Plagioclase-spinel intergrowths in alkali basaltic rocks from the Southern Highlands, N.S.W.

Suzanne Y. Wass

doi:10.1007/BF00373880

Plagioclase-spinel intergrowths in alkali basaltic rocks from the Southern Highlands, N.S.W.

Suzanne Y. Wass^*

^*Corresponding author for this work

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

Research output: Contribution to journal › Article › peer-review

10 Citations (Scopus)

Abstract

Dominant plagioclase (An₅₉) and minor spinel form possible cumulates in alkali basaltic flows from the Southern Highlands, N.S.W. The mode of occurrence of the spinel, and the chemical composition of both the spinel and the plagioclase suggest the spinel originated by exsolution from plagioclase formed at high pressure.

Original language	English
Pages (from-to)	167-175
Number of pages	9
Journal	Contributions to Mineralogy and Petrology
Volume	38
Issue number	2
DOIs	https://doi.org/10.1007/BF00373880
Publication status	Published - Jun 1973

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@article{77977ca2074d49eb9dcd26364f379e99,

title = "Plagioclase-spinel intergrowths in alkali basaltic rocks from the Southern Highlands, N.S.W.",

abstract = "Dominant plagioclase (An59) and minor spinel form possible cumulates in alkali basaltic flows from the Southern Highlands, N.S.W. The mode of occurrence of the spinel, and the chemical composition of both the spinel and the plagioclase suggest the spinel originated by exsolution from plagioclase formed at high pressure.",

author = "Wass, \{Suzanne Y.\}",

year = "1973",

month = jun,

doi = "10.1007/BF00373880",

language = "English",

volume = "38",

pages = "167--175",

journal = "Contributions to Mineralogy and Petrology",

issn = "0010-7999",

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TY - JOUR

T1 - Plagioclase-spinel intergrowths in alkali basaltic rocks from the Southern Highlands, N.S.W.

AU - Wass, Suzanne Y.

PY - 1973/6

Y1 - 1973/6

N2 - Dominant plagioclase (An59) and minor spinel form possible cumulates in alkali basaltic flows from the Southern Highlands, N.S.W. The mode of occurrence of the spinel, and the chemical composition of both the spinel and the plagioclase suggest the spinel originated by exsolution from plagioclase formed at high pressure.

AB - Dominant plagioclase (An59) and minor spinel form possible cumulates in alkali basaltic flows from the Southern Highlands, N.S.W. The mode of occurrence of the spinel, and the chemical composition of both the spinel and the plagioclase suggest the spinel originated by exsolution from plagioclase formed at high pressure.

UR - https://www.scopus.com/pages/publications/3743091396

U2 - 10.1007/BF00373880

DO - 10.1007/BF00373880

M3 - Article

AN - SCOPUS:3743091396

SN - 0010-7999

VL - 38

SP - 167

EP - 175

JO - Contributions to Mineralogy and Petrology

JF - Contributions to Mineralogy and Petrology

IS - 2

ER -

Plagioclase-spinel intergrowths in alkali basaltic rocks from the Southern Highlands, N.S.W.

Abstract

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