scholarly journals STRUCTURAL AND PETROGRAPHIC STUDY OF CRYSTALLINE ROCKS IN PART OF OBAN MASSIF, SOUTH- EASTERN NIGERIA.

2021 ◽  
Author(s):  
Godspower Ubit ◽  
Nsikak E Bassey ◽  
Iniemem J Inim
Keyword(s):  
Crystalline Rocks ◽  
South Eastern ◽  
Oban Massif ◽  
Petrographic Study

scholarly journals Groundwater chemistry of the Oban Massif, South-Eastern Nigeria

2012 ◽  
Vol 7 (1) ◽  
pp. 51-66 ◽  
Author(s):  
Azubuike Solomon Ekwere ◽  
Aniekan E. Edet ◽  
Solomon John Ekwere
Keyword(s):  
Groundwater Chemistry ◽  
South Eastern ◽  
Oban Massif

Mesoscopic Structural Analysis of the Schist Enclaves in Oban Massif, South-Eastern Nigeria

2016 ◽  
Vol 1 (1) ◽  
pp. 1-14
Author(s):  
Enah Asinya ◽  
Michael Oden ◽  
Bassey Ephraim ◽  
Efosa Udinmwen ◽  
Selong Edem
Keyword(s):  
Structural Analysis ◽  
South Eastern ◽  
Oban Massif

scholarly journals Identification and application of petrophysical anomalies for the forecast of ore mineralization on Antei uranium deposit (South-Eastern Tansbaikalia)

2016 ◽  
pp. 24-33
Author(s):  
V. A. Minaev ◽  
A. A. Burmistrov ◽  
V. A. Petrov ◽  
V. V. Poluektov
Keyword(s):  
Uranium Deposit ◽  
Petrophysical Parameters ◽  
South Eastern ◽  
Ore Mineralization ◽  
Petrographic Study

Determination of petrophysical parameters in conjunction with the geological-structural and mineralogical and petrographic study of rocks is necessary to assess the conditions of localization of uranium-molybdenum ore prospects of their processing and assessment of the extent of mineralization at largest vein-stockwork Antei deposit in Russia, located in the granitoid basis of Strel'tsovskaya caldera in the southeastern Transbaikalia.

Etude geologique de la partie centrale du massif granitique de Gueret (Creuse, Massif Central francais)

1959 ◽  
Vol S7-I (8) ◽  
pp. 857-861
Author(s):  
Pierre Vialon
Keyword(s):  
Late Stage ◽  
Close Relationships ◽  
Crystalline Rocks ◽  
Massif Central ◽  
Petrographic Study ◽  
Age Determinations

Abstract The crystalline rocks of the Gueret plateau in the Central Massif of France consist essentially of the so-called Gueret granite and anatexites known as the Aubusson gneiss. The granite exhibits both intrusive and anatectic features. A detailed petrographic study indicates close relationships between the granite and the gneiss and, together with lead-alpha age determinations on zircon, supports the conclusion that the Gueret granite represents a local late-stage product of the Aubusson gneiss formed during remobilization of the migmatitic basement.

Sign in / Sign up

Export Citation Format

Share Document