Add to ORKGThis presentation illustrates how myrmekite can be a clue that some garnetiferous gneisses are derived from deformed mafic igneous rocks rather than from metamorphism of pelites. The terrane that supports this hypothesis is th
The following nine illustrations in this presentation include three photomicrographs and seven field...
ABSTRACT. Textures produced by reactions involving garnet in a sillimanite-staurolite schist have be...
In a belt through the central and western Mojave Desert of southern California are several muscovite...
This presentation illustrates how myrmekite can be a clue that some garnetiferous gneisses are deriv...
Myrmekite, an intergrowth of plagioclase and quartz vermicules, often occurs in felsic-to-intermedia...
Myrmekite is a common textural feature in many magmatic and metamorphic rock types. Nevertheless, th...
Myrmekite, an intergrowth of plagioclase and quartz vermicules, often occurs in felsic-to-intermedia...
Two different generally-accepted hypotheses for the origin of myrmekite are examined in seven differ...
Garnet stability in high-grade (deep-seated) pseudotachylytes may be obscured by the peculiar thermo...
In this presentation questions are raised about a melt-restite unmixing model proposed by Barton and...
In this presentation, Ca-metasomatism of deformed K-feldspar to produce myrmekite in granite at Alas...
Myrmekitic and non-myrmekitic plagioclase compositions in gneisses from Broken Hill, New South Wales...
The following nine illustrations in this presentation include three photomicrographs and seven field...
In only a few places in the world is myrmekite found with very coarse vermicules. In each of these p...
SUMMARY. Grain boundary migration and the exsolution f albite from alkali feldspar, followed by the ...
The following nine illustrations in this presentation include three photomicrographs and seven field...
ABSTRACT. Textures produced by reactions involving garnet in a sillimanite-staurolite schist have be...
In a belt through the central and western Mojave Desert of southern California are several muscovite...
This presentation illustrates how myrmekite can be a clue that some garnetiferous gneisses are deriv...
Myrmekite, an intergrowth of plagioclase and quartz vermicules, often occurs in felsic-to-intermedia...
Myrmekite is a common textural feature in many magmatic and metamorphic rock types. Nevertheless, th...
Myrmekite, an intergrowth of plagioclase and quartz vermicules, often occurs in felsic-to-intermedia...
Two different generally-accepted hypotheses for the origin of myrmekite are examined in seven differ...
Garnet stability in high-grade (deep-seated) pseudotachylytes may be obscured by the peculiar thermo...
In this presentation questions are raised about a melt-restite unmixing model proposed by Barton and...
In this presentation, Ca-metasomatism of deformed K-feldspar to produce myrmekite in granite at Alas...
Myrmekitic and non-myrmekitic plagioclase compositions in gneisses from Broken Hill, New South Wales...
The following nine illustrations in this presentation include three photomicrographs and seven field...
In only a few places in the world is myrmekite found with very coarse vermicules. In each of these p...
SUMMARY. Grain boundary migration and the exsolution f albite from alkali feldspar, followed by the ...
The following nine illustrations in this presentation include three photomicrographs and seven field...
ABSTRACT. Textures produced by reactions involving garnet in a sillimanite-staurolite schist have be...
In a belt through the central and western Mojave Desert of southern California are several muscovite...