Abstract The Central Anatolian segment of the Alpine-Himalayan orogen contains “interior”
basins, the largest of which is the Tuzgölü (Salt Lake) basin (> 20,000 km2). It is bounded on …

Abstract In the Central Sakarya area of Turkey there are two main Alpine continental units,
separated by a south verging ophiolitic complex which represents the root zone of the İzmir …

Carpholite+ chloritoid+ pyrophyllite association occurs widely in the Triassic metaclastic
rocks of the Afyon Zone in west-central Turkey. Fe-Mg-carpholite is associated with rare …

Field evidence from north–south transects tests three tectonic models for Tethys in Western
Turkey for when a Late Palaeozoic ocean was closing and an Early Mesozoic ocean …

Vein stockworks and lacustrine developments of cryptocrystalline magnesium carbonates of
Neogene and Quaternary age occur within the partially serpentinized, discontinuous …

Abstract The Tauride–Anatolide continent, stretching for c. 900 km across western and
central Turkey, is one of the world's best example of a subducted, exhumed passive margin …

Afyon Zone, which was derived from the Anatolide–Tauride platform during closure of the
Neo-Tethys, is made up of pre-Mesozoic basement and unconformably overlying Triassic …

Abstract The northeast of Konya (Altınekin) is one of the important centers of agriculture and
animal husbandry throughout its thousands of years of history. Heavy metal accumulation is …

There are many abandoned mines that have completed their economic life in the world and
in our country. Because of limited capital power and manpower, it is very difficult to recover …

Metamorphic rocks host the majority of the thermal waters of the Emet area. Only Dereli
springs are hosted by non-metamorphic carbonates and ophiolitic rocks. The carbonated …