WebMay 19, 2015 · Paleopiezometry estimation indicates that flame perthite formed under the influence of low to moderate differential stress on granitoids. Most of the perthites occurs in these granitoids are compositionally albite to oligoclase in nature. The composition ranges X Ab: 0.98–0.49 for the Malanjkhand and X Ab: 0.96–0.49 for Dongargarh granitoids. WebIn addition, development of fine to medium grained micro-perthite (patches and strings of albite in microcline) viz., vein, string, patchy and flame perthite (Fig. 3h) suggests deuteric activity ...
Modelling of dissolution–reprecipitation ion-exchange …
WebLocal occurrence of flame perthite is attributed to late greenschist-facies deformation and recrystallization (Pryer and Robin, 1995; Parsons et al., 2005). ... WebPasschier (1985) described flame perthites in which the distribution of flames was directly related to the amount of deformation within a K-feldspar grain, the model, flames grow by replacement behind a coherently propagating tip; the external stress influences the free energy of the process and thereby controls the orientation and extent of … fmg flow meter group
(PDF) Retrograde metamorphic reactions in deforming granites …
WebJan 1, 2002 · Flame perthite bearing K-feldspar is common. Braid and vein perthites occur occasionally. Paleopiezometry estimation indicates that flame perthite formed under the influence of low to moderate ... WebMay 19, 2015 · Three varieties of perthites have been identified in these granitoids i.e. flame, braid, and vein types. Flame perthite bearing K-feldspar is common. Braid and … WebSince flame growth is controlled by the imposed differential stress and not by strain in the host rock, flame perthite has potential as a palaeostress-direction indicator. Albite flames result from the replacement of K-feldspar by albite through alkali exchange. In flame perthites from deformed granites within the Grenville Front Tectonic Zone ... greensburg orthopedic doctors