| Reference Type | Journal (article/letter/editorial) |
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| Title | Fluid Inclusion Study of Vinjamuru Precambrian Stratiform Baryte Deposit, Nellore Schist Belt, A.P., India |
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| Journal | Journal Geological Society of India |
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| Authors | Moeen, S. | Author |
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| Year | 1992 (August 1) | Volume | 40 |
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| Page(s) | 162-168 | Issue | 2 |
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| Publisher | Geological Society of India | Place | Bangaluru, India |
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| URL | |
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| DOI | doi:10.17491/jgsi/1992/400207Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 18245213 | Long-form Identifier | mindat:1:5:18245213:4 |
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| GUID | 0 |
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| Full Reference | Moeen, S. (1992) Fluid Inclusion Study of Vinjamuru Precambrian Stratiform Baryte Deposit, Nellore Schist Belt, A.P., India. Journal Geological Society of India, 40 (2). 162-168 doi:10.17491/jgsi/1992/400207 |
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| Plain Text | Moeen, S. (1992) Fluid Inclusion Study of Vinjamuru Precambrian Stratiform Baryte Deposit, Nellore Schist Belt, A.P., India. Journal Geological Society of India, 40 (2). 162-168 doi:10.17491/jgsi/1992/400207 |
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| In | (1992, August) Journal of the Geological Society of India Vol. 40 (2). Geological Society of India |
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| Abstract/Notes | Abstract
The fluid inclusions in Vinjamuru baryte can be broadly classified into primary and pseudo-secondary types. Primary inclusions are represented by monophase carbonic and mixed carbonic-aqueous types. CO2 densities lie in the range of 0.78-0.88 g/cm3. The pseudo-secondary inclusions are represented by aqueous bi-phase type, coexisting with vapor-rich inclusions. Their Th overlaps in the range of 220-230°C suggestive of entrapment from boiling fluids. The primary carbonic inclusions appear to be volcanic entrapments and the fluids in pseudo-secondary inclusions were entrapped from hydrothermal solutions. |
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