2002
DOI: 10.1016/s0301-9268(02)00014-1
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Supercooled rocks: development and significance of varioles, spherulites, dendrites and spinifex in Archaean volcanic rocks, Abitibi Greenstone belt, Canada

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Cited by 66 publications
(47 citation statements)
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“…The typical morphological variation is from a spherulite-rich margin to a microlite-rich core, but Fowler et al (2002) suggest that some tubes and large pillows can have varioles concentrated toward pillow centers, similar to those observed (Figure 20). Moreover, Fowler et al (1986) suggested that plagioclase spherulites formed because of pronounced undercooling from a superheated basaltic melt.…”
Section: Discussionsupporting
confidence: 76%
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“…The typical morphological variation is from a spherulite-rich margin to a microlite-rich core, but Fowler et al (2002) suggest that some tubes and large pillows can have varioles concentrated toward pillow centers, similar to those observed (Figure 20). Moreover, Fowler et al (1986) suggested that plagioclase spherulites formed because of pronounced undercooling from a superheated basaltic melt.…”
Section: Discussionsupporting
confidence: 76%
“…Additional support for a proximal setting for pillow lavas mapped in the New Bidlamaque region (Figures 10 and 11) is the presence of varioles and aphyric nature, which are indicative of high temperature lava. Varioles observed within pillow margins are similar to those described by Gélinas et al (1976) and are probably composed of spherulites of acicular plagioclase originating from a central point (Fowler et al, 2002).…”
Section: Discussionsupporting
confidence: 72%
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“…Manley, 1992). One exception for glass devitrification (in response to heating to 250-700°C and the presence of an alkali-rich fluid phase; Lofgren, 1971a) could be later hydrothermal-fluid circulation during vesicle-filling (Fowler et al, 2002). Within the Loskop…”
Section: Cooling Historymentioning
confidence: 99%