Gold-Bearing Breccias of the Rain Mine, Carlin Trend, Nevada

Abstract

The Rain mine includes two mined-out open pits that contained 36.4 t (1.17 Moz) gold, averaging 1.8 g/t gold, and underground reserves, including underground production, estimated at 4.9 t (157,000 oz) gold averaging 7.7 g/t. Rain orebodies are localized in a breccia complex within the hanging wall of the Rain fault and hosted within the Mississippian Webb Formation immediately overlying the contact with the Devonian Devils Gate Limestone. The ore host includes four texturally and genetically distinct breccia types: (1) crackle breccia; (2) hydrothermal breccia; (3) tuffisite with accretionary lapilli; and (4) collapse breccia. Crackle breccia forms a capping over multistage hydrothermal breccias that are cut by tabular-to pipe-shaped tuffisite dikes, with some containing accretionary lapilli. Pre-and synore hydrothermal breccias formed during at least three episodes of convective fluidization, followed by quartz-sulfide-barite cementation. High-grade gold was deposited as a late phase along the upper portion of the hydrothermal breccia mass and extended into the crackle breccia zone. Collapse breccias occur along the floor of the composite breccia mass and have irregular upper and lower contacts. The lower contact occurs on a dissolution boundary with the Devils Gate Limestone. Matrix-supported, heterolithic, hydrothermal breccias at Rain consist of sedimentary rock fragments composed of sandstone, siltstone, mudstone, limestone, and conglomerate. Some fragments contain as much as 8 percent introduced biotite in veinlets and/or fragment matrix replacements. The veinlets consist of euhedral quartz, biotite, sphalerite, and pyrite. Barite constitutes as much as 60 percent of the hydrothermal breccias in the form of fragments and as a cement to the breccias. Quartz replacement of fragments and as a breccia cement is pervasive. The total sulfide content in unoxidized ores is less than 5 volume percent. The Rain orebody resulted from five interpreted stages of development: (1) structural preparation along the right-lateral oblique Rain fault system and conjugate left-lateral oblique northeast-striking faults; (2) multiple episodes of hydrothermal breccia formation, with high-grade gold deposition immediately following the last brecciation event; (3) late channelized and fluidized rock fragments and fine clays forming tuffisite bodies with accretionary lapilli; (4) postmineral extensional reactivation of structures; and (5) collapse brecciation resulting from postore supergene acidic fluid ponding on and dissolving the upper Devils Gate Limestone. The age of the Rain orebody is poorly constrained. It is older than 22 Ma supergene alunite, but no maximum age constraints other than the Mississippian host rock are known.

Diatreme Breccias at the Kelian Gold Mine, Kalimantan, Indonesia: Precursors to Epithermal Gold Mineralization

“…A7 sandstone is considered to have formed during high-water/magma ratio explosions and/or as a result of highly efficient fuel-coolant mixing. Accretionary lapilli are sometimes used to indicate formation in a subaerial environment; however, they have been identified in subvolcanic breccias at Mount Leyshon (Wormald, 1991), in gas segregation pipes in the Oruanui Ignimbrite in New Zealand (Self, 1983), and in dikes cutting breccias at the Rain mine (Williams et al, 2000), Cripple Creek (T. Thompson, pers. Water supply and magma-sediment mixing may have become greater with time due to the increased abundance of the sand-to mud-sized component in the pipes after successive explosion events.…”

Igneous Geology of the Carlin Trend, Nevada: Development of the Eocene Plutonic Complex and Significance for Carlin-Type Gold Deposits

“…For example, SiO 2 in the Primeaux lavas varies by almost 6 wt percent but La varies only 38 to 46 ppm and does not correlate with SiO 2 . Breccias and orebodies were controlled by, and spread along, the west-northwest-striking Rain fault for about 8 km, especially near intersections with northeast-striking faults (Williams et al, 2000;Mathewson, 2001;Longo et al, 2002). 8).…”

The Hydrothermal Breccia of Berglia-Glassberget, Trøndelag, Norway: Snapshot of a Triassic Earthquake

“…Such fault rocks represent implosion breccias, formed by the 'sudden creation of void space and fluid pressure differentials at dilational fault jogs during earthquake rupture propagation' [2]. This implosion forms commonly fitted-fabric to chaotic fault breccias, cemented by hydrothermal fluids e.g., [36,[69][70][71][72][73][74]. The implosion hypothesis envisages that faulting-induced voids are transient and filled coseismically by a dilated mass of rock fragments.…”