Dating the India–Eurasia collision through arc magmatic records

2013/03/01 by Pierre Bouilhol, Oliver Jagoutz, John M. Hanchar +2 · 4 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.1016/j.epsl.2013.01.023

crossref issued 2013/03/01 · crossref published 2013/03/01 · crossref published-print 2013/03/01 · openalex publication_date 2013/03/01 · crossref created 2013/03/29 · crossref deposited 2020/05/07 · openalex created_date 2025/10/10 · crossref indexed 2026/07/31 · openalex updated_date 2026/07/31

Citations

• Major and trace element composition of the depleted MORB mantle (DMM)
• Geochemical Architecture of the Lower- to Middle-crustal Section of a Paleo-island Arc (Kohistan Complex, Jijal–Kamila Area, Northern Pakistan): Implications for the Evolution of an Oceanic Subduction Zone
• Geologic Evolution of the Himalayan-Tibetan Orogen
• Partial Melting of Mantle and Crustal Sources beneath South Karakorum, Pakistan: Implications for the Miocene Geodynamic Evolution of the India-Asia Convergence Zone
• Anatomy, age and evolution of a collisional mountain belt: the Baltoro granite batholith and Karakoram Metamorphic Complex, Pakistani Karakoram

Cited by

• Early Eocene ( c . 50 Ma) collision of the Indian and Asian continents: Constraints from the North Himalayan metamorphic rocks, southeastern Tibet
• Geophysical upheavals and evolutionary diversification of plant species in the Himalaya
• Early Eocene fossils suggest that the mammalian order Perissodactyla originated in India
• Eocene [wikipedia]