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Geochemical characterization of miocene core sediments from Shahbazpur gas-wells (Bangladesh) in terms of elemental abundances by instrumental neutron activation analysis.
- Source :
- Journal of Radioanalytical & Nuclear Chemistry; Jul2021, Vol. 329 Issue 1, p239-252, 14p, 1 Color Photograph, 1 Illustration, 3 Charts, 7 Graphs
- Publication Year :
- 2021
-
Abstract
- Geochemical characterization of Shahbazpur structure (Bengal Foredeep) in terms of elemental abundances obtained from INAA are presented by investigating core samples from Shabazpur gas-field, Bangladesh. Major oxides' abundances were 12.4–20.8, 0.63–1.03, 4.45–8.02, 0.05–0.09, 2.60–4.10 and 1.31–1.87% for Al<subscript>2</subscript>O<subscript>3</subscript>, TiO<subscript>2</subscript>, Fe<subscript>2</subscript>O<subscript>3</subscript>(T), MnO, K<subscript>2</subscript>O and Na<subscript>2</subscript>O, respectively. Elemental ratios and enrichment pattern (× 1.10–2.11 UCC) indicate that sedimentary processes originated from Himalayan felsic source-rock. Weathering index and Th/U(= 5.90–6.59), V/Cr(= 1.07–1.38) ratios revel that sediments/rocks were experienced moderate to high degree of chemical weathering with oxidizing environment. La-Th-Sc immobile trace elements diagram invoke depositional tectonic settings which was transitional between active and passive continental margin. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 02365731
- Volume :
- 329
- Issue :
- 1
- Database :
- Complementary Index
- Journal :
- Journal of Radioanalytical & Nuclear Chemistry
- Publication Type :
- Academic Journal
- Accession number :
- 151918497
- Full Text :
- https://doi.org/10.1007/s10967-021-07770-4