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lead zinc mineralization of the benue trough

Contrasting styles of leadzincbarium mineralization in

Contrasting styles of leadzincbarium mineralization in

Topics LeadZincBarium mineralization, Benue Trough, epigenetic, vein deposits, Mineralización PlomoZincBario, Benue Trough, Epigénesis, Vetas., Geology, QE1996.5

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Risks associated with the mining of PbZn minerals in some

Risks associated with the mining of PbZn minerals in some

The environmental effects of the mining of leadzinc mineralization in Enyigba area, Southern Benue trough were examined. The samples used for this study were obtained from abandoned mine sites, mine tailings, streams, handdug wells, mine pond and borehole. Collected samples were subjected to Xray fluorescence, Xray diffraction analyses, atomic absorption spectrometry and permeability tests.

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Genesis of the Lead Zinc Mineralization, Upper Benue

Genesis of the Lead Zinc Mineralization, Upper Benue

Leadzinc mineralization in the upper Benue Trough is confined towelldefined steeply dipping fractures and faults striking inan NS direction. A close examination of the mineralized structures of abandoned mine workings revealed that the strike length of the veins varies from a few meters with thickness ranging from

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1. Introduction  SCIRP

1. Introduction SCIRP

A brief look at the geology of Nigeria is important to give an idea of the geological composition of the country in terms of the ore bearing rock groupings, while the review of PbZn mineralization is intended to give credence to findings in previous studies that the Benue Trough houses some of the complex sulphide minerals including the leadZinc deposits under study [8] .

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GEOLOGY AND MINERALISATION IN THE ALBIAN SEDIMENTS

GEOLOGY AND MINERALISATION IN THE ALBIAN SEDIMENTS

ABSTRACT The epigenetic leadzincbarite fluorite deposits of the Benue Trough are localized in NS trending fractures developed within the lower Cretaceous

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Contrasting styles of leadzincbarium mineralization in

Contrasting styles of leadzincbarium mineralization in

Olade, M. A. (1976). On the genesis of the leadzinc deposits in Nigerians Benue rift (aulacogen) a reinterpretation. Nigerian Journal of Mining Geology, 13, 2027. [ Links ] Olade, M. A. Morton, R. D. (1985). Origin of leadzinc mineralization in the southern Benue Trough, Nigeria, fluid inclusion and trace element studies.

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lead zinc mineralization in nigeria

lead zinc mineralization in nigeria

Title Origin of leadzinc mineralization in the southern Benue Trough, Nigeria Fluid inclusion and trace element studies Authors Olade, M. A.; Morton, R. D. Published in Mineralium Deposita · 1985Authors M A Olade · Roger D MortonAffiliation University of Ibadan · University of AlbertaAbout Zinc · Trace element.

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Origin of leadzinc mineralization in the southern BenueCited by 33

Origin of leadzinc mineralization in the southern Benue

· Origin of leadzinc mineralization in the southern Benue Trough, Nigeria Fluid inclusion and trace element studies. M. A. Olade 1 R. D. Morton 2 Mineralium Deposita volume 20, pages 7680 (1985)Cite this article

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BENUE TROUGH PDF  otel Seven Brothers

BENUE TROUGH PDF otel Seven Brothers

Jun 12, 2021· Leadzincbaritefluorite mineralization occurs along the km axis of the trough in three discrete subbasins trugh coincide with the lower, middle and upper mineral districts of the Benue Valley. Main ionospheric trough in the daytime sector studied on the basis of vertical sounding data.

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Contrasting styles of leadzincbarium mineralization in

Contrasting styles of leadzincbarium mineralization in

Contrasting styles of leadzincbarium mineralization in the Lower Benue Trough, Southeastern Nigeria . and GabuOshina which together constitute the four main areas of mineralization in the Lower Benue Trough, show that mineralization appears restricted to NWSE and NS fractures while the more common NESW fractures are barren. Apart from

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Ishiagu leadzinc deposit, Nkanu East, Enugu, Nigeria

Ishiagu leadzinc deposit, Nkanu East, Enugu, Nigeria

The geologic setting of leadzinc deposits at Ishiagu, southeastern Nigeria. Journal of African Earth Sciences (1983), 2 (2), 97101. Olade, M. A., Morton, R. D. (1985). Origin of leadzinc mineralization in the southern Benue Trough, NigeriaFluid inclusion and trace element studies.

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Geological Characterization of Azara Barite Mineralization

Geological Characterization of Azara Barite Mineralization

The Azara Barites Mineralization in The Middle Benue Trough Occurs as Vein Infilling Materials associated with LeadZinc Lodes. A Fracture Formed as Single Linear Structures with

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Geological Characterization of Azara Barite Mineralization

Geological Characterization of Azara Barite Mineralization

The Azara Barites Mineralization in The Middle Benue Trough Occurs as Vein Infilling Materials associated with LeadZinc Lodes. A Fracture Formed as Single Linear Structures with thickness of generally not more than 0.5m. The Geological Characterization of The Azara Barite Deposits which Include; Geotechnical, Petrological

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Model of Pb/Zn mineralization genesis in the CretaceousCited by 4

Model of Pb/Zn mineralization genesis in the Cretaceous

Jan 01, 1990· The leadzinc mineralization of the Benue Trough, distributed along the main anticlinal structures, forms a belt running for about 500 km. They occur in tensional submeridian fractureas resulting from the tectonic regime prevailing during the early stage of the Benue Trough infilling.

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Ishiagu leadzinc deposit, Nkanu East, Enugu, Nigeria

Ishiagu leadzinc deposit, Nkanu East, Enugu, Nigeria

The geologic setting of leadzinc deposits at Ishiagu, southeastern Nigeria. Journal of African Earth Sciences (1983), 2 (2), 97101. Olade, M. A., Morton, R. D. (1985). Origin of leadzinc mineralization in the southern Benue Trough, NigeriaFluid inclusion and trace element studies.

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Lead Reservoirs and Metallization in Nigeria Example of a</h3>IntroductionGeological SettingMethodologyDiscussionConclusionsAcknowledgmentsAuriferous fields within the Gondwana continental landmass in Nigeria and NE Brazil include Archaean to Early Proterozoic crystalline cores of the West African and Congo cratons, the PanAfrican mobile belt between the cratons and their Phanerozoic cover rocks (Figure 1) (Dada, 1995). The heterogeneous nature of the late Proterozoic continental collision thermotectonic event, particularly its allpervasive structural and metamorphic obliteratory effect on the preexisting older rocks, has necessitated the depl

Lead Reservoirs and Metallization in Nigeria Example of a

IntroductionGeological SettingMethodologyDiscussionConclusionsAcknowledgmentsAuriferous fields within the Gondwana continental landmass in Nigeria and NE Brazil include Archaean to Early Proterozoic crystalline cores of the West African and Congo cratons, the PanAfrican mobile belt between the cratons and their Phanerozoic cover rocks (Figure 1) (Dada, 1995). The heterogeneous nature of the late Proterozoic continental collision thermotectonic event, particularly its allpervasive structural and metamorphic obliteratory effect on the preexisting older rocks, has necessitated the deplChat
Raven Minerals Lead Zinc business opportunity in Nigeria

Raven Minerals Lead Zinc business opportunity in Nigeria

Mar 06, 2011· unexplored parts of middle Benue Trough in which there where either insufficient or no formation but with geological settings favoring a successful predictive exploration were targeted during our cause of research. Previously most Nigerian geologist were of the opinion

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OLADE  What does OLADE stand for? The Free Dictionary

OLADE What does OLADE stand for? The Free Dictionary

Contrasting styles of leadzincbarium mineralization in the Lower Benue Trough, Southeastern Nigeria/Contraste de estilos de mineralizacion de plomozincbario en la parte baja de la Formacion Benue Trough, en el sudeste de Nigeria

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Mapping Geological Structures Controlling Mineralization

Mapping Geological Structures Controlling Mineralization

Abakaliki leadzinc mineralization is believed to be of hydrothermal origin emplaced at a low temperature of about 1400 and it is made up of primarily four lodes namely Ishiagu, Enyigba, Ameri, Ameka in the lower Benue Trough (Kaliberng, 2011).

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Origin of leadzinc mineralization in the southern Benue

Origin of leadzinc mineralization in the southern Benue

The geochemical studies of the Enyingba leadzinc mineralization in the Lower Benue Trough was carried out to unravel the elemental association of the mineralization along with the gangue minerals

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regional geology of the benue trough

regional geology of the benue trough

2007126 · 2. Benue trough The Benue trough (Fig. 1a) is a linear depression filled with up to 6 m of Cretaceous (AlbianMaastrichtian) sediments. The earlier (AlbianSantonian) sediments in the trough are mainly marine in character and their deposition was terminated by an episode of (PDF) The Southern Benue Trough and Anambra Basin

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Exploration of LeadZinc (PbZn) Mineralization Using Very

Exploration of LeadZinc (PbZn) Mineralization Using Very

Lower Benue Trough during the early Cretaceous separation of Africa and America [6]. The PbZn deposits in Ishiagu area appear to be the southern limit of mineralization in the Benue Trough and the PbZn mineralized zone extends over a distance of 500 km in a narrow belt from Ishiagu in the lower Benue Trough to

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Logo Lead/zinc project

Logo Lead/zinc project

Regional mineralization style indicate lead/zinc sulphide ores often associated with Barites and small amount of copper, occurring in lodes filling the fractures within the

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Discovery and Definition of Sedimentary Exhalative

Discovery and Definition of Sedimentary Exhalative

Discovery and definition of sedimentary exhalative mineralization enhances leadzincsilver resources in the Benue Trough, Nigeria Introduction Occurrences of lead, zinc, silver and barites have been recorded in parts of the Benue Trough [Abakaliki, Ishiagu, Arufu/Akwana areas]. Useful contributions include McConnel 1957, Pargeter 1959, Olade 1976.

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regional geology of the benue trough

regional geology of the benue trough

2007126 · 2. Benue trough The Benue trough (Fig. 1a) is a linear depression filled with up to 6 m of Cretaceous (AlbianMaastrichtian) sediments. The earlier (AlbianSantonian) sediments in the trough are mainly marine in character and their deposition was terminated by an episode of (PDF) The Southern Benue Trough and Anambra Basin

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Geochemistry of termite mounds in the sediment hosted

Geochemistry of termite mounds in the sediment hosted

LeadZinc mineralization in the area is almost confined to the highly variable Bima Sandstone (Figure 3). Several contrasting models try to explain the processes of formation of leadzinc deposits in the Upper Benue Trough. These include the magmatichydrothermal model which, on the bases of veins morphology and

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Structural controls of PbZn mineralization of Enyigba

Structural controls of PbZn mineralization of Enyigba

Abakaliki anticlinorium in the Lower 4 Benue Trough. The occurrences of leadzinc in the study area are associated with saline water intrusion in the sedimentary basin. Mineralization occurs along a narrow belt of approximately 30 to 50 km wide and extends for about 560 to 600 km length of the Benue trough in Adamawa,

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Alteration Mapping for LeadZincBarium Mineralization in

Alteration Mapping for LeadZincBarium Mineralization in

LeadZincBarium mineralization has been known in the southern Benue Trough for over a century. However, the first known documentation was in the form of a preliminary report by MacKay (1946), this was followed by a set of generalized but welldocumented field

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Geochemical investigation of surface water from the effect

Geochemical investigation of surface water from the effect

Geological map of the Benue Trough, showing the units of the Middle Benue and Upper Benue subdivisions and leadzinc occurrences. (modified from Cratchley and Jones, 1965 Whiteman, 1982). as well as base metals from clays and feldspars which combined with sulphur to form ores along permeable zones.

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Structural controls of PbZn mineralization of Enyigba

Structural controls of PbZn mineralization of Enyigba

Abakaliki anticlinorium in the Lower 4 Benue Trough. The occurrences of leadzinc in the study area are associated with saline water intrusion in the sedimentary basin. Mineralization occurs along a narrow belt of approximately 30 to 50 km wide and extends for about 560 to

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lead zinc mineralization of the benue trough

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