Locality type: | Intrusion |
Classification |
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Species: | Cancrinite |
Formula: | (Na,Ca,◻)8(Al6Si6O24)(CO3,SO4)2 · 2H2O |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Cancrinite data |
Locality Data: | Click here to view Mauze Intrusion, Africa |
Data Identifiers |
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Mindat Occurrence Record ID: | 1429820 |
Long-form Identifier: | 1:3:1429820:4 |
GUID (UUID V4): | a289ea31-1d53-4a22-bbd1-2e12333ee61f |
References |
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Reference Search (possible matching items) |
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| | Report (chapter) | traced southwards through Mozambique into South Africa, with the change in structural style corresponding...of the vicinity (Bloomfield 1965). The largest intrusion of the northern part of the province is the 22...the alluvial plain west of Lake Chilwa; this intrusion consists of syenite and quartz syenite and is...in Chikala and Chaone. Junguni is an isolated intrusion of nepheline syenite lying to the N of Mongolowe...are exposed in some small hills NE of the main intrusion where the country rocks show the effects of fenitization | | | Report (volume) | Island 269 FITTON, J. G. The Cameroon line, West Africa: a comparison between oceanic and continental alkaline... LARSEN, L. M. & SORENSEN, H. The Ilimaussaq intrusion--progressive crystallization and formation of...of the classic alkaline provinces, such as East Africa, southern Greenland and the Kola Peninsula, are...was subordinate or absent (e.g. the Ilimaussaq intrusion, Larsen & Serensen). The giant dykes, therefore...Kogarko (Kola Peninsula). The Cameroon line in West Africa (Fitton) includes both continental and oceanic |
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