Alice Springs age shear zones from the southeastern Reynolds Range, central Australia
Titel:
Alice Springs age shear zones from the southeastern Reynolds Range, central Australia
Auteur:
Cartwright, I. Buick, I. S. Foster, D. A. Lambert, D. D.
Verschenen in:
Australian journal of earth sciences
Paginering:
Jaargang 46 (1999) nr. 3 pagina's 355-363
Jaar:
1999-06
Inhoud:
The southeast Reynolds Range, central Australia, is cut by steep northwest-trending shear zones that are up to hundreds of metres wide and several kilometres long. Amphibolite-facies shear zones cut metapelites, while greenschist-facies shear zones cut metagranites. Rb-Sr and 40Ar-39Ar data suggest that both sets of shear zones formed in the 400-300 Ma Alice Springs Orogeny, with the sheared granites yielding well-constrained 40Ar-39Ar ages of ca 334 Ma. These data imply that the shear zones represent a distinct tectonic episode in this terrain, and were not formed during cooling from the ca 1.6 Ga regional metamorphism. A general correlation between regional metamorphic grade and the grade of Alice Springs structures implies a similar distribution of heat sources for the two events. This may be most consistent with both phases of metamorphism being caused by the burial of anomalously radiogenic heat-producing granites. The sheared rocks commonly have undergone metasomatism implying that the shear zones were conduits of fluid flow during Alice Springs times.