Banded Iron Formations (BIF) is one of the unique and important rock types in the Archaean greenstone belts and Proterozoic metasedimentary series. They occupy a unique position in the sedimentation history of this time range, as they have no modern analogues. This virtual confinement of BIF in space and in time has made them extremely useful for the understanding of the Precambrian exogenic processes and the atmospheric – environmental changes that occurred during the early history of the earth. The BIF are described with different names in different parts of the world such as, Taconite – U.S.A.; Jaspilite – Australia; Itabirite – Brazil. BIF are of economic interest as they host the world’s largest iron ore deposits. There are several major aspects related to the origin and evolution of BIF for which no satisfactory and generally agreed explanation are available. Various genetic models have been proposed which, however, differ considerably from each other. The divergent conclusions of these workers bring to the fore, the problem of deciphering the origin of BIF in Nigeria and how they relate to other major BIF occurrences of the world. The workers differ in their conclusions rega
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Banded Iron Formations (BIF) is one of the unique and important rock types in the Archaean greenstone belts and Proterozoic metasedimentary series. They occupy a unique position in the sedimentation history of this time range, as they have no modern analogues. This virtual confinement of BIF in space and in time has made them extremely useful for the understanding of the Precambrian exogenic processes and the atmospheric – environmental changes that occurred during the early history of the earth. The BIF are described with different names in different parts of the world such as, Taconite – U.S.A.; Jaspilite – Australia; Itabirite – Brazil. BIF are of economic interest as they host the world’s largest iron ore deposits. There are several major aspects related to the origin and evolution of BIF for which no satisfactory and generally agreed explanation are available. Various genetic models have been proposed which, however, differ considerably from each other. The divergent conclusions of these workers bring to the fore, the problem of deciphering the origin of BIF in Nigeria and how they relate to other major BIF occurrences of the world. The workers differ in their conclusions rega
Aliyu A. Ibrahim, Ph.D: Studied Mineral Exploration at Ahmadu Bello University Zaria, Nigeria. A lecturer in Geochemistry, Ore deposits, Ore evaluation and Mineral economics. I was a Mining Geologist in the Geological Survey Nigeria, and then a Lecturer at Hussaini Adamu Polytechnic. Now a lecturer at Ahmadu Bello University Zaria, Nigeria.
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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Banded Iron Formations (BIF) is one of the unique and important rock types in the Archaean greenstone belts and Proterozoic metasedimentary series. They occupy a unique position in the sedimentation history of this time range, as they have no modern analogues. This virtual confinement of BIF in space and in time has made them extremely useful for the understanding of the Precambrian exogenic processes and the atmospheric environmental changes that occurred during the early history of the earth. The BIF are described with different names in different parts of the world such as, Taconite U.S.A.; Jaspilite Australia; Itabirite Brazil. BIF are of economic interest as they host the world s largest iron ore deposits. There are several major aspects related to the origin and evolution of BIF for which no satisfactory and generally agreed explanation are available. Various genetic models have been proposed which, however, differ considerably from each other. The divergent conclusions of these workers bring to the fore, the problem of deciphering the origin of BIF in Nigeria and how they relate to other major BIF occurrences of the world. The workers differ in their conclusions rega 168 pp. Englisch. N° de réf. du vendeur 9783845411255
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Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Abdu Ibrahim AliyuAliyu A. Ibrahim, Ph.D: Studied Mineral Exploration at Ahmadu Bello University Zaria, Nigeria. A lecturer in Geochemistry, Ore deposits, Ore evaluation and Mineral economics. I was a Mining Geologist in the Geologic. N° de réf. du vendeur 5481092
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Taschenbuch. Etat : Neu. Banded Iron Formation: Petrology, Geochemistry and Genesis | case study of Maru Schist Belt, Nigeria | Aliyu Abdu Ibrahim | Taschenbuch | 168 S. | Englisch | 2011 | LAP LAMBERT Academic Publishing | EAN 9783845411255 | Verantwortliche Person für die EU: OmniScriptum GmbH & Co. KG, Bahnhofstr. 28, 66111 Saarbrücken, info[at]akademikerverlag[dot]de | Anbieter: preigu. N° de réf. du vendeur 106898710
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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -Banded Iron Formations (BIF) is one of the unique and important rock types in the Archaean greenstone belts and Proterozoic metasedimentary series. They occupy a unique position in the sedimentation history of this time range, as they have no modern analogues. This virtual confinement of BIF in space and in time has made them extremely useful for the understanding of the Precambrian exogenic processes and the atmospheric - environmental changes that occurred during the early history of the earth. The BIF are described with different names in different parts of the world such as, Taconite - U.S.A.; Jaspilite - Australia; Itabirite - Brazil. BIF are of economic interest as they host the world's largest iron ore deposits. There are several major aspects related to the origin and evolution of BIF for which no satisfactory and generally agreed explanation are available. Various genetic models have been proposed which, however, differ considerably from each other. The divergent conclusions of these workers bring to the fore, the problem of deciphering the origin of BIF in Nigeria and how they relate to other major BIF occurrences of the world. The workers differ in their conclusions regaVDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 168 pp. Englisch. N° de réf. du vendeur 9783845411255
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Taschenbuch. Etat : Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Banded Iron Formations (BIF) is one of the unique and important rock types in the Archaean greenstone belts and Proterozoic metasedimentary series. They occupy a unique position in the sedimentation history of this time range, as they have no modern analogues. This virtual confinement of BIF in space and in time has made them extremely useful for the understanding of the Precambrian exogenic processes and the atmospheric environmental changes that occurred during the early history of the earth. The BIF are described with different names in different parts of the world such as, Taconite U.S.A.; Jaspilite Australia; Itabirite Brazil. BIF are of economic interest as they host the world s largest iron ore deposits. There are several major aspects related to the origin and evolution of BIF for which no satisfactory and generally agreed explanation are available. Various genetic models have been proposed which, however, differ considerably from each other. The divergent conclusions of these workers bring to the fore, the problem of deciphering the origin of BIF in Nigeria and how they relate to other major BIF occurrences of the world. The workers differ in their conclusions rega. N° de réf. du vendeur 9783845411255
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