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Late Jurassic–Early Cretaceous intra-arc sedimentation and volcanism linked to plate motion change in northern Japan (Record no. 4937)

000 -LEADER
fixed length control field 02273nab a2200241 4500
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control field GSMBLIc
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 210419b ||||| |||| 00| 0 eng d
041 ## - LANGUAGE CODE
Language code of text/sound track or separate title Einglish Language
100 ## - MAIN ENTRY--PERSONAL NAME
Personal name Takashima, Reishi.
9 (RLIN) 10441
245 ## - TITLE STATEMENT
Title Late Jurassic–Early Cretaceous intra-arc sedimentation and volcanism linked to plate motion change in northern Japan
300 ## - PHYSICAL DESCRIPTION
Extent 753 - 770 pp.
Other physical details Illustration
520 ## - SUMMARY, ETC.
Summary, etc. The Sorachi Group, composed of Upper Jurassic ophiolite and Lower Cretaceous island-arc volcano-sedimentary cover, provides a record of Late Jurassic–Early Cretaceous sedimentation and volcanism in an island-arc setting off the eastern margin of the Asian continent. Stratigraphic changes in the nature and volume of the Sorachi Group volcanic and volcaniclastic rocks reveal four tectonic stages. These stages resulted from changes in the subduction direction of the Pacific oceanic plate. Stage I in the Late Jurassic was characterized by extensive submarine eruptions of tholeiitic basalt from the back-arc basin. Slab roll-back caused rifting and sea-floor spreading in the supra-subduction zone along the active Asian continental margin. Stage II corresponded to the Berriasian and featured localized trachyandesitic volcanism that formed volcanic islands with typical island-arc chemical compositions. At the beginning of this stage, movement of the Pacific oceanic plate shifted from northeastward to northwestward. During Stage III, in the Valanginian, submarine basaltic volcanism was followed by subsidence. The Pacific oceanic plate motion turned clockwise, and the plate boundary between the Asian continent and the Pacific oceanic plate changed from convergent to transform. During Stage IV in the Hauterivian–Barremian, in situ volcanism ceased in the Sorachi–Yezo basin, and the volcanic front migrated west of the Sorachi–Yezo basin.
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Cretaceous
9 (RLIN) 10442
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Jurassic
9 (RLIN) 8214
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Island-arc
9 (RLIN) 10443
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Volcanism
9 (RLIN) 3371
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Tectonics
9 (RLIN) 7992
650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Asia
9 (RLIN) 213
700 ## - ADDED ENTRY--PERSONAL NAME
Personal name Nishi, Hiroshi.
9 (RLIN) 10444
700 ## - ADDED ENTRY--PERSONAL NAME
Personal name Yoshida, Takeyoshi.
9 (RLIN) 10445
773 0# - HOST ITEM ENTRY
Host Biblionumber 1899
Host Itemnumber 2187
Place, publisher, and date of publication London Cambridge University Press 2006
Other item identifier 002538
Title Geological magazine : Vol. 143 Iss. 1-6 Year. 2006
International Standard Serial Number 00167568
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme
Call number suffix {082b}
Koha item type Article
Holdings
Withdrawn status Lost status Source of classification or shelving scheme Damaged status Not for loan Collection code Permanent Location Current Location Shelving location Date acquired Barcode Date last seen Price effective from Koha item type
          Bound Journal Collection Library and Information Centre Library and Information Centre Periodical Section 2021-04-19 002538_85 2021-04-19 2021-04-19 Article

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