Hydrosulphide complexing of Au (I) in hydrothermal solutions from 150–400°C and 500–1500 bar
about
The geomicrobiology of gold.Role of CO2 in the formation of gold deposits.The formation of gold-rich seafloor sulfide deposits: Evidence from the Beebe hydrothermal vent field, Cayman TroughGold enrichment in active geothermal systems by accumulating colloidal suspensionsAssociation of gold with uraninite and pyrobitumen in the metavolcanic rock hosted hydrothermal Au-U mineralisation at Rompas, Peräpohja Schist Belt, northern FinlandEpigenetic BIF-hosted gold lodes at the Abu Marawat area, Eastern Desert, Egypt: integrated mineralogical, structural control and fluid inclusion studies
P2860
Hydrosulphide complexing of Au (I) in hydrothermal solutions from 150–400°C and 500–1500 bar
description
im Juni 1996 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 1996
@uk
name
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en-gb
Hydrosulphide complexing of Au
@nl
type
label
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en-gb
Hydrosulphide complexing of Au
@nl
prefLabel
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en-gb
Hydrosulphide complexing of Au
@nl
P1476
Hydrosulphide complexing of Au ...... rom 150–400°C and 500–1500 bar
@en
P2093
Terry M. Seward
P304
P356
10.1016/0016-7037(96)00061-0
P577
1996-06-01T00:00:00Z