Distinctive compositional characteristics and evolutionary trend of Precambrian glaucony: Example from Bhalukona Formation, Chhattisgarh basin, India
• Glaucony usually formed in a shallow marine environment in the Precambrian. • Precambrian glaucony exhibits high K2O, Al2O3 and MgO and low Fe2O3 contents. • Maturation of glaucony takes place by the addition of total Fe2O3 at a constant K2O. • ‘Pseudomorphic replacement’ theory explains origin of...
Ausführliche Beschreibung
Autor*in: |
Banerjee, Santanu [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2015 |
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Schlagwörter: |
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Umfang: |
16 |
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Übergeordnetes Werk: |
Enthalten in: OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study - Salunkhe, R. ELSEVIER, 2017, Amsterdam [u.a.] |
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Übergeordnetes Werk: |
volume:271 ; year:2015 ; pages:33-48 ; extent:16 |
Links: |
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DOI / URN: |
10.1016/j.precamres.2015.09.026 |
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Distinctive compositional characteristics and evolutionary trend of Precambrian glaucony: Example from Bhalukona Formation, Chhattisgarh basin, India |
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• Glaucony usually formed in a shallow marine environment in the Precambrian. • Precambrian glaucony exhibits high K2O, Al2O3 and MgO and low Fe2O3 contents. • Maturation of glaucony takes place by the addition of total Fe2O3 at a constant K2O. • ‘Pseudomorphic replacement’ theory explains origin of glaucony. |
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• Glaucony usually formed in a shallow marine environment in the Precambrian. • Precambrian glaucony exhibits high K2O, Al2O3 and MgO and low Fe2O3 contents. • Maturation of glaucony takes place by the addition of total Fe2O3 at a constant K2O. • ‘Pseudomorphic replacement’ theory explains origin of glaucony. |
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• Glaucony usually formed in a shallow marine environment in the Precambrian. • Precambrian glaucony exhibits high K2O, Al2O3 and MgO and low Fe2O3 contents. • Maturation of glaucony takes place by the addition of total Fe2O3 at a constant K2O. • ‘Pseudomorphic replacement’ theory explains origin of glaucony. |
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10.1016/j.precamres.2015.09.026 |
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2024-07-06T20:05:25.114Z |
_version_ |
1803861439402737664 |
fullrecord_marcxml |
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