Pseudomorphs after olivine in Markle basalt
Published online by Cambridge University Press: 14 March 2018
Summary
Pseudomorphs after olivine in Markle basalt from Holyrood Park, Edinburgh, consist of an intimate mixture of hematite and chlorite, along with a small percentage of quartz. A definite relationship exists between the orientations of the two main constituents and is dependent upon their structures.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 32 , Issue 247 , December 1959 , pp. 324 - 331
- Copyright
- Copyright © 1959, The Mineralogical Society
References
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