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Alanyalılar (Muratdağı)

Kütahya, Muratdağı region (Gediz), Turkey

Epithermal depositsSb

Type
Hot-spring stibnite (post-Miocene silica-carbonate deposits)

Muratdağı antimony region (western Turkey), more than ten intermittently mined occurrences: post-Miocene mineralisation tied to silica-carbonate deposits of active or fossil hot springs, on downthrown blocks of NW-SE normal faults and in contact with carbonate rocks (Muratdağı mélange, Aşağıbelova Formation, Miocene sediments); acicular stibnite, antimony ochres and kermesite, late quartz and calcite. Gökçe and Spiro (1994): stibnite from -3.6 to -0.7 ‰ in δ34S, sulfur ascribed to the mafic and ultramafic rocks of the mélange; meteoric fluid of about -7 ‰ near 140 °C. Stratiform A-1 mineralisation in a thin silica-carbonate layer deposited in a small fault-zone pool, very close to the serpentinite-schist contact, and fault veins ("Alanyalilar" in the article). Stibnite GC-30 at -0.7 ‰, the heaviest of the region. Coordinates not published (simplified geological map only).

δ34S in ‰ (per mil) Values of the same system

Standard : V-CDT

ValueRangenMineral or matrixSource
−0.7 ‰1idiomorphic acicular stibnite
Single analysis (GC-30).
Gökçe & Spiro (1994), Stable isotope study of antimony deposits in the Muratdagi region, …

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Alanyalılar (Muratdağı), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/alanyal-lar-muratdag/ (accessed 2026-10-19).

@misc{isofind2026alanyallarmuratdagisotopesign,
  title = {Alanyalılar (Muratdağı), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/alanyal-lar-muratdag/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19