Distribution, morphology, and morphometry of circular mounds in the elongated basin of northern Terra Sirenum, Mars

• 資料種別: 記事
• タイトル: Distribution, morphology, and morphometry of circular mounds in the elongated basin of northern Terra Sirenum, Mars
• 著者・編者: Ryodo Hemmi; Hideaki Miyamoto
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2017-09-11
• 出版年（W3CDTF）: 2017-09-11
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 4(26)
• 掲載巻: 4(26)
• 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/s40645-017-0141-x; https://doi.org/10.1186/s40645-017-0141-x
• 国立国会図書館永続的識別子: info:ndljp/pid/10980293; https://dl.ndl.go.jp/pid/10980293
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• 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; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2017-10-30T20:11:03+09:00
• 保存日（W3CDTF）: 2017-10-27
• 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（URI）: https://progearthplanetsci.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/10369577; https://dl.ndl.go.jp/pid/10369577
• 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; https://dl.ndl.go.jp

• 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/s40645-017-0141-x; https://doi.org/10.1186/s40645-017-0141-x
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/10980293; https://dl.ndl.go.jp/pid/10980293; http://link.springer.com/article/10.1186/s40645-017-0141-x/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40645-017-0141-x.pdf
• 参照: High-Resolution Topographic Analyses of Mounds in Southern Acidalia Planitia, Mars: Implications for Possible Mud Volcanism in Submarine and Subaerial Environments; https://cir.nii.ac.jp/crid/1360848664417599616; 「泥火山」定義，概念，成因，および最近の研究動向; https://cir.nii.ac.jp/crid/1390003825175620864; 世界の海底泥火山の分布と山体形態に関する一考察; https://cir.nii.ac.jp/crid/1390848250105755264; Morphology and Morphometry of Sub-kilometer Craters on the Nearside of Phobos and Implications for Regolith Properties; https://cir.nii.ac.jp/crid/1390848250126052096; Cold-based glaciation of Pavonis Mons, Mars : evidence for moraine deposition during glacial advance; https://cir.nii.ac.jp/crid/2050870367070986880
• 参照: Assessment of pingo distribution and morphometry using an IfSAR derived digital surface model, western Arctic Coastal Plain, Northern Alaska; https://cir.nii.ac.jp/crid/1360001114173830784; Formation and evolution of the chaotic terrains by subsidence and magmatism: Hydraotes Chaos, Mars; https://cir.nii.ac.jp/crid/1360011144675032320; An assessment of evidence for pingos on Mars using HiRISE; https://cir.nii.ac.jp/crid/1360011144951617664; Possible pingo fields in the Utopia basin, Mars: Geological and climatical implications; https://cir.nii.ac.jp/crid/1360011146275531904; Unique characteristics of cones in Central Elysium Planitia, Mars; https://cir.nii.ac.jp/crid/1360011146613124224; Morphometry of scoria cones located on a volcano flank: A case study from Mt. Etna (Italy), based on high-resolution LiDAR data; https://cir.nii.ac.jp/crid/1360292618750490880; Mud volcanoes in the geologic record of Mars: The case of Firsoff crater; https://cir.nii.ac.jp/crid/1360292621519571072; Worldwide distribution of submarine mud volcanoes and associated gas hydrates; https://cir.nii.ac.jp/crid/1360574092887925888; Mud volcanoes: Indicators of stress orientation and tectonic controls; https://cir.nii.ac.jp/crid/1360574092889482496; Classification of mud volcanoes in the South Caspian Basin, offshore Azerbaijan; https://cir.nii.ac.jp/crid/1360574092893602048; The relation of catastrophic flooding of Mangala Valles, Mars, to faulting of Memnonia Fossae and Tharsis Volcanism; https://cir.nii.ac.jp/crid/1360574093526311936; Martian cratering 8: Isochron refinement and the chronology of Mars; https://cir.nii.ac.jp/crid/1360574094112091776; Standard techniques for presentation and analysis of crater size-frequency data; https://cir.nii.ac.jp/crid/1360574095772574464; Episodic massive mud eruptions from submarine mud volcanoes examined through topographical signatures; https://cir.nii.ac.jp/crid/1360846639279833216; The Thermal Emission Imaging System (THEMIS) for the Mars 2001 Odyssey Mission; https://cir.nii.ac.jp/crid/1360855567868736256; SIGNIFICANCE OF MUD VOLCANISM; https://cir.nii.ac.jp/crid/1360855567868740992; The spatial, temporal and volumetric analysis of a large mud volcano province within the Eastern Mediterranean; https://cir.nii.ac.jp/crid/1360855569447692032; Ultrahigh resolution topographic mapping of Mars with MRO HiRISE stereo images: Meter‐scale slopes of candidate Phoenix landing sites; https://cir.nii.ac.jp/crid/1360855569889157248; The Evolution of the Martian Hydrosphere: Implications for the Fate of a Primordial Ocean and the Current State of the Northern Plains; https://cir.nii.ac.jp/crid/1361137045459910144; Numerical modelling of mud volcanoes and their flows using constraints from the Gulf of Cadiz; https://cir.nii.ac.jp/crid/1361418519947757312; Northern lowlands of Mars: Evidence for widespread volcanic flooding and tectonic deformation in the Hesperian Period; https://cir.nii.ac.jp/crid/1361418519957212288; Map-projection-independent crater size-frequency determination in GIS environments—New software tool for ArcGIS; https://cir.nii.ac.jp/crid/1361418520944619904; Mars Orbiter Laser Altimeter: Experiment summary after the first year of global mapping of Mars; https://cir.nii.ac.jp/crid/1361699993420207872; An automated, open-source pipeline for mass production of digital elevation models (DEMs) from very-high-resolution commercial stereo satellite imagery; https://cir.nii.ac.jp/crid/1361699995699745792; Mars/Moon Cratering Rate Ratio Estimates; https://cir.nii.ac.jp/crid/1361699995767548416; Tharsis‐radial graben systems as the surface manifestation of plume‐related dike intrusion complexes: Models and implications; https://cir.nii.ac.jp/crid/1361699996315902464; Pingos of the Tuktoyaktuk Peninsula Area, Northwest Territories; https://cir.nii.ac.jp/crid/1361981469370684672; Morphologic evidence of subsurface sediment mobilization and mud volcanism in Candor and Coprates Chasmata, Valles Marineris, Mars; https://cir.nii.ac.jp/crid/1361981470024369920; Cratering Chronology and the Evolution of Mars; https://cir.nii.ac.jp/crid/1361981471101477760; Crater-based dating of geological units on Mars: Methods and application for the new global geological map; https://cir.nii.ac.jp/crid/1362262945440059520; Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE); https://cir.nii.ac.jp/crid/1362262945730178432; Distribution and formation of chlorides and phyllosilicates in Terra Sirenum, Mars; https://cir.nii.ac.jp/crid/1362544418602992000; A quaternary monogenetic volcanic field in the Xalapa region, eastern Trans-Mexican volcanic belt: Geology, distribution and morphology of the volcanic vents; https://cir.nii.ac.jp/crid/1362825894148048768; Geologic map of the northern plains of Mars; https://cir.nii.ac.jp/crid/1362825894803320576; Possible Frost Mounds in an Ancient Martian Lake Bed; https://cir.nii.ac.jp/crid/1362825896245498240; Scoria cones on Mars: Detailed investigation of morphometry based on high‐resolution digital elevation models; https://cir.nii.ac.jp/crid/1363107370916709760; Icelandic pseudocraters as analogs to some volcanic cones on Mars; https://cir.nii.ac.jp/crid/1363388844837652608; Fault geometries on Uranus’ satellite Miranda: Implications for internal structure and heat flow; https://cir.nii.ac.jp/crid/1363388845313867264; Context Camera Investigation on board the Mars Reconnaissance Orbiter; https://cir.nii.ac.jp/crid/1363670318472153856; Columbus crater and other possible groundwater-fed paleolakes of Terra Sirenum, Mars; https://cir.nii.ac.jp/crid/1363670319386958080; Mars: Review and analysis of volcanic eruption theory and relationships to observed landforms; https://cir.nii.ac.jp/crid/1363670319777386624; Evidence for pervasive mud volcanism in Acidalia Planitia, Mars; https://cir.nii.ac.jp/crid/1363951794420220032; Pitted cones and domes on Mars: Observations in Acidalia Planitia and Cydonia Mensae using MOC, THEMIS, and TES data; https://cir.nii.ac.jp/crid/1363951794524030592; Ancient hydrothermal seafloor deposits in Eridania basin on Mars; https://cir.nii.ac.jp/crid/1363951794815506304; Planetary surface dating from crater size–frequency distribution measurements: Partial resurfacing events and statistical age uncertainty; https://cir.nii.ac.jp/crid/1363951795043365760; Hydrovolcanic tuff rings and cones as indicators for phreatomagmatic explosive eruptions on Mars; https://cir.nii.ac.jp/crid/1363951796136657280; Geochemical Consequences of Widespread Clay Mineral Formation in Mars’ Ancient Crust; https://cir.nii.ac.jp/crid/1364233268408659200; Mesoscale raised rim depressions (MRRDs) on Earth: A review of the characteristics, processes, and spatial distributions of analogs for Mars; https://cir.nii.ac.jp/crid/1364233269985505792; 北海道南部の泥火山の構造的特徴と活動履歴; https://cir.nii.ac.jp/crid/1390282681215063040
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja