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Publikováno v:
Economic Geology. 66:748-756
The Flat Gap ore body is a strata-bound, low-grade sphalerite deposit in Lower Ordovician carbonate beds that have a 37 degree dip. The mineralization is localized in breccia bodies formed in the Mascot and Kingsport Formations when the beds were fla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d16fa6fc8b336acc671235bfcdebd7ec
https://doi.org/10.2113/gsecongeo.66.5.748
https://doi.org/10.2113/gsecongeo.66.5.748
