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postcollisional magmatism (17) 17
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LITHOS, ISSN 0024-4937, 11/2016, Volume 264, pp. 348 - 359
Adakite-like lavas from the Iranian segment of the Arabia–Eurasia collision zone have been considered as partial melts derived from a subducted Neotethyan... 
Zircon U–Pb age | Slab melt | Iran | Lower crust | Quaternary | Adakite | U-PB GEOCHRONOLOGY | ZIRCON GEOCHRONOLOGY | ZAGROS MOUNTAINS | SUBDUCTION HISTORY BENEATH | POSTCOLLISIONAL MAGMATISM | Zircon U-Pb age | EASTERN CHINA | ARC-MAGMATISM | GEOCHEMISTRY & GEOPHYSICS | SISTAN SUTURE ZONE | MINERALOGY | TECTONIC EVOLUTION | Earth | Basalt | Silicates | Mantle | Analysis | Sediments (Geology) | Zirconium
Journal Article
Tectonophysics, ISSN 0040-1951, 2009, Volume 477, Issue 1, pp. 36 - 48
Rising as “the roof of the world” the Tibetan plateau is now underlain with the thickest continental crust on Earth. How and when was this crust formed, which... 
Postcollisional adakite | Basaltic underplating | India–Asia collision | Tibet | Neotethyan subduction | Crustal thickening | India-Asia collision | U-PB | GANGDESE BATHOLITH | HIMALAYAN TECTONICS | MANTLE | GEOCHEMISTRY & GEOPHYSICS | EAST-WEST EXTENSION | LU-HF | SOUTHEASTERN TIBET | CONTINENTAL COLLISION ZONES | SIERRA-NEVADA | TECTONIC EVOLUTION | Roots | Hafnium | Geochemistry | Isotopes | Crusts | Zircon | Thickening
Journal Article
LITHOS, ISSN 0024-4937, 12/2014, Volume 210-211, pp. 209 - 223
Oligocene–Miocene granitoids exposed within the 1500-km-long Gangdese arc of southern Tibet exhibit adakitic compositions. Five plutonic samples from the... 
Postcollisional | Slab tearing | Adakitic granitoids | Eastern Himalayan syntaxis | SE Tibet | UNDERPLATED BASALTIC CRUST | ZIRCON U-PB | GANGDESE BATHOLITH | GEOCHEMISTRY & GEOPHYSICS | ASIA COLLISION | MANTLE SOURCE CHARACTERISTICS | CONTINENTAL COLLISION ZONES | GEOCHEMICAL CONSTRAINTS | HF-O ISOTOPES | MINERALOGY | TECTONIC EVOLUTION | Magmatism | Evolution | Zirconium | Granite
Journal Article
The Journal of Geology, ISSN 0022-1376, 11/2012, Volume 120, Issue 6, pp. 647 - 669
The Oligocene to the Miocene was a critical period for the growth of the Tibetan Plateau. This growth is commonly considered to have been controlled by deep... 
Melting | Geology | Crystallization | Rocks | Enclaves | Asthenosphere | Mantle | Lithospheres | Magma | Isotopes | TRACE-ELEMENT | EAST-WEST EXTENSION | CONTINENTAL COLLISION | GEOLOGY | INDO-ASIAN COLLISION | MANTLE BENEATH TIBET | POSTCOLLISIONAL MAGMATISM | ZIRCON U-PB | THICKENED LOWER CRUST | HF ISOTOPIC COMPOSITIONS | SR-ND-PB | Intrusions (Geology) | Research | Geodynamics | Petrogenesis
Journal Article
Journal of Asian Earth Sciences, ISSN 1367-9120, 07/2015, Volume 106, pp. 19 - 33
Hundreds of compositionally diverse volcanoes have erupted on the Turkish–Iranian Plateau in the last 15 Myr, attributed to one or more of the processes of... 
Geochemistry | Iran | Collision | Adakite | Intraplate basalt | EDGE-DRIVEN CONVECTION | SUBDUCTION ZONES | ISLAND-ARC | POSTCOLLISIONAL MAGMATISM | INTRAPLATE MAGMATISM | OROGENIC PLATEAU | HIGH-NB BASALT | GEOSCIENCES, MULTIDISCIPLINARY | GEOCHEMICAL CONSTRAINTS | LITHOSPHERIC STRUCTURE | ARABIA-EURASIA COLLISION | Earth | Magmatism | Basalt | Mantle | Petrogenesis
Journal Article