Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria

The Mubi-Hong area constitutes part of the northeast basement complex of Nigeria and has experienced tectono-metamorphic deformation distinguished into D1, D2 and D3 events. The resultant effect is production of varied ductile and brittle structures (faults, folds, mineral stretching and foliation)...

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Main Authors: S. N. Yusuf, A. Y. Kuku, Y. Ibrahim, S. Kasidi
Format: Article
Language:English
Published: Faculty of Engineering and Technology 2019-09-01
Series:Nigerian Journal of Technological Development
Subjects:
Online Access:https://journal.njtd.com.ng/index.php/njtd/article/view/310
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author S. N. Yusuf
A. Y. Kuku
Y. Ibrahim
S. Kasidi
author_facet S. N. Yusuf
A. Y. Kuku
Y. Ibrahim
S. Kasidi
author_sort S. N. Yusuf
collection DOAJ
description The Mubi-Hong area constitutes part of the northeast basement complex of Nigeria and has experienced tectono-metamorphic deformation distinguished into D1, D2 and D3 events. The resultant effect is production of varied ductile and brittle structures (faults, folds, mineral stretching and foliation) which trends mostly in NNW-SSE direction, with other components NNE-SSW and NE-SW. Deformation and metamorphism in the area can be described as being progressive as indicated by the varied nature of synclinal-anticlinal folds. The tensile tectonism is also responsible for the structures and subsequent emplacement of large volumes of granitoids during Pan-African (600+150Ma). A Multi directional orientation of brittle, planar and linear structures in the area suggests that the area have undergone polyphase deformation similar to those in other parts of the Nigerian basement complex.
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spelling doaj.art-a750a03feb674559959fe6f8f07ad8602022-12-22T02:52:31ZengFaculty of Engineering and TechnologyNigerian Journal of Technological Development2437-21102019-09-01164Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, NigeriaS. N. Yusuf0A. Y. Kuku1Y. Ibrahim2S. KasidiUNIVERSITY OF JOSUNIVERSITY OF MAIDUGURIUNIVERSITY OF MAIDUGURI The Mubi-Hong area constitutes part of the northeast basement complex of Nigeria and has experienced tectono-metamorphic deformation distinguished into D1, D2 and D3 events. The resultant effect is production of varied ductile and brittle structures (faults, folds, mineral stretching and foliation) which trends mostly in NNW-SSE direction, with other components NNE-SSW and NE-SW. Deformation and metamorphism in the area can be described as being progressive as indicated by the varied nature of synclinal-anticlinal folds. The tensile tectonism is also responsible for the structures and subsequent emplacement of large volumes of granitoids during Pan-African (600+150Ma). A Multi directional orientation of brittle, planar and linear structures in the area suggests that the area have undergone polyphase deformation similar to those in other parts of the Nigerian basement complex. https://journal.njtd.com.ng/index.php/njtd/article/view/310Tectono-metamorphic, Structures, Deformation, Ductile, Brittle, Basement complex
spellingShingle S. N. Yusuf
A. Y. Kuku
Y. Ibrahim
S. Kasidi
Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria
Nigerian Journal of Technological Development
Tectono-metamorphic, Structures, Deformation, Ductile, Brittle, Basement complex
title Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria
title_full Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria
title_fullStr Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria
title_full_unstemmed Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria
title_short Tectono-Metamorphic Deformation and Structures of Mubi-Hong Area, NE, Nigeria
title_sort tectono metamorphic deformation and structures of mubi hong area ne nigeria
topic Tectono-metamorphic, Structures, Deformation, Ductile, Brittle, Basement complex
url https://journal.njtd.com.ng/index.php/njtd/article/view/310
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