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15-May-2017 14:09
Paralleling this alteration was the formation of abrupt pyrite-pyrrhotite transitions, and a zonation from sphalerite to galena to chalcopyrite.
The characteristic folded and breccia ores were not the result of ductile or fluid-assisted deformation of preexisting sulphide-siltstone interlayers, but instead formed by shear-controlled carbonate alteration that was ultimately replaced by sulphides.
I believe that this paper, along with the article, will conclusively demonstrated that there is no credible historical, geographical, archaeological or Biblical evidence to support the thesis that Mt. These researchers “speak the truth in love” but state that Ron Wyatt has not been truthful in his claims.
During the course of writing the first article, other proponents of Jebel al-Lawz requested that I not mention Ron Wyatt.
A completely different ore genesis paradigm may result and exploration concepts may need to be substantially modified.
Progressively further inwards, it changes to mica and albite-bearing ‘buff alteration’, commonly into siderite, magnetite and stilpnomelane, through a chloritic zone, to ultimately massive ‘silica-dolomite’ alteration.This is the same event as that which formed the copper ore (Perkins, 1984; Swager, 1985a) and indicates copper-lead-zinc to be a zoned late-stage epigenetic system.A succession of stratigraphically-constrained samples traced into the orebody reveals the progressive development of an alteration system that formed from well-laminated carbonaceous siltstones and mudstones.Layer-parallel mineralisation commonly terminates abruptly on or near extensional dolomite veins that formed progressively through the last major deformation event in the mine.