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XIII.—Crystal Growth of Forsteritic Olivine in Magmas and Melts
Abstract
Synopsis One of the writers' main aims has been to help to prepare the way for a new approach to problems in which the natural occurrence of forsteritic olivines is a vital factor. Variation in their shapes and textural relations in minor intrusions, lavas and melts is examined and the historical development of concepts of their growth and resorption, particularly in magmas, is traced. Particular attention is focused on the olivines of picritic, minor intrusions. It is concluded that in the interpretation of olivine shapes there has been discrimination in favour of magmatic resorption rather than skeletal crystallization. From a wide and detailed survey of forsteritic olivines it is established that they tend to grow rapidly and that their phenomenal variation in habit and shape is probably due to a specific growth sensitivity to slight environmental differences. Concepts of the physical conditions leading to skeletal crystallization are briefly reviewed and discussed.
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Ultrabasic lavas were produced in the early Precambrian, older than 2800 million years.
“recently a number of careful studies of the fabric and mode of occurrence of such lavas has clearly demonstrated that they were produced in the early Precambrian (older than 2800My).”
From Speculations on the Thermal and Tectonic History of the Earth (2007) · cites this paper as Drever & Johnston (1957)
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Sorted by citations
Speculations on the Thermal and Tectonic History of the Earth
McKenzie, D., & Weiss, N. (2007) · Geophysical Journal of the Royal Astronomical Society · doi:10.1111/j.1365-246x.1975.tb05855.x · Cited by 335
Metadata
- Authors
- Drever, H. I., & Johnston, R.
- ORCID
- Johnston, R.
- Venue
- Transactions of the Royal Society of Edinburgh
- Publisher
- Cambridge University Press (CUP)
- Published
- 1958
- Volume
- 63
- Issue
- 2
- Pages
- 289-315
- ISSN
- 0080-4568 (ISSN-L)
- 2053-5945
- OpenAlex
- W4248111221
- Cited by
- 55
- References
- 39
- Citations by year
- 2025: 1 · 2024: 1 · 2022: 1 · 2021: 1 · 2020: 1 · 2019: 1 · 2018: 11
- FWCI
- 6.30
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Transactions of the Royal Society of Edinburgh (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Mineralogy and Gemology Studies
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Keywords
- forsteritic olivine, crystal growth, picritic magma, lava, melts
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