Significant inferences on deep crustal structure of Deccan Trap region from spectral analyses of Bouguer anomalies

Qualitative interpretation of the regional Bouguer anomaly map of the Decca n Trap region of peninsular India, based on the anomaly size, its gradient and minor contribution from the shallow crust assessed by the results of ot her geophysical methods, suggests that the major part of the these anomalie s have deep seated origin with 'lows' corresponding to the zones of subside nce and 'highs' to the uplifts involving the crust. Deep faults along the w est coast and segmented faults demarcating the Narmada rift valley and Narm ada-Son Lineament (NSL) have been delineated. Spectral analysis, matched fi lter technique for deconvolving gravity effect of sources at a particular d epth and a single interface gravimetric inversion scheme have been utilised to delineate density discontinuities and their 3D configurations. The deco nvolved gravity effect due to the deepest density interface at a mean depth of 117 km seems to reflect lithospheric variations and is used to distingu ish the stable crust from the metastable one. The Moho relief map, apart fr om structural features, exhibits a good agreement with the results by Deep Seismic Sounding (DSS) in Koyna area and across NSL. The block-wise analyses reveal higher average depths to Moho and Conrad, wh ich are typical of stable shield crust, in the southern part whereas the no rthern blocks associated with rift tectonics exhibit considerably, thin upp er crust (5.8 to 12.6 km) with another crustal interface at a depth in the range of 16.3 to 26.8 km. The latter depth forms the base of the middle cru stal layer i.e., top of the lower crustal layer comprising lower mantle der ivatives. These inferences are based on the correlation between Bouguer ano maly and upper crustal thickness and layered velocity structure brought out by DSS data across the NSL. Filtered Bouguer anomaly maps have further fac ilitated the interpretation and better demarcation of structural features i nferred from qualitative interpretation.