この文献の参照には次のURLをご利用ください : https://doi.org/10.15027/53103
Journal of science of the Hiroshima University. Series C, Geology and mineralogy 8 巻 2 号
1983-11-30 発行

Growth Condition of Plagioclase Porphyroblasts in Sambagawa Schist from Central Shikoku, Japan

MAEDA Masaru
HARA Ikuo
全文
3 MB
JSHUC_8-2_131.pdf
Abstract
Microtextures of plagioclase porphyroblasts in a fold of pelitic schist in the biotite zone of the Sambagawa belt of Central Shikoku, Japan, have been described. It has been clarified that the growth of plagioclase porphyroblasts occurred as mimetic crystallization after the folding and under non-deformational condition.
About This Article
Other Article
New Middle Miocene Mollusca from the Katsuta Group at Shinden, Tsuyama City, Okayama Prefecture, Southwest Japan. Part 1. Description of Perna oyamai sp. nov. and its Paleoecology
PP. 95 - 102
Intrusion Mechanism of a Granite Batholith
PP. 103 - 122
Epidote Porphyroblasts in Sambagawa Schists of Central Shikoku, Japan
PP. 123 - 129
Growth Condition of Plagioclase Porphyroblasts in Sambagawa Schist from Central Shikoku, Japan
PP. 131 - 134
Deformation and Recrystallization of Amphiboles in Sambagawa Schist with Special Reference to History of Sambagawa Metamorphism
PP. 135 - 148
Contact Metamorphic Effect on Basaltic Rocks by the Koyama Gabbro Complex, Susa Area, Southwest Japan
PP. 149 - 163
Late Mesozoic to Early Tertiary Basic-Acid Dyke Swarms in the Chugoku-Setouchi District, Southwest Japan
PP. 165 - 188
Amphiboles in the Paleogene Namariyama Granophyres, Eastern San'in District, Southwest Japan
PP. 189 - 211
"Microscopic" Cleavages in Bornite from the Jinmu Mine, SW Japan and their Implications
PP. 213 - 219