Zobrazeno 1 - 7
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pro vyhledávání: '"Ryan M. Currier"'
Autor:
T P Flood, Ryan M. Currier
Publikováno v:
Journal of Petrology. 60:2077-2100
The Orestes Melt Zone (OMZ) is a massive contact melt zone (∼20 m thick by several kilometers long), located in the McMurdo Dry Valleys of Antarctica. The OMZ formed at shallow crustal depths by melting of the A-type Orestes Granite owing to intrus
Publikováno v:
Precambrian Research. 321:1-12
The well-known rapakivi texture has been extensively studied through a geochemical lens. Presented here is a detailed textural analysis of two classical rapakivi granites from the Proterozoic: The Wiborg Batholith, Finland and the Wolf River Batholit
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Journal of Volcanology and Geothermal Research. 336:155-167
The ultimate shape of a laccolith is the result of competition between internal magmatic phenomena (e.g. overpressure and the process of solidification), and the state of the external host rock (e.g. thickness of the overburden, the presence of fault
Autor:
Ryan M. Currier, Tim P. Flood
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Bruce D. Marsh, Ryan M. Currier
Publikováno v:
Journal of Volcanology and Geothermal Research. 302:211-224
The dynamics of solidification front growth along the margins of magmas have been widely found to be fundamental in controlling magma transport and emplacement. In this vein, the role of solidification fronts in determining the basic growth mechanics
Publikováno v:
Contributions to Mineralogy and Petrology. 162:1115-1138
In the Central American Volcanic Arc, adakite-like volcanism has often been described as volumetrically insignificant. However, extensive silicic adakitic volcanism does occur in the Panamanian arc and provides an opportunity to evaluate the origin o