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

Shigeyuki Suzuki

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

Faculty of Science

Research output: Contribution to journal › Article

Original language	English
Pages (from-to)	1-16
Number of pages	16
Journal	Okayama University Earth Science Report
Volume	3
Publication status	Published - 1996

Cite this

Suzuki, S. (1996). Provenance of Lower Cretaceous sediments in the Nariwa and Hokubo area, Okayama Prefecture, deduced from detrital modes and geochemistry of sandstone. Okayama University Earth Science Report, 3, 1-16.

@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",

}