Reference Type | Journal (article/letter/editorial) |
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Title | Clinobisvanite, eulytite, and namibite from the pala pegmatite district, San Diego Co., California, USA |
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Journal | Mineralogical Magazine | ISSN | 0026-461X |
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Authors | Foord, Eugene E. | Author |
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Year | 1996 (April) | Volume | 60 |
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Issue | 399 |
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Publisher | Mineralogical Society |
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Download URL | https://rruff.info/doclib/MinMag/Volume_60/60-399-387.pdf+ |
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DOI | doi:10.1180/minmag.1996.060.399.14Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 38 | Long-form Identifier | mindat:1:5:38:7 |
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|
GUID | 0 |
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Full Reference | Foord, Eugene E. (1996) Clinobisvanite, eulytite, and namibite from the pala pegmatite district, San Diego Co., California, USA. Mineralogical Magazine, 60 (399) 387-388 doi:10.1180/minmag.1996.060.399.14 |
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Plain Text | Foord, Eugene E. (1996) Clinobisvanite, eulytite, and namibite from the pala pegmatite district, San Diego Co., California, USA. Mineralogical Magazine, 60 (399) 387-388 doi:10.1180/minmag.1996.060.399.14 |
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In | (1996, April) Mineralogical Magazine Vol. 60 (399) Mineralogical Society |
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Abstract/Notes | The 100 Ma complex LCT-type composite pegmatite- aplite dykes, intruded into various units of the Southern California Batholith, are known to contain bismuth minerals. Jahns and Wright (1951) reported the following primary and secondary bismuth minerals from the quartz-rich cores of a number of dykes in the Pala district, San Diego Co., California: native bismuth, bismuthinite, bismite, bismutite, and beyerite. |
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