35 research outputs found

    Strain partitioning and dimensional preferred orientation in a syn-tectonic granitoid, southeast Nigeria

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    Uwet granodiorite, a syn-tectonic granitoid of Pan-African age in southeastern Nigeria is partly porphyritic, containing megacrysts of Kfeldspars,xenoliths and ellipsoidal bodies. The preferred orientations of the feldspar phenocrysts are in the NE-SW, NW-SE and N-S, the strongest being the NW-SE trend. The E-W sectors show minimum grain orientation. Calculated values of strain–arithmetic mean R , geometric mean G and harmonic mean H, show minimum strain for grains in E-W orientation and maximum strain for grains in N-S orientation. Phenocrysts in NE-SW and NW-SE orientations showed intermediate values of strain, with the latter axis having higher values than the former. Generally, irrespective of orientation or axis, the relationship R > G>H was found to hold. The analysis favours the interpretation that when two simple shears and a pure shear operatesimultaneously in a viscous/ductile matrix at high temperature, undera non-hydrostatic stress state, dimensional preferred orientation andstrain are partitioned unequally along those axes. The paucity of phenocryst orientation and low strain values in the E-W axis are anindication that maximum compressive stress (á1) was oriented in thisdirection, during the Pan-African Orogeny

    Physico-chemical properties and industrial potential of some clay deposits in Calabar area, south eastern Nigeria

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    Clay samples collected from 10 locations in Calabar, Cross River State, Nigeria were evaluated to determine their suitability for industrial applications. The samples were pulverized, dried, sieved and quantitatively analyzed. Physical properties determined were viscosity (11-15 secs), density (1072-1769 kg m-3), plasticity index (33-50%), particle size and firing characteristics. The clays were classified as fat clays or elastic silt. Results showed that all the clay samples were uniformly graded with fine texture and have the ideal silica value averaging 47.73% but the alumina content of the samples are lower than theoretical values of pure montmorillonite (28.3%) and kaolinite (39.5%), with averaging 18.0%. X-ray analysis indicated that the dominant clay mineral found in all the samples is kaolin with occasional illite and the main non-clay mineral as quartz. Considerable amounts of Fe2O3 (2.79-6.95%) along withsome impurity oxides such as MgO (0.08-0.98%), CaO (0.12-0.95%), K2O (0.28-1.82%), Na2O (1.02- 1.87%) and TiO2 (0.96-1.20%) were found in all the clay minerals. These properties indicated that the clays are of low grade (non- refractory) due to the low alumina content. The low alumina content with the relatively high plasticity index and the pleasant color characteristics of the clays on firing, suggest that the clays have the potentials for use in the production of brick, ceramic and pottery products

    Effects of Weathering on Mechanical Properties of Granite Gneiss and Dolerite: A Case Study of Oban and Obudu Basement Rocks South-Eastern Nigeria

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    This paper describes the geotechnical characteristics of granite gneiss and dolerite from Oban and Obuduregions in South-eastern Nigeria. The suitability of these rocks for civil construction purposes and the effects of weathering on their mechanical properties are examined. The results indicate that compressive strength ranges from 19.31 to 77.37 MN/m2 and 40.5 to 140.0MN/m2 for the granite gneiss and dolerite respectively. Their respective Young Modulus ranged 13.60 to 84.20GPa and 24.45 to 102.50 GPa.The low values obtained for compressive strength and Young Modulus in this work are the direct effects of the humid tropical conditions that cause weathering of the rocks at the base of the overburden aided by water. In addition to weathering, structural defects such as fractures, joints, faults and the mechanical drilling process tend to introduce micro-pores/fractures in the samplesthereby leading to a decrease in the strength and modulus of these rocks.Furthermore, the moisture content (W%) and the degree of weathering decrease with increasing hardness (H), specific gravity (SG),compressive strength (α) and Young Modulus(E). The relationship between moisture content, the degree of weathering and the mechanical properties – particularly compressive strength (α) and Young modulus (E)also showsthat the fresh (FR) to slightly weathered(SW) rocks are generally suitable for most civil construction works than the extremely weathered(EW) to highly weathered (HW) rocks.KEYWORDS: BasementRocks,Mechanical Properties,Weathering Grades(FR-EW),Oban/Obudu

    A comparative study of ree geochemistry in precambrian pegmatites and associated host rocks from western Oban Massif, Se – Nigeria

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    The area of study (Igbofia-Akwa Ibami-Iwuru) is located between Latitudes 5o20'N and 5o27'N, and Longitudes 8o09'E and 8o18'E, south-eastern Nigeria. The pegmatites of this area have been studied by several authors for several decades till now. The present study evaluates the use of trace and rare-earth elements (REE) as finger prints in comparing the geochemistry of pegmatites and their associated host rocks, and to deduce if there is any co-genetic relationship between them. Sixteen representative samples of pegmatites and their host rocks (schist andgranodiorites) were collected and analysed using the ICP-MS analytical method. The pegmatites were found to be richer than their host rocks in SiO2, Al2O3 Na2O+K2O (alkali), Rb, Li, Cs, Be, Na, Zn, Nb, and Ga while they are poorer in Fe2O3, CaO, Sr, Ba, Zr, U, Cr, Th, and all the REEs. Only in the MgO contents are the rocks similar. Compared trace elements and REE data of schist and granodiorite (host rocks) against associated pegmatite samples in this work, show that the pegmatites are not necessarily products of their host rocks
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