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標(biāo)題: Titlebook: Geology and Mineral Resources of Nigeria; Nuhu George Obaje Book 2009 Springer-Verlag Berlin Heidelberg 2009 Crystalline rock.Geological e [打印本頁]

作者: ACORN    時(shí)間: 2025-3-21 18:45
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作者: Petechiae    時(shí)間: 2025-3-21 22:50
Introduction the centrally-located city of Abuja; previously, the Nigerian government was headquartered in Lagos. Nigeria is famous for her huge population of about 140 million people – the largest national population on the African continent.
作者: Bronchial-Tubes    時(shí)間: 2025-3-22 01:28
Book 2009r, an account of the previous and current mining policies (including that of petroleum) of the Nigerian government is given and goes ahead to list some specific investment opportunities in the solid minerals sector..
作者: 強(qiáng)壯    時(shí)間: 2025-3-22 07:23
0930-0317 possible the reserves estimation. Thereafter, an account of the previous and current mining policies (including that of petroleum) of the Nigerian government is given and goes ahead to list some specific investment opportunities in the solid minerals sector..978-3-662-51910-3978-3-540-92685-6Series ISSN 0930-0317 Series E-ISSN 1613-2580
作者: 混亂生活    時(shí)間: 2025-3-22 11:57
0930-0317 ded into three parts. Part 1 discusses the geology of the crystalline rocks and their regional distribution while the sedimentary basins constitute the subject of Part 2. Part 3 takes the mineral resources of Nigeria one on one, their geological environment, mode of occurrence, localities and where
作者: Germinate    時(shí)間: 2025-3-22 15:35
https://doi.org/10.1007/978-94-015-9727-2rar Bous in the north of Niger is Ordovician in age, with progressively younger ages southwards. The most southerly ring complex of Afu is Late Jurassic in age (Bowden et al., 1976). Aeromagnetic anomalies suggest that a series of buried NE–SW lineaments of incipient rifts controlled the disposition of the individual complexes (Ajakaiye, 1983).
作者: Germinate    時(shí)間: 2025-3-22 18:16
Differential Mathematical Models,s, namely, Cameroon, Central African Republic, Niger, Chad, and Nigeria. The Bornu Basin falls between latitudes 11°N and 14°N and longitudes 9°E and 14°E, covering Borno State and parts of Yobe and Jigawa States of Nigeria.
作者: cauda-equina    時(shí)間: 2025-3-22 22:43

作者: abolish    時(shí)間: 2025-3-23 02:45
Book 2009geology of the crystalline rocks and their regional distribution while the sedimentary basins constitute the subject of Part 2. Part 3 takes the mineral resources of Nigeria one on one, their geological environment, mode of occurrence, localities and where possible the reserves estimation. Thereafte
作者: 思考而得    時(shí)間: 2025-3-23 06:58

作者: carotid-bruit    時(shí)間: 2025-3-23 09:53

作者: 虛情假意    時(shí)間: 2025-3-23 15:53
https://doi.org/10.1007/978-3-319-58184-2tion declined considerably, particularly in metallic minerals. The tempo of mining activities shifted to industrial non-metallic minerals needed for construction, building and industrial applications in domestic industries.
作者: BLAND    時(shí)間: 2025-3-23 19:51

作者: ABHOR    時(shí)間: 2025-3-23 22:27

作者: helper-T-cells    時(shí)間: 2025-3-24 04:01

作者: synovial-joint    時(shí)間: 2025-3-24 10:03

作者: Myelin    時(shí)間: 2025-3-24 11:09
Vector Fields and Differential Equations,ng over 100 anticlines and synclines (Benkhelil, 1989). Major such deformational structures include the Abakaliki anticlinorium and the Afikpo syncline in the Lower Benue, the Giza anticline and the Obi syncline in the Middle Benue, and the Lamurde anticline and the Dadiya syncline in the Upper Benue Trough.
作者: 充氣球    時(shí)間: 2025-3-24 15:15
Cretaceous – Cenozoic Magmatism and Volcanismult zone, which was reactivated in the Cretaceous. The flood basalts of the Biu Plateau are situated on the Zambuk Ridge of the Upper Benue Trough, and the smaller Longuda Plateau lies near the bifurcation of the Upper Benue Trough, which has been identified as a possible secondary triple junction (Fig. 3.1).
作者: 鍵琴    時(shí)間: 2025-3-24 22:39
The Benue Troughng over 100 anticlines and synclines (Benkhelil, 1989). Major such deformational structures include the Abakaliki anticlinorium and the Afikpo syncline in the Lower Benue, the Giza anticline and the Obi syncline in the Middle Benue, and the Lamurde anticline and the Dadiya syncline in the Upper Benue Trough.
作者: APO    時(shí)間: 2025-3-25 00:21
The Younger Granitesrar Bous in the north of Niger is Ordovician in age, with progressively younger ages southwards. The most southerly ring complex of Afu is Late Jurassic in age (Bowden et al., 1976). Aeromagnetic anomalies suggest that a series of buried NE–SW lineaments of incipient rifts controlled the disposition of the individual complexes (Ajakaiye, 1983).
作者: Addictive    時(shí)間: 2025-3-25 06:31

作者: 有惡臭    時(shí)間: 2025-3-25 07:35
Petroleum Resources are put at 35 billion barrels for oil and 180 trillion standard cubit feet for gas. At the moment production is entirely from fields in the Niger Delta region while exploration campaigns have been carried and/or ongoing in different segments of Nigeria’s sedimentary basins.
作者: 個(gè)阿姨勾引你    時(shí)間: 2025-3-25 14:13
978-3-662-51910-3Springer-Verlag Berlin Heidelberg 2009
作者: Folklore    時(shí)間: 2025-3-25 19:36

作者: 售穴    時(shí)間: 2025-3-25 22:54
Differential Geometry of Foliationsa. There are thirty six (36) federating states alongside the Federal Capital Territory (FCT) that make up the Federal Republic of Nigeria (Fig. 1). A total of 774 local government councils are recognized in the Constitution of the Federal Republic of Nigeria. Since 1991, the Nigeran capital has been
作者: 兇兆    時(shí)間: 2025-3-26 02:30

作者: Infirm    時(shí)間: 2025-3-26 05:45

作者: MELON    時(shí)間: 2025-3-26 10:45

作者: Palpable    時(shí)間: 2025-3-26 15:35
Vector Fields and Differential Equations,imit is the northern boundary of the Niger Delta, while the northern limit is the southern boundary of the Chad Basin (Fig. 4.1). The trough contains up to 6,000 m of Cretaceous – Tertiary sediments of which those predating the mid-Santonian have been compressionally folded, faulted, and uplifted in
作者: hermitage    時(shí)間: 2025-3-26 16:54
Differential Mathematical Models,try. It represents about one-tenth of the total area extent of the Chad Basin, which is a regional large structural depression common to five countries, namely, Cameroon, Central African Republic, Niger, Chad, and Nigeria. The Bornu Basin falls between latitudes 11°N and 14°N and longitudes 9°E and
作者: GREEN    時(shí)間: 2025-3-27 00:38

作者: cluster    時(shí)間: 2025-3-27 04:54

作者: generic    時(shí)間: 2025-3-27 05:16

作者: indigenous    時(shí)間: 2025-3-27 10:41
https://doi.org/10.1007/978-3-642-11102-0 separation of the continents of South America and Africa in the late Jurassic (Whiteman, 1982). Subsidence of the African continental margin and cooling of the newly created oceanic lithosphere followed this separation in early Cretaceous times. Marine sedimentation took place in the Benue Trough a
作者: 玷污    時(shí)間: 2025-3-27 15:56
Linear Structures on Manifolds,ccording to reports by the Geological Survey of Nigeria Agency, Nigeria has some 34 known major mineral deposits distributed in locations across the country and offers considerable attraction for investors. Exploration in Nigeria for several solid minerals, e.g. tin, niobium, lead, zinc and gold, go
作者: FACET    時(shí)間: 2025-3-27 19:06
Time, Uncertainty and Incomplete Markets and exporter on the African continent and is currently closely followed in production level by Angola, Libya and Gabon. Current reserves (as at 2008) are put at 35 billion barrels for oil and 180 trillion standard cubit feet for gas. At the moment production is entirely from fields in the Niger Del
作者: CODA    時(shí)間: 2025-3-28 00:57

作者: DUCE    時(shí)間: 2025-3-28 05:21
https://doi.org/10.1007/978-3-540-92685-6Crystalline rock; Geological environment; Mineral resources; Mining; Nigeria; Petroleum; crystal; developme
作者: 極大的痛苦    時(shí)間: 2025-3-28 08:15
Nuhu George ObajeIncludes supplementary material:
作者: APO    時(shí)間: 2025-3-28 14:14
Differential Operators on Manifoldsaverage elevation varying from 250 to 400 m above sea-level. This plain is occasionally interrupted by low mesas. A low escarpment, known as the “Dange Scarp” is the most prominent feature in the basin and it is closely related to the geology.
作者: BALE    時(shí)間: 2025-3-28 16:55

作者: 較早    時(shí)間: 2025-3-28 21:54
Introductiona. There are thirty six (36) federating states alongside the Federal Capital Territory (FCT) that make up the Federal Republic of Nigeria (Fig. 1). A total of 774 local government councils are recognized in the Constitution of the Federal Republic of Nigeria. Since 1991, the Nigeran capital has been
作者: 不給啤    時(shí)間: 2025-3-29 00:42
The Basement Complexplex forms a part of the Pan-African mobile belt and lies between the West African and Congo Cratons (Fig. 1.2) and south of the Tuareg Shield (Black, 1980). It is intruded by the Mesozoic calc-alkaline ring complexes (Younger Granites) of the Jos Plateau and is unconformably overlain by Cretaceous
作者: Retrieval    時(shí)間: 2025-3-29 06:14
The Younger Granites 200?km wide and 1,600?km long extending from northern Niger to south central Nigeria. Rb/Sr whole rock dating indicates that the oldest complex of Adrar Bous in the north of Niger is Ordovician in age, with progressively younger ages southwards. The most southerly ring complex of Afu is Late Jurass
作者: 值得    時(shí)間: 2025-3-29 09:40

作者: angiography    時(shí)間: 2025-3-29 11:35

作者: 強(qiáng)化    時(shí)間: 2025-3-29 16:33
The Bornu Basin (Nigerian Sector of the Chad Basin)try. It represents about one-tenth of the total area extent of the Chad Basin, which is a regional large structural depression common to five countries, namely, Cameroon, Central African Republic, Niger, Chad, and Nigeria. The Bornu Basin falls between latitudes 11°N and 14°N and longitudes 9°E and
作者: 畸形    時(shí)間: 2025-3-29 22:20
The Sokoto Basin (Nigerian Sector of the Iullemmeden Basin)average elevation varying from 250 to 400 m above sea-level. This plain is occasionally interrupted by low mesas. A low escarpment, known as the “Dange Scarp” is the most prominent feature in the basin and it is closely related to the geology.
作者: 群居動(dòng)物    時(shí)間: 2025-3-30 03:01
The Mid-Niger (Bida) Basinn Niger State of Nigeria to areas slightly beyond Lokoja in the south. It is delimited in the northeast and southwest by the basement complex while it merges with Anambra and Sokoto basins in sedimentary fill comprising post orogenic molasse facies and a few thin unfolded marine sediments (Adeleye,
作者: 完成才能戰(zhàn)勝    時(shí)間: 2025-3-30 07:17
The Dahomey Basinto southwestern Nigeria. It is separated from the Niger Delta by a subsurface basement high referred to as the Okitipupa Ridge. Its offshore extent is poorly defined. Sediment deposition follows an east-west trend. In the Republic of Benin, the geology is fairly well known (Billman, 1976; De Klasz,




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