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Petrology of Obachettapalem Ongole Area Prakasam District South India: Igneous and Metamorphic Complex - Softcover
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.
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Satya 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.University, Tirupati. In his research cheerer he published more than 40 publications in national and international journals.
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- PublisherLAP LAMBERT Academic Publishing
- Publication date2013
- ISBN 10 3659477885
- ISBN 13 9783659477881
- BindingPaperback
- Number of pages120
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Petrology of Obachettapalem Ongole Area Prakasam District South India: Igneous and Metamorphic Complex
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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
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Petrology of Obachettapalem Ongole Area Prakasam District South India : Igneous and Metamorphic Complex
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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
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Petrology of Obachettapalem Ongole Area Prakasam District South India Igneous and Metamorphic Complex
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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
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