Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Asuman Kahya"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 165, Iss 165, Pp 63-75 (2021)
Zebra dolomites and carbonate - hosted Au - Ag - Zn ± Pb deposits of Maden village is located in the shelf type carbonate rocks of the Bolkar Mountains. The Zebra dolomite (ZD) locally form and there is no evidence for relation between dolomitizatio
Externí odkaz:
https://doaj.org/article/98b4147f4c644384a741a6c1619725bf
Autor:
Asuman Kahya, Ercan Kuşcu
Publikováno v:
Neues Jahrbuch für Mineralogie - Abhandlungen. 198:85-99
Publikováno v:
Volume: 165, Issue: 165 63-75
Bulletin of the Mineral Research and Exploration
Bulletin of the Mineral Research and Exploration, Vol 165, Iss 165, Pp 63-75 (2021)
Bulletin of the Mineral Research and Exploration
Bulletin of the Mineral Research and Exploration, Vol 165, Iss 165, Pp 63-75 (2021)
Zebra dolomites and carbonate - hosted Au - Ag - Zn +/- Pb deposits of Maden village is located in the shelf type carbonate rocks of the Bolkar Mountains. The Zebra dolomite (ZD) locally form and there is no evidence for relation between dolomitizati
Autor:
Asuman Kahya
Publikováno v:
Afyon Kocatepe University Journal of Sciences and Engineering. 18:648-663
Publikováno v:
Journal of the Geological Society of India. 91:496-504
The sediment-hosted huntite-magnesite deposits are located in the Egirdir-Hoyran lake basin in the Isparta Angle (southern Turkey). The deposits occur at two different localities in the region: (1) Kemersirti huntite deposit, (2) Koytepe huntite-magn
Autor:
Öznur Kanaat, Asuman Kahya
Publikováno v:
Neues Jahrbuch für Mineralogie - Abhandlungen. 195:11-25
WOS: 000427023000002
Auriferous quartz veins of Guneykoy (Usak, Esme) are hosted in Precambrian greenschist facies granitic gneisses of the Menderes Massif, West Anatolia. The auriferous quartz veins occur as fissure fillings either discordant o
Auriferous quartz veins of Guneykoy (Usak, Esme) are hosted in Precambrian greenschist facies granitic gneisses of the Menderes Massif, West Anatolia. The auriferous quartz veins occur as fissure fillings either discordant o
Autor:
Mustafa Kuşcu, Asuman Kahya
Publikováno v:
Universal Journal of Geoscience. 4:128-143
Host rock of magnesite occurrences in three areas (Suleymaniye, Margi, Tutluca) are the altered peridotite which on the northernmost outcrops of the Izmir-Ankra suture zone. Magnesite is formed in the cracks and fractures of highly altered harzburgit
WOS: 000468487000004
The Maden Village carbonate-hosted Au-Ag-Zn +/- Pb deposits in the Bolkar Mountains that are part of the Tauride platform, south of Turkey, contain significant none- sulfide ore and relicts of sulfide bodies. The deposits ho
The Maden Village carbonate-hosted Au-Ag-Zn +/- Pb deposits in the Bolkar Mountains that are part of the Tauride platform, south of Turkey, contain significant none- sulfide ore and relicts of sulfide bodies. The deposits ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aaa0860bd8c72abf1f6172de91df9c9d
https://hdl.handle.net/20.500.12451/2033
https://hdl.handle.net/20.500.12451/2033
Publikováno v:
Arabian Journal of Geosciences. 10
Vein-stockwork magnesite in the Madenli area, sedimentary huntite-magnesite in the Asagitirtar area, and lacustrine hydromagnesite in the Salda Lake area are located in the Beysehir-Hoyran and Lycian nappe rocks around Isparta and Burdur, Southwest A
Autor:
Asuman KAHYA, Mustafa KUŞCU
Kahya, Asuman ( Aksaray, Yazar )
The Eskişehir magnesite deposits (Süleymaniye, Margı, and Tutluca) are located in the western part of the İzmir–Ankara Suture Zone, northwestern Turkey. These vein and stockwork type magnesite deposits, whi
The Eskişehir magnesite deposits (Süleymaniye, Margı, and Tutluca) are located in the western part of the İzmir–Ankara Suture Zone, northwestern Turkey. These vein and stockwork type magnesite deposits, whi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0003942df7e56eb37e47a7f14e358e6a
https://hdl.handle.net/20.500.12451/1237
https://hdl.handle.net/20.500.12451/1237