GEOCHEMICAL CHARACTER OF THE HYDROTHERMAL ALTERATION ZONES AROUND THE MADENKOY-SIIRT MASSIVE SULFIDE DEPOSIT AND IMPLICATIONS FOR GEOCHEMICAL-EXPLORATION

Date

1989-04-01

Author

ERLER, A

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The Madenkoy-Siir region lies in southeastern Anatolia, Turkey to the northeast of Siirt. The study area is in the southeastern Anatolian Thrust Belt, which forms the boundary between the Border Folds on the northern edge of the Arabian plate and the Taurids. In the region, limestones of the Midyat Group of Eocene-Miocene age and alternating marls and sandstones of the Lice Formation of Early-Middle Miocene age are the autochthonous units. Three thrust slices were emplaced over the autochthonous units during the Miocene Epoch. The lowest slice consists of interbedded sandstones, mudstones, marls, limestones, and conglomerates of the Sason flysch, the Madenkoy spilite, and the Toptepe conglomerate, all of Eocene age; the middle slice consists of the Guleman ultramafic rocks of Cretaceous age; and the uppermost slice consists of the Bitlis metamorphic rocks of Paleozoic age.

Subject Keywords

Economic geology, Geochemistry and petrology

URI

https://hdl.handle.net/11511/64246

Journal

JOURNAL OF GEOCHEMICAL EXPLORATION

DOI

https://doi.org/10.1016/0375-6742(89)90083-6

Collections

Department of Geological Engineering, Article

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Citation Formats

A. ERLER, “GEOCHEMICAL CHARACTER OF THE HYDROTHERMAL ALTERATION ZONES AROUND THE MADENKOY-SIIRT MASSIVE SULFIDE DEPOSIT AND IMPLICATIONS FOR GEOCHEMICAL-EXPLORATION,” JOURNAL OF GEOCHEMICAL EXPLORATION, pp. 405–407, 1989, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/64246.