An X-ray examination of the displacive transformation analbite-monalbite-analbite in the plagioclases at temperatures up to 1100° C.
I tiakina i:
| Kaituhi matua: | |
|---|---|
| Hōputu: | Pukapuka |
| Reo: | Ingarihi |
| I whakaputaina: |
Zurich
1961
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| Ngā Tūtohu: |
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Ngā tūemi rite: An X-ray examination of the displacive transformation analbite-monalbite-analbite in the plagioclases at temperatures up to 1100° C.
- X-ray studies in the plagioclases 1. Lattice changes in heat-treated plagioclases - the existence of monalbite at room temperature. - 2. The crystallographic and petrologic significance of peristerite unmixing in the acid plagioclases
- Low-Temperature x-ray diffraction.
- High-Temperature x-ray Diffraction Techniques.
- X-RAYS
- Crystals and X-Rays.
- Studies of developmental anomalies in the descendants of X-rayed mice