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The catchment drains exposures of two main rock units, the Neranleigh Fernvale Beds and the Bunya Phyllite.
b Geo Coverage landsat ETM (2000) overlay DEM showing the main rock units in the study area.
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The main mode of deformation in late Miocene and younger rock units was strike-slip faulting, which produced oblique-slip normal faults and en-echélon folds.
Some method of correlating rock units must be found.
There are several source rock units in the Zagros Basin.
Litharenite and lithic quartz sandstone are the main rock types.
Relative geologic ages can be deduced in rock sequences consisting of sedimentary, metamorphic, or igneous rock units.
This is because the rocks have been dated using only biostratigraphy, a process in which paleontologists compare the fossils preserved in a rock unit of uncertain age with rock units of known age that preserve similar fossils.
All these rock units are complicatedly stacked in 3-D with the HP/UHP rocks being obliquely southwestward extruded.
Biostratigraphy is the differentiation of rock units based upon the fossils which they contain.
Furthermore, the overall hydrochemical profiles revealed the main hydrochemical facies as Ca Mg -HCO3 (dominant) and Na(K)-HCa Mg -HCO3 water types which can be attributedominantsolution of minerand iNathe various rocK -HCO3 in the study area.
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