Chemical Weathering and
Chemical Sedimentary Minerals
Roger Weller, geology instructor
wellerr@cochise.edu
copyright
2007-R.Weller
The primary igneous minerals, those found in Bowen's reaction series, are
susceptible
to chemical weathering.
Water (H2O), carbon dioxide
(CO2), and volcanic gases such as
sulfur dioxide (SO2),
hydrogen sulfide (H2S), sulfuric
acid (H2SO4),
chlorine (Cl2), hydrochloric
acid (HCl), and others are the prime
chemicals responsible for the chemical
weathering
processes which release cations. The secondary or sedimentary minerals that form can be
changed
into
sedimentary rocks by evaporation and deposition.
primary
cations
secondary
chemical
igneous
released
by
sedimentary
sedimentary
minerals
weathering
minerals
rocks
olivine
Mg+2
CaCO3-calcite
------------------limestone
pyroxene
Fe+2
(Ca,Mg)CO3-dolomite
-----------dolomite
(dolostone)
amphibole
Ca+2
CaSO4.2H2O-gypsum
-----------gypsum
(gypstone)
biotite
Na+1
NaCl-halite
---------------------------salt
plagioclase
Al+3
clay
minerals
-----------------------shale
orthoclase
K+1
KCl-sylvite
----------------------------potash salt
quartz
Si+4
SiO2-quartz
---------------------------chert,
flint, jasper
muscovite
SiO2.nH20-opal
---------------------opalite,
sinter
Fe3O4-magnetite ------------------iron ore
Fe2O3-hematite --------------------iron ore
Fe2O3.nH2O-limonite ------------iron
ore