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  • 1
    Keywords: arc migration ; plate margins ; tectonic processes
    Description / Table of Contents: Chapter 1: Intermittent Formation, Sedimentation and Deformation History of Cenozoic Forearc Basins along the Northwestern Pacific Margins as an Indicator of Tectonic Scenarios by Osamu Takano --- Chapter 2: Cretaceous Research: Paleolatitudes and Northward Migration of Crustal Fragments in the NW Pacific Inferred from Paleomagnetic Studies by Yasuto Itoh and Reishi Takashima --- Chapter 3: Stratigraphic and Petrological Insights into the Late Jurassic– Early Cretaceous Tectonic Framework of the Northwest Pacific Margin by Reishi Takashima, Hiroshi Nishi and Takeyoshi Yoshida --- Chapter 4: Cretaceous Research: A New Constraint on the Paleostress Regime of Southwest Japan Based on Microfabric Analysis of a Granitic Pluton by Yasuto Itoh --- Chapter 5: Tectonic Synthesis: A Plate Reconstruction Model of the NW Pacific Region Since 100 Ma by Yasuto Itoh, Osamu Takano and Reishi Takashima
    Pages: Online-Ressource (120 Seiten)
    ISBN: 9789535132226
    Language: English
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  • 2
    Keywords: sedimentary basin formation ; earth and planetary sciences
    Description / Table of Contents: This book is devoted to the mechanisms of sedimentary basin formation on active plate margins, which show enormous diversity reflecting complex tectonic processes. Multidisciplinary approach pursuing basin-forming mechanism is based on geology, sedimentology, geochronology and geophysics. Some chapters are dedicated to the genetic analysis of sedimentary basins in wrench deformation zones in forearc and intra-arc regions. Another block of chapters deals with basin formation in peripheral regions of Eurasia and intra-arc / foreland basins under the influence of the fluctuation of stress regimes. Finally geophysical approaches to basin analyses are shown in some chapters from microscopic to regional scales. Diverse contents of the chapters provide the audience with the present accomplishments of basin researches on active margins by Earth scientists.
    Pages: Online-Ressource (304 Seiten)
    ISBN: 9789535111931
    Language: English
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  • 3
    Keywords: margins ; boundaries ; plate convergence
    Description / Table of Contents: Chapter 1: Deposition and Deformation of Modern Accretionary-Type Forearc Basins: Linking Basin Formation and Accretionary Wedge Growth by Atsushi Noda and Ayumu Miyakawa --- Chapter 2: Cenozoic Fault Zone Activity and Geologic Evolution of the Offshore Regions of Fukushima and Miyagi Prefectures, Northeastern Japan, Based on Petroleum Exploration Data by Hiroyuki Arato --- Chapter 3: Three-Dimensional Architecture of the Median Tectonic Line in Southwest Japan Based on Detailed Reflection Seismic and Drilling Surveys by Yasuto Itoh, Tomotaka Iwata and Keiji Takemura --- Chapter 4: Inconsistent Structure and Motion of the Eastern Median Tectonic Line, Southwest Japan, during the Quaternary by Shigekazu Kusumoto, Keiji Takemura and Yasuto Itoh --- Chapter 5: Fission Track Thermochronology of Late Cretaceous Sandstones of the Izumi Group Adjacent to the Median Tectonic Line Active Fault System in Southwest Japan by Yasuto Itoh, Paul F. Green, Keiji Takemura and Tomotaka Iwata --- Chapter 6: Alteration Reaction and Mass Transfer via Fluids with Progress of Fracturing along the Median Tectonic Line, Mie Prefecture, Southwest Japan by Yumi Kaneko, Toru Takeshita, Yuto Watanabe, Norio Shigematsu and Ko-Ichiro Fujimoto --- Chapter 7: Structural Features Along the Median Tectonic Line in Southwest Japan: An Example of Multiphase Deformation on an Arc-Bisecting Fault by Yasuto Itoh and Tomotaka Iwata --- Chapter 8: Paleomagnetic Studies on Miocene Sequences of Hokutan and Tottori Groups in Southwest Japan: Implications for Middle Miocene Rotational Movement of Southwest Japan Block Associated with the Japan Sea Opening by Naoto Ishikawa, Takashi Suzuki and Shiro Ishida --- Chapter 9: Oki-Dozen Dike Swarm: Effect of the Regional Stress Field on Volcano-Tectonic Orientations by Daisuke Miura, Kiyoshi Toshida, Ken-ichi Arai, Takeshi Wachi and Yutaka Wada --- Chapter 10: Effectiveness for Determination of Depositional Age by Detrital Zircon U–Pb Age in the Cretaceous Shimanto Accretionary Complex of Japan by Tetsuya Tokiwa, Makoto Takeuchi, Yusuke Shimura, Kazuho Shobu, Akari Ota, Koshi Yamamoto and Hiroshi Mori
    Pages: Online-Ressource (240 Seiten)
    ISBN: 9789535132882
    Language: English
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  • 4
    Electronic Resource
    Electronic Resource
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 13 (2004), S. 0 
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract  The late Pleistocene Kamitakara Pyroclastic Flow Deposit (KPFD) and its correlative Kasamori (Ks22) Tephra in central Japan are found to preserve stable thermoremanent magnetization (TRM) and detrital remanent magnetization (DRM), respectively. Untilted site-mean declinations of the KPFD are characterized by a fairly large scatter with easterly deflection, while those of the Ks22 show significantly smaller deflections. Because northerly paleomagnetic directions consistently characterize shallow marine sediments intercalating the Ks22 layer, the directional discordance is not attributed to different acquisition timing between TRM and DRM, but is probably due to a recent tectonic rotation  in  central  Japan.  Large scatter in TRM  declinations of the KPFD implies that a number of right-lateral active faults around the depositional area of the pyroclastic flow raised differential rotation of crustal blocks in central Japan, even during the late Pleistocene.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 12 (2003), S. 0 
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract  This paper provides untilted paleomagnetic data obtained from the early Miocene strata around the Kanazawa-Iozen area, in the eastern part of south-west Japan. A thick pile of volcaniclastics and marine transgressive sediments underlie the area; they were deposited in the early stage of the Japan Sea opening event. Progressive thermal demagnetization tests isolated stable primary magnetic vectors from eight sites in the upper part of the Iozen Formation. Overall, the tilt-corrected mean direction of this unit is D = 36.4°, I = 51.6° and α95 = 12.1. Together with a published paleomagnetic and chronological database, the present results suggest that clockwise rotation of south-west Japan, linked to the back-arc opening, commenced in the early Miocene and accelerated at the same time as rapid subsidence along the Japan Sea coast. Post-opening, differential rotation within the eastern part of south-west Japan is assumed, based on selected paleomagnetic data from the latest Early Miocene.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Melbourne, Australia : Blackwell Science Pty
    The @island arc 8 (1999), S. 0 
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Cenozoic basin-forming processes in northwestern Kyushu were studied on the basis of geological and geophysical data. Gravity anomaly analysis delineated four sedimentary basins in the study area: Goto-nada, Nishisonogi, Amakusa-nada, and Shimabara. Borehole stratigraphy and reflection seismic interpretation suggest that the Goto-nada Basin was subdivided into the Paleogene and Plio-Pleistocene depocenters (Goto-nada 1 and 2). In the Paleogene, Amakusa-nada Basin was rapidly subsiding together with the Shimabara Basin as part of a large graben. Goto-nada 1 and Nishisonogi basins belonged to another depositional area. After stagnant subsidence stage in the early Miocene, the study area became a site of basaltic activity (since 10 Ma) and vigorous subsidence in the Plio-Pleistocene. Goto-nada 2 Basin is accompanied with numerous east–west active faults, and separated from the Amakusa-nada Basin by a northeast– southwest basement high, Nomo Ridge. Plio-Pleistocene subsidence of the Amakusa-nada Basin is related with low-angle normal faulting on the eastern flank of the Nomo Ridge. Shimabara Basin is a composite volcano-tectonic depression which is studded by east–west faults. Focal mechanism on active faults suggests transtensional stress regime in the study area.
    Type of Medium: Electronic Resource
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