T. Itaya et al., ARGON RELEASE SYSTEMATICS OF HYPOGENE AND SUPERGENE ALUNITE BASED ON PROGRESSIVE HEATING EXPERIMENTS FROM 100 TO 1000-DEGREES-C, Geochimica et cosmochimica acta, 60(22), 1996, pp. 4525-4535
Few minerals have as many different geological applications for K-Ar o
r Ar-39/Ar-40 dating as alunite (KAl3(SO4)(2)(OH)(6)): but a basic und
erstanding of the systematics of argon release from this mineral is la
cking. Progressive heating experiments from 100-1000 degrees C at 100
degrees C intervals were conducted in this study to obtain argon relea
se patterns from hypogene and supergene alunite. The samples analyzed
were selected from well understood deposits and are representative of
the principal natural environments of acid-sulfate generation and rela
ted advanced argillic alteration and alunite formation. For gas extrac
tion and purification, a low-blank metallic extraction-purification sy
stem used for dating silicates was complemented with a quartz-Pyrex gl
ass line that included an external resistance furnace. The resulting p
atterns of argon release vs. temperature are well defined and similar
for all the samples. Quantitative release of radiogenic Ar-40 occurs d
uring the dehydroxylation reaction of alunite at temperatures >400 and
<700 degrees C, in association with the first phase transformation of
alunite during thermal decomposition to alum and alumina. This observ
ation applies to alunites of different origin, regardless of character
istics such as grain size, crystal habit, growth temperature, and natu
re or origin of alunite-formation fluids. It applies as well to alunit
e treated chemically to remove small amounts of contaminant phases, su
ch as illite. Argon released at <300 degrees C is dominated by atmosph
eric argon adsorbed on the mineral surfaces, and Ar released at >800 d
egrees C is mainly derived from the extraction system. The results ind
icate that the retentivity of Ar in fine-grained supergene alunite is
similar to that of coarsely crystalline hypogene alunite. The data sup
port the reliability of K-Ar dating of hypogene and supergene alunite
and provide practical information to conduct routine high precision an
alyses.