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CAUSAL MODEL OF SOME SOCIO-PSYCHOLOGICAL VARIABLES AS DETERMINANTS OF ACHIEVEMENT IN SECONDARY SCHOOL SOCIAL STUDIES
Published 1995-05ThesisFull Text AvailableAccess Repository -
Remote telehealth hearing assessment in a rural community : a validation study
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PERSONAL, HOME AND SOCIAL FACTORS AS DETERMINANTS OF FEMALE STUDENTS’ ENROLMENT AND COMPLETION IN UNIVERSITY EDUCATION IN SOUTHWESTERN NIGERIA, 2001-2010
Published 2016ThesisFull Text AvailableAccess Repository -
A roadmap of career capital accrual for knowledge workers
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Development and evaluation of an organizational citizenship behaviour and counterproductive work behaviour structural model
Published 2019Get full text
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Estimation of indoor radon from concrete blocks used In construction of wall in typical Nigerian dwellings
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Cambial responsiveness in four eucalypt varieties to onset of drought as well as spring conditions
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Accelerating deep reinforcement learning for autonomous racing
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Conflict detection and resolution for autonomous vehicles
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Parkinson's disease and the influence of the forebrain dopaminergic system on dreaming
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Towards the development of a substantive professional-in-training model for the human resource profession
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High-temperature metamorphism in the western Namaqua-Natal Metamorphic Province (South Africa): implications for low-pressure granulite terranes
Published 2019“…Semipelite and Mg-Al-rich gneisses yield poorly-constrained estimates that span the range derived from other lithologies. All samples record peak pressure of ∼5-6 kbar, and followed a roughly isobaric heating path from andalusite-greenschist / lower-amphibolite facies conditions through a tight clockwise loop at near-peak conditions, followed by near-isobaric cooling. …”
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High-temperature metamorphism in the western Namaqua-Natal Metamorphic Province (South Africa): implications for low-pressure granulite terranes
Published 2019“…Semipelite and Mg-Al-rich gneisses yield poorly-constrained estimates that span the range derived from other lithologies. All samples record peak pressure of ∼5-6 kbar, and followed a roughly isobaric heating path from andalusite-greenschist / lower-amphibolite facies conditions through a tight clockwise loop at near-peak conditions, followed by near-isobaric cooling. …”
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