The Investigation of Rodingits Petrogrophy from middlePart of SabzevarOphiolite (Village of Soleimaniye and Baghjar)

Category Petrology
Group GSI.IR
Location 21th symposium on geosciences
Holding Date 21 May 2008

Abstract:
      Processes of Rodingitization, is the most observed in the basic rocks within ultramafic rocks.
   These rocks are composed commonly of hydro-grossular, grossular, andradite, diopside, vesuvianite, epidot, prehnite, pectolite, xenotlite and etc.
   They occur as metasomatically altered dykes and other lithic tectonic inclusion within the serpentinite bodies.    

General:
     Processes of Rodingitization, is the most observed in the basic rocks within ultramafic rocks.
   These rocks are composed commonly of hydro-grossular, grossular, andradite, diopside, vesuvianite, epidot, prehnite, pectolite, xenotlite and etc.
   They occur as metasomatically altered dykes and other lithic tectonic inclusion within the serpentinite bodies.

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