Abstract
Rock thermal conductivity is an essential parameter for the determination of heat flow of the Earth and geothermal modelling studies. It has important applications in hydrocarbon exploration, geothermal energy and geo-engineering investigations. We report thermal conductivity measurements of 55 core samples of Deccan flood basalt recovered from four boreholes KBH-1, KBH-5, KBH-6 and KBH-7 drilled in Koyna–Warna region of the western Deccan Volcanic Province (DVP). The cores represent a substantial thickness of the deep, unexposed sections of the Deccan basalt formation and allow sampling of the full spectrum of the compositional variations in the lava flows starting from the earliest flows in the region. We compare the data with those reported earlier from other parts of the DVP as well as with other continental flood basalt provinces worldwide. The salient results are as follows. (1) Thermal conductivity of flood basalts from the Koyna–Warna region fall in a relatively narrow range 1.29–1.87 Wm−1K−1 with a mean of 1.61±0.13 (SD) Wm−1K−1. When compared with massive basalt, the vesicular/amygdaloidal basalt samples show larger variability, likely due to the varying degrees of vesicularity and the composition of the secondary mineral fillings. (2) Thermal conductivity data obtained on a 1251-m long basalt core comprising 40 simple flows and 6 compound flows in the borehole KBH-7 yield a similar narrow range of 1.3–1.7 Wm−1K−1 and do not show any systematic trend with depth. (3) The conductivity range for basalts of the Koyna–Warna region is consistent with those reported previously from the northern, eastern and southeastern parts of the DVP including the Wardha–Yavatmal, Killari and Pune–Ahmednagar areas that expose basalt flows from different elevations and stratigraphic units. (4) The mean values of thermal conductivity of continental flood basalts from other flood basalt provinces worldwide such as Snake River Plain, Columbia River, Parana and Karoo are comparable to Deccan flood basalts.
Research Highlights
-
Thermal conductivity of Deccan flood basalts from Koyna region varies in a relatively narrow range 1.29–1.87 Wm-1K-1 with a mean of 1.61±0.13 (SD) Wm-1K-1.
-
Thermal conductivity data obtained on a 1251 m long, vertical, continuous basalt core do not show a systematic trend with depth.
-
The data is consistent with those reported previously from other parts of Deccan Traps.
-
Thermal conductivity data from continental flood basalt provinces worldwide including Columbia River, Parana, Karoo and Deccan Traps are comparable.
Similar content being viewed by others
References
Beane J E, Turner C A, Hooper P R, Subbarao K V and Walsh J N 1986 Stratigraphy, composition and form of the Deccan Basalts, Western Ghats, India; Bull. Volcanol. 48 61–83, https://doi.org/10.1007/BF01073513.
Behera L and Sen M K 2014 Tomographic imaging of sub-basalt Mesozoic sediments and shallow basement geometry for hydrocarbon potential below the Deccan Volcanic Province (DVP) of India; Geophys. J. Int. 199 296–314, https://doi.org/10.1093/gji/ggu261.
Birch F 1950 Flow of heat in the Front Range, Colorado; Bull. Geol. Soc. Am. 61 567–630.
Blackwell D D, Steele J L, Kelley S A and Korosec M 1990 Heat flow in the state of Washington and thermal conditions in the Cascade Range; J. Geophys. Res. 95(B12) 19,495–19,516, https://doi.org/10.1029/JB095iB12p19495.
Brott C A, Blackwell D D and Mitchell J C 1976 Heat flow study of the Snake River Plain region. Idaho; Idaho Dep. Water Resour. Water Inf. Bull. 30(8) 195, https://doi.org/10.2172/7300489.
Brott C A, Blackwell D D and Ziagos J P 1981 Thermal and tectonic implications of heat flow in the eastern Snake River Plain, Idaho; J. Geophys. Res. 86 11,709–11,734, https://doi.org/10.1029/JB086iB12p11709.
Chapman D S 1986 Thermal gradients in the continental crust; Geol. Soc. Spec. Publ. 24 63–70, https://doi.org/10.1144/GSL.SP.1986.024.01.07.
Coffin M F and Eldholm O 1994 Large igneous provinces: crustal structure, dimensions, and external consequences; Rev. Geophys. 32 1–36, https://doi.org/10.1029/93RG02508.
Courtillot V, Besse J, Vandamme D, Montigny R, Jaeger J J and Cappetta H 1986 Deccan flood basalts at the Cretaceous/Tertiary boundary?; Earth Planet Sci. Lett. 80 361–374, https://doi.org/10.1016/0012-821X(86)90118-4.
Courtillot V, Féraud G, Maluski H, Vandamme D, Moreau M G and Besse J 1988 Deccan flood basalts and the Cretaceous/Tertiary boundary; Nature 333 843–846, https://doi.org/10.1038/333843a0.
Cox K G and Hawkesworth C J 1985 Geochemical stratigraphy of the Deccan Traps at Mahabaleshwar, Western Ghats, India, with implications for open system magmatic processes; J. Petrol. 26(2) 355–377, https://doi.org/10.1093/petrology/26.2.355.
Drury M J 1987 Heat flow provinces reconsidered; Phys. Earth Planet. Inter. 49 78–96, https://doi.org/10.1016/0031-9201(87)90133-6.
Duncan R and Pyle D 1988 Rapid eruption of the Deccan flood basalts at the Cretaceous/Tertiary boundary; Nature 333 841–843, https://doi.org/10.1038/333841a0.
Fountain D M, Salisbury M H and Furlong K P 1987 Heat production and thermal conductivity of rocks from the Pikwitonei-Sachigo continental cross section, central Manitoba: Implications for the thermal structure of Archaean crust; Can. J. Earth Sci. 24 1583–1594, https://doi.org/10.1139/e87-154.
Furlong K and Chapman D S 1987 Crustal heterogeneities and the thermal structure of the continental crust; Geophys. Res. Lett. 14 314–317, https://doi.org/10.1029/GL014i003p00314.
GSI 1995 Geological Quadrangle Map (47G), Mahabaleshwar Quadrangle, Maharashtra; Scale: 1: 250,000.
GSI 2002 Geothermal Energy Resources of India; Geol. Soc. India Spec. Publ. 69 12–29.
Gupta H K, Arora K, Rao N P, Roy S and Tiwari V M et al. 2017 Investigations of continued reservoir triggered seismicity at Koyna, India; In: Tectonics of the Deccan Large Igneous Province (eds) Mukherjee S, Misra A A, Calve`s G and Nemčok M, Geol. Soc. London, Spec. Publ. 445 151–188, https://doi.org/10.1144/SP445.11.
Gupta M L and Gaur V K 1984 Surface heat flow and probable evolution of Deccan Volcanism; Tectonophys. 105 309–318, https://doi.org/10.1016/0040-1951(84)90210-5.
Hot Springs Committee Report 1968; Government of India, unpublished.
Huenges E, Burkhardt H and Erbas K 1990 Thermal conductivity profile of the KTB pilot corehole; Sci. Drill. 1 224–230.
Hurter S J and Pollack H N 1996 Terrestrial heat flow in the Parana Basin, southern Brazil; J. Geophys. Res. 101 8659–8671, https://doi.org/10.1029/95JB03743.
Jaupart C and Mareschal J C 2007 Heat flow and thermal structure of the lithosphere; In: Treatise on Geophysics (ed.) Schubert G, Elsevier Ltd., Oxford 6 217–252, https://doi.org/10.1016/b978-044452748-6.00104-8.
Jones M Q W 1992 Heat flow anomaly in Lesotho: Implications for the southern boundary of the Kaapvaal craton; Geophys. Res. Lett. 19 2031–2034, https://doi.org/10.1029/92GL02207.
Lachmar T E, Freeman T G, Kessler J A et al. 2019 Evaluation of the geothermal potential of the western Snake River Plain based on a deep corehole on the Mountain Home AFB near Mountain Home, Idaho; Geotherm. Energy 7 26, https://doi.org/10.1186.
Mahoney J J and Coffin M F 1997 Large igneous provinces: Continental, oceanic and planetary flood volcanism; AGU Geophys. Mono. 100 438, https://doi.org/10.1029/GM100.
McGrail B P, Schaef H T, Ho A M, Chien Y J, Dooley J J and Davidson C L 2006 Potential for carbon dioxide sequestration in flood basalts; J. Geophys. Res. 111 B12201, https://doi.org/10.1029/2005JB004169.
Mishra S, Misra S, Vyas D, Nikalje D, Warhade A and Roy S 2017 A 1251 m thick Deccan flood basalt pile recovered by scientific drilling in the Koyna region, Western Maharashtra; J. Geol. Soc. India 90 788–794, https://doi.org/10.1007/s12594-017-0792-7.
Mitchell C and Widdowson M 1991 A geological map of the southern Deccan Traps, India and its structural implications; J. Geol. Soc. London 148 495–505, https://doi.org/10.1144/gsjgs.148.3.0495.
Morgan W J 1972 Plate motions and deep mantle convection; Geol. Soc. Am. Memoir 132 7–22, https://doi.org/10.1130/MEM132-P7.
Murty A S N, Prasad B R, Rao P K, Raju S and Sateesh T 2010 Delineation of subtrappean Mesozoic sediments in Deccan Syneclise, India, using traveltime inversion of seismic refraction and wide-angle reflection data; Pure Appl. Geophys. 167 233–251, https://doi.org/10.1007/s00024-010-0050-z.
Nagaraju P and Roy S 2014 Effect of water saturation on rock thermal conductivity measurements; Tectonophys. 626 137–143, https://doi.org/10.1016/j.tecto.2014.04.007.
Podugu N, Ray L, Singh S P and Roy S 2017 Heat flow, Heat production and crustal temperatures in the Archaean Bundelkhand craton, north-central India: Implications for thermal regime beneath the Indian shield; J. Geophys. Res. 122(7) 5766–5788, https://doi.org/10.1002/2017JB014041.
Popov Y, Beardsmore G, Clauser C and Roy S 2016 ISRM suggested methods for determining thermal properties of rocks from laboratory tests at atmospheric pressure; Rock Mech. Rock Eng. 49 4179–4207, https://doi.org/10.1007/s00603-016-1070-5.
Popov Y, Pevzner S, Pimenov V and Romushkevich R 1999 New geothermal data from the Kola superdeep borehole SG-3; Tectonophys. 30 177–196, https://doi.org/10.1016/S0040-1951(99)00065-7.
Prasad P S R, Srinivasa Sarma D and Nirmal Charan S 2012 Mineral trapping and sequestration of carbon-dioxide in Deccan basalts: SEM, FTIR and Raman spectroscopic studies on secondary carbonates; J. Geol. Soc. India 80 546–552, https://doi.org/10.1007/s12594-012-0175-z.
Pribnow D and Sass J 1995 Determination of thermal conductivity for deep boreholes; J. Geophys. Res. 100 9981–9994, https://doi.org/10.1029/95JB00960.
Rao R U M, Roy S and Srinivasan R 2003 Heat-flow researches in India: Results and perspectives, In: Indian Continental Lithosphere: Emerging Research Trends (eds) Mahadevan, T M, Arora B R and Gupta K R, Geol. Soc. India Memoir 53 347–391.
Ray L, Bhattacharya A and Roy S 2007 Thermal conductivity of Higher Himalayan Crystallines from Garhwal Himalaya, India; Tectonophys. 434 71–79, https://doi.org/10.1016/j.tecto.2007.02.003.
Ray L, Forster H J, Schilling F R and Forster A 2006 Thermal diffusivity of felsic to mafic granulites at elevated temperatures; Tectonophys. 251 241–253, https://doi.org/10.1016/j.epsl.2006.09.010.
Ray L, Chopra N, Hiloidari S, Naidu N N and Kumar V 2021a Thermal conductivity of granitoids of varying composition up to 300°C and implications for crustal thermal models; Geophys. J. Int. ggab191, https://doi.org/10.1093/gji/ggab191.
Ray L, Gupta R K, Chopra N, Gopinadh D and Dwivedi S K 2021b Thermal and physical properties of Deccan Basalt and Neoarchean basement cores from a deep scientific borehole in the Koyna−Warna seismogenic region, Deccan Volcanic Province, western India: Implications on thermal modeling and seismogenesis; Earth Space Sci. 8(10), https://doi.org/10.1029/2021EA001645.
Ray L, Kumar P S, Reddy G K, Roy S, Rao G V, Srinivasan R and Rao R U M 2003 High mantle heat-flow in a Precambrian granulite province: Evidence from southern India; J. Geophys. Res. 108(B2) 2084, https://doi.org/10.1029/2001JB000688.
Roy S 1997 Geothermal studies in the Indian shield: ground temperature history and crustal thermal structure; PhD Thesis (unpublished), Banaras Hindu University, Varanasi, India, 218p.
Roy S 2008 Heat flow studies in India during the Past Five Decades; In: Five Decades of Geophysics in India (eds) Dimri V P and Singh B, Geol. Soc. India Memoir 68 89–122.
Roy S and Rao R U M 1999 Geothermal investigations in the 1993 Latur earthquake area, Deccan Volcanic Province, India; Tectonophys. 306 237–252, https://doi.org/10.1016/S0040-1951(99)00051-7.
Roy S and Rao R U M 2000 Heat flow in the Indian shield; J. Geophys. Res. 105 25,587–25,604, https://doi.org/10.1029/2000JB900257.
Roy S and Rao R U M 2003 Towards a crustal thermal model for the Archaean Dharwar craton, southern India; Phys. Chem. Earth 28 361–373, https://doi.org/10.1016/S1474-7065(03)00058-5.
Rybach L, Wilhelm J and Gorhan H 2003 Geothermal use of tunnel waters – a Swiss specialty; International Geothermal Conference, Reykjavík, Session #5.
Sain K, Zelt C A and Reddy P R 2002 Imaging of subvolcanic Mesozoics in the Saurashtra peninsula of India using traveltime inversion of wide-angle seismic data; Geophys. J. Int. 150(3) 820–826, https://doi.org/10.1046/j.1365-246X.2002.01749.x.
Sass J H, Lachenbruch A H and Munroe R J 1971 Thermal conductivity of rocks from measurements on fragments and its application to heat flow determinations; J. Geophys. Res. 76 3391–3401, https://doi.org/10.1029/JB076i014p03391.
Sass J H, Lachenbruch A H, Moses T H Jr and Morgan P 1992 Heat flow from a scientific research well at Cajon Pass, California; J. Geophys. Res. 97 5017–5030, https://doi.org/10.1029/91JB01504.
Seipold U 1988 Simultaneous measurements of thermal diffusivity and thermal conductivity under high pressure using thermal pulses of finite length; High Temp. - High Pres. 20 609–613.
Sheth H C 1999 Flood basalts and large igneous provinces from deep mantle plumes: Fact, fiction, and fallacy; Tectonophys. 311 1–29, https://doi.org/10.1016/S0040-1951(99)00150-X.
Subbarao K V and Hooper P R 1988 Reconnaissance map of the Deccan Basalt Group in the Western Ghats, India; In: Deccan Flood Basalts (ed.) Subbarao K V, Geol. Soc. India Memoir 10 393.
TeKa 2019 TK04 thermal conductivity meter user manual; https://www.te-ka.de/images/teka/download/TK04-Manual.pdf.
Venkatesan T R, Pande K and Gopalan K 1986 40Ar–39Ar dating of Deccan basalts; J. Geol. Soc. India 27 102–109.
West W D 1959 The source of the Deccan Trap flows; J. Geol. Soc. India 1 44–52.
Wignall P B 2001 Large igneous provinces and mass extinctions; Earth Sci. Rev. 53 1–33, https://doi.org/10.1016/S0012-8252(00)00037-4.
Williams C F and DeAngelo J 2008 Mapping geothermal potential in the western United States; GRC Trans. 32 155–161.
Williams C F and DeAngelo J 2011 Evaluation of approaches and associated uncertainties in the estimation of temperatures in the upper crust of the Western United States; GRC Trans. 35 1599–1605.
Woodside W and Messmer J H 1961 Thermal conductivity of porous media; J. Appl. Phys. 32 1688–1706.
Zhou S 1996 A revised estimation of the steady-state geotherm for the continental lithosphere and its implication for mantle melting; Terra Nova 8 514–524, https://doi.org/10.1111/j.1365-3121.1996.tb00780.x.
Acknowledgements
We thank Secretary, Ministry of Earth Sciences for support and encouragement in carrying out scientific drilling studies in Koyna region, Maharashtra. Core drilling was carried out in association with CSIR-NGRI, Hyderabad. Samples were collected from BGRL Core Repository, Karad. Satrughna Mishra provided invaluable support during laboratory data acquisition. Digant Vyas and Ashish Warhade helped with sampling and sample preparation. We thank Director, NCPOR for permission to use rock crushing facilities and Parijat Roy for help in the preparation of samples.
Author information
Authors and Affiliations
Contributions
Nagaraju Podugu: Designing of the research problem, literature survey, data generation, interpretation and manuscript preparation; Sukanta Roy: Drilling and sample collection, data interpretation and manuscript preparation.
Corresponding author
Additional information
Communicated by N V Chalapathi Rao
Corresponding editor: N V Chalapathi Rao
This article is part of the Topical Collection: Deccan Traps and other Flood Basalt Provinces – Recent Research Trends.
Rights and permissions
About this article
Cite this article
Podugu, N., Roy, S. Thermal conductivity of Deccan flood basalts. J Earth Syst Sci 131, 112 (2022). https://doi.org/10.1007/s12040-022-01868-3
Received:
Revised:
Accepted:
Published:
DOI: https://doi.org/10.1007/s12040-022-01868-3