Use of downstream and downfan variation in particle size, roundness, lithology, and form as complements to clast fabric data in paleocurrent analysis
礫層の古流系を復元するには, 礫のファブリックのほかに何が有効か?

Takeyuki Ueki
2000 Journal of the Sedimentological Society of Japan  
doi:10.4096/jssj1995.51.45 fatcat:ln2u4eft3vfzjaaaqeocrtu5si