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Saturday, May 2, 2020 | History

1 edition of Izu-Ogasawara Bonin arc and trench investigations found in the catalog.

Izu-Ogasawara Bonin arc and trench investigations

Izu-Ogasawara Bonin arc and trench investigations

June and October-November 1974, GH 74-3 and -6 cruises

  • 184 Want to read
  • 17 Currently reading

Published by Geological Survey of Japan in Hisamoto .
Written in English

    Places:
  • Japan.,
  • Philippine Sea.
    • Subjects:
    • Island arcs -- Japan.,
    • Geology -- Philippine Sea.

    • Edition Notes

      Statementedited by Eiji Inoue.
      SeriesCruise report - Geological Survey of Japan ; no. 5, Cruise report ;, no. 5.
      ContributionsInoue, Eiji, 1922-
      Classifications
      LC ClassificationsQE511.2 .I94
      The Physical Object
      Pagination68 p. :
      Number of Pages68
      ID Numbers
      Open LibraryOL4632187M
      LC Control Number77463670

      Xu, X., H. You, K. Du and F. Han (). "An Archaeopteryx-like theropod from China and the origin of Avialae." Nature ():   Serpentinite Mud Volcanism: Observations, Processes, and Implications Serpentinite Mud Volcanism: Observations, Processes, and Implications Fryer, Patricia Large serpentinite mud volcanoes form on the overriding plate of the Mariana subduction zone. Fluids from the descending plate hydrate (serpentinize) the forearc mantle and enable serpentinite muds to rise along Author: Fryer, Patricia.

      oceanic trench in the western Pacific, consisting of the Izu Trench and the Bonin Trench. KAIREI KRE03 Cruise Data KRE Cruise Information. DOI. Data List. Related Cruises. Seismic study at the Izu-Ogasawara region: Proposal Title: Crustal growth of the Izu-Ogasawara oceanic island arc - Seismic study for IODP Project IBM - Cruise Track Enlarge Image. Ports of call.

      This banner text can have markup.. web; books; video; audio; software; images; Toggle navigation. Full text of "Subseafloor Biosphere Linked to Hydrothermal Systems [electronic resource]: TAIGA Concept" See other formats.


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Izu-Ogasawara Bonin arc and trench investigations Download PDF EPUB FB2

Izu-Ogasawara Bonin arc and trench investigations: June and October-NovemberGH and -6 cruises. The Izu–Bonin–Mariana (IBM) arc system is a tectonic-plate convergent IBM arc system extends over km south from Tokyo, Japan, to beyond Guam, and includes the Izu Islands, Bonin Islands, and Mariana Islands; much more of the IBM arc system is submerged below IBM arc system lies along the eastern margin of the Philippine Sea Plate in the Western Pacific Ocean.

Abstract. The Bonin Arc is a well-developed island arc, associated with a deep trench, an active volcanic chain, and a back-arc basin. The Bonin Arc is approximately km long, extending north—south from latitude 35°N to 25°N within longitude °E and °E, facing the Pacific plate in front and the Shikoku Basin behind (Fig.

1).Cited by: The Izu–Ogasawara (Bonin)–Mariana (IBM) Islands arc is located along the convergent boundary between the subducting Pacific plate (PA) and the overriding Philippine Sea plate (PS) in the western Pacific ().Many geological and geophysical studies have targeted the IBM arc as an example of an intraoceanic convergent margin (cf.

Stern et al., ).Cited by: Volcanic history of the back-arc region of the Izu-Bonin (Ogasawara) arc Article in Geological Society London Special Publications (1) January with 76 Reads How we measure 'reads'.

Izu-Ogasawara Trench - The Izu-Ogasawara Trench (伊豆・小笠原海溝, Izu-Ogasawara Kaikō), also known as Izu-Bonin Trench is an oceanic trench in the western Pacific Ocean. It stretches from Japan to the northernmost section of Mariana Trench.

The. Interestingly, the across-arc seismic profile revealed that the rift structure in the Izu-Bonin arc shares some common features, such as normal faults in the shallow crust and crustal thinning. A trench fan in the Izu Ogasawara Trench on the Boso Trench triple junction, Japan.

Mar. Geol., The Mogi Trench Fan, 18 km in diameter, is located in the km deep Izu Ogasawara Trench. Analysis of the morphology and internal structure of the Mogi Fan was based on kHz records, seismic reflection profiles and Seabeam by: 7.

The Japan Arc is considered to have developed through the collision and accretion of bathymetric highs (e.g., Taira, ); here, an ongoing continental growth process is observed.

The collision between the Ogasawara Plateau and the Izu–Ogasawara forearc causes shoaling of. These islands rest along the Izu-Ogasawara Arc Trench System. The property totals 7, ha comprising a terrestrial area of 6, ha and a marine area of 1, ha.

Today only two of the islands within the property are inhabited, Chichijima and Hahajima. Yuasa M, Nohara M () Petrographic and geochemical along-arc variations of volcanic rocks on the volcanic front of the Izu-Ogasawara (Bonin) Arc. Bull Geol Surv Jpn – Google Scholar Yuasa M, Uchiumi S, Nishimura A, Shibata K () K-Ar age of a forearc seamount adjacent to the volcanic front of the Izu-Ogasawara by: 5.

Izu-Ogasawara Trench Also known as Izu-Bonin Trenchat a depth of 9, metres and located N, E based on Wikipedia library, it is the sixth deepest ocean trench in the world.

[] ikeda y., yuasa m. ; volcanism in nascent back-arc basins behind the shichito ridge and adjacent area in the izu-ogasawara arc, northwest pacific: evidence for mixing between e-type morb and island arc magmas at the initiation of back-arc rifting ; contrib.

PUBLICATIONS BOOKS EDITED: Seamounts, Islands, and Atolls, Keating, B. H., Fryer, P., Batiza, R., and Boehlert, G. W., editors, Geophysical Monograph Series, Wide-angle seismic profiling of oceanic island arc in the southern Izu-Ogasawara arc 44 JAMSTEC Rep. Res. Dev., Volume 3, March43–52 to 4 March.

After OBS retrieval, we conducted a sea trial of a new transponder system. We left the survey area on 10 March and arrived at Shingu port on 11 March. These activities are listed in Table 1.

Trench-Forearc Geology: Sedimentation and Tectonics in Modern and Ancient Active Plate Margins (Geological Society Special Publication No. 10) arc mantle crust volcanic fig subduction spreading ridge basin south journal You can write a book review and share your experiences.

Other. OGASAWARA (BONIN) lSLANDS I. LIST OF COLLECTED SPECIES WITH COMMENTS ON SOME SPECIES AKIRA ASAKURA*, SHIROU NISHIHAMA**, AND YASUO KONDO*"" The Ogasawara (Bonin) Islands are subtropical, oceanic islands, located in the north west Pacific (Lat.

27" N, Long. " E). The nearest landmass is the Japan Islands situated. DeepDyve is the largest online rental service for scholarly research with thousands of academic publications available at your fingertips. DeepDyve is the easiest way to get instant access to the academic journals you : Nishimura, Takuya.

Chapter 2 Intra-oceanic Subduction Zones T.V. Gerya Introduction According to the common definition, intra-oceanic subduction brings oceanic slabs under the overriding plates of oceanic origin.

As a consequence oceanic magmatic arcs are formed worldwide (Fig. ) with typical examples such as the Izu-Bonin-Mariana arc. Cambridge Core - Marine Biology - The Hadal Zone - by Alan JamiesonCited by:.

The seamount is located about 24 km northwest of Chichi Island and is characterized by submarine hydrothermal polymetallic mineralization of the back-arc basin type.

Three of five drill holes intersected polymetallic mineralized parts enriched in Cu and Zn and characterized by pyrite, chalcopyrite and zincblende, making it the first recovery of Cited by: 2.

The Tokyo metropolitan government has published more findings from a panel of earthquake experts commissioned to predict the number of casualties likely to result from a Nankai Trough earthquake. According to the estimates, about 1, deaths are predicted on casualties are expected on the Izu and Ogasawara island chains off.

Regional location map. PSP = Philippine Sea Plate, PP = Pacific Plate, IBM = Izu-Bonin-Mariana Trenches, MT = Mariana Trough. Bathymetry of the central Mariana arc-trench system from combined surveys, sunlit from the east, showing EW seismic lines.

Interpreted lines are shown in red. Boxes 1 and 2 locate Figs 3, 6 and by: