Samsuddin, M., Ramachandran, K. K., Dora, Y. L. (1992) Quartz Grain Surface Textures as Indicators of Depositional History of Beach and Strand Plain Sediments Along the North Kerala Coast. Journal Geological Society of India, 40 (6). 501-508 doi:10.17491/jgsi/1992/400602
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Quartz Grain Surface Textures as Indicators of Depositional History of Beach and Strand Plain Sediments Along the North Kerala Coast | ||
| Journal | Journal Geological Society of India | ||
| Authors | Samsuddin, M. | Author | |
| Ramachandran, K. K. | Author | ||
| Dora, Y. L. | Author | ||
| Year | 1992 (December 1) | Volume | 40 |
| Page(s) | 501-508 | Issue | 6 |
| Publisher | Geological Society of India | Place | Bangaluru, India |
| URL | |||
| DOI | doi:10.17491/jgsi/1992/400602Search in ResearchGate | ||
| Generate Citation Formats | |||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 18245870 | Long-form Identifier | mindat:1:5:18245870:9 |
| GUID | 0 | ||
| Full Reference | Samsuddin, M., Ramachandran, K. K., Dora, Y. L. (1992) Quartz Grain Surface Textures as Indicators of Depositional History of Beach and Strand Plain Sediments Along the North Kerala Coast. Journal Geological Society of India, 40 (6). 501-508 doi:10.17491/jgsi/1992/400602 | ||
| Plain Text | Samsuddin, M., Ramachandran, K. K., Dora, Y. L. (1992) Quartz Grain Surface Textures as Indicators of Depositional History of Beach and Strand Plain Sediments Along the North Kerala Coast. Journal Geological Society of India, 40 (6). 501-508 doi:10.17491/jgsi/1992/400602 | ||
| In | (1992, December) Journal of the Geological Society of India Vol. 40 (6). Geological Society of India | ||
| Abstract/Notes | Abstract SEM analysis of quartz grain surfaces from the strand plain show many of the characteristic textures that are produced under sub-aqueous environments with second generation features of wind action. It is inferred that the initial stage of deposition of the strand plain sediments was associated with a wave dominated environment. With emergence of this coast, the strand plain sediments were exposed to sub-aerial action, thus registering both sub-aqueous and sub-aerial action features. | ||
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