Page 246 - Handbook of Gold Exploration and Evaluation
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Sedimentation and detrital gold  217

            4.3.1 Channel networks

            The basic pattern of drainage is established and channel networks develop most
            rapidly during early stages of denudation. Subsequent changes are due largely to
            headward erosion and expansion of tributaries. Effectively, the networks are
            open systems in which the inputs are water, energy and sediment. The outputs
            are losses of energy expended in friction, erosion and transport; sediment
            deposition in flood plains and deltas; and water discharged into lakes and
            oceans. Channels aggrade as a result of net sediment deposition when changes in
            channel geometry are inadequate to cope with increased sediment loadings. The
            same channel beds erode and downcutting occurs when the capacity of the
            stream to transport sediments is greater than needed to deal with the actual
            sediment input. Network efficiency is determined by how quickly the channels
            adjust to any changing flow conditions.
              Individual channels are descriptive of the nature of the underlying rocks and
            may be interpreted to assess the texture of a landscape and to identify features
            pointing to differences in rock type and structure associated with possible
            metallogenic settings. The most productive channel systems (in terms of placer
            concentration) are developed where exposed primary gold-bearing veins are
            controlled structurally in relation to basin development. Figure 4.12 illustrates
            the effect of multi-source vs. single-source provenances on the possible extent of
            placer deposits formed in main trunk streams. Major alluvial goldfields such as
            those in California and Australia are all associated with drainage systems having
            extensive and closely spaced networks of tributaries in individually confined
            basin settings. Parameters relating to drainage density and stream frequency are
            interrelated features; the density of a drainage network is the total length of
























                   4.12 Effects of single-source and multi-source gold provenances on patterns
                   of paystreak development.
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