The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences

Unusual feldspar intergrowths were found in two metamorphosed basalt dykes from Departure Rocks, Antarctica. They are composed of host calcic plagioclase (Kf 0 _3 An7 5_9 1 Ab9_25) and potassium-rich alkali feldspar (Kf90 _96 Ano_5 Ab0_8) lamellae. Their bulk composition is estimated to be Kf An 21...

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Bibliographic Details
Main Author: Ai, Y
Format: Thesis
Language:English
Published: 1987
Subjects:
Online Access:https://eprints.utas.edu.au/18931/
https://eprints.utas.edu.au/18931/1/whole_AiYang1988_thesis.pdf
id ftunivtasmania:oai:eprints.utas.edu.au:18931
record_format openpolar
spelling ftunivtasmania:oai:eprints.utas.edu.au:18931 2023-05-15T14:00:15+02:00 The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences Ai, Y 1987 application/pdf https://eprints.utas.edu.au/18931/ https://eprints.utas.edu.au/18931/1/whole_AiYang1988_thesis.pdf en eng https://eprints.utas.edu.au/18931/1/whole_AiYang1988_thesis.pdf Ai, Y 1987 , 'The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences', Coursework Master thesis, University of Tasmania. cc_utas Dikes (Geology) Feldspar Plagioclase Thesis NonPeerReviewed 1987 ftunivtasmania 2020-05-30T07:32:48Z Unusual feldspar intergrowths were found in two metamorphosed basalt dykes from Departure Rocks, Antarctica. They are composed of host calcic plagioclase (Kf 0 _3 An7 5_9 1 Ab9_25) and potassium-rich alkali feldspar (Kf90 _96 Ano_5 Ab0_8) lamellae. Their bulk composition is estimated to be Kf An 21 65 Ab14. The complex and yet regular lamella textures of these intergrowths suggest that they are exsolution products. This requires the existence of a formerly homogeneous plagioclase, compositionally equivalent to the estimated bulk composition of these intergrowths. Experimental studies in the binary system anorthite K-feldspar and in the albite-poor ternery feldspar system have proven the existence of such homogeneous plagioclase, which has been synthesized at 1150°C and 10 [(bar under dry conditions. The unusual feldspar intergrowths were homogenized under these same conditions, further supporting the hypothesized exsolution origin of these intergrowths. In an experiment of plagioclase crystallization in a synthetic rock system, a K-rich plagioclase (Kf 19.6 An70 Ab10 . 4) was obtained from a K-rich melt at 1140°C and 10 kbar, indicating that the proposed parental plagioclase for the unusual feldspar intergrowths can be formed in a complex (rock) system. Such K-rich melt could be generated through interaction of the dyke magma and its surrounding charnockitic magma. It is concluded that limits of solid solutions in feldspar systems are increased at high pressures due to the increase of feldspar melting temperatures. Pressure may have an effect on the extend of feldspar solid solutions, but it is considered to be very small. Thesis Antarc* Antarctica Departure Rocks University of Tasmania: UTas ePrints Departure Rocks ENVELOPE(62.819,62.819,-67.612,-67.612)
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic Dikes (Geology)
Feldspar
Plagioclase
spellingShingle Dikes (Geology)
Feldspar
Plagioclase
Ai, Y
The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
topic_facet Dikes (Geology)
Feldspar
Plagioclase
description Unusual feldspar intergrowths were found in two metamorphosed basalt dykes from Departure Rocks, Antarctica. They are composed of host calcic plagioclase (Kf 0 _3 An7 5_9 1 Ab9_25) and potassium-rich alkali feldspar (Kf90 _96 Ano_5 Ab0_8) lamellae. Their bulk composition is estimated to be Kf An 21 65 Ab14. The complex and yet regular lamella textures of these intergrowths suggest that they are exsolution products. This requires the existence of a formerly homogeneous plagioclase, compositionally equivalent to the estimated bulk composition of these intergrowths. Experimental studies in the binary system anorthite K-feldspar and in the albite-poor ternery feldspar system have proven the existence of such homogeneous plagioclase, which has been synthesized at 1150°C and 10 [(bar under dry conditions. The unusual feldspar intergrowths were homogenized under these same conditions, further supporting the hypothesized exsolution origin of these intergrowths. In an experiment of plagioclase crystallization in a synthetic rock system, a K-rich plagioclase (Kf 19.6 An70 Ab10 . 4) was obtained from a K-rich melt at 1140°C and 10 kbar, indicating that the proposed parental plagioclase for the unusual feldspar intergrowths can be formed in a complex (rock) system. Such K-rich melt could be generated through interaction of the dyke magma and its surrounding charnockitic magma. It is concluded that limits of solid solutions in feldspar systems are increased at high pressures due to the increase of feldspar melting temperatures. Pressure may have an effect on the extend of feldspar solid solutions, but it is considered to be very small.
format Thesis
author Ai, Y
author_facet Ai, Y
author_sort Ai, Y
title The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
title_short The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
title_full The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
title_fullStr The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
title_full_unstemmed The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
title_sort solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences
publishDate 1987
url https://eprints.utas.edu.au/18931/
https://eprints.utas.edu.au/18931/1/whole_AiYang1988_thesis.pdf
long_lat ENVELOPE(62.819,62.819,-67.612,-67.612)
geographic Departure Rocks
geographic_facet Departure Rocks
genre Antarc*
Antarctica
Departure Rocks
genre_facet Antarc*
Antarctica
Departure Rocks
op_relation https://eprints.utas.edu.au/18931/1/whole_AiYang1988_thesis.pdf
Ai, Y 1987 , 'The solubility of potassium-feldspar in calcic plagioclase : experimental study and application to natural occurrences', Coursework Master thesis, University of Tasmania.
op_rights cc_utas
_version_ 1766269282419736576