Cited by 55Geological and Geochemical AnalysisMineralogy and Gemology StudiesHigh-pressure geophysics and materials

The DOI matches its Crossref record; 39 of the 39 references it cites were found in a registry or an index.

XIII.—Crystal Growth of Forsteritic Olivine in Magmas and Melts

Drever, H. I., Johnston, R.·1958·Transactions of the Royal Society of Edinburgh

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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Registry

Crossref · 10.1017/s0080456800009509

Cites

39 of 39 references verified0 citation errors · 0 not checkable

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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)

Citations

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Flagged first, then by citations

Research works printed but not linked: 31

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  2. Schwantke, 1904, Die Basalte der Gegend von Hornberg an der Ohen insbesondere der Dolerit des Hohen Berges bei Ofleiden, Neues. Jb. Min. Geol. Paläont, 18, 460
  3. Penck, 1878, Studien uber lockere vulcanische Auswütflinge, Z. Dtsch. Geol. Ges., 30, 97
  4. Harris, 1937, A Petrological Study of the Portrush Sill and its Veins, Proc. Roy. Irish Acad., 43, 95
  5. Frankel, 1942, Studies on Karroo Dolerites. 2. Some Younger Intrusions of Olivine Basaltic Dolerite, Trans. Geol. Soc. S. Afr., 45, 1
  6. Vogt, 1884, Studier om Slagger, Bih. Svensk. Vetensk Akad. Handl., 9
  7. Fouqué, 1882, Synthèse des Minéraux et des Roches
  8. Iddings, 1911, Rock Minerals
  9. Ernst, 1936, Der Melilith-Basalt des Westberges bei Hofgeismar, nördlich von Kassel, ein Assimilationsprodukt ultrabasischer Gesteine, Chemie der Erde, 10, 631
  10. Du Toit, 1910, Report on the copper-nickel deposits of the Insizwa, Mount Ayliff, East Griqualand, Rep. Geol. Comm. C. G. H., 1910, 111
  11. Drever, 1948, Some Basaltic Rocks from West Greenland, Proc. Roy. Soc. Edin., 63, 97
  12. Cohen, 1880, Ueber Laven von Hawaii und einigen anderem Inseln des Grossen Oceans nebst einigen Bemerkungen über glasige Gesteine im allgemeinen, Neues Jb. Min. Geol. Paläont., 2, 23
  13. Drever, 1952, The Origin of some Ultramafic Rocks. A Preliminary Survey of the Evidence for and against Gravitative Accumulation of Olivine, Medd. fra Geologisk Forening, 12, 227
  14. Abelson, 1954, Annual Report of the Director of the Geophysical Laboratory, Yearb. Carneg. Instn., 53, 95
  15. Bodmer-Beder, 1898, Über Olivindiabase aus dem Plessurgebirge, Graubünden, Neues Jb. Min. Geol. Paläont., 12, 248
  16. Tammann, 1925, Glasses as Supercooled Liquids, J. Soc. Glass Tech., 9, 166
  17. Clough, 1898, On a Coarsely Spherulitic (‘Variolitic’) Basalt in Skye, Trans. Geol. Soc. Edin., 7, 281
  18. Lawson, 1904, The Orbicular Gabbro at Dehesa, San Diego Co., California, Bull. Dept. Geol. Univ. Calif., 3, 383
  19. Rinne, 1891, Ueber Olivin—und Plagioklasskellete, Neues. J. Min. Geol. Paläont., 2, 272
  20. Shafranovsky, 1953, On the question of the distinctive features of the rounded solution forms of crystals, Min. Sbornik, Lvov Geol. Soc., 7, 21
  21. Wervecke, 1879, Beitrag zur Kenntniss der Limburgite, Neues. Jb. Min. Geol. Paläont., 1, 481
  22. Gansser, 1950, Geological and Petrological Notes on Gorgona Island in relation to north-western S. America, Schweiz. Min. Petrogr. Mitt., 30, 219
  23. Drever, 1956, The Geology of Ubekendt Ejland, Part II. The Picritic Sheets and Dykes of the East Coast, Medd. Grønland, 137, 1
  24. Buckley, 1951, Crystal Growth
  25. Brauns, 1904, Der oberdevonische Pikrit und die aus ihm hervorgegangenen Neubildungen, Neues Jb. Geol. Paläont., 18, 285
  26. Lacroix, 1936, Le Volcan Actif de l'ile de la Réunion et ses Produits
  27. Yoder, 1952, The MgO–Al2O3–SiO2–H2O System and the Related Metamorphic Facies, Amer. J. Sci., 569–627
  28. Bentor, 1955, La Chaine des puys, Bull. Serv. Carte Géol. Fr., 52
  29. Hughes, 1956, Geological Investigations in East Greenland, Pt. VI. A differentiated basic sill, etc., Medd. Grønland, 137, 1
  30. Drever, 1955, Geology in St Andrews
  31. Osborn, 1952, The System Diopside-Forsterite-Anorthite, Amer. J. Sci., 413–433

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Metadata

Authors
Drever, H. I., & Johnston, R.
Venue
Transactions of the Royal Society of Edinburgh
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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