Deformation Traits in the Charnockitic Rocks of Akure Area, Southwestern Nigeria
The charnockitic rocks of Akure constitute one of the petrologic units of the precambrian basement complex of Southwest Nigeria. The field studies indicate fresh outcrops that show little signs of weathering although the surfaces are rough. The rock is in contact with migmatite and granite gneiss of the migmatite gneiss complex. On the outcrops are the occurrences of pegmatite, aplite and quartz veins as minor intrusions. Petrographic studies revealed hornblende, plagioclase, hypersthene, biotite, quartz, muscovite and opaque minerals as major minerals while zircon is accessory. Bent lamellae in plagioclase, distorted twinning in plagioclase and micro-cracks in virtually all the minerals in the thin sections indicate some element of deformation. Joint sets trend N-S, E-W and NNE-SSW with the N-S set predominating. The trends of the joint sets tally with those of the minor intrusions. The directions of maximum compressional and tensional stresses inferred from the rose diagram are in consonance with the general directions imprinted by the Pan African orogenic events which affected the basement complex rocks. Since, virtually all minerals in the thin sections exhibit traits of deformation indicating that the deformation is penetrative, it is inferred that the cause of the deformation might be tectonic.
Charnockitic rocks generally have diverse origins, spanning a range of metamorphic
and igneous derivations (Kilpatrick and Ellis, 1992)
which implies that igneous or metamorphic fabric can be exhibited. In Nigeria,
charnockitic rocks constitute one of the major petrologic units of the precambrian
basement complex (Olarewaju, 2006). The charnockitic
rocks of Akure area form a part of this unit. The rock suite has been of interest
to the earth scientists partly because of aesthetic value particularly when
polished and partly because of the controversy surrounding the origin. Oyawoye
(1962, 1964) presented a model of metasomatic origin,
Olarewaju (1988) presented the fractional crystallization
model while Rahaman et al. (1988) presented the
tectonic model and Dada et al. (1989) presented
an igneous origin model.
The Nigerian basement complex lies within the remobilized zone of the West
African basement. The major rock types in the area as classified by Adekoya
et al. (2003) are (a) the gneiss-migmatite-quartzite complex; (b)
the schist belts which are low to medium grade supracrustal and meta-igneous
rocks; (c) the Pan African granitoids (Older Granites) and other related rocks
such as charnockitic rocks and syenites and (d) minor felsic and mafic intrusives.
The rock intruded into the migmatite-gneiss-quartzite complex. The study area
lies within longitudes 5°00E and 5°17E and latitudes 7°10N
and 7°20N in the Southwestern part of Nigeria (Fig.
||Geological map of Akure showing study areas, Adapted from
the Geological Map of Nigeria produced by the Geological Survey of Nigeria
In the opinion of Adekoya (1977), tectonic joints are
quantitative and directional manifestations of operative forces that can give
a clue to possible stress distribution in a deformed rock. Workers that reported
on the age/origin of the charnockitic rocks of the precambrian basement complex
of the Southwestern and Southeastern Nigeria include Ekwueme
and Kroner (2006), Rahaman (1976, 1988),
Olarewaju (1988), Oyinloye and Obasi
(2006) and Olarewaju (2006). It is suggested that
the medium-coarse-grained hypersthene-granodiorite of Eastern Hebei Province,
China is the product of crystallization of anatectic magmas of the same composition.
Shitta (2007) described the three types of charnockitic
rocks in Akure area on the basis of their textural characteristics as (1) coarse-grained
as exemplified by the Akure body, (2) massive fine-grained which form along
the margins of the granitic bodies as seen in Ijare, Uro and Edemo-Idemo and
(3) the gneissic fine-grained types which were recognized within the bodies
of the gneisses in Ilara and Iju. The charnockitic rocks of Akure-Ikerre-Ado
Ekiti have earlier been described as an association (Olarewaju,
2006). It is concluded that alteration pathways from fresh to weathered
charnokitic rocks are clearly different under each climate conditions.
MATERIALS AND METHODS
The outcrops of the rock in the area were observed for their texture, mineralogy,
structure, field relationship and mode of occurrence. The joint system was studied
for the density and trend. Samples were collected for laboratory studies. The
petrography was studied with the petrographic microscope and the modal analysis
was done by visual counting. The photomicrographs were further studied with
an application by the Sun Microsystems, Inc., 4150 Network Circle, Santa Clara,
California 95054, USA, known as Image J version 1.40c (2008). To trace the grains
with this application, click file and go to open. Select the photomicrograph
to be studied. Then go to process and select find edges. The rose diagram was
plotted with a bin size of 20 while the minimum and maximum values of the axis
are 0 and 25, respectively.
RESULTS AND DISCUSSION
Mode of Occurrence and Field Characteristics
Charnockitic rocks in the study area occurred as small intrusions and pavement
outcrops within the migmatite-gneiss-quartzite complex. The rock type was massive,
greenish in color and medium to coarse grained. The outcrops were fresh showing
little signs of weathering but the surfaces were rough with a lot of pegmatite
intrusions that trend N-S, E-W and NNE-SSW cutting through the outcrops (Fig.
2 a, b). Joint sets trending N-S, E-W and NNE-SSW occurred
on the outcrops. Some of the E-W trending joints cut through some of the veins.
Hornblende, plagioclase, hypersthene, biotite, orthoclase, quartz, muscovite
and opaque minerals (probably iron oxide) were the major minerals while zircon
was the accessory identified in the thin section of the rock. The modal analysis
of the thin sections of the rock gave an average of 25, 24, 14, 11, 8, 7, 6,
4 and 0.6%, respectively.
The grains carried inclusions of quartz and some particularly orthoclase displayed
carlsbad twinning. The hornblende would likely to be of secondary growth. Plagioclase
displayed albite twinning but some of the grains showed bent or distorted twinning,
undulose extinction and most of them exhibited micro-cracks (Fig.
3a, b). Hypersthene grains showed a lot of cracks while
biotite flakes carried inclusions of zircon (Fig. 4). Some
of the muscovite flakes showed distorted cleavage and some carry inclusions
of quartz and zircon. The opaque minerals which are most likely alteration products,
probably iron oxide, had symplectic relation with hornblende and biotite.
Generally, the minerals had irregular shapes and possessed sutured edges in
thin section. There were no evidences of weathering and virtually all minerals
possessed micro-cracks and/or distorted twinning, bent lamellae and compressed
twin plane (Fig. 3a-d).
||(a) N-S, E-W, NNE-SSW trending pegmatite veins in charnockitic
rock and (b) pegmatite vein cutting through an outcrop of the charnockitic
||Photomicrographs of the charnockitic rock showing signs of
stress. Figure 3a, b and d
were under crossed nicol while Fig. c was under plane polarized light. X40.
(a) Plagioclase showing undulose extinction and distorted twinning; micro-cracks
in diopside (hypersthene) and biotite with inclusions of zircon, (b) micro-cracks
in almost all grains of the minerals and plagioclase showing undulose extinction
as well as bent lamellae, (c) some of the minerals in the rock exhibiting
micro-cracks and (d) some of the minerals in the rock exhibiting micro-cracks
Grain trace of the photomicrographs with Image J provided clear evidences of distorted twinning in plagioclase (Fig. 4), undulose extinction and bent lamellae in plagioclase (Fig. 5) and compressed plane of carlsbad twin in orthoclase (Fig. 6).
The trend of the joints were analyzed and applied to plot a rose diagram
(Fig. 7). The density of the joints as shown by the study
was an average of 6 strike (N-S trending), 4 dip (E-W trending) and 2 oblique
(NNE-SSW trending) joints per ten square meters. The result showed the predominance
of the N-S trending set followed by the set that trend E-W and the set that
Observations of the studied rock in the field revealed massive, medium to coarse-grained
texture and grains that are not aligned or elongated except at the margins of
minor intrusions. This observation is in line with Rahaman
(1976, 1988) and Shitta (2007)
reports of massive coarse-grained rock in Akure. On the basis of textural characteristics,
these workers differentiated the rocks from the massive fine-grained and the
gneissic types in the area which implies that the rock is not deformed.
The trends of the joints are consistent with the trends of the minor intrusions
registered in the rock (Fig. 2a, b). According to Turner
and Verhoogen (1960), joint of tectonic origin are expected to have a simple
relation to the rest of the rock fabric. This is an indication that the joints
recorded in this work would most likely be of tectonic origin.
||Grain trace of photomicrograph (Fig. 3a)
with Image J showing distorted twinning in plagioclase
||Grain trace of photomicrograph (Fig. 3b)
with Image J showing undulose extinction and bent lamellae in plagioclase
||Grain trace of photomicrograph (Fig. 3d)
with Image J showing compressed plane of carlsbard twin in orthoclase
||Rose diagram of the joints in the charnockitic rock
Read and Watson (1962) suggested that joints are visible
expressions of residual forces released after deformation. The presence of three
joint sets is therefore an indication that the rock must have experienced deformation.
Odeyemi (1981) suggested that the precambrian basement
complex of Nigeria, of which this rock is a lithologic unit, experienced polycyclic
The petrography reveals (1) undulose extinction in quartz and plagioclase;
(2) distorted twinning in plagioclase; (3) bent lamellae in plagioclase; (4)
compressed plane of carlsbad twin of orthoclase and (5) micro-cracks in virtually
all minerals of the rock. All these are traits of deformation and therefore
a confirmation that the rock has indeed experienced deformation. Ekwueme
and Kroner (2006) reported indications that zircons have recorded several
precambrian high-grade metamorphisms which is an indication that granulite facies
metamorphism affected the basement of Southeastern Nigeria. This is in consonance
with the model of origin proposed by Olarewaju (2006)
for the Idanre-Akure-Ado Ekiti charnockitic rock. The presence of zircon in
this rock and the correlations in the proposals of Ekwueme
and Kroner (2006) and Olarewaju (2006), makes it
reasonable to infer that the rock, like those of the Southeastern Nigeria, might
have experienced several precambrian high-grade metamorphisms with the consequence
of accompanying deformation. Generally, since inclusions predate their hosts,
the presence of inclusions of quartz and zircon in other minerals in the rock
points to the fact that the rock has a transformation history.
Grain trace of the photomicrographs with ImageJ shows clearly the distortion of the albite twins in plagioclase as a result of compressional force (Fig. 4), undulosity and bent lamellae in plagioclase (Fig. 5) and compressed carlsbad twin plane in orthoclase (Fig. 6). All these signs of deformation confirm a directional stress which might have happened as a result of high grade metamorphism.
In line with the opinion of Adekoya (1977), the rose
diagram (Fig. 7) shows the predominance of strike joint set
which is an indication that N-S is the direction of least compressional stress.
The dip joint set, which is less prominent, runs perpendicularly to the foliation
meaning that E-W is the direction of maximum compressional stress. This follows
the general trend of the Pan African orogenic event that affected the basement
complex rocks which therefore, is an indication that the rock experienced some
form of deformation.
Evidences from joint and petrographic studies suggest that the charnockitic rock in Akure area experienced deformation leaving imprints of sets of joints, undulosity, bent lamellae, distorted twinning, compressed twin plane and micro-structures. It is evident that this is a result of high grade metamorphism as virtually all minerals in the rock were affected in one way or the other showing the penetrative effect of the deformation. This implies that the deformation suffered by the rock will most likely be of tectonic origin.
Prof. Adekoya, J. A. of the Department of Applied Geology, the Federal University of Technology, Akure, is highly appreciated for his supervisory role during the course of this research.
1: Adekoya, J.A., 1977. A note on jointing in the basement complex of the Ibadan area, Oyo State, Nigeria. J. Min. Geol., 14: 48-52.
2: Adekoya, J.A., O.O. Kehinde-Phillips and A.M. Odukoya, 2003. Geological Distribution of Mineral Resources in Southwest Nigeria. In: Prospects for Investment in Mineral Resources of Southwestern Nigeria, Elueze, A.A. (Ed.). Elsevier, USA., ISBN: 978-36831-0-1, pp: 1-13
3: Oyinloye, A.O. and R. Obasi, 2006. Geology, geochemistry and geotectonic setting of Pan-African granites and charnockites around Ado-Ekiti, Southwestern Nigeria. Pak. J. Sci. Ind. Res., 49: 299-308.
Direct Link |
4: Dada, S.S., J.R. Lancelot and Briqueu, 1989. Age and origin of the annular charnockitic complex at Toro, Northern Nigeria: U-Pb and Rb-Sr evidence. J. Afr. Earth Sci., 9: 227-234.
5: Ekwueme, B.N. and A. Kroner, 2006. Single zircon ages of migmatitic gneisses and granulites in the Obudu Plateau: Timing of granulite-facies metamorphism in southeastern Nigeria. J. Afr. Earth Sci., 44: 459-469.
6: Holland, T.H., 1900. The Charnockite Series, A Group of Archaean Hypersthenic Rocks in Peninsular India. In: Geological Survey India Memoir 28, Part 2, Reprinted in Granulites of South India, Radhakrishna, B.P., M. Ramakrishnan and B. Mahabaleswar (Eds.). Geological Society of India Memoir, India, pp: 7-27
7: Hubbard, F.H., 1975. Precambrian crustal development in Western Nigeria: Indication from the Iwo region. Geol. Soc. Am. Bull., 86: 548-554.
CrossRef | Direct Link |
8: Shitta, K.A., 2007. Lithostratigraphy of Nigeria: An overview. Proceedings of 32nd Workshop on Geothermal Reservoir Engineering, Jan. 22-24, Stanford University, Stanford, California, pp: 18-23
9: Kilpatrick, J.A. and D.J. Ellis, 1992. C-type magmas : Igneous charnokites and their extrusive equivalents. Trans. R. Soc. Edinburgh Earth Sci., 83: 155-164.
Direct Link |
10: Kroner, A., B.N. Ekwueme and R.T. Pidgeon, 2001. The oldest rock in West Africa: SHRIMP zircon age for early archean migmatitic orthogneiss at Kaduna, Northern Nigeria. J. Geol., 109: 399-406.
Direct Link |
11: Odeyemi, I., 1981. A review of the orogenic events in the Precambrian basement of Nigeria, West Africa. Geologische Rundschau, 70: 897-909.
CrossRef | Direct Link |
12: Olarewaju, V.O., 1988. Petrology and Geochemistry of the Charnockitic and Associated Granitic Rocks of Ado-Ekiti, Akure, S.W. Nigeria. Geological Survey of Nigeria Publication, Nigeria, pp: 231-239
13: Olarewaju, V.O., 2006. The Charnockitic Intrusive of Nigeria. In: The Basement Complex of Nigeria and its Mineral Resources, Oshin, O. (Ed.). Akin Jinad Co., Ibadan, Nigeria, pp: 45-70
14: Oyawoye, M.O., 1962. The petrology of the district around Bauchi, Northern Nigeria. J. Geol., 70: 604-615.
Direct Link |
15: Oyawoye, M.O., 1964. The contact relationship of charnockite and biotite gneiss at Bauchi, Northern Nigeria. Geol. Magazine, 10: 138-144.
Direct Link |
16: Rahaman, M.A., 1976. A Review of the Basement Geology of South Western Nigeria. In: Geology of Nigeria, Kogbe, C.A. (Ed.). Elizabethan Publishing, Surulere, Lagos State, Nigeria, pp: 41-58
17: Rahaman, M.A., T.R. Ajayi, I.O. Oshin and F.O.I. Asubiojo, 1988. Trace Element Geochemistry and Geotechnic Setting of Ife-Ilesha Schist Belt. In: Precambrian Geology of Nigeria, Oluyide, P.O., W.C. Mbonu, A.E. Ogezi, I.G. Egbuniwe, A.C. Ajibade and A.C. Umeji (Eds.). Geological Survey of Niceria, Publication, Niceria, pp: 241-256
18: Rahaman, M.A., 1988. Recent Advances in the Study of the Basement Complex of Nigeria. In: Precambrian Geology of Nigeria, Oluyide, P.O., W.C. Mbonu, A.E. Ogezi, I.G. Egbuniwe, A.C. Ajibade and A.C. Umeji (Eds.). Geological Survey of Nigeria, Kaduna, Nigeria, pp: 11-43
19: Read, H.H. and J. Watson, 1962. Introduction to Geology. Vol. 1, The Macmillan Press Ltd., London, UK., pp: 693
20: Turner, F.J. and J. Verhoogen, 1960. Igneous and Metarmorphic Petrology. 2nd Edn., McGraw-Hill, New York, pp: 694