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Flexural subsidence analysis of the Laxmi Basin, Arabian Sea and its tectonic implications

Published online by Cambridge University Press:  18 December 2018

D. K. Pandey Open the ORCID record for D. K. Pandey [Opens in a new window] ,
Anju Pandey ,
Peter D. Clift ,
Nisha Nair Open the ORCID record for Nisha Nair [Opens in a new window] ,
Prerna Ramesh ,
Denise K. Kulhanek Open the ORCID record for Denise K. Kulhanek [Opens in a new window]  and
Rajeev Yadav
D. K. Pandey*
Affiliation:
ESSO–National Centre for Polar and Ocean Research, Goa 403804, India
Anju Pandey
Affiliation:
ESSO–National Centre for Polar and Ocean Research, Goa 403804, India
Peter D. Clift
Affiliation:
Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA
Nisha Nair
Affiliation:
ESSO–National Centre for Polar and Ocean Research, Goa 403804, India
Prerna Ramesh
Affiliation:
ESSO–National Centre for Polar and Ocean Research, Goa 403804, India
Denise K. Kulhanek
Affiliation:
International Ocean Discovery Program, Texas A&M University, College Station, Texas 77845, USA
Rajeev Yadav
Affiliation:
ESSO–National Centre for Polar and Ocean Research, Goa 403804, India
*
Email: [email protected]
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Abstract

Two-dimensional flexural backstripping and thermal modelling (assuming laterally variable stretching) is applied along regional depth-converted interpreted seismic profiles from the Laxmi Basin in the Arabian Sea. Results from reverse post-rift flexural modelling reveal considerable basin-wide subsidence in response to the crustal geodynamics during and after the last extensional phase. Unloading of the stratigraphy allows us to estimate the degree of laterally varying extension, assuming thermal subsidence and pure shear. High degrees of extension in the basin centre predict considerable water depths at the time of rift cessation, consistent with deep drilling data. We suggest that regional extension prior to Paleocene time could have fuelled variable subsidence in the Laxmi Basin but that extension is less than seen in typical oceanic lithosphere. Volcanic loading by the seamounts shortly after extension has flexed the basin and implies an effective elastic thickness (Te) at that time of ∼6 km. Reconstruction of the seamount top near sea level at the end of emplacement indicates no major transient uplift potentially linked to the Deccan mantle plume activity. Backstripping of post-rift sediments from interpreted seismic profiles supports the presence of a hyper-thinned crust underneath the Laxmi Basin, with β factors reaching >7 in the basin centre and ∼3 across much of the basin width. Computations of decompacted sediment accumulation rates in light of new results from IODP Expedition 355 show that basin sedimentation peaked during early–middle Miocene time, possibly coeval with uplift and erosion of the Himalayan–Tibetan Plateau driven by strong summer monsoon rains.

Keywords

continental riftingflexural subsidenceLaxmi BasinSite U1457IODP Expedition 355Arabian SeaJOIDES Resolution
Type
Original Article
Information
Geological Magazine , Volume 157 , Special Issue 6: Climate-tectonic interactions in the eastern Arabian Sea , June 2020 , pp. 834 - 847
Copyright
© Cambridge University Press 2018

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References

Agrawal, A and Rogers, JJW (1992) Structure and tectonic evolution of the western continental margin of India: evidence from subsidence studies for a 25–20 Ma plate reorganization in the Indian Ocean. In Basement Tectonics 8: Characterization and Comparison of Ancient and Mesozoic Continental Margins – Proceedings of the 8th International Conference on Basement Tectonics, pp. 583–90. Dordrecht, The Netherlands: Kluwer Academic Publishers.CrossRefGoogle Scholar
Allen, PA and Allen, JR (2006) Basin Analysis: Principles and Applications. Oxford: Blackwell Publishing Ltd, 549 pp.Google Scholar
Basu, DN, Banerjee, A and Tamhane, DM (1982) Facies distribution and petroleum geology of the Bombay offshore basin, India. Journal of Petroleum Geology 5, 51–75.CrossRefGoogle Scholar
Baxter, K, Cooper, GT, Hill, KC and O’Brien, GW (1999) Late Jurassic subsidence and passive margin evolution in the Vulcan Sub-basin, northwest Australia: constraints from basin modelling. Basin Research 11, 97–111.CrossRefGoogle Scholar
Bhattacharya, GC, Chaubey, AK, Murty, GPS, Srinivas, K, Sarma, KVLNS, Subrahmanyam, V and Krishna, KS (1994) Evidence for seafloor spreading in the Laxmi basin, northeastern Arabian Sea. Earth and Planetary Science Letters 125, 211–20.CrossRefGoogle Scholar
Bhattacharya, GC and Yatheesh, V (2015) Plate-tectonic evolution of the deep ocean basins adjoining the western continental margin of India—A proposed model for the early opening scenario. In Petroleum Geosciences (ed. Mukherjee, S). Cham: Indian Contexts, Springer Geology.Google Scholar
Biswas, SK (1982) Rift basins in western margin of India and their hydrocarbon prospects with special reference to Kutch Basin. American Association of Petroleum Geologists Bulletin 66, 1497–513.Google Scholar
Biswas, SK (1989) Hydrocarbon exploration in western offshore basins of India. Geological Survey of India Special Publication 24, 185–94.Google Scholar
Biswas, SK (1999) A review on the evolution of the rift basins in India during Gondwana with special reference to Western Indian basins and their hydrocarbon prospects. Proceedings of Indian National Science Academy 65, 261–83.Google Scholar
Calvès, G, Clift, PD and Inam, A (2008) Anomalous subsidence on the rifted volcanic margin of Pakistan: no influence from Deccan plume. Earth and Planetary Science Letters 272, 231–9.CrossRefGoogle Scholar
Calvès, G, Huuse, M, Clift, PD and Brusset, S (2015) Giant fossil mass wasting off the coast of West India: the Nataraja submarine slide. Earth and Planetary Science Letters 432, 265–72.CrossRefGoogle Scholar
Calvès, G, Schwab, AM, Huuse, M, Clift, PD, Gaina, C, Jolley, D, Tabrez, AR and Inam, A (2011) Seismic volcanostratigraphy of the western Indian rifted margin: the pre-Deccan igneous province. Journal of Geophysical Research: Solid Earth 116, doi: 10.1029/2010JB000862.CrossRefGoogle Scholar
Chand, S and Subrahmanyam, C (2003) Rifting between India and Madagascar – mechanism and isostasy. Earth and Planetary Science Letters 210, 317–32.CrossRefGoogle Scholar
Chaubey, AK, Gopala Rao, D, Srinivas, K, Ramprasad, T, Ramana, MV and Subrahmanyam, V (2002) Analyses of multichannel seismic reflection, gravity and magnetic data along a regional profile across the central-western continental margin of India. Marine Geology 182, 303–23.CrossRefGoogle Scholar
Clift, PD (2005) Sedimentary evidence for moderate mantle temperature anomalies associated with hotspot volcanism. In Plates, Plumes and Paradigms (eds Foulger, GR, Natland, JH, Presnall, DC and Anderson, DL), pp. 279–87. Geological Society of America, Special Paper no. 388.Google Scholar
Clift, PD (2006). Controls on the erosion of Cenozoic Asia and the flux of clastic sediment to the ocean. Earth and Planetary Science Letters 241, 571–80.CrossRefGoogle Scholar
Clift, PD and Gaedicke, C (2002) Accelerated mass flux to the Arabian Sea during the Middle–Late Miocene. Geology 30, 207–10.2.0.CO;2>CrossRefGoogle Scholar
Clift, PD, Gaedicke, C, Edwards, R, Lee, JI, Hildebrand, P, Amjad, S, White, RS and Schülter, HU (2002) The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea. Marine Geophysical Research 23, 223–45.CrossRefGoogle Scholar
Clift, PD, Turner, J and ODP Leg 152 Scientific Party (1995) Dynamic support of the Icelandic Plume and its effect on the subsidence of the northern Atlantic margins. Journal of the Geological Society, London 52, 935–41.CrossRefGoogle Scholar
Cloetingh, S, Gradstein, F, Kooi, H, Grant, AC and Kaminski, M (1990) Plate reorganization: a cause of rapid late Neogene subsidence and sedimentation around the North Atlantic? Journal of the Geological Society, London 147, 495–506.CrossRefGoogle Scholar
Collier, JS, Sansom, V, Ishizuka, O, Taylor, RN, Minshull, TA and Whitmarsh, RB (2008) Age of Seychelles–India breakup. Earth and Planetary Science Letters 272, 264–77.CrossRefGoogle Scholar
Corfield, RI, Carmichael, S, Bennett, J, Akhter, S, Fatimi, M and Craig, T (2010) Variability in the crustal structure of the West Indian Continental Margin in the Northern Arabian Sea. Petroleum Geoscience 16, 257–65.CrossRefGoogle Scholar
Courtillot, V, Besse, J, Vandamme, D, Montigny, R, Jaeger, JJ and Cappetta, H (1986) Deccan flood basalts at the Cretaceous/Tertiary boundary? Earth and Planetary Science Letters 80, 361–74.CrossRefGoogle Scholar
Eagles, G and Wibisono, AD (2013) Ridge push, mantle plumes, and the speed of the Indian plate. Geophysical Journal International 194, 670–7.CrossRefGoogle Scholar
Farnetani, CG and Richards, MA (1995) Numerical investigations of the mantle plume initiation model for flood basalt events. Journal of Geophysical Research 99, 13813–33.CrossRefGoogle Scholar
Gaedicke, C, Schlueter, HU, Roeser, HA, Prexl, A, Schreckenberger, B, Meyer, H, Reichert, C, Clift, P and Amjad, S (2002) Origin of the northern Indus Fan and Murray Ridge, northern Arabian Sea; interpretation from seismic and magnetic imaging. Tectonophysics 355, 127–43.CrossRefGoogle Scholar
Gaina, C, van Hinsbergen, DJJ and Spakman, W (2015) Tectonic interactions between India and Arabia since the Jurassic reconstructed from marine geophysics, ophiolite geology, and seismic tomography. Tectonics 34, 875–906.CrossRefGoogle Scholar
Gombos, AM, Powell, WG and Norton, IO (1995) The tectonic evolution of western India and its impact on hydrocarbon occurrences—an overview. Sedimentary Geology 96, 119–29.CrossRefGoogle Scholar
Gradstein, FM, Ogg, JG, Schmitz, M and Ogg, G (2012) The Geologic Time Scale 2012. Amsterdam: Elsevier Publications, 1176 pp.Google Scholar
Gupta, AK, Singh, RK, Joseph, S and Thomas, E (2004) Indian Ocean high-productivity event (10-8 Ma): linked to global cooling or to the initiation of the Indian monsoons? Geology 32, 753–6.CrossRefGoogle Scholar
Haq, BU, Hardenbol, J and Vail, PR (1987) Chronology of fluctuating sea levels since the Triassic. Science 235, 1156–67.CrossRefGoogle ScholarPubMed
Hopper, J and Buck, WR (1996) Effects of lower crustal flow on continental extension and passive margin formation. Journal of Geophysical Research 101, 20175–94.CrossRefGoogle Scholar
Jarvis, GT and McKenzie, DP (1980) Sedimentary basin formation with finite extension rates. Earth and Planetary Science Letters 48, 42–52.CrossRefGoogle Scholar
Karner, GD and Watts, AB (1982) On isostasy at Atlantic-type continental margins. Journal of Geophysical Research 87, 2923–48.CrossRefGoogle Scholar
Kolla, V and Coumes, F (1987) Morphology, internal structure, seismic stratigraphy, and sedimentation of Indus Fan. American Association of Petroleum Geologists Bulletin 71, 650–77.Google Scholar
Krishna, KS, Rao, DG and Sar, D (2006) Nature of the crust in the Laxmi Basin (14°–20°N), western continental margin of India. Tectonics 25, doi: 10.1029/2004TC001747.CrossRefGoogle Scholar
Kusznir, NJ, Hunsdale, R and Roberts, AM (2004) Timing of depth-dependent lithosphere stretching on the S. Lofoten rifted margin offshore mid-Norway: pre- breakup or post-breakup? Basin Research 16, 279–96.CrossRefGoogle Scholar
Kusznir, NJ, Roberts, AM and Morley, C (1995) Forward and reverse modelling of rift basin formation. In Hydrocarbon Habitat in Rift Basins (ed. Lambiase, J), pp. 33–56. Geological Society of London, Special Publication no. 80.Google Scholar
Mathur, RB and Nair, KR (1993). Exploration of Bombay offshore basin. In Proceedings of the 2nd Seminar on Petroleum Basins of India, Dehradun, India, Vol. 2, pp. 365–96. KDMIPE and ONGC, Indian Petroleum Publishers.Google Scholar
McKenzie, DP (1978) Some remarks on the development of sedimentary basins. Earth and Planetary Science Letters 40, 25–32.CrossRefGoogle Scholar
McKenzie, DP and Bickle, M (1988) The volume and composition of melt generated by extension of the lithosphere. Journal of Petrology 29, 625–79.CrossRefGoogle Scholar
McKenzie, DP and Sclater, JG (1971) The evolution of the Indian Ocean since the late Cretaceous. Geophysical Journal of the Royal Astronomical Society 24, 437–528.CrossRefGoogle Scholar
Miles, PR, Munschy, M and Segoufin, J (1998) Structure and early evolution of the Arabian Sea and East Somali Basin. Geophysical Journal International 134, 876–88.CrossRefGoogle Scholar
Minshull, TA, Lane, CI, Collier, JS and Whitmarsh, RB (2008) The relationship between rifting and magmatism in the northeastern Arabian Sea. Nature Geoscience 1, 463–67.CrossRefGoogle Scholar
Mishra, A, Chaubey, AK, Sreejith, KM and Kumar, S (2018) Crustal underplating and effective elastic plate thickness of the Laxmi Ridge, northern Arabian Sea. Tectonophysics 744, 82–92.CrossRefGoogle Scholar
Misra, AA, Sinha, N and Mukherjee, S (2015) Repeat ridge jumps and microcontinent separation: insights from NE Arabian Sea. Marine and Petroleum Geology 59, 406–28.CrossRefGoogle Scholar
Mitra, P, Zutshi, PL, Chourasia, RA, Chugh, ML, Ananthanarayanan, S and Shukla, B (1983) Exploration in western offshore basins. Petroleum Asia Journal VI, 15–24.Google Scholar
Mohan, M (1985) Geohistory analysis of Bombay high region. Marine and Petroleum Geology 2, 350–60.CrossRefGoogle Scholar
Mohanty, SN, Jain, M and Jamkhindikar, A (2013) New insight to hydrocarbon potential of shelf margin basin west of DCS area in Mumbai Offshore Basin, India. In 10th Biennial Conference on Hydrocarbon Exploration and Exposition, Kochi, India, p. 243.Google Scholar
Naini, BR and Talwani, M (1982) Structural framework and the evolutionary history of the continental margin of Western India. In Studies in Continental Margin Geology (eds Watkins, JS and Drake, CL), pp. 167–91. Tulsa: American Association of Petroleum Geologists vol. 34.Google Scholar
Nair, KM, Singh, NK, Ram, J, Gavarshetty, CP and Muraleekrishanan, B (1992) Stratigraphy and sedimentation of Bombay offshore basin. Journal of Geological Society of India 40, 415–42.Google Scholar
Pandey, DK, Clift, PD, Kulhanek, DK and the Expedition 355 Scientists (2016) Arabian Sea Monsoon. Proceedings of the International Ocean Discovery Program, vol. 355. College Station, Texas:International Ocean Discovery Program.Google Scholar
Pandey, DK, Nair, N, Pandey, A and Sriram, G (2017) Basement tectonics and flexural subsidence along western continental margin of India. Geoscience Frontiers 8, 1009–24.CrossRefGoogle Scholar
Pandey, A and Pandey, DK (2015) Mechanism of crustal extension in the Laxmi Basin, Arabian Sea. Geodesy and Geodynamics 6, 409–22.CrossRefGoogle Scholar
Planke, S and Eldholm, O (1994) Seismic response and construction of seaward dipping wedges of flood basalts: Voring volcanic margin. Journal of Geophysical Research 99, 9263–78.CrossRefGoogle Scholar
Raju, DSN, Bhandari, A and Ramesh, P (1999) Relative sea-level fluctuations during Cretaceous and Cenozoic in India. ONGC Bulletin 36, 185–202.Google Scholar
Rao, PR and Srivastava, DC (1984) Regional seismic facies analysis of western offshore India. Bulletin of the Oil and Natural Gas Commission 21, 83–96.Google Scholar
Roberts, AM, Kusznir, NJ, Yielding, G and Styles, P (1998) 2D flexural backstripping of extensional basins; the need for a sideways glance. Petroleum Geoscience 4, 327–38.CrossRefGoogle Scholar
Royden, L and Keen, CE (1980) Rifting process and thermal evolution of the continental margin of eastern Canada determined from subsidence curves. Earth and Planetary Science Letters 51, 343–61.CrossRefGoogle Scholar
Royer, J-Y, Chaubey, AK, Dyment, J, Bhattacharya, GC, Srinivas, VY and Ramprasad, T (2002) Paleogene plate tectonic evolution of the Arabian and Eastern Somali basins. In The Tectonic and Climatic Evolution of the Arabian Sea Region (eds Clift, P, Kroon, D, Gaedicke, C and Craig, J), pp. 7–23. Geological Society of London, Special Publication no. 195.Google Scholar
Sclater, JG and Christie, PAF (1980) Continental stretching: an explanation of the post-Mid-Cretaceous subsidence of the central North Sea Basin. Journal of Geophysical Research 85, 3711–39.CrossRefGoogle Scholar
Sleep, NH (1990) Hotspots and mantle plumes: some phenomenology. Journal of Geophysical Research 95, 6715–36.CrossRefGoogle Scholar
Storey, M, Mahoney, JJ, Saunders, AD, Duncan, RA, Kelley, SP and Coffin, MF (1995) Timing of hotspot-related volcanism and the breakup of Madagascar and India. Science 267, 852–5.CrossRefGoogle Scholar
Stein, CA and Stein, S (1992) A model for the global variation in oceanic depth and heatflow with lithospheric age. Nature 359, 123–9.CrossRefGoogle Scholar
Venkatesan, TR, Pande, K and Gopalan, K (1993) Did Deccan volcanism pre-date the Cretaceous transition. Earth and Planetary Science Letters 119, 181–90.CrossRefGoogle Scholar
Watts, AB (2001) Isostasy and Flexure of the Lithosphere. Cambridge, UK: Cambridge University Press, 472 pp.Google Scholar
White, RS (1999) The lithosphere under stress. Philosophical Transactions of the Royal Society of London A: Mathematical, Physical and Engineering Sciences 357, 901–15.CrossRefGoogle Scholar
White, RS and McKenzie, D (1989) Magmatism at rift zones: the generation of volcanic continental margins and flood basalts. Journal of Geophysical Research 94, 7685–729.CrossRefGoogle Scholar
Whiting, BM, Karner, GD and Driscoll, NW (1994) Flexural and stratigraphic development of the west Indian continental margin. Journal of Geophysical Research 99, 13791–811.CrossRefGoogle Scholar
Whitmarsh, RB (1974) Some aspects of plate tectonics in the Arabian Sea. In Initial Reports of the Deep Sea Drilling Project vol. 23 (eds Whitmarsh, RB, Weser, OE, Ali, S, Boudreaux, JE, Fleisher, RL, Jipa, D, Kidd, RB, Mallik, TK, Matter, A, Nigrini, C, Siddiquie, HN and Stoffers, P), pp. 527–35.CrossRefGoogle Scholar
Zhang, P, Molnar, P and Downs, WR (2001) Increased sedimentation rates and grain sizes 2-4 Myr ago due to the influence of climate change on erosion rates. Nature 410, 891–97.Google Scholar
Zutshi, PL, Sood, A, Mohapatra, P, Ramani, KKV, Dwivedi, AK and Srivastava, HC (1993) Lithostratigraphy of Indian petroliferous basins. Documents-V, Bombay Offshore Basin, 383, 117 pp. Dehradun: KDMIPE, ONGC.Google Scholar