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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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