Basal reversals in layered intrusions are evidence for emplacement of compositionally stratified magma
- 1 October 1986
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 323 (6089) , 616-618
- https://doi.org/10.1038/323616a0
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Implication of vertical and lateral compositional variations across the pyroxene marker and its associated rocks in the upper part of the main zone in the eastern Bushveld ComplexEconomic Geology, 1985
- Two-dimensional study of a layered intrusion — the Hyllingen Series, NorwayGeological Magazine, 1985
- Investigations in the Stillwater Complex: Part II. Petrology and Petrogenesis of the Ultramafic SeriesJournal of Petrology, 1984
- The J-M platinum-palladium reef of the Stillwater Complex, Montana; II, Origin by double-diffusive convective magma mixing and implications for the Bushveld ComplexEconomic Geology, 1983
- The Geology of the Great 'Dyke', Zimbabwe: The Ultramafic RocksJournal of Petrology, 1982
- Igneous Petrology of the Synorogenic Fongen-Hyllingen Layered Basic Complex, South-Central Scandinavian CaledonidesJournal of Petrology, 1981
- Chapter 8. Magmatic Infiltration Metasomatism, Double-Diffusive Fractional Crystallization, and Adcumulus Growth in the Muskox Intrusion and other Layered IntrusionsPublished by Walter de Gruyter GmbH ,1980
- The origin of rhythmic layeringMineralogical Magazine, 1978