A method of an estimation of a time change of source grain-size distributions of tephra by using two-dimensional tephra transport theory in a steady velocity field and its application to a small eruptive event at Shinmoe-dake volcano, Japan (abs.)

Authors=Yu IRIYAMA

Journal/Book_names=Programme and Abstracts, the Volcanological Society of Japan (online)

volume=2021

pages=61-61

Publish_year=2021

Publisher=Volcanological Society of Japan

Language_of_Text=JA

ISSN=21897190

ID=300022229