Provenance of Lower Cretaceous sediments in the Nariwa and Hokubo area, Okayama Prefecture, deduced from detrital modes and geochemistry of sandstone.

Research output: Contribution to journalArticle

Original languageEnglish
Pages (from-to)1-16
Number of pages16
JournalOkayama University Earth Science Report
Volume3
Publication statusPublished - 1996

Cite this

@article{2903fece283343fbaacb715216769f2b,
title = "Provenance of Lower Cretaceous sediments in the Nariwa and Hokubo area, Okayama Prefecture, deduced from detrital modes and geochemistry of sandstone.",
author = "Shigeyuki Suzuki",
year = "1996",
language = "English",
volume = "3",
pages = "1--16",
journal = "Okayama University Earth Science Report",

}

TY - JOUR

T1 - Provenance of Lower Cretaceous sediments in the Nariwa and Hokubo area, Okayama Prefecture, deduced from detrital modes and geochemistry of sandstone.

AU - Suzuki, Shigeyuki

PY - 1996

Y1 - 1996

M3 - Article

VL - 3

SP - 1

EP - 16

JO - Okayama University Earth Science Report

JF - Okayama University Earth Science Report

ER -