Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Teiji Yamazaki"'
Tsunamiites: Features and Implications, Second Edition, is an overview of the state-of-the art developments in sedimentology of tsunami-induced and tsunami-affected deposits, namely tsunamiites. It also highlights new problems and issues calling for
Publikováno v:
Sedimentary Geology. 220:218-226
The Early Miocene Tateyamazaki Dacite infills a 3.2 km diameter caldera. It comprises poorly sorted, massive, biotite-bearing dacite pumice lapilli tuff, in which huge blocks of densely welded dacite lapilli tuff, basaltic andesite lava, and other li
Publikováno v:
Journal of the Japanese Association for Petroleum Technology. 70:207-215
This paper describes occurrence of marine sediments and associated trace fossils at Shiose-no-Misaki (Cape), Oga Peninsula, NE Japan. The marine sediments constitute an upward-fining succession from sandstone to mudstone, and contain many trace fossi
Autor:
Tsunemasa Shiki, Teiji Yamazaki
Publikováno v:
Sedimentary Geology. 104:175-188
The Tsubutegaura conglomeratic tsunamiites occur in the middle section of the Miocene storm-related sand-silt alternation system in the Chita Peninsula, central Japan. Deposition of the system in the upper bathyal environment in a bay and synsediment
This book is an overview of the state-of-the art developments in sedimentology of tsunami-induced and tsunami-affected deposits, namely tsunamiites. It also highlights new problems and issues calling for additional investigation, and provides insight
Autor:
Teiji Yamazaki, Tsunemasa Shiki
Publikováno v:
Sedimentary Geology. 41:201-220
A new technique using an “Ultrasonic vibrator” for sieving fine-grained sediments was adopted in the study of the grain-size characteristics of fine-grained turbidites from the Okinawa Trough. Important results of the grain-size analysis were: (1
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 70:305-314
The argillaceous xenoliths within the andesitic lavas of the N??jo-san and Amatakiyama districts were recrystallized successively by the thermal effects of the magma. The mineral assemblages of these xenoliths can be classified into the large-grained
Autor:
TEIJI YAMAZAKI
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 54:92-103
Autor:
Teiji Yamazaki, Hitoshi Onuki
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 62:249-263