57fe mössbauer spectroscopy study of organic rich sediments (source rocks) from test well ct-1, chinnewala structure of jaisalmer basin, india
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ID: 224053
2016
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Abstract
57Fe Mössbauer spectroscopic study was carried out on the organic rich sedimentary samples collected at different depth intervals from newly drilled test well Chinnewala Tibba-1 (CT-1) located in Jaisalmer Petroliferous basin India. It is found that iron is mainly distributed in high spin Fe3+ and Fe2+ state in clay minerals. The plot of Fe2+/(Fe2+ + Fe3+) indicates the presence of poor redox conditions in the samples. Results obtained are also compared with those already reported in the literature. This comparison shows that there may exist a correlation between prospecting of the basin, the redox environment in sediments and the nature of iron bearing minerals distributed in the sedimentary sequence.
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tripathi2016geoscience57fe
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| Authors | ;R.P. Tripathi;Beena Bhatia;R. Sharma;K.R. Patel;S.S. Meena;Girish Ganwani;S.C. Mathur |
| Journal | neuroscience research |
| Year | 2016 |
| DOI |
10.1016/j.gsf.2015.09.007
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