Pb-Zn deposits hosted by Triassic carbo-nates of the Eastern and Southern Alps are classified as APT deposits. The intial resources and reserves are totally estimated with up to 10.18 t Pb+Zn Geological, mineralogical, geochemical and isotopic data indicate APT deposits as a subclass of low temperature Pb-Zn deposits hosted by carbonates which are usually referred as MVT deposits.
CITATION STYLE
Schroll, E. (2005). Alpine type Pb-Zn-deposits (APT) hosted by Triassic carbonates. In Mineral Deposit Research: Meeting the Global Challenge (pp. 175–178). Springer Berlin Heidelberg. https://doi.org/10.1007/3-540-27946-6_46
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