2 edition of use of geochemical stream-drainage samples for detecting bulk- minable gold deposits in Alaska found in the catalog.
use of geochemical stream-drainage samples for detecting bulk- minable gold deposits in Alaska
M. A. Wiltse
|Statement||by M.A. Wiltse.|
|Series||Report of investigations / State of Alaska, Department of Natural Resources, Division of Geological and Geophysical Surveys -- 88-13., Report of investigations (Alaska. Division of Geological and Geophysical Surveys) -- 88-13.|
|Contributions||Alaska. Division of Geological and Geophysical Surveys.|
|The Physical Object|
|Pagination||iii, 13 p. :|
|Number of Pages||13|
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Get this from a library. The use of geochemical stream-drainage samples for detecting bulk-minable gold deposits in Alaska. [M A Wiltse; Alaska. Division of Geological and Geophysical Surveys.]. Buy The use of geochemical stream-drainage samples for detecting bulk-minable gold deposits in Alaska (Report of investigations / State of Alaska, Department of Geological and Geophysical Surveys) by M.
A Wiltse (ISBN:) from Amazon's Book Store. Author: M. A Wiltse. Fletcher, W.K. STREAM SEDIMENT GEOCHEMISTRY IN TODAY’S EXPLORATION WORLD 1. behind large boulders, logs etc., 2.
in low energy pools at the tail-end of bars or between riffles shutes; or, 3. infilling voids below the surface of cobble-gravel bars. Geochemical surveys based on the chemical analysis of samples of active stream sediment from drainage courses have long been used as an exploration tool worldwide.
The underlying premise is that stream sediments are composite products of erosion and weathering and thus represent the source catchment area of the stream drainage network.
ABSTRACT Worldwide use of stream sediment geochemistry for almost 50 years has shown it to be a robust method for identifying areas of high mineral potential.
The basic premise is that a stream sediment is representative of the products of weathering and erosion upstream of the sample site. However, detailed studies show that this premise greatly oversimplifies the real situation.1/5(1).
Geochemical zonality is one of the most outstanding features of the primary geochemical haloes of non-metallic deposits in general and hydrothermal and meta-morphic ones in particular.
The oxial geochemical zonality of the primary haloes of deposits is universal, that is to say there is an ordered distribution of element haloes up the dip of.
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