Origin of phenocrysts and compositional diversity in pre-Mazama rhyodacite lavas, Crater Lake, Oregon

Journal of Petrology
By: , and 

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Abstract

Phenocrysts in porphyritic volcanic rocks may originate in a variety of ways in addition to nucleation and growth in the matrix in which they are found. Porphyritic rhyodacite lavas that underlie the eastern half of Mount Mazama, the High Cascade andesite/dacite volcano that contains Crater Lake caldera, contain evidence that bears on the general problem of phenocryst origin. Phenocrysts in these lavas apparently formed by crystallization near the margins of a magma chamber and were admixed into convecting magma before eruption. About 20 km3 of pre-Mazama rhyodacite magma erupted during a relatively short period between ~400 and 500 ka; exposed pre-Mazama dacites are older and less voluminous. The rhyodacites formed as many as 40 lava domes and flows that can be assigned to three eruptive groups on the basis of composition and phenocryst content. -from Authors

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Origin of phenocrysts and compositional diversity in pre-Mazama rhyodacite lavas, Crater Lake, Oregon
Series title Journal of Petrology
DOI 10.1093/petrology/35.1.127
Volume 35
Issue 1
Year Published 1994
Language English
Publisher Oxford Academic
Contributing office(s) Volcano Hazards Program, Volcano Science Center
Description 36 p.
First page 127
Last page 162
Country United States
State Oregon
Other Geospatial Crater Lake
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