Results 191 to 200 of about 10,226 (223)
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Lattice structural variation in K-feldspar megacrysts of associated charnockite and alkali granite
Mineralogical Magazine, 1982AbstractThe perthite megacrysts from charnockitic and non-charnockitic members of a sialic intrusive complex in the Varberg area of south-west Sweden have been investigated by powder X-ray diffraction. The extent of Al/Si order in the K-feldspar host lattices of the megacrysts is restricted in all but the major alkali granite differentiate.
D. R. Iball, F. H. Hubbard
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Journal of the Geological Society, 1997
Alkali feldspar phenocrysts in the Lower Devonian Shap granite are compositionally and microtexturally zoned. Most of each phenocryst has exsolved to form microperthite with an approximate bulk composition of Or 72 Ab 28 An <1 , but sub-millimetre wide zones within ...
M. R. LEE, I. PARSONS
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Alkali feldspar phenocrysts in the Lower Devonian Shap granite are compositionally and microtexturally zoned. Most of each phenocryst has exsolved to form microperthite with an approximate bulk composition of Or 72 Ab 28 An <1 , but sub-millimetre wide zones within ...
M. R. LEE, I. PARSONS
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Contributions to Mineralogy and Petrology, 1996
The extremely young (2.5 Ma) I-type Eldzhurtinskiy granite complex (Central Caucasus) is uniform with respect to modal composition, major and trace element chemistries of bulk rocks and mineral phases. In contrast, it reveals two types of alkali feldspar megacrysts differing in tetrahedral Al-content (2t1) and exsolution microtextures:
G. Witt-Eickschen +4 more
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The extremely young (2.5 Ma) I-type Eldzhurtinskiy granite complex (Central Caucasus) is uniform with respect to modal composition, major and trace element chemistries of bulk rocks and mineral phases. In contrast, it reveals two types of alkali feldspar megacrysts differing in tetrahedral Al-content (2t1) and exsolution microtextures:
G. Witt-Eickschen +4 more
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Petrogenetic Significance of Alkali Feldspar Megacrysts and their Inclusions in Cornubian Granites
Nature, 1968Petrogenetic Significance of Alkali Feldspar Megacrysts and their Inclusions in Cornubian ...
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Alkali Feldspars from Gneisses and Granites of the Västervik Area, SE. Sweden
Geologiska Föreningen i Stockholm Förhandlingar, 1968Abstract Metamorphosed Precambrian sedimentary rocks and associated late-kinematic granites of the Vastervik area in southeastern Sweden contain abundant potassium feldspar. The alkali feldspar from the metasediments shows zero to low obliquity and contains from 8 to 10 % albite in solid solution.
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Journal of African Earth Sciences (1983), 1986
Abstract The Jabalat post-tectonic granite pluton is composed of albite- and oligoclase-bearing, low-calcium, F-, Sn- and Rb-rich subsolvus granites. These granites display evidence of late-magmatic, granitophile- and metallic-element specialization, resulting ultimately in the development of post-magmatic, metalliferous hydrothermal systems ...
Jaffar Al Tayyar +2 more
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Abstract The Jabalat post-tectonic granite pluton is composed of albite- and oligoclase-bearing, low-calcium, F-, Sn- and Rb-rich subsolvus granites. These granites display evidence of late-magmatic, granitophile- and metallic-element specialization, resulting ultimately in the development of post-magmatic, metalliferous hydrothermal systems ...
Jaffar Al Tayyar +2 more
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Mineralogical Magazine, 1978
SummaryThe variation in the structural state of potassium feldspars from the St. George pluton, New Brunswick, Canada, is discussed. Monoclinic potassium feldspars occur near the eastern end of the pluton whereas the granites at the western end contain triclinic potassium feldspars. Although the bulk compositions of the host rocks are all very near the
Michael E. Cherry, Lowell T. Trembath
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SummaryThe variation in the structural state of potassium feldspars from the St. George pluton, New Brunswick, Canada, is discussed. Monoclinic potassium feldspars occur near the eastern end of the pluton whereas the granites at the western end contain triclinic potassium feldspars. Although the bulk compositions of the host rocks are all very near the
Michael E. Cherry, Lowell T. Trembath
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Intraplate, rift-related magmatism: mainly the A-type, alkali feldspar granites
1997Contrary to general opinion, a distinctly bimodal magmatism involving rather ordinary biotite granites and coeval basalts has been a feature of the earth’s cratons since the Early Proterozoic. Although I shall concern myself here mainly with the alkalic granites of this same environment, it is important to emphasize that they are really of small volume
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Contributions to Mineralogy and Petrology, 1993
The ratios Na/Li, K/Li, Na/Cs and K/Cs have been calculated for exchange equilibria among the Li and Cs silicates spodumene, petalite, eucryptite, and pollucite, and the alkali feldspars albite and K-feldspar plus quartz, in pure water and in chloride solutions at temperatures from 100° to 700°C and pressures from 0.5 to 4 kbar, using available ...
Williams-Jones, A. E., Wood, S. A.
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The ratios Na/Li, K/Li, Na/Cs and K/Cs have been calculated for exchange equilibria among the Li and Cs silicates spodumene, petalite, eucryptite, and pollucite, and the alkali feldspars albite and K-feldspar plus quartz, in pure water and in chloride solutions at temperatures from 100° to 700°C and pressures from 0.5 to 4 kbar, using available ...
Williams-Jones, A. E., Wood, S. A.
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Geological Magazine, 2014
AbstractThe Mingshui–Jilasitai–Suolun area, located in the central part of the Great Xing’an Range, is characterized by large volumes of alkali feldspar granites. However, the formation time and tectonic setting of these rocks remains controversial owing to a lack of precise geochronological and detailed geochemical data.
Zhang, YL +4 more
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AbstractThe Mingshui–Jilasitai–Suolun area, located in the central part of the Great Xing’an Range, is characterized by large volumes of alkali feldspar granites. However, the formation time and tectonic setting of these rocks remains controversial owing to a lack of precise geochronological and detailed geochemical data.
Zhang, YL +4 more
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