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Naik, Ashutosh
- A Revision of the Structure and Stratigraphy of Sargipali Area, Sundargarh District, Orissa
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Authors
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1 Department of Earth Sciences, Sambalpur University, Jyoti Vihar Burla, Sambalpur 768 019, IN
1 Department of Earth Sciences, Sambalpur University, Jyoti Vihar Burla, Sambalpur 768 019, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 68, No 2 (2006), Pagination: 269-276Abstract
The metasedtmenrary assemblage of Sargipali area In western pat of Sundargarh district is considered to be the western extension of Gangpur sequence Detailed mapping reveals the assemblage to be composed of a variety of rocks like conglomerate, quartzite, banded biotite schist, quartz- biotite schist, calc-gneiss, limestone etc folded in the form of a large syncline The order of superposition of beds established on the basis of the sedimentary structures and analysss of structural data is found to be just the reverse of the order suggested by earlier workers.Keywords
Structure, Stratigraphy, Revision, Sargipali Area, Sundargarh District, Orissa.- Magnetite Pebbles in the Conglomerate of Silpunji Area, Sundargarh District, Orissa
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Authors
Affiliations
1 Department of Mining Engineering, Regional Engineering College, Rouikela, Sundargarh, IN
2 Department of Earth Sciences, Sambalpur University, Jyoti Vihar, Burla, Sambalpur, IN
1 Department of Mining Engineering, Regional Engineering College, Rouikela, Sundargarh, IN
2 Department of Earth Sciences, Sambalpur University, Jyoti Vihar, Burla, Sambalpur, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 63, No 6 (2004), Pagination: 670-672Abstract
An unusual occurrence of magnetite pebbles of variable shapes and sizes is recorded in the matrix supported conglomerate band exposed around Silpunji, in the eastern part of Sundargarh district, Orissa. The metasediments (Chandiposh Group) with which the paraconglomerate band is associated, is intruded by 2809±12 Ma old Tamperkola Granite which suggests the conglomerate to be of Archaean period. Although Koira (Iron Ore) Group is very close to the Chandiposh Group, it is unlikely to be the source area for the magnetite pebbles, as Banded Iron Formation of Koira (Iron Ore). Group is dominantly haematitic in composition. The magnetite pebbles thus indirectly suggest the existence of a rock sequence other than Koira (Iron Ore) Group having iron ore bearing lithogic unit.- Contact Course on Shear Zones - Mapping and Analysis
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Authors
Affiliations
1 Department of Geology, University of Calcutta Kolkata - 700 019, IN
2 Department of Earth Sciences, Sambalpur University Jyott ViharPO Sambalpur - 768 019, IN
1 Department of Geology, University of Calcutta Kolkata - 700 019, IN
2 Department of Earth Sciences, Sambalpur University Jyott ViharPO Sambalpur - 768 019, IN