2015, ISBN: 3659369454

[EAN: 9783659369452], Neubuch, [PU: LAP LAMBERT Academic Publishing Feb 2015], This item is printed on demand - it takes 3-4 days longer - Neuware -The Qinling Orogenic Belt is located in… Mehr…

[EAN: 9783659369452], Neubuch, [PU: LAP LAMBERT Academic Publishing Feb 2015], This item is printed on demand - it takes 3-4 days longer - Neuware -The Qinling Orogenic Belt is located in the central of China and distributes in east-west direction, there are large-scale igneous rocks within this belt, and they are very important record for orogenesis. The investigation on the feature of the source and origin is critical for understanding the composition of lower crust in orogenic belt, dynamic process in depth of orogenesis, and crust-mantle interaction during orogenic process. Nonetheless, the studies of the igneous rocks are mainly focused on the intermediate and acid intrusions, minor investigation on the mafic dykes though they can provide useful information on the geodynamic evolution of an area. This study using geochronological, geochemical, and Sr-Nd-Hf isotopic data of the mafic dykes from Gansu and Shaanxi provinces. Based on the systematic study, the main results are as follows: the mafic dykes were derived from the partial melting of an enriched mantle source due to the collision between the North China Craton and southern Qinling block during 446-450 Ma. In addition, the parental magmas of these dykes then fractionated clinopyroxene, Fe-Ti-bearing phases, biotite, and plagioclase, along with crustal contamination. 60 pp. Englisch, Books<

2015, ISBN: 9783659369452

[ED: Taschenbuch], [PU: LAP LAMBERT Academic Publishing], The Qinling Orogenic Belt is located in the central of China and distributes in east-west direction, there are large-scale igneou… Mehr…

[ED: Taschenbuch], [PU: LAP LAMBERT Academic Publishing], The Qinling Orogenic Belt is located in the central of China and distributes in east-west direction, there are large-scale igneous rocks within this belt, and they are very important record for orogenesis. The investigation on the feature of the source and origin is critical for understanding the composition of lower crust in orogenic belt, dynamic process in depth of orogenesis, and crust-mantle interaction during orogenic process. Nonetheless, the studies of the igneous rocks are mainly focused on the intermediate and acid intrusions, minor investigation on the mafic dykes though they can provide useful information on the geodynamic evolution of an area. This study using geochronological, geochemical, and Sr-Nd-Hf isotopic data of the mafic dykes from Gansu and Shaanxi provinces. Based on the systematic study, the main results are as follows: the mafic dykes were derived from the partial melting of an enriched mantle source due to the collision between the North China Craton and..., DE, [SC: 0.00], Neuware, gewerbliches Angebot, 60, [GW: 107g], Banküberweisung, PayPal, [CT: Sonstiges / Sonstiges]<

ISBN: 9783659369452

Paperback, [PU: LAP LAMBERT Academic Publishing], The Qinling Orogenic Belt is located in the central of China and distributes in east-west direction, there are large-scale igneous rocks … Mehr…

Paperback, [PU: LAP LAMBERT Academic Publishing], The Qinling Orogenic Belt is located in the central of China and distributes in east-west direction, there are large-scale igneous rocks within this belt, and they are very important record for orogenesis. The investigation on the feature of the source and origin is critical for understanding the composition of lower crust in orogenic belt, dynamic process in depth of orogenesis, and crust-mantle interaction during orogenic process. Nonetheless, the studies of the igneous rocks are mainly focused on the intermediate and acid intrusions, minor investigation on the mafic dykes though they can provide useful information on the geodynamic evolution of an area. This study using geochronological, geochemical, and Sr-Nd-Hf isotopic data of the mafic dykes from Gansu and Shaanxi provinces. Based on the systematic study, the main results are as follows: the mafic dykes were derived from the partial melting of an enriched mantle source due to the collision between the North China Craton and southern Qinling block during 446-450 Ma. In addition, the parental magmas of these dykes then fractionated clinopyroxene, Fe-Ti-bearing phases, biotite, and plagioclase, along with crustal contamination., Geology & The Lithosphere<

2015, ISBN: 3659369454

[EAN: 9783659369452], Neubuch, [PU: LAP LAMBERT Academic Publishing], GEOWISSENSCHAFTEN GEOLOGIE ORIGIN ORDOVICIAN MAFIC DYKES GANSU AND SHAANXI PROVINCES QINLING OROGENIC BELT, Dieser Ar… Mehr…

[EAN: 9783659369452], Neubuch, [PU: LAP LAMBERT Academic Publishing], GEOWISSENSCHAFTEN GEOLOGIE ORIGIN ORDOVICIAN MAFIC DYKES GANSU AND SHAANXI PROVINCES QINLING OROGENIC BELT, Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Liu ShenShen Liu, Professor, Northwest University, who was born on 03 Oct., 1974 and is now focused on the mafic dykes from North China Craton and the volcanic rocks from northern Tibet.The Qinling Orogenic Belt is located in the., Books<

ISBN: 9783659369452

Gebundene Ausgabe

Ordovician mafic dykes from Qinling Orogenic Belt China ab 39.99 € als Taschenbuch: . Aus dem Bereich: Bücher, Taschenbücher, Naturwissenschaft, Medien > Bücher nein Taschenbuch Hardcover… Mehr…

Ordovician mafic dykes from Qinling Orogenic Belt China ab 39.99 € als Taschenbuch: . Aus dem Bereich: Bücher, Taschenbücher, Naturwissenschaft, Medien > Bücher nein Taschenbuch Hardcover;Naturwissenschaften, Medizin, Informatik, Technik;Geologie, LAP LAMBERT Academic Publishing<