Oxygen isotopic and geochemical evidence for a short-lived, high-temperature hydrothermal event in the Chegem caldera, Caucasus Mountains, Russia

Author:

Gazis Carey,Taylor Hugh P.,Hon Ken,Tsvetkov Andrei

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference75 articles.

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2. Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake Oregon;Bacon;Earth Planet. Sci. Lett.,1989

3. Experimental welding of volcanic ash;Bierwith,1982

4. 2.5 Ma ash-flow caldera at Chegem River in the northern Caucasus Mountains (USSR), contemporaneous granites and associated ore bodies;Bogatikov;Izv. Russian Acad. Sci. Ser. Geol.,1992

5. THE UPPER CHEGEM CALDERA COMPLEX IN THE NORTH CAUCASUS

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