Moreover, a great quantity of winding and rub can not only produce more
mylonite or other broken coals but also seal original cleats, micro-fractures, and seepage pores for C[O.sub.2] transport [49].
A shear zone of about 10 m thick is associated to this fault, mainly constituted by foliated cataclasites and
mylonites (Fig.
In the case of LF1 quartz
mylonite, we have simulated different AMS responses based on quantitative texture analysis.
Ductile fault zones (
mylonites) show elongated cavities along the foliation, showing evidences of fluid circulations.
In the west, the Strazek Moldanubicum is demarcated by the Pribyslav
mylonite zone; in the northeast the Strazek Moldanubicum joins the Nasavrky Massif, or the southernmost spur of the Hlinsko zone and the Svratka crystalline complex.
P-T conditions have been constrained using geothermobarometers in high temperature
mylonites while to constraint the P-T conditions during the ductile to brittle tectonic evolution of the MCTZ zone fluid inclusion analyses have been performed on quartz lenses from kyanite bearing gneisses and micaschists sampled from the Main Central Thrust Zone and in quartz inclusions trapped in garnet crystals.
In this paper we report U-Pb age data on titanite from an augen granitoid
mylonite in the eastern part of the DPDZ.
North Tirek- The Tirek North licence is located on the eastern edge of the In Ouzzal mole, which consists of a band of
mylonites between 300 and 3,000 metres thick corresponding to a major tectonic deformation rift (called the In Ouzzal Fault Zone).
On the northern part of the Miroslav horst are placed the
mylonites of Brunnia, on its southern part and in the Krhovice foreland Moravicum and on the south Dunkelsteiner Moldanubicum.
It is built up of metadacites, phyllites, mica schists, gneisses, and
mylonites.
Authors divided fault rocks into three basic types namely cataclasites,
mylonites and metamorphic rocks.
In the west of Iran recognized shear zone, accommodated
mylonite zone that related to the closure of Neo-Tethys and Zagros orogeny contractional event (Mohajjel and Fergusson, 2000; Agard et al., 2005; Allen and Amstrong, 2008; Agard et al., 2011; Mouthereau et al., 2012).
