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Book Description Condition: New. Seller Inventory # ABLIING23Mar3113020287789
Book Description Condition: New. PRINT ON DEMAND Book; New; Fast Shipping from the UK. No. book. Seller Inventory # ria9783659477881_lsuk
Book Description PF. Condition: New. Seller Inventory # 6666-IUK-9783659477881
Book Description PAP. Condition: New. New Book. Shipped from UK. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000. Seller Inventory # L0-9783659477881
Book Description Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The area under investigation lie on the eastern side of the Cuddapah basin and is situated in the Eastern Ghats Precambrian mobile belt (Lat. 15o35' - 15o41' N and Long. 79o43' - 79o53' E). The rocks encountered in the area of study are khondalite group, charnockites, granites and dolerites. Petrographic and Petrochemical (Major, Trace and REE) study of various rocks my be summarized that khondalites (pelitic gneisses, quartzites and pyroxene granulites) are the sediments which have subsequently metamorphosed under granulite facies conditions. During this high grade metamorphism, there is a possibility of anatectic melts developed forming the charnockites which are seen as lenses within the gneisses and granulites and the latter may represent restites. Some of the hydrous minerals like biotite and hornblende in the granulites and charnockites may indicate retrogression suffered by the emplacement of granite. At this stage the whole crust has become rigid and yielded to fractures, which forms the channel ways for the dolerites to emplace. 120 pp. Englisch. Seller Inventory # 9783659477881
Book Description Taschenbuch. Condition: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The area under investigation lie on the eastern side of the Cuddapah basin and is situated in the Eastern Ghats Precambrian mobile belt (Lat. 15o35' - 15o41' N and Long. 79o43' - 79o53' E). The rocks encountered in the area of study are khondalite group, charnockites, granites and dolerites. Petrographic and Petrochemical (Major, Trace and REE) study of various rocks my be summarized that khondalites (pelitic gneisses, quartzites and pyroxene granulites) are the sediments which have subsequently metamorphosed under granulite facies conditions. During this high grade metamorphism, there is a possibility of anatectic melts developed forming the charnockites which are seen as lenses within the gneisses and granulites and the latter may represent restites. Some of the hydrous minerals like biotite and hornblende in the granulites and charnockites may indicate retrogression suffered by the emplacement of granite. At this stage the whole crust has become rigid and yielded to fractures, which forms the channel ways for the dolerites to emplace. Seller Inventory # 9783659477881
Book Description PAP. Condition: New. New Book. Delivered from our UK warehouse in 4 to 14 business days. THIS BOOK IS PRINTED ON DEMAND. Established seller since 2000. Seller Inventory # L0-9783659477881
Book Description Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Katta Sathya Sai PrasadSatya Sai Prasad. Katta Born on 22nd June 1957 Completed his M.Sc., in 1979 and Ph.D. in 1987. After that he worked as U.G.C. R A up to 2000. Later occupied as Asst. Professor in Dept. of Geology, S.V.Unive. Seller Inventory # 5158514