Origin of chert, limestone and basalt complex in Japan.

Soichi Osozawa

Research output: Contribution to journalArticle

5 Citations (Scopus)

Abstract

The chert, limestone and basalt accumulated during the period of 100, 30 and 20 million years, respectively. Place of their accumulation was under oceanic condition without influx of terrigenous sediments. Most of the limestone are clastic. The limestone, together with underlying basalt, collapsed and rock fragments were fluxed into deep sea floor mainly by gravity flow where chert and other pelagic limestone were deposited. The other basalt extruded over and intruded into pelagic sediments.-from English summary

Original languageEnglish
Pages (from-to)709-722
Number of pages14
JournalJournal - Geological Society of Japan
Volume92
Issue number10
Publication statusPublished - 1986 Jan 1

ASJC Scopus subject areas

  • Environmental Science(all)
  • Engineering(all)
  • Earth and Planetary Sciences(all)

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