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The skarns at Gryll’s Bunny are dominated by garnet and magnetite with small amounts of hornblende, epidote, apatite and tourmaline. They formed discordantly within a succession of metabasalts and metapelites (the Mylor Slate formation) within the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7c772751fc5fe1c8bce8bb0fc047214
https://doi.org/10.5194/egusphere-egu22-4200
https://doi.org/10.5194/egusphere-egu22-4200
Autor:
Ece Kirat, Halim Mutlu
The Keban Pb-Zn-(Cu) skarn deposit in the Elazığ region, Turkey, was formed at the contact zone of the Permo-Triassic metamorphics and the Late Cretaceous plutonic rocks in the Eastern Taurus orogenic belt. The mineralization is hosted by skarn and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6908dec6345f39a2ebb36ee5ea78946
https://doi.org/10.5194/egusphere-egu2020-4435
https://doi.org/10.5194/egusphere-egu2020-4435
Publikováno v:
Volume: 26, Issue: 3 206-226
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
We investigate rare earth element geochemistry, microthermometric characteristics, and radiogenic isotope systematics of fluorites and stable isotope compositions of gangue minerals from several fluorite deposits in central Turkey. In the deposits, f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::507efc1526c6aef3e1fe1ffd9c99df71
https://dergipark.org.tr/tr/pub/tbtkearth/issue/35158/390092
https://dergipark.org.tr/tr/pub/tbtkearth/issue/35158/390092