Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin
The Cauvery sedimentary basin of India, a part of the Eastern Continental Margin of India (ECMI), has evolved as a consequence of its breakup from East Antarctica in the early Cretaceous. This study covers approximately 10,000 km2 in the southern part of the Cauvery basin. A total of 5,161 gravity-m...
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Frontiers Media S.A.
2023-07-01
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| Series: | Frontiers in Earth Science |
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| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2023.1190106/full |
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| author | Shuva Shankha Ganguli Sanjit K. Pal |
| author_facet | Shuva Shankha Ganguli Sanjit K. Pal |
| author_sort | Shuva Shankha Ganguli |
| collection | DOAJ |
| description | The Cauvery sedimentary basin of India, a part of the Eastern Continental Margin of India (ECMI), has evolved as a consequence of its breakup from East Antarctica in the early Cretaceous. This study covers approximately 10,000 km2 in the southern part of the Cauvery basin. A total of 5,161 gravity-magnetic observations were made in an area bounded by 78°–79°E longitude and 9°–10°N latitude. The gravity anomaly map shows a dominant NE-SW trend with a total relief of 83 mGal from −77 mGal to 6 mGal. The map reveals very prominent NE-SW trending linear gravity high bands and two circular/elliptical gravity lows around Madurai and Ramanathapuram, respectively. The residual gravity map reveals NE-SW trending alternative bands of gravity highs and lows, revealing a ridge-depression structure. The gravity modeling shows the presence of underplated material, which may be related to magmatic activity during the Cretaceous. The magnetic map reveals two prominent E-W trending linear structures, which probably represent the disposition of a shear zone under the Cauvery Basin. Based on the filtered magnetic and gravity map, we have prepared an interpreted basement geology map. The magnetic map and residual gravity map suggest that the basement rock of the basin is crystalline (granite/gneiss) and may not comprise a high-grade metamorphic rock Eastern Ghat Orogeny. |
| first_indexed | 2024-03-12T23:04:15Z |
| format | Article |
| id | doaj.art-f55b287499b843f495390570cf241eae |
| institution | Directory Open Access Journal |
| issn | 2296-6463 |
| language | English |
| last_indexed | 2024-03-12T23:04:15Z |
| publishDate | 2023-07-01 |
| publisher | Frontiers Media S.A. |
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| series | Frontiers in Earth Science |
| spelling | doaj.art-f55b287499b843f495390570cf241eae2023-07-19T07:04:12ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632023-07-011110.3389/feart.2023.11901061190106Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted marginShuva Shankha Ganguli0Sanjit K. Pal1PSS-P&M-I, Geological Survey of India, Kolkata, IndiaDepartment of Applied Geophysics, Indian Institute of Technology (Indian School of Mines), Dhanbad, IndiaThe Cauvery sedimentary basin of India, a part of the Eastern Continental Margin of India (ECMI), has evolved as a consequence of its breakup from East Antarctica in the early Cretaceous. This study covers approximately 10,000 km2 in the southern part of the Cauvery basin. A total of 5,161 gravity-magnetic observations were made in an area bounded by 78°–79°E longitude and 9°–10°N latitude. The gravity anomaly map shows a dominant NE-SW trend with a total relief of 83 mGal from −77 mGal to 6 mGal. The map reveals very prominent NE-SW trending linear gravity high bands and two circular/elliptical gravity lows around Madurai and Ramanathapuram, respectively. The residual gravity map reveals NE-SW trending alternative bands of gravity highs and lows, revealing a ridge-depression structure. The gravity modeling shows the presence of underplated material, which may be related to magmatic activity during the Cretaceous. The magnetic map reveals two prominent E-W trending linear structures, which probably represent the disposition of a shear zone under the Cauvery Basin. Based on the filtered magnetic and gravity map, we have prepared an interpreted basement geology map. The magnetic map and residual gravity map suggest that the basement rock of the basin is crystalline (granite/gneiss) and may not comprise a high-grade metamorphic rock Eastern Ghat Orogeny.https://www.frontiersin.org/articles/10.3389/feart.2023.1190106/fullgravity-magneticcauvery basineastern continental margin of India (ECMI)regional-residual analysisgravity modeling |
| spellingShingle | Shuva Shankha Ganguli Sanjit K. Pal Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin Frontiers in Earth Science gravity-magnetic cauvery basin eastern continental margin of India (ECMI) regional-residual analysis gravity modeling |
| title | Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin |
| title_full | Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin |
| title_fullStr | Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin |
| title_full_unstemmed | Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin |
| title_short | Gravity-magnetic appraisal of the southern part of the Cauvery Basin, Eastern Continental Margin of India (ECMI): evidence of a volcanic rifted margin |
| title_sort | gravity magnetic appraisal of the southern part of the cauvery basin eastern continental margin of india ecmi evidence of a volcanic rifted margin |
| topic | gravity-magnetic cauvery basin eastern continental margin of India (ECMI) regional-residual analysis gravity modeling |
| url | https://www.frontiersin.org/articles/10.3389/feart.2023.1190106/full |
| work_keys_str_mv | AT shuvashankhaganguli gravitymagneticappraisalofthesouthernpartofthecauverybasineasterncontinentalmarginofindiaecmievidenceofavolcanicriftedmargin AT sanjitkpal gravitymagneticappraisalofthesouthernpartofthecauverybasineasterncontinentalmarginofindiaecmievidenceofavolcanicriftedmargin |