dc.contributor.author |
Mahender, K. |
|
dc.contributor.author |
Fernandes, B. |
|
dc.date.accessioned |
2015-06-03T08:09:01Z |
|
dc.date.available |
2015-06-03T08:09:01Z |
|
dc.date.issued |
2002 |
|
dc.identifier.citation |
Recent Researches on the Proterozoic Basins of India, Ed. by: R. Guhey, P. Thakur, R. Sridhar Rao. Govt. Science College, Raipur. 2002; 17-25. |
en_US |
dc.identifier.uri |
http://irgu.unigoa.ac.in/drs/handle/unigoa/1503 |
|
dc.description.abstract |
The Late Proterozoic Cave-Temple Arenite member of Badami Group comprising predominantly of sandstone forms one of the most interesting litho-units exposed around Badami for its prominent topographic expression (flat topped barren hillocks) along with a host of sedimentary structures viz. Cross-bedding, ripple marks, groove casts, convolute lamination etc. These sandstones are medium to coarse grained, moderate well sorted, subrounded to well rounded and belong to the quartz arenite to sub-arkose categories. Compositionally these rocks show considerabie maturity with abundant quartz (78-96 percent) and subordinate feldspars having undergone both the physical (compaction and pressure solution) and chemical (silica, calcite and hematite cementation) diagenetic changes. Mineralogical composition of these sandstones indicates a principal recycled orogen source. The variety of sedimentary structures and the textural characters suggest a shallow marine depositional environment of the sandstones. |
|
dc.subject |
Earth Science |
en_US |
dc.title |
Petrography, diagenesis and depositional environment of the Late Proterozoic cave-temple arenites of Badami Group, Karnataka |
en_US |
dc.type |
Conference article |
en_US |