Textural characteristics of ore mineral dendrites in banded quartz veins from low-sulfidation epithermal deposits: implications for the formation of bonanza-type precious metal enrichment

Author:

Tharalson Erik R.ORCID,Taksavasu Tadsuda,Monecke Thomas,Reynolds T. James,Kelly Nigel M.,Pfaff Katharina,Bell Aaron S.,Sherlock Ross

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference101 articles.

1. Aseto CO (2012) Geology, geochemistry and geochronology of the mid-Miocene, low-sulfidation epithermal gold-silver ores on War Eagle Mountain, Silver City district, Idaho. Unpublished MS thesis, Auburn University p 170

2. Bettermann P, Liebau F (1975) The transformation of amorphous silica to crystalline silica under hydrothermal conditions. Contrib Mineral Petrol 53:25–36

3. Bobis RE (1994) A review of the description, classification and origin of quartz textures in low sulphidation epithermal veins. J Geol Soc Philipp 49:15–39

4. Bodnar RJ, Lecumberri-Sanchez P, Moncada D, Steele-MacInnis M (2014) Fluid inclusions in hydrothermal ore deposits. In: Holland HD, Turekian KK (eds) Treatise on geochemistry, vol 13. Elsevier, Oxford, pp 119–142

5. Brenner W, Blank Z, Okamoto Y (1966) Growth of single crystals of lead sulphide in silica gels near ambient temperatures. Nature 212:392–393

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