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Goldich dissolution series information


The Goldich dissolution series is a method of predicting the relative stability or weathering rate of common igneous minerals on the Earth's surface, with minerals that form at higher temperatures and pressures less stable on the surface than minerals that form at lower temperatures and pressures.

Discontinuous
Series
Continuous
Series
High
OlivinePlagioclase
(Calcium rich)
Pyroxene
Amphibole
Biotite
(Black Mica)
Plagioclase
(Sodium rich)
Relative
Weathering
potential
Orthoclase
Muscovite
(White Mica)
Quartz
Low

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Goldich dissolution series

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The Goldich dissolution series is a method of predicting the relative stability or weathering rate of common igneous minerals on the Earth's surface, with...

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Anorthite

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normally would be due to its high weathering potential in the Goldich dissolution series. It also makes up much of the lunar highlands; the Genesis Rock...

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Escarpment

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different rock types weather at different speeds, according to Goldich dissolution series so different stages of deformation can often be seen in the layers...

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Sedimentary rock

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rock-forming minerals to weathering is expressed by the Goldich dissolution series. In this series, quartz is the most stable, followed by feldspar, micas...

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Olivine

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the less stable common minerals on the surface according to the Goldich dissolution series. It alters into iddingsite (a combination of clay minerals, iron...

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Sandstone

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to weathering processes at the Earth's surface, as seen in the Goldich dissolution series. Framework grains can be classified into several different categories...

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Soil

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minerals commonly weather relatively quickly, according to the Goldich dissolution series. The plants are supported by the porous rock as it is filled with...

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Red beds

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hydrolysis of hornblende and other iron-bearing detritus follows Goldich dissolution series. This is controlled by the Gibbs free energy of the particular...

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Quartz

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rocks. Quartz has the lowest potential for weathering in the Goldich dissolution series and consequently it is very common as a residual mineral in stream...

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Trace metal stable isotope biogeochemistry

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589–592. doi:10.6028/jres.068A.056. PMC 6592378. PMID 31834740. Shields WR, Goldich SS, Garner EL, Murphy TJ (January 1965). "Natural variations in the abundance...

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