A new method for the empirical conversion of logging data to clay mineral fraction in the Nankai accretionary prism
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- Material Type
- 記事
- Author/Editor
- Suguru YabeRina FukuchiYohei Hamada
- Publication, Distribution, etc.
- Publication Date
- 2020-10-31
- Publication Date (W3CDTF)
- 2020-10-31
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 72(166)
- Volume
- 72(166)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-020-01303-1
- Persistent ID (NDL)
- info:ndljp/pid/11616251
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2021-01-13T14:13:05+09:00
- Date Captured (W3CDTF)
- 2021-01-13
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/11467692
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- 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/s40623-020-01303-110.21203/rs.3.rs-57479/v110.21203/rs.3.rs-57479/v2
- Related Material (URI)
- Is Referenced By
- Multiple Types of Porosity – P‐Wave Velocity Relationships for the Nankai Trough
- References
- Dynamic weakening of smectite‐bearing faults at intermediate velocities: Implications for subduction zone earthquakesMid-Quaternary decoupling of sediment routing in the Nankai Forearc revealed by provenance analysis of turbiditic sandsStructure of the Nankai Trough Accretionary Zone from multichannel seismic reflection dataThe origin of strata within the inner accretionary prism of Nankai Trough: Evidence from clay mineral assemblages along the NanTroSEIZE transectSite C0018Expedition 314 summaryDepositional architecture, provenance, and tectonic/eustatic modulation of Miocene submarine fans in the Shikoku Basin: Results from <b>Nankai Trough Seismogenic Zone Experiment</b>Crustal velocity field of southwest Japan: Subduction and arc‐arc collisionSite C0011Expedition 315 Site C0001MethodsSite C0022Data report: clay mineral assemblages in the Shikoku Basin, NanTroSEIZE subduction inputs, IODP Sites C0011 and C0012Release of mineral-bound water prior to subduction tied to shallow seismogenic slip off SumatraGeneric Mapping Tools: Improved Version ReleasedEvolution of tectono-sedimentary systems in the Kumano Basin, Nankai Trough forearcGeologically current plate motionsOrigin of a zone of anomalously high porosity in the subduction inputs to Nankai TroughSediment provenance and controls on slip propagation: Lessons learned from the 2011 Tohoku and other great earthquakes of the subducting northwest Pacific plateExpedition 314 Site C0001Data report: clay mineral assemblages and illite/smectite diagenesis in cuttings from Hole C0002P, IODP Expedition 348, Nankai Trough accretionary prismSpatial and temporal evolution of the megasplay fault in the Nankai TroughMaking and breaking an island arc: A new perspective from the Oligocene Kyushu‐Palau arc, Philippine SeaThe Philippine Sea: New survey results reveal the structure and the history of the marginal basinsAn expression of Philippine Sea plate rotation: the Parece Vela and Shikoku BasinsClay-mineral assemblages across the Nankai-Shikoku subduction system, offshore Japan: A synthesis of results from the NanTroSEIZE projectNanTroSEIZE: The IODP Nankai Trough Seismogenic Zone ExperimentZircon and apatite thermochronology of the Nankai Trough accretionary prism and trench, Japan: Sediment transport in an active and collisional margin settingDeformation and fluid pressure variation during initiation and evolution of the plate boundary décollement zone in the Nankai accretionary prismExpedition 315 Site C0002Site C0011Data report: clay mineral assemblages from the Nankai Trough accretionary prism and the Kumano Basin, IODP Expeditions 315 and 316, NanTroSEIZE Stage 1Expedition 316 Site C0004Heat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, JapanSite C0024Data report: clay mineral assemblages in the upper Shikoku Basin, results from IODP Expedition 333, Sites C0011 and C0012Site C0012Site C0009Expedition 316 Site C0006Expedition 314 Site C0002Site C0012Data report: clay mineral assemblages in cuttings from Hole C0002F, IODP Expedition 338, upper Nankai Trough accretionary prismSite C0012Data report: clay mineral assemblages in slope basin sediments and mass-transport deposits at Sites C0018 and C0021, IODP Expeditions 333 and 338Site C0010Site C0002Transition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zoneMethodsSite C0018Site C0021Expedition 314 Site C0004On the mechanical role of smectite in subduction zonesExpedition 315 methodsMechanisms of sediment accretion in the Middle America Trench off MexicoExpedition 314 Site C0006Expedition 316 Site C0007Expedition 314 methodsExpedition 358 summaryUse of spectral gamma-ray data to refine subsurface fluvial stratigraphy: late Cretaceous strata in the Book Cliffs, Utah, USASite C0002Site C0002Data report: clay mineral assemblages and illite/smectite diagenesis in cuttings from Hole C0002P, IODP Expedition 348, Nankai Trough accretionary prismSite C0010Evolution of the Shikoku Basin.Origin and evolution of a splay fault in the Nankai accretionary wedgeSimultaneous estimation of in situ porosity and thermal structure from core sample measurements and resistivity log data at Nankai accretionary prismFrictional properties of incoming pelagic sediments at the Japan Trench : implications for large slip at a shallow plate boundary during the 2011 Tohoku earthquakeRe-evaluation of temperature at the updip limit of locked portion of Nankai megasplay inferred from IODP Site C0002 temperature observatoryDistribution and depth of bottom-simulating reflectors in the Nankai subduction marginPunctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossrefCrossrefCrossref科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11616251