Madhavaraju, J.; Ramasamy, S.; Mohan, S.P.; Asir, N. Gladwin Gnana (2002) Ooids in Sillakkudi Formation of Ariyalur Group of Tiruchirapalli Cretaceous, Tamil Nadu: Implications for Origin and Depositional Environment. Journal of the Geological Society of India, 60 (3). 317-322 doi:10.17491/jgsi/2002/600308
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Ooids in Sillakkudi Formation of Ariyalur Group of Tiruchirapalli Cretaceous, Tamil Nadu: Implications for Origin and Depositional Environment | ||
| Journal | Journal of the Geological Society of India | ||
| Authors | Madhavaraju, J. | Author | |
| Ramasamy, S. | Author | ||
| Mohan, S.P. | Author | ||
| Asir, N. Gladwin Gnana | Author | ||
| Year | 2002 (September 1) | Volume | 60 |
| Page(s) | 317-322 | Issue | 3 |
| Publisher | Geological Society of India | Place | Bangaluru, India |
| URL | |||
| DOI | doi:10.17491/jgsi/2002/600308Search in ResearchGate | ||
| Generate Citation Formats | |||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 19391372 | Long-form Identifier | mindat:1:5:19391372:3 |
| GUID | 0 | ||
| Full Reference | Madhavaraju, J.; Ramasamy, S.; Mohan, S.P.; Asir, N. Gladwin Gnana (2002) Ooids in Sillakkudi Formation of Ariyalur Group of Tiruchirapalli Cretaceous, Tamil Nadu: Implications for Origin and Depositional Environment. Journal of the Geological Society of India, 60 (3). 317-322 doi:10.17491/jgsi/2002/600308 | ||
| Plain Text | Madhavaraju, J.; Ramasamy, S.; Mohan, S.P.; Asir, N. Gladwin Gnana (2002) Ooids in Sillakkudi Formation of Ariyalur Group of Tiruchirapalli Cretaceous, Tamil Nadu: Implications for Origin and Depositional Environment. Journal of the Geological Society of India, 60 (3). 317-322 doi:10.17491/jgsi/2002/600308 | ||
| In | (2002, September) Journal of the Geological Society of India Vol. 60 (3). Geological Society of India | ||
| Abstract/Notes | Abstract An ooid-rich limestone band of Sillakkudi Formation is encountered in a well section near Ariyalur. The ooids are believed to be deposited in a marine regime. They contain berthierine as the major mineral and haematite, siderite and quartz as minor minerals. They exhibit alternate rings of berthierine and haematite which shows that these minerals were developed under changing physico-chemical conditions. In the present paper, the petrographical characters, mineralogy, origin and depositional environment of the ooids are discussed. | ||
See Also
These are possibly similar items as determined by title/reference text matching only.
