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Lithostratigraphy and Petrography of Mesozoic Sedimentary Rocks of Lemi Area, North Shewa, Central Ethiopia

Received: 4 May 2024     Accepted: 20 May 2024     Published: 4 July 2024
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Abstract

The Mesozoic sedimentary basins in Ethiopia, particularly the Central Ethiopia, and Blue Nile Basin within the central main Ethiopian rift region are characterized by a diverse range of volcano-sedimentary rocks dominated by sedimentary sequences. The lithostratigraphy and petrology of Mesozoic sedimentary rocks of Lemi area, North Shewa, in Central Ethiopia within the Blue Nile basin, is described based on detailed field observations, lithostratigraphic analysis, petrographic examinations. The lithological units identified during fieldwork include Mudstone, Sandstone, and Basaltic rock formations. The sandstone unit in the study covers an estimated average thickness is 237 meters with intercalations of thinly bedded mudstone. The average thickness of each sandstone units (coarse (23 meters), medium (90 meters) and fine-grained (115 meters) sandstone unit) are varying from place to place within the study area. The stratigraphic section logs in four each block (Geza Washa, Dalota, Ruka, and Gosh Wiha) shows coarsening upward indicating the depositional environment transition from deep marine to the fluvial environment. The results of the study reveal the geological history and paleoenvironmental conditions of the Mesozoic sedimentary rocks in the Lemi area. This study contributes to our understanding of the geological processes that have influenced the formation of the Lemi area and provides valuable interpretations of regional geology.

Published in Earth Sciences (Volume 13, Issue 4)
DOI 10.11648/j.earth.20241304.11
Page(s) 116-126
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Lemi, Lithostratigraphy, Mesozoic, Petrography, Sedimentary Rocks

References
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[2] Alemu, T. (2021). Tectonic Evolution of the Pan-African Belt in Western Ethiopia, Southern Arabian-Nubian Shield. In: Hamimi, Z., Fowler, AR., Liégeois, JP., Collins, A., Abdelsalam, M. G., Abd EI-Wahed, M. (eds) The Geology of the Arabian-Nubian Shield. Regional Geology Reviews. Springer, Cham.
[3] Amene, S., & Tamrat, M. (1999). The Geology of Mugher Cement Factory Area, Abay Basin, North Shewa, GSE, Addis Ababa, Ethiopia.
[4] Assefa, G. (1981). Gohatsion Formation: A new Lias-Malm lithostratigraphic unit from the Abay River basin, Ethiopia. Geoscience Journal, 2(1), 63-88.
[5] Assefa, G. (1991). Lithostratigraphy and environment of deposition of the Late Jurassic - Early Cretaceous sequence of the central part of Northwestern Plateau, Ethiopia. Neues Jahrbuch Für Geologie Und Paläontologie - Abhandlungen, 182(3), 255–284.
[6] Berhe, S. M., Desta, B., Nicoletti, M., & Teferra, M. (1987). Geology, geochronology, and geodynamic implications of the Cenozoic magmatic province in W and SE Ethiopia. Journal - Geological Society (London), 144(2), 213–226.
[7] Beyth, M. (1972). Paleozoic-Mesozoic Sedimentary Basin of Mekele Outlier, Northern Ethiopia. AAPG Bulletin, 56(12), 2426-2439.
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[11] Gani, N., Abdelsalam., G., Gera, M., & Gani, R. (2008). Stratigraphic and Structural Evolution of the Blue Nile Basin, Northwestern Ethiopian Plateau. Geological Journal, 44(1), 30–56.
[12] Getaneh, W. (2002). Geochemistry Provenance and Depositional Tectonic Setting of the Adigrat Sandstone Northern Ethiopia. Journal of African Earth Sciences, 35(2), 185-198.
[13] Getaneh, W., & Atnafu, B. (2020). Journal of African Earth Sciences Geochemistry and lithostratigraphy of the mugher mudstone : Insights into the late Jurassic-early cretaceous clastic sedimentation in Ethiopia and its surroundings. Journal of African Earth Sciences, 164(August 2019), 103770.
[14] Kazmin, V., Shifferaw, A., & Balcha, T. (1978). The Ethiopian basement: Stratigraphy and possible manner of evolution. Geologische Rund., 67(2), 531–546.
[15] Mohammedyasin, M. S., & Wudie, G. (2018). The provenance of the cretaceous Debre Libanos Sandstone in the Blue Nile Basin, Ethiopia: Evidence from petrography and geochemistry. Sedimentary Geology.
[16] Russo, A., Getaneh, A & Balemwal, A. (1994). Sedimentary Evolution of the Abay River (Blue Nile) Basin, Ethiopia. Journal of Geology. 16: 91-107.
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    Wuletaw, A., Mihret, B. (2024). Lithostratigraphy and Petrography of Mesozoic Sedimentary Rocks of Lemi Area, North Shewa, Central Ethiopia. Earth Sciences, 13(4), 116-126. https://doi.org/10.11648/j.earth.20241304.11

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    ACS Style

    Wuletaw, A.; Mihret, B. Lithostratigraphy and Petrography of Mesozoic Sedimentary Rocks of Lemi Area, North Shewa, Central Ethiopia. Earth Sci. 2024, 13(4), 116-126. doi: 10.11648/j.earth.20241304.11

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    AMA Style

    Wuletaw A, Mihret B. Lithostratigraphy and Petrography of Mesozoic Sedimentary Rocks of Lemi Area, North Shewa, Central Ethiopia. Earth Sci. 2024;13(4):116-126. doi: 10.11648/j.earth.20241304.11

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  • @article{10.11648/j.earth.20241304.11,
      author = {Ajebush Wuletaw and Bishaw Mihret},
      title = {Lithostratigraphy and Petrography of Mesozoic Sedimentary Rocks of Lemi Area, North Shewa, Central Ethiopia
    },
      journal = {Earth Sciences},
      volume = {13},
      number = {4},
      pages = {116-126},
      doi = {10.11648/j.earth.20241304.11},
      url = {https://doi.org/10.11648/j.earth.20241304.11},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20241304.11},
      abstract = {The Mesozoic sedimentary basins in Ethiopia, particularly the Central Ethiopia, and Blue Nile Basin within the central main Ethiopian rift region are characterized by a diverse range of volcano-sedimentary rocks dominated by sedimentary sequences. The lithostratigraphy and petrology of Mesozoic sedimentary rocks of Lemi area, North Shewa, in Central Ethiopia within the Blue Nile basin, is described based on detailed field observations, lithostratigraphic analysis, petrographic examinations. The lithological units identified during fieldwork include Mudstone, Sandstone, and Basaltic rock formations. The sandstone unit in the study covers an estimated average thickness is 237 meters with intercalations of thinly bedded mudstone. The average thickness of each sandstone units (coarse (23 meters), medium (90 meters) and fine-grained (115 meters) sandstone unit) are varying from place to place within the study area. The stratigraphic section logs in four each block (Geza Washa, Dalota, Ruka, and Gosh Wiha) shows coarsening upward indicating the depositional environment transition from deep marine to the fluvial environment. The results of the study reveal the geological history and paleoenvironmental conditions of the Mesozoic sedimentary rocks in the Lemi area. This study contributes to our understanding of the geological processes that have influenced the formation of the Lemi area and provides valuable interpretations of regional geology.
    },
     year = {2024}
    }
    

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  • TY  - JOUR
    T1  - Lithostratigraphy and Petrography of Mesozoic Sedimentary Rocks of Lemi Area, North Shewa, Central Ethiopia
    
    AU  - Ajebush Wuletaw
    AU  - Bishaw Mihret
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    DO  - 10.11648/j.earth.20241304.11
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 116
    EP  - 126
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.20241304.11
    AB  - The Mesozoic sedimentary basins in Ethiopia, particularly the Central Ethiopia, and Blue Nile Basin within the central main Ethiopian rift region are characterized by a diverse range of volcano-sedimentary rocks dominated by sedimentary sequences. The lithostratigraphy and petrology of Mesozoic sedimentary rocks of Lemi area, North Shewa, in Central Ethiopia within the Blue Nile basin, is described based on detailed field observations, lithostratigraphic analysis, petrographic examinations. The lithological units identified during fieldwork include Mudstone, Sandstone, and Basaltic rock formations. The sandstone unit in the study covers an estimated average thickness is 237 meters with intercalations of thinly bedded mudstone. The average thickness of each sandstone units (coarse (23 meters), medium (90 meters) and fine-grained (115 meters) sandstone unit) are varying from place to place within the study area. The stratigraphic section logs in four each block (Geza Washa, Dalota, Ruka, and Gosh Wiha) shows coarsening upward indicating the depositional environment transition from deep marine to the fluvial environment. The results of the study reveal the geological history and paleoenvironmental conditions of the Mesozoic sedimentary rocks in the Lemi area. This study contributes to our understanding of the geological processes that have influenced the formation of the Lemi area and provides valuable interpretations of regional geology.
    
    VL  - 13
    IS  - 4
    ER  - 

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