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A guiding dictum followed by field geologists is ‘Rocks cannot speak, but they can tell us wonderful first-hand stories of Earth history if we can converse with them after acquiring the skill of understanding their language.’ Problems arise when in situ, fresh and ‘dependable’ rock exposures are not available for requisite interpolation and/or extrapolation. Geophysicists have the key to sort out those problems. The mutual complementary and supplementary relations existing between the two siblings of Geosciences are remarkable.
The relentless efforts of innumerable Himalayan geoscientists from all over the globe through almost the last two centuries have generated data which, with sound geological reasoning, can now be fitted together nicely to solve the ‘jigsaw puzzle’ of the big picture of Himalayan tectonic-geodynamic evolution. The present work does this, and highlights the profound need for systematic and collaborative geophysical studies, particularly seismic sounding, along several well-chosen transects cutting across the Himalayas, for necessary authentication.
[Abbreviations used: ITS = Indus Tsangpo Suture, STDS = South Tibetan Detachment System, MCT = Main Central Thrust, MBT = Main Boundary Thrust, MFT = Main Frontal Thrust, TMSU = Tethyan Marine Sedimentary Unit, HHCU = Higher Himalayan Crystalline Unit, LHMU = Lesser Himalayan Metasedimentary Unit.]