WebApr 26, 2016 · The advanced argillic alteration zone ranges from the surface to ~2 km (quartz-alunite zone: surface to ~1 km; quartz-pyrophyllite zone: ~1 to ~2 km). The sericite zone is situated at depths between ~1.5 and ~2 km, and the potassic zone is located deeper than ~2 km. Therefore, this correlation shows that the maximum source depth is ~2 km, … WebAdvanced argillic alteration lithocaps have been described from a number of porphyry-epithermal deposits and prospects worldwide, and coupled with the occurrence of a …
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WebApr 5, 2024 · Target 1 is located in the center of the Borsko Project (Figure 2) and represents an undercover preserved advanced argillic alteration lithocap. The target covers a strike length approximately 1.6 ... WebJan 17, 2024 · Alteration types modeled in this way can be stratified relative to acid producing and neutralizing potential to aid in geoenvironmental watershed studies. This mapping was performed in support of multidisciplinary studies involving the predictive modeling of mineral deposit occurrence and geochemical environments at watershed to … chad smith snare samples
Gold mineralisation and advanced argillic alteration at the …
WebAug 24, 2024 · The alteration on Mt Ruapehu was classified using ground samples as non-altered, supergene argillic, intermediate argillic, and advanced argillic. The first two classes have a paragenesis that is consistent with surficial infiltration and circulation of low-temperature (<40°C) neutral to mildly acidic fluids, inducing chemical weathering and ... Argillic alteration is hydrothermal alteration of wall rock which introduces clay minerals including kaolinite, smectite and illite. The process generally occurs at low temperatures and may occur in atmospheric conditions. Argillic alteration is representative of supergene environments where low temperature groundwater becomes acidic. Argillic assemblages include kaolinite replacing plagioclase and montmorillonite replacing amphibole and … WebDec 11, 2024 · This volumetrically dominant epithermal alteration in Fig. 2 corresponds to variably siliceous advanced argillic alteration including minor vuggy quartz. Compared with other epithermal deposits, it stands out due to the high abundance of anhydrite and only local occurrence minor alunite. hansgrohe 98282000