Microfacies and depositional setting of the Upper Triassic mid-oceanic atoll-type carbonates of the Sambosan Accretionary Complex (southern Kyushu, Japan)

Jérôme Chablais, Rossana Martini, Elias Samankassou, Tetsuji Onoue, Hiroyoshi Sano

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

The Upper Triassic shallow-water limestones of the Sambosan Accretionary Complex are reconstructed as a remnant of a mid-oceanic atoll-type build-up upon a seamount in the Panthalassan Ocean. The Sambosan atoll-type carbonates and its pedestal were accreted along with deep-water ribbon-chert and related siliceous rocks to the eastern margin of Asia during the Late Jurassic to Early Cretaceous. Studied limestones crop out in southern Kyushu Island, southwest Japan. Although the prevailing and intense deformation during the accretionary process prevents measurement of sections in stratigraphic successions, and sedimentary structures are poorly preserved, microfacies description and foraminifers analysis allow us to speculate the depositional setting of the Sambosan limestones. Seventeen microfacies are distinguished and several foraminifers of Tethyan affinity are identified. Foraminifers indicate a Late Carnian to Rhaetian age. The Tethyan affinity of the macro- and microfaunas suggests that the Sambosan seamount was located presumably in a low- to middle-latitudinal zone of the southern hemisphere during the Late Triassic.

Original languageEnglish
Pages (from-to)249-278
Number of pages30
JournalFacies
Volume56
Issue number2
DOIs
Publication statusPublished - Apr 1 2010

Fingerprint

microfacies
atoll
foraminifera
Triassic
limestone
seamount
carbonate
Rhaetian
Carnian
sedimentary structure
chert
Southern Hemisphere
shallow water
deep water
Jurassic
Cretaceous
crop
ocean
rock

All Science Journal Classification (ASJC) codes

  • Geology
  • Stratigraphy
  • Palaeontology

Cite this

Microfacies and depositional setting of the Upper Triassic mid-oceanic atoll-type carbonates of the Sambosan Accretionary Complex (southern Kyushu, Japan). / Chablais, Jérôme; Martini, Rossana; Samankassou, Elias; Onoue, Tetsuji; Sano, Hiroyoshi.

In: Facies, Vol. 56, No. 2, 01.04.2010, p. 249-278.

Research output: Contribution to journalArticle

Chablais, Jérôme ; Martini, Rossana ; Samankassou, Elias ; Onoue, Tetsuji ; Sano, Hiroyoshi. / Microfacies and depositional setting of the Upper Triassic mid-oceanic atoll-type carbonates of the Sambosan Accretionary Complex (southern Kyushu, Japan). In: Facies. 2010 ; Vol. 56, No. 2. pp. 249-278.
@article{e3f30966602f4dd0b88814085e899218,
title = "Microfacies and depositional setting of the Upper Triassic mid-oceanic atoll-type carbonates of the Sambosan Accretionary Complex (southern Kyushu, Japan)",
abstract = "The Upper Triassic shallow-water limestones of the Sambosan Accretionary Complex are reconstructed as a remnant of a mid-oceanic atoll-type build-up upon a seamount in the Panthalassan Ocean. The Sambosan atoll-type carbonates and its pedestal were accreted along with deep-water ribbon-chert and related siliceous rocks to the eastern margin of Asia during the Late Jurassic to Early Cretaceous. Studied limestones crop out in southern Kyushu Island, southwest Japan. Although the prevailing and intense deformation during the accretionary process prevents measurement of sections in stratigraphic successions, and sedimentary structures are poorly preserved, microfacies description and foraminifers analysis allow us to speculate the depositional setting of the Sambosan limestones. Seventeen microfacies are distinguished and several foraminifers of Tethyan affinity are identified. Foraminifers indicate a Late Carnian to Rhaetian age. The Tethyan affinity of the macro- and microfaunas suggests that the Sambosan seamount was located presumably in a low- to middle-latitudinal zone of the southern hemisphere during the Late Triassic.",
author = "J{\'e}r{\^o}me Chablais and Rossana Martini and Elias Samankassou and Tetsuji Onoue and Hiroyoshi Sano",
year = "2010",
month = "4",
day = "1",
doi = "10.1007/s10347-009-0204-6",
language = "English",
volume = "56",
pages = "249--278",
journal = "Facies",
issn = "0172-9179",
publisher = "Springer Verlag",
number = "2",

}

TY - JOUR

T1 - Microfacies and depositional setting of the Upper Triassic mid-oceanic atoll-type carbonates of the Sambosan Accretionary Complex (southern Kyushu, Japan)

AU - Chablais, Jérôme

AU - Martini, Rossana

AU - Samankassou, Elias

AU - Onoue, Tetsuji

AU - Sano, Hiroyoshi

PY - 2010/4/1

Y1 - 2010/4/1

N2 - The Upper Triassic shallow-water limestones of the Sambosan Accretionary Complex are reconstructed as a remnant of a mid-oceanic atoll-type build-up upon a seamount in the Panthalassan Ocean. The Sambosan atoll-type carbonates and its pedestal were accreted along with deep-water ribbon-chert and related siliceous rocks to the eastern margin of Asia during the Late Jurassic to Early Cretaceous. Studied limestones crop out in southern Kyushu Island, southwest Japan. Although the prevailing and intense deformation during the accretionary process prevents measurement of sections in stratigraphic successions, and sedimentary structures are poorly preserved, microfacies description and foraminifers analysis allow us to speculate the depositional setting of the Sambosan limestones. Seventeen microfacies are distinguished and several foraminifers of Tethyan affinity are identified. Foraminifers indicate a Late Carnian to Rhaetian age. The Tethyan affinity of the macro- and microfaunas suggests that the Sambosan seamount was located presumably in a low- to middle-latitudinal zone of the southern hemisphere during the Late Triassic.

AB - The Upper Triassic shallow-water limestones of the Sambosan Accretionary Complex are reconstructed as a remnant of a mid-oceanic atoll-type build-up upon a seamount in the Panthalassan Ocean. The Sambosan atoll-type carbonates and its pedestal were accreted along with deep-water ribbon-chert and related siliceous rocks to the eastern margin of Asia during the Late Jurassic to Early Cretaceous. Studied limestones crop out in southern Kyushu Island, southwest Japan. Although the prevailing and intense deformation during the accretionary process prevents measurement of sections in stratigraphic successions, and sedimentary structures are poorly preserved, microfacies description and foraminifers analysis allow us to speculate the depositional setting of the Sambosan limestones. Seventeen microfacies are distinguished and several foraminifers of Tethyan affinity are identified. Foraminifers indicate a Late Carnian to Rhaetian age. The Tethyan affinity of the macro- and microfaunas suggests that the Sambosan seamount was located presumably in a low- to middle-latitudinal zone of the southern hemisphere during the Late Triassic.

UR - http://www.scopus.com/inward/record.url?scp=77952671707&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=77952671707&partnerID=8YFLogxK

U2 - 10.1007/s10347-009-0204-6

DO - 10.1007/s10347-009-0204-6

M3 - Article

AN - SCOPUS:77952671707

VL - 56

SP - 249

EP - 278

JO - Facies

JF - Facies

SN - 0172-9179

IS - 2

ER -