Andere Kunden interessierten sich auch für
![Metamorphic and metasomatic complexes of the Ukrainian Shield]( "Metamorphic and metasomatic complexes of the Ukrainian Shield")
Metamorphic and metasomatic complexes of the Ukrainian Shield51,99 €![Complexes métamorphiques et métasomatiques du Pobuzhye moyen]( "Complexes métamorphiques et métasomatiques du Pobuzhye moyen")
Complexes métamorphiques et métasomatiques du Pobuzhye moyen42,99 €![Tectonic evolution of South Sinai metamorphic complexes]( "Tectonic evolution of South Sinai metamorphic complexes")
Tectonic evolution of South Sinai metamorphic complexes51,99 €![Element of geology]( "Element of geology")
Element of geology39,99 €![Abu Khruq and El Kahfa alkaline ring complexes]( "Abu Khruq and El Kahfa alkaline ring complexes")
Abu Khruq and El Kahfa alkaline ring complexes36,99 €![Metamorphe und metasomatische Komplexe des mittleren Pobuzhye]( "Metamorphe und metasomatische Komplexe des mittleren Pobuzhye")
Metamorphe und metasomatische Komplexe des mittleren Pobuzhye64,90 €![Metamorphic Rocks as the Key to Understanding Geodynamic Processes]( "Metamorphic Rocks as the Key to Understanding Geodynamic Processes")
Metamorphic Rocks as the Key to Understanding Geodynamic Processes135,00 €
Five unstratified metamorphic complexes of Archean to Cenozoic age were identified and described on the basis of structural relationships in the reference section along the Bug River. Petrotypes of complexes have been identified in the section section of about 200 km, their mappability, mapping features, structural position and age have been shown. Eight metasomatic complexes were identified. All the selected complexes are brought together in a unified scheme by their relative age; the correctness of the constructions is verified by the results of isotope-geochronological studies. The presence of gneiss-dome formations has been confirmed and a new type of tectonic structures for the Middle Pobuzhye - metamorphic melanges of shear-thrust morphology - has been established. Widespread development of low-amplitude Alpine thrusts has been established. The structural position of the known gold ore occurrences is clarified and two new prospecting areas for ore gold are proposed. The methodology used allows the results to be obtained directly in the field and can be verified by alternative methods.