Comparative rhyolite systems: Inferences from vent patterns and eruptive episodicities: Eastern California and Laguna del Maule
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Abstract
Distilling my experience in having field mapped in detail the volcanic fields at Laguna del Maule and Long Valley and having worked out their time-volume-composition magmatic histories, I compare and contrast the postglacial rhyolites of the former with six multi-vent eruptive sequences of rhyolite in California. Compilations and discussions are made of volcanic-field areas and longevities, their compositions, vent distributions, individual batch and total volumes, eruptive episodicities, and tectonic influences. Growth of long-lived pluton-scale reservoirs of granitic crystal mush, from which the rhyolite melts separated, are interpreted in terms of conceptual models I published previously—(1) fundamentally basaltic transcrustal magmatism, 1981; (2) the deep-crustal MASH zone model, 1988; and (3) the rhyolite-melt crystal-mush model, 2001. Inferences and speculations are advanced concerning processes and timescales of rhyolite-melt separation from granitic mush and of prompt or long-delayed subsequent eruption.
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Comparative rhyolite systems: Inferences from vent patterns and eruptive episodicities: Eastern California and Laguna del Maule |
Series title | Journal of Geophysical Research |
DOI | 10.1029/2020JB020879 |
Volume | 126 |
Issue | 7 |
Year Published | 2021 |
Language | English |
Publisher | American Geophysical Union |
Contributing office(s) | Volcano Science Center |
Description | e2020JB020879, 53 p. |
Country | Argentina, Chile, United States |
State | California |
Other Geospatial | Laguna del Maule (LdM) volcanic field, Mono Lake basin |
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