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The crustal structure of the Himalayan fold-thrust belt in NW Himalaya is constrained using spectral analysis, wavelet transform (WT) and forward modeling of the Bouguer gravity anomaly. The data covers the Himalayan range from the Sub Himalayan zone in the hanging wall of Himalayan Frontal Thrust (HFT) to the Karakoram fault across the Indus Tsangpo Suture Zone (ITSZ), along about 450 km long (projected distance), the Kiratpur-Manali-Leh-Panamik transect. The spectral analysis of power spectrum of the gravity data yielded three layer interfaces. The short wavelength data is modeled on the basis of density contrast across the litho-tectonic boundaries and regional structural geometries along the profile section. The average depth and location obtained using the wavelet

Crustal configuration of NW Himalaya based on modeling of gravity data