ABSTRACT
The Ankara volcanics comprise a small volcanic field immediately
to the north of Ankara, Turkey. This volcanic field is composed of
a mixture of flows, tuffs, and agglomerates, with the flows
ranging in composition from high-K basaltic andesite to rhyolite.
Dacitic flows are the most common. A potassium-argon date gives a
Middle Eocene age of 42.0 ± 1.6 m.y. The volcanics unconformably
overlie Paleozoic sediments of the "Cimmerian continent" to the
south and Mesozoic rocks of the Ankara melange to the north.
Results of analyses on 25 samples for major elements and Y, Sr,
Rb, Ni, Cr, V, Co, Zn, Cu, Nb, and Zr are presented. Major
elements and most trace elements show well defined trends when
plotted on SiO2 variation diagrams, indicating a chemical
consanguinity. The processes of partial melting, fractional
crystallization, and mixing/contamination are evaluated in terms
of the roles they may have played in the generation of these
magmas. A model based on fractional crystallization best explains
the observed chemical trends; xenocrystic phases and
disequilibrium phenomena in plagioclase indicate that
mixing/contamination processes may have played a lesser role.
Comparison of major and trace element abundances of the Ankara
rocks to those of other suites of calc-alkaline rocks reveals that
these volcanic rocks most resemble those that have been produced
by magmatic arcs built upon continental basement. This is
consistent with the hypothesis that these rocks are related to the
Eocene subduction and convergence which closed the northern
branches of Neo-Tethys.
Ach, J.A., 1982. The Petrochemistry of the Ankara Volcanics,
Central Turkey.
Unpublished MSc. thesis, State University of New York at Albany.
146 pp., +x; 1 folded plate (map)
University at Albany Science Library call number: SCIENCE
Oversize (*) QE 40 Z899 1982 A34
thesis (scanned text) - 3.8MB
pdf file
Plate 1 - Generalized
geology and sample locations, Ankara region, Turkey
(uncoloured geological map, scale 1: 50,000) -
2.4MB pdf file
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the Geological Sciences Program, University at Albany