Major and Trace Element Variations in the Lavas of Shergarh Sar Area and Their Significance with Respect to the Kohistan Tectonic Anomaly
Abstract
A belt of dark-green volcanics along with serpentinite, peridotiie, pyroxenite and greenschist marks the spatial disposition of the Indus suture zone in Allai Kohistan of Hazara division. Major and trace element analyses of selected lava samples are used to investigate geochemical variations in the Shergarh Sar Pashtu village section of the volcanic belt. The lavas are mostly glassy but occasionally show phenocrysts of plagioclase, clinopyroxene and, very rarely, brown hornblende. On the basis of normative mineralogy, two compositional groups, e.g. olivine tholeiite and quartz tholeiite, are identified. Fractionation control of the observed phenocrysts over the major and trace element distribution in the lava$ is established through the solutions of chemical data in the C.M.A.S. model and conventional two-dimensional plots. The major and trace element constraints of the studied lavas are corresponding more closely to tholeiites developed in the island arc type environments and substantiate, through a chemical comparison, the assumed prevalence of such structure(s) in the Tethys ocean before the complete closure as proposed in the tectonic models of the Himalayan development.
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