The magnetic properties and differentiation of dolerite sills; a critical discussion

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ID: 299098
1956
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Abstract
Takes exception to the hypothesis that differentiation in thick dolerite sills takes place by a stoping mechanism involving the settling of relatively large blocks of crystal mush, as proposed in a recent paper by Jaeger and Joplin, rather than by gravitational settling of individual crystals. A rejoinder by Jaeger and Joplin, and further discussion by H. H. Hess are appended.
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openalex_W1976097320 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors F. Walker, J. C. Jaeger, Germaine A. Joplin, H. H. Hess
Journal american journal of science
Year 1956
DOI
10.2475/ajs.254.7.433
URL
https://ajs.scholasticahq.com/article/58612.pdf
Keywords Keywords not found

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