Abstract
Evidence from the eastern Indian Ocean implies a Greater India in Gondwanaland. Translated without distortion to Asia, the northeast part of Greater India is found to correspond in shape with the Tibetan Plateau. With geophysical evidence, this suggests that the northeast part of Greater India underlies, presumably by underthrusting, the Tibetan Plateau.
Original language | English |
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Pages (from-to) | 383-387 |
Number of pages | 5 |
Journal | Earth and Planetary Science Letters |
Volume | 27 |
Issue number | 3 |
DOIs | |
Publication status | Published - 1975 |