| Reference Type | Journal (article/letter/editorial) |
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| Title | The origin of heteradcumulate and adcumulate textures in the Jimberlana Norite |
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| Journal | Geological Magazine |
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| Authors | Campbell, I. H. | Author |
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| Year | 1968 (August) | Volume | 105 |
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| Issue | 4 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800054431Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 249962 | Long-form Identifier | mindat:1:5:249962:2 |
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| GUID | 0 |
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| Full Reference | Campbell, I. H. (1968) The origin of heteradcumulate and adcumulate textures in the Jimberlana Norite. Geological Magazine, 105 (4) 378-383 doi:10.1017/s0016756800054431 |
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| Plain Text | Campbell, I. H. (1968) The origin of heteradcumulate and adcumulate textures in the Jimberlana Norite. Geological Magazine, 105 (4) 378-383 doi:10.1017/s0016756800054431 |
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| In | (1968, August) Geological Magazine Vol. 105 (4) Cambridge University Press (CUP) |
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| Abstract/Notes | SUMMARYIn the Jimberlana Norite the heteradcumulate and adcumulate rocks are found in adjacent layers. The heteradcumulate occur immediately before the heterad minerals appear as cumulus grains in an adcumulate rock. It is considered that both heteradcumulate and adcumulate textures result from supercooling in the magma. Heteradcumulates develop when seeds of the heterad mineral are not available in the magma and adcumulates after they have formed. |
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