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Field photographs of Ninama Basin. (a) Sukhbhadar river at Ninama village exposing Sukhbhadar Formation and Ninama Limestone. (b) Ninama well comprising of Sukhbahadar Formation with lithic arenite bands. (c) Ninama hill exposing Ninama limestone intercalated with calcareous shale, and topped by grey limestone (Hammer length = 33cm). (d) Thin siltstone layer intercalated with the mudstone of Sukhbhadar Formation in Sukhbhadar stream section (Ruler length = 15cm). (e) Motamatra well section, lower Sukhbhadar Formation and Ninama Limestone overlain by basalt.

Field photographs of Ninama Basin. (a) Sukhbhadar river at Ninama village... Available to Purchase

Published: 01 September 2023
Fig. 5. Field photographs of Ninama Basin. (a) Sukhbhadar river at Ninama village exposing Sukhbhadar Formation and Ninama Limestone. (b) Ninama well comprising of Sukhbahadar Formation with lithic arenite bands. (c) Ninama hill exposing Ninama limestone intercalated with calcareous shale
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(a) Sub-provinces of the DVP of India with infratrappean, intertrappean, intratrappean, and supratrappean localities, (modified after Deshmukh and Sehagal, 1988, Mahoney, 1988; Kapur et al., 2018; Kapur and Khosla, 2019; Kale, Dole, et al., 2020; Mittal, 2021). (b) Geological map of Saurashtra (modified after Khan and Ahmad, 1998) with studied sections of intra-, intertrappeans, 1. Ninama hill section (N 22° 18' 14.58"; E 71° 19' 46.272"; 2.Ninama Sukhbhadar stream (N 22° 17' 59.73"; E 71° 20' 03.66"); 3. Ninama well section (N 22° 18' 11.81"; E 71° 19' 59.19"); 4.Motamatra well section (N 22° 15' 52.25"; E 71° 23' 02.89"); 5. Motamatra road section (N 22° 16' 00"; E 71° 22’ 48.36"); 6. Sekhdod hill (N 22° 16' 24.24"; E 71° 20’ 51.72"); 7. Lakhavad (N 22° 15' 18.86"; E 71° 19' 6.6"); 8. Chanpa hill section (N 22° 24' 41.328"; E 71° 09' 45.288"); 9. Bamanbor - Navagam section (N 22° 25' 17.287’; E 71° 03' 19.26); 10. Bamanbor road cut section (N 22° 22' 40.44"; E 71° 03' 27.899"); 11. Rangpar section (GIDC) (N 22° 26' 57.84"; E 71° 03' 58.859"); 12. Redren industry section (N 22° 27' 12.21"; E 71° 03' 39.01"); 13. Garida road section (N 22° 28' 42.24"; E 71° 02' 49.74"); 14. Jalida section (N 22° 27' 40.931"; E 71° 01' 26.112"); 15. Jalsika road section (N 22° 29' 11.83"; E 70° 58' 35.43").

(a) Sub-provinces of the DVP of India with infratrappean, intertrappean, i... Available to Purchase

Published: 01 September 2023
map of Saurashtra (modified after Khan and Ahmad, 1998 ) with studied sections of intra-, intertrappeans, 1. Ninama hill section (N 22° 18' 14.58"; E 71° 19' 46.272"; 2.Ninama Sukhbhadar stream (N 22° 17' 59.73"; E 71° 20' 03.66"); 3. Ninama well section (N 22° 18' 11.81"; E 71° 19' 59.19"); 4
Journal Article

Lithostratigraphy of the Paleogene Deccan Intra-, Intertrappeans of the Saurashtra, Western India and their Prevalence in Large Igneous Provinces Available to Purchase

Satish J. Patel, Nishi H. Shah
Published: 01 September 2023
Jour. Geol. Soc. India (2023) 99 (9): 1199–1210.
DOI: https://doi.org/10.1007/s12594-023-2452-4
...Fig. 5. Field photographs of Ninama Basin. (a) Sukhbhadar river at Ninama village exposing Sukhbhadar Formation and Ninama Limestone. (b) Ninama well comprising of Sukhbahadar Formation with lithic arenite bands. (c) Ninama hill exposing Ninama limestone intercalated with calcareous shale...
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View PDF for article title, Lithostratigraphy of the Paleogene Deccan Intra-, Intertrappeans of the Saurashtra, Western India and their Prevalence in Large Igneous Provinces
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Aquilapollenites and other triprojectate pollen from the Late Cretaceous to Early Paleocene Deccan intertrappean deposits of India Available to Purchase

B. Samant, D.M. Mohabey, K.N. Paudayal
Journal: Palynology
Published: 01 December 2013
Palynology (2013) 37 (2): 298–315.
DOI: https://doi.org/10.1080/01916122.2013.787125
...) 10. Aquilapollenites proteus Jansonius & Hills 1976 in Simpson emend. Srivastava 1975 Krishna-Cauvery Basin, Ninama IT Prasad & Pundeer (2002) ; Present study 11. Aquilapollenites pachypolus Martin 1968 Cauvery Basin Krishna-Godavari Basin Mehrotra et al. (2002 , 2005...
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View PDF for article title, Aquilapollenites and other triprojectate pollen from the Late Cretaceous to Early Paleocene Deccan intertrappean deposits of India
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Flood basalt structures and textures as guides to cooling histories and palaeoclimates: the Deccan Traps of Saurashtra, western India Available to Purchase

Hetu Sheth, Raymond A. Duraiswami, Vivek Ghule, Anmol Naik, Tarulata Das
Published: 16 May 2022
Geological Magazine (2022) 159 (8): 1415–1436.
DOI: https://doi.org/10.1017/S0016756822000279
...) is 15 cm long. Besides these, such flows are also found, for example, at Osham Hill at 21° 37′ 53.6″ N, 70° 17′ 30.7″ E. Fig. 4. Features of sheet lobes exposed 3 km southwest of Talaja on the road to Mahuva. Location of the outcrop is 21° 19′ 59.9″ N, 72° 00′ 49.4″ E, elevation 36 m...
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View PDF for article title, Flood basalt structures and textures as guides to cooling histories and palaeoclimates: the Deccan Traps of Saurashtra, western India
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Journal Article

Palynology of the uppermost Cretaceous to lowermost Paleocene Deccan volcanic associated sediments of the Mandla Lobe, central India Available to Purchase

Deepali Thakre, Bandana Samant, Dhananjay M. Mohabey, Steven R. Manchester, Satish Sangode
Journal: Palynology
Published: 08 April 2024
Palynology (2024) 48 (2): 2288669.
DOI: https://doi.org/10.1080/01916122.2023.2288669
... Stover & Partridge 1973 23 Heteroclavatus gen.et sp. nov 24 Heteroclavatus chitaleyae sp. nov. 25 Inaperturopollenites sp. 26 Incrotonipollis neyvelii ( Baksi, Deb & Siddhanta) Jansonius & Hills 1981 27 Intertrappeapollis gen. et. sp. nov. 28...
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View PDF for article title, Palynology of the uppermost Cretaceous to lowermost Paleocene Deccan volcanic associated sediments of the Mandla Lobe, central India
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Journal Article

The Deccan Volcanic Province (DVP), India: A Review: Part 2: Geochemistry, petrological evolution, petrogenesis, mantle sources, age and erupted volume relations, Upper Cretaceous-Palaeogene (K-Pg) mass extinctions, economic aspects, summary and future studies in DVP Available to Purchase

P. Krishnamurthy
Published: 01 August 2020
Jour. Geol. Soc. India (2020) 96 (2): 111–147.
DOI: https://doi.org/10.1007/s12594-020-1521-1
... by fractional crystallisation of olivine, clinopyroxene and plagioclase mentioned previously. The Bhimashankar Formation is one of the thinner formations (c. 150 m) within this Subgroup and contains only two flows, namely a plagiophyric type (c. 140 m) overlain by the Giravili and Monkey Hill GPBs ( Khadri et...
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View PDF for article title, The Deccan Volcanic Province (DVP), India: A Review: Part 2: Geochemistry, petrological evolution, petrogenesis, mantle sources, age and erupted volume relations, Upper Cretaceous-Palaeogene (K-Pg) mass extinctions, economic aspects, summary and future studies in DVP
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Add to Citation Manager for The Deccan Volcanic Province (DVP), India: A Review: Part 2: Geochemistry, petrological evolution, petrogenesis, mantle sources, age and erupted volume relations, Upper Cretaceous-Palaeogene (K-Pg) mass extinctions, economic aspects, summary and future studies in DVP