Evolution of the calc-alkaline magma feeding system of the Komakusadaira pyroclastics in Zao volcano, NE Japan
Author:
Funder
Ministry of Education, Culture, Sports, Science and Technology
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/s00445-020-01430-3.pdf
Reference30 articles.
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2. Andújar J, Scaillet B, Pichavant M, Druitt TH (2016) Generation conditions of dacite and rhyodacite via the crystallization of an andesitic magma. Implications for the plumbing system at Santorini (Greece) and the origin of tholeiitic or calc-alkaline differentiation trends in arc magmas. J Petrol 57:1887–1920
3. Ban M, Yamamoto T (2002) Petrological study of Nasu-Chausudake Volcano (ca. 16 ka to Present), northeastern Japan. Bull Volcanol 64:100–116
4. Ban M, Sagawa H, Miura K, Hirotani S (2008) Evidence for a short lived stratified magma chamber: petrology of the Z-To 5 tephra layer (c. 5.8ka) at Zao volcano, NE Japan. In: Annen C, Zellmer GF (eds) Dynamics of crustal magma transfer, storage and differentiation. Geological Society, London, Special Publications 304:149–168
5. Ban M, Oikawa N, Yamazaki S (2015) Geological map of Zao volcano. Geological survey of, Japan, AIST
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3. Pre-eruptive magmatic processes of historical activities at Zao volcano, northeastern Japan: Insights from compositional zoning in orthopyroxene phenocrysts;Journal of Volcanology and Geothermal Research;2022-12
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