Classification |
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Species: | 'Columbite-(Fe)-Columbite-(Mn) Series' (not an IMA approved species) |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Columbite-(Fe)-Columbite-(Mn) Series data |
Locality Data: | Click here to view Pegmatite field, Argelès-sur-Mer, Céret, Pyrénées-Orientales, Occitanie, France |
Data Identifiers |
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Mindat Occurrence Record ID: | 888025 |
Long-form Identifier: | 1:3:888025:3 |
GUID (UUID V4): | f25370c1-0a21-4c6e-b96c-9629514eda8f |
References |
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Berbain, Christian, Riley, Tim, Favreau, Georges, Meisser, Nicolas, Wyart, Jean, Mills, Stuart (2012) Phosphates des pegmatites du massif des Albères (Pyrénées-Orientales) [Phosphates from pegmatites of the Albères massif (Pyrénées-Orientales)], in Special Phosphates. Le Cahier des Micromonteurs 117(3), 121-172 |
Reference Search (possible matching items) |
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| | Journal (article/letter/editorial) | DOI: 10.3749/canmin.1600075 THE SVECONORWEGIAN PEGMATITE PROVINCE – THOUSANDS OF PEGMATITES WITHOUT PARENTAL...Sveconorwegian pegmatite province in southern Norway and southwest Sweden hosts seven rareelement pegmatite districts...magmatism during post-orogenic extension. The pegmatite formation principally comprises four periods restricted...sectors). The observed relationships between pegmatite formation and regional high-grade metamorphism...In light of this, the genetic criteria of the pegmatite family classification scheme [NYF versus Lithium-Cesium-Tantalum | | | Thesis/Dissertation | respectively. The Lindvikskollen pegmatite area was the focus of field work and sampling of rocks and tourmalines...in the area. In the case of the Lindvikskollen pegmatite, which intruded a metagabbro body and its albitized...tourmaline and bulk rock chemistry indicates that the pegmatite was probably formed by mixed partial melting of...albitite host rocks. In addition, the nearby Tangen pegmatite intrudes the same metagabbro, and its overlapping...host rock tourmaline-bearing gneiss to be the pegmatite melt source. This thesis concludes that the source |
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