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Wasim, S. M.
- Facies Controlled Diagenetic Evolution of the Delhi Group Sandstones, Bayana Basin, Rajasthan
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Affiliations
1 Department of Geology, Aligarh Muslim University, Aligarh - 202 002, IN
1 Department of Geology, Aligarh Muslim University, Aligarh - 202 002, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 77, No 3 (2011), Pagination: 261-268Abstract
The Bayana Basin forms the eastern most limit of north Delhi fold belt covering parts of northeastern Rajasthan. The deposition of sediments took place during middle Proterozoic in fluvial and shallow marine environments. The rocks are mainly clastics and include conglomerate, sandstone and shale. During mechanical compaction rearrangement of grains took place and point and long contacts were formed. The sandstones are cemented by iron oxide, silica, carbonate and barite. The porosity has developed due to dissolution of iron, carbonate cement and feldspar grains. Dissolution of quartz along grain boundaries and silica rich compaction pore water seems to be the main source of silica. These observations suggest progressive compaction which initiated at the sediment water interface and continued till deep burial diagenesis in a rapidly subsiding basin.Keywords
Facies Controlled Diagenetic Evolution, Delhi Group, Bayana Basin, Rajasthan.- Some Foraminiferal Taxa in the Middle to Late Jurassic Sediments of Kaiya Dome, Kutch
Abstract Views :180 |
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Authors
Affiliations
1 Department of Geology, Aligarh Muslim University, Aligarh - 202 002, IN
2 K-69, Gyansarover, Aligarh - 202 002, IN
3 Department of Geology, Dharam Samaj College, Aligarh - 202 001, IN
4 Paleontology Lab, KDMIPE, ONGC Ltd., 9, Kaulagarh Road, Dehradun - 248 195, IN
1 Department of Geology, Aligarh Muslim University, Aligarh - 202 002, IN
2 K-69, Gyansarover, Aligarh - 202 002, IN
3 Department of Geology, Dharam Samaj College, Aligarh - 202 001, IN
4 Paleontology Lab, KDMIPE, ONGC Ltd., 9, Kaulagarh Road, Dehradun - 248 195, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 79, No 2 (2012), Pagination: 161-168Abstract
The Chari Formation exposed at Kaiya Dome, Kutch yielded a foraminiferal assemblage comprising 41 species dominated by the family Vaginulinidae. A systematic account of 11 species, reported for the first time form the Indian subcontinent, is presented. The foraminiferal assemblage is employed for preliminary interpretations regarding age, palaeoecology, and palaeobiogeography. The assemblage suggests a Callovian to Oxfordian age for the exposed sequence at Kaiya Dome. A near shore, open marine environment ranging from mid to outer shelf with fluctuating strandline is interpreted on the basis of the recovered foraminiferal assemblage. The Kaiya Dome foraminiferal assemblage exhibits a Tethyan affinity and suggests that the Kutch region, along with neighbouring regions, was engulfed by a shallow southwestern arm of Tethys during Middle to Late Jurassic times.Keywords
Jurassic Foraminifera, First Report, Systematics, Age, Palaeoecology, Palaeobiogeography, Kutch.References
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