Abstract
The Trans-Hudson Orogen (THO) of North America and the Himalaya-Karakoram-Tibetan Orogen (HKTO) of Asia preserve a Paleoproterozoic and Cenozoic record, respectively, of continent-continent collision that is notably similar in scale, duration, and character.
Original language | English |
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Pages (from-to) | 161 |
Number of pages | 1 |
Journal | Himalayan Journal of Sciences |
Volume | 5 |
Issue number | 7 |
DOIs | |
Publication status | Published - 2008 |
Event | 23rd Himalaya-Karakoram-Tibet Workshop - Leh, Ladakh, India Duration: 8 Aug 2008 → 11 Aug 2008 Conference number: 23 |
Programme Area
- Programme Area 4: Mineral Resources