the southern Mariana fore-arc crust: Implications for the scale of Eocene volcanism in the western PacificMegamullions and mullion structure defining oceanic metamorphic core complexes on the Mid‐Atlantic RidgeMelt/peridotite interaction in the Southern Lanzo peridotite: Field, textural and geochemical evidenceCharacterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretationThe anatomy and ontogeny of modern intra-oceanic arc systemsLife cycle of oceanic core complexesUpper mantle tectonics: three-dimensional deformation, olivine crystallographic fabrics and seismic propertiesCoupled major and trace elements as indicators of the extent of melting in mid-ocean-ridge peridotitesLattice preferred orientation of olivine aggregates deformed in simple shearThe petrological significance of misorientations between grainsThe Lherz spinel lherzolite: Refertilized rather than pristine mantleExperimental cpx/melt partitioning of 24 trace elementsThe Seismic anisotropy of the Earth's mantle: From single crystal to polycrystalOxygen fugacity of basaltic magmas and the role of gas‐forming elementsSpatial and temporal evolution of the subducting Pacific plate structure along the western Pacific marginNature and distribution of slab‐derived fluids and mantle sources beneath the Southeast Mariana forearc riftThe Atlantis Bank Gabbro Massif, Southwest Indian RidgeGeochemical characteristics of back-arc basin lower crust and upper mantle at final spreading stage of Shikoku Basin : an example of Mado Megamullion
- 参照（URI）
- 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
- 雑誌記事索引データベースCrossref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CrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 12307829