International Peer-Reviewed JournalOpen AccessISSN 2456-8880
irejournals@gmail.com+91-7433024337

Home / Current Issue / Paper 1710360

1710360 Vol 9 · Issue 2 Download Paper

Petrology and Geochemistry of Dolerite Samples from Crushed Rock Quarry Site in Ishiagu Area of the Lower Benue Trough, Southern Nigeria

Bariborve Kpegeol

Subject area: Science,Engineering and Technology  ·  Area of research: Petrology and Geochemistry

Abstract

Ten (10) Igneous rock samples were collected at random from freshly dug parts of the Crushed Rock Quarry pit located at Ishiagu in Ebonyi State, Nigeria which is found on the Lower Benue Trough. After the physical observation, three of the samples were later subjected to chemical analysis which revealed that igneous intrusions in ishiagu are mainly intermediate to basic in terms of classification, and also the igneous intrusions found there have a wide range of varieties from acid to basic. The rock samples obtained from the Crushed Rock Quarry site suggest acid or intermediate rock from physical observation. The petrographic study (thin section analysis) show a high percentage estimate of plagioclase (50%) in one of the samples. Other minerals observed were olivine, muscovite, microcline, hornblende, biotite, and pyroxene, which further suggests that the rocks are basic. Geochemical analysis, which is the most precise, put silica (SiO2) percentage content at between 46.96-47.40%, and also a relatively high average content of Cr (233.3ppm), Ni (216ppm), Sr (231.3ppm), V (166.3ppm), Ce (18.2ppm), and Nd (10.5) in trace and rare earth element analyses. Discrimination diagrams plot the rock samples in Komatiite+Basalt+Dolerite field and Ocean Island Basalt field. The existence of this different classes of igneous rock in the same outcrop can be explained by the process known as magma mixing or magma mingling and caused by varying degrees of partial melting of the source magma that formed the rocks.

Keywords

Dolerite, Lower Benue Trough, Petrology, Geochemistry, Igneous Intrusion, Basalt Field

References

[1] Obaje, N. G. (2009). The Benue Trough. Geology and Mineral Resources of Nigeria. Springer, p.98 ISBN 0-04-556001-3.

[2] Wright, J. B. (1976). South Atlantic Continental Drift and the Benue Trough. Tectono-physics, 6:301-310.

[3] Ofoegbu, C. O. (1985). A Review of the Geology of the Benue Trough of Nigeria. Journal of African Earth Science. 3:283-291.

[4] Reyment, R. A. (1965). Ibadan University Press, 23-70.

[5] Grant, N. K. (1971). South Atlantic, Benue Trough and Gulf of Guinea Cretaceous Triple Junction. Geological Society of America Bulletin. 82:2299-2302.

[6] Freeth, S. J. (1977). Earth Planet Science Letter. 82:2299-2302.

[7] Chukwuebuka, K. C., Egesi, N., and Beka F. T. (2010). Structural Geology of the Lower Benue Trough : A case study of the Ishiagu Area of Ebonyi State, Nigeria. AAPG Search and Discovery Article number 90115 copyright 2010. AAPG African Regional Annual Conference, Abuja, Nigeria, 14-19 November.

[8] Fatoye, F. B. and Gideon, Y. B. (2013). Geology and Mineral resources of the lower Benue Trough, Nigeria. Advances in Applied Science Research. 4(6):21-28. www.pelagic research library.com. .

[9] Chiadikobi, K. C., Beka, F. T., and Chiaghanam, O. I. (2011). Structural Attributes of igneous intrusives in Ishiagu Area of Ebonyi State, Nigeria. Archives of Applied Science Research. 3(5):390-403.

[10] Wright, J. B. (1985). The Benue Trough. Geology and Mineral Resources of West Africa. Springer, p.98, ISBN 0-40-55600-3.

[11] Obioha, Y. E. (2018). Ba - Pb Mineralization in Ugwuajirija Ishiagu Area, Lower Benue Trough, Southeastern Nigeria: Geological Evidence. Global Journal of Pure and Applied Sciences. 24:161-170. http://DX.

[12] Ani, E. C. and Oha, I. A. (2020). Petrological Characteristics of some Cretaceous igneous rocks, in Southwest of Gboko, Southern Benue Trough, Nigeria. Journal of Geology and Mining Research. 12(2):35-44.

[13] Etuk, E. E., Ukpabi, N., Ukaegbu, V. U. and Akpabio, I. O. (2008). Structural Evolution, Magmatism, and Effects of Hydrocarbon Maturation in Lower Benue Trough, Nigeria: A Case Study Lokpaukwu, Uturu, and Ishiagu. The Pacific Journal of Science and Technology. 9(2).

[14] Ajakaiye, D. E., Hall, D. H., Miller, T. W., Verheijen, P. J. T., Awad, M. B. and Ojo, S. B. (1986). Aeromagnetic Anomalies and Tectonic Trends in and around the Benue Trough of Nigeria. Nature Physical Science. 3:582-584.

[15] Nwachukwu, M. A., Chinaka, C. and Nwachukwu, M. I. (2010). Petrographic analysis for naming and classifying an igneous intrusive rock of the Lower Benue Trough Nigeria. Journal of geology and mining research, 3:63-72.

[16] Ukaegbu, V. U. and Okonny, I. P. (2003). Introduction to Igneous and Metamorphic Petrology (Volume 1). Spendid (Publishing). Revised Edition, p.18, ISBN 978-33620-9-0.

[17] Owuamalam, E. (2012). Petrology and Geochemistry of igneous rock samples from Crushed Rock Quarry pit in Ishiagu area of the Lower Benue Trough. An unpublished work submitted to the Geology and Mining Department, School of Science Laboratory Technology, University of Port Harcourt, Nigeria.

[18] Wood, D. A. (1980). The Application of a Th- Hf-Ta Diagram to problems Tectomagmatic classification and to Establishing the Nature of Crustal Contamination of Basaltic Lavas of the British Tertiary Volcanic Province. Earth and Planetary Science Letters, 50:11-30.

[19] Meschede, M. (1986). A method of Discrimination between Different Types of Mid-oceanic Ridge Basalts and Continental Tholeiites with the Nb-Zr-Y Diagram. Chemical Geology, 56:207-218.

How to cite this paper

Bariborve Kpegeol "Petrology and Geochemistry of Dolerite Samples from Crushed Rock Quarry Site in Ishiagu Area of the Lower Benue Trough, Southern Nigeria" Iconic Research And Engineering Journals Volume 9 Issue 2 2025 Page 1064-1071
Bariborve Kpegeol "Petrology and Geochemistry of Dolerite Samples from Crushed Rock Quarry Site in Ishiagu Area of the Lower Benue Trough, Southern Nigeria" Iconic Research And Engineering Journals, vol. 9, no. 2, Aug. 2025
Bariborve Kpegeol (2025). Petrology and Geochemistry of Dolerite Samples from Crushed Rock Quarry Site in Ishiagu Area of the Lower Benue Trough, Southern Nigeria. Iconic Research And Engineering Journals, 9(2).
Bariborve Kpegeol "Petrology and Geochemistry of Dolerite Samples from Crushed Rock Quarry Site in Ishiagu Area of the Lower Benue Trough, Southern Nigeria" Iconic Research And Engineering Journals, vol. 9, no. 2, Aug. 2025.
@article{1710360,
      author = {Bariborve Kpegeol},
      title = {Petrology and Geochemistry of Dolerite Samples from Crushed Rock Quarry Site in Ishiagu Area of the Lower Benue Trough, Southern Nigeria},
      journal = {Iconic Research And Engineering Journals},
      year = {2025},
      volume = {9},
      number = {2},
      pages = {1064-1071},
      issn = {2456-8880},
      url = {https://www.irejournals.com/formatedpaper/1710360.pdf},
      abstract = {Ten (10) Igneous rock samples were collected at random from freshly dug parts of the Crushed Rock Quarry pit located at Ishiagu in Ebonyi State, Nigeria which is found on the Lower Benue Trough. After the physical observation, three of the samples were later subjected to chemical analysis which revealed that igneous intrusions in ishiagu are mainly intermediate to basic in terms of classification, and also the igneous intrusions found there have a wide range of varieties from acid to basic. The rock samples obtained from the Crushed Rock Quarry site suggest acid or intermediate rock from physical observation. The petrographic study (thin section analysis) show a high percentage estimate of plagioclase (50%) in one of the samples. Other minerals observed were olivine, muscovite, microcline, hornblende, biotite, and pyroxene, which further suggests that the rocks are basic. Geochemical analysis, which is the most precise, put silica (SiO2) percentage content at between 46.96-47.40%, and also a relatively high average content of Cr (233.3ppm), Ni (216ppm), Sr (231.3ppm), V (166.3ppm), Ce (18.2ppm), and Nd (10.5) in trace and rare earth element analyses. Discrimination diagrams plot the rock samples in Komatiite+Basalt+Dolerite field and Ocean Island Basalt field. The existence of this different classes of igneous rock in the same outcrop can be explained by the process known as magma mixing or magma mingling and caused by varying degrees of partial melting of the source magma that formed the rocks.},
      keywords = {Dolerite, Lower Benue Trough, Petrology, Geochemistry, Igneous Intrusion, Basalt Field},
      month = {August},
  }