Rai, A.K.; Himadri, Basu; Zakaulla, S.; Umamaheswar, K. (2008) A Discussion on the Physico-chemical Factors for the Development of Pits in Gulcheru Quartzite in the Southwestern Margin of Cuddapah Basin, A.P. Journal of the Geological Society of India, 72 (4). 467-470 doi:10.17491/jgsi/2008/720404
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | A Discussion on the Physico-chemical Factors for the Development of Pits in Gulcheru Quartzite in the Southwestern Margin of Cuddapah Basin, A.P. | ||
| Journal | Journal of the Geological Society of India | ||
| Authors | Rai, A.K. | Author | |
| Himadri, Basu | Author | ||
| Zakaulla, S. | Author | ||
| Umamaheswar, K. | Author | ||
| Year | 2008 (October 1) | Volume | 72 |
| Page(s) | 467-470 | Issue | 4 |
| Publisher | Geological Society of India | Place | Bangaluru, India |
| URL | |||
| DOI | doi:10.17491/jgsi/2008/720404Search in ResearchGate | ||
| Generate Citation Formats | |||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 19425022 | Long-form Identifier | mindat:1:5:19425022:3 |
| GUID | 0 | ||
| Full Reference | Rai, A.K.; Himadri, Basu; Zakaulla, S.; Umamaheswar, K. (2008) A Discussion on the Physico-chemical Factors for the Development of Pits in Gulcheru Quartzite in the Southwestern Margin of Cuddapah Basin, A.P. Journal of the Geological Society of India, 72 (4). 467-470 doi:10.17491/jgsi/2008/720404 | ||
| Plain Text | Rai, A.K.; Himadri, Basu; Zakaulla, S.; Umamaheswar, K. (2008) A Discussion on the Physico-chemical Factors for the Development of Pits in Gulcheru Quartzite in the Southwestern Margin of Cuddapah Basin, A.P. Journal of the Geological Society of India, 72 (4). 467-470 doi:10.17491/jgsi/2008/720404 | ||
| In | (2008, October) Journal of the Geological Society of India Vol. 72 (4). Geological Society of India | ||
| Abstract/Notes | Abstract Miniature pits of varying size and shape are found in the topmost arenaceous layers of the Gulcheru quartzite Though pits in sedimentary rocks form in a variety of ways, in clean beach sands they owe their origin to mainly physical processes Small pits, found in the Gulcheru quartzite, have been formed as a result of interplay of different physicochemical factors which prevailed in syn- as well as post-depositional environments In addition to different agents of physical weathering, which played a vital role in the formation of pits in the Gulcheru quartzite, syn-depositional precipitation of iron oxides and their syn- to post-dragenetic chemical changes are believed to be the main chemical factors | ||
See Also
These are possibly similar items as determined by title/reference text matching only.
