Dyke Swarms: Keys for Geodynamic Interpretation
Keys for Geodynamic Interpretation
(Sprache: Englisch)
Dykes occur in a wide variety of geological and tectonic settings and their detailed study through space and time is imperative for understanding several geological events. Dykes are believed to be an integral part of continental rifting and when they occur...
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Dykes occur in a wide variety of geological and tectonic settings and their detailed study through space and time is imperative for understanding several geological events. Dykes are believed to be an integral part of continental rifting and when they occur as spatially extensive swarms of adequate size, they can be of immense utility in continental reconstructions and also help to identify Large Igneous Provinces (LIPs). It is known that continental flood basalts and major dyke swarms have their origin related in some way to the up-rise of hot mantle plumes which may lead to rifting and eventual continental break-up. Dykes signify crustal extension and are important indicators of crustal stabilisation events, supercontinental assembly and dispersal, crust-mantle interaction and play a significant role in the delineation of crustal provinces as well as in deciphering crustal evolution events. Many economic mineral deposits of the world are also associated with a variety of dykes. The volume will provide state-of-the-art information on all aspects of dykes with emphasis on the origin, evolution and emplacement of dykes.
Dykes occur in a wide variety of geological and tectonic settings and their detailed study through space and time is imperative for understanding several geological events. Dykes are believed to be an integral part of continental rifting and when they occur as spatially extensive swarms of adequate size, they can be of immense utility in continental reconstructions and also help to identify Large Igneous Provinces (LIPs). It is known that continental flood basalts and major dyke swarms have their origin related in some way to the up-rise of hot mantle plumes which may lead to rifting and eventual continental break-up. Dykes signify crustal extension and are important indicators of crustal stabilisation events, supercontinental assembly and dispersal, crust-mantle interaction and play a significant role in the delineation of crustal provinces as well as in deciphering crustal evolution events. Many economic mineral deposits of the world are also associated with a variety of dykes. The volume will provide state-of-the-art information on all aspects of dykes with emphasis on the origin, evolution and emplacement of dykes.
Inhaltsverzeichnis zu „Dyke Swarms: Keys for Geodynamic Interpretation “
From the contents:1: Geochemical and petrological characteristics of Mesozoic dykes from Schirmacher oasis (East Antarctica)Nadezhda Sushchevskaya and Boris Belyatsky MS9: Mafic dykes of Rewa Basin, central India: Implications on magma dispersal and petrogenesisTrisha Lala, A. K. Choudhary, S. K. Patil and D. K. Paul MS24: Petrogenetic comparison of the mafic dykes in the Kohistan paleo-island arc-back-arc system, Himalayas of North PakistanTahseenullah Khan, Mamuro Murata, Mohammad Zafar and Hafiz Ur Rehman MS25: A Comparison of Chronometers Applied to Monastery Kimberlite and the Feasibility of U-Pb Ilmenite GeochronologyA. K. Noyes, L. M. Heaman and R. A. Creaser Dykes in Laurasia MS26: Precise U-Pb age for the Great Whin Dolerite Complex, N.E. England and its significanceM. A. Hamilton and D. G. PearsonKsenia Dokukina and Alexander Konilov MS29: Small dacite dyke, Southern Urals, Russia: rapidly quenched liquid or fine-grained cumulate?S. Yu. Chistyakova and R. M. Latypov S. Yu. Chistyakova and R. M. LatypovS. Yu. Chistyakova and R. M. Latypov MS27: The Melville Bugt dyke swarm of Greenland: a connection to the 1.5-1.6 Ga Scandinavian rapakivi granite province?H. C. Halls, M. A. Hamilton and S. W. DenyszynKsenia Dokukina and Alexander Konilov MS29: Small dacite dyke, Southern Urals, Russia: rapidly quenched liquid or fine-grained cumulate?S. Yu. Chistyakova and R. M. Latypov S. Yu. Chistyakova and R. M. LatypovS. Yu. Chistyakova and R. M. Latypov MS28: Mafic melt emplacement during the shock deformation in the subvolcanic environment example from Tastau volcanoplutonic ring complex, Eastern Kazakhstan MS30: Primary and secondary chemical zonation in mafic dykes: a case study of the Vochelambina dolerite dyke, Kola Peninsula, Russia MS30: Primary and secondary chemical zonation in mafic dykes: a case study of the Vochelambina dolerite dyke, Kola Peninsula, Russia MS24: Petrogenetic comparison of the mafic dykes in the Kohistan paleo-island arc-back-arc system,
... mehr
Himalayas of North PakistanTahseenullah Khan, Mamuro Murata, Mohammad Zafar and Hafiz Ur Rehman MS25: A Comparison of Chronometers Applied to Monastery Kimberlite and the Feasibility of U-Pb Ilmenite GeochronologyA. K. Noyes, L. M. Heaman and R. A. Creaser Dykes in Laurasia MS26: Precise U-Pb age for the Great Whin Dolerite Complex, N.E. England and its significanceM. A. Hamilton and D. G. PearsonKsenia Dokukina and Alexander Konilov MS29: Small dacite dyke, Southern Urals, Russia: rapidly quenched liquid or fine-grained cumulate?S. Yu. Chistyakova and R. M. Latypov S. Yu. Chistyakova and R. M. Latypov S. Yu. Chistyakova and R. M. Latypov
... weniger
Bibliographische Angaben
- Autor: Rajesh Srivastava
- 2010, XXX, 605 Seiten, Maße: 16,7 x 24,4 cm, Gebunden, Englisch
- Verlag: Springer, Berlin
- ISBN-10: 364212495X
- ISBN-13: 9783642124952
- Erscheinungsdatum: 28.03.2011
Sprache:
Englisch
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