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Stratigraphic Order in the Sung Village-Len Bac Mountain Section, Yen Hoa Commune, Minh Hoa District, Quang Binh Province, North-Central Vietnam

Received: 5 August 2022    Accepted: 13 September 2022    Published: 28 September 2022
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Abstract

The Sung-Len Bac Mountain Section is one of the best section to study stratigraphy and paleontology of the Middle-Upper Devonian, Lower Carboniferous to Middle Permian sediments in North-central Vietnam, including formations in the ascending order: The Dong Tho Formation (D2-3 dt) is composed of silstone and quartz sandstone, 250m thick containing fish Bothiolepis sp, brachiopod? Holynetes caurongensis, tentaculite Homoctenus sp, plant Lepidodendropsis sp. of the Late Givetian-Early Frasnian. The Xom Nha Formation is composed of stylolitic limestone, 20m thick containing conodonts of the Palmatolepis glabra Zone of the Famennian age. The La Khe Formation is composed of silstone, shale, sandstone, cherty limestone bearing abundant crinoids, brachiopods, ammonoids, trilobites, plants of the Viséan age. The Muong Long Formation is composed of thick-bedded limestone over 1000m thick, containig foraminifers Millerella, Eostafella, Quydatella, Fusulinella, Obsoletes, Triticites, Schwagerina, Robustoschwagerina, Misellina, Neoschwagerina; and brachiopod Phricodothyris asiatica of the Carboniferous-Middle Permian age. An abundant fossil assemblage of plants Archaeocalamites sp., Sigillaria sp., Lepidodendron sp. associated with brachiopods Plicatifera sp., Chonetes sp., Lingula sp.; bivalve Mytilarca sp.; ammonoids Sulcogirtyoceras cf. limatum, Neoglyphioceras sp.; trilobites Linguaphillipsia cf. subconical, Phillipsia propiqua of nearshore facies has been found in the upper part of the La Khe Formation by the Hanoi Fossil Museum in 2022.

Published in Earth Sciences (Volume 11, Issue 5)
DOI 10.11648/j.earth.20221105.14
Page(s) 269-276
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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

Stratigraphy, Paleontology, Dong Tho, Xom Nha, La Khe, Muong Long Formations, North-Central Vietnam

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  • APA Style

    Nguyen Huu Hung, Nguyen Ba Hung. (2022). Stratigraphic Order in the Sung Village-Len Bac Mountain Section, Yen Hoa Commune, Minh Hoa District, Quang Binh Province, North-Central Vietnam. Earth Sciences, 11(5), 269-276. https://doi.org/10.11648/j.earth.20221105.14

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    ACS Style

    Nguyen Huu Hung; Nguyen Ba Hung. Stratigraphic Order in the Sung Village-Len Bac Mountain Section, Yen Hoa Commune, Minh Hoa District, Quang Binh Province, North-Central Vietnam. Earth Sci. 2022, 11(5), 269-276. doi: 10.11648/j.earth.20221105.14

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    AMA Style

    Nguyen Huu Hung, Nguyen Ba Hung. Stratigraphic Order in the Sung Village-Len Bac Mountain Section, Yen Hoa Commune, Minh Hoa District, Quang Binh Province, North-Central Vietnam. Earth Sci. 2022;11(5):269-276. doi: 10.11648/j.earth.20221105.14

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  • @article{10.11648/j.earth.20221105.14,
      author = {Nguyen Huu Hung and Nguyen Ba Hung},
      title = {Stratigraphic Order in the Sung Village-Len Bac Mountain Section, Yen Hoa Commune, Minh Hoa District, Quang Binh Province, North-Central Vietnam},
      journal = {Earth Sciences},
      volume = {11},
      number = {5},
      pages = {269-276},
      doi = {10.11648/j.earth.20221105.14},
      url = {https://doi.org/10.11648/j.earth.20221105.14},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20221105.14},
      abstract = {The Sung-Len Bac Mountain Section is one of the best section to study stratigraphy and paleontology of the Middle-Upper Devonian, Lower Carboniferous to Middle Permian sediments in North-central Vietnam, including formations in the ascending order: The Dong Tho Formation (D2-3 dt) is composed of silstone and quartz sandstone, 250m thick containing fish Bothiolepis sp, brachiopod? Holynetes caurongensis, tentaculite Homoctenus sp, plant Lepidodendropsis sp. of the Late Givetian-Early Frasnian. The Xom Nha Formation is composed of stylolitic limestone, 20m thick containing conodonts of the Palmatolepis glabra Zone of the Famennian age. The La Khe Formation is composed of silstone, shale, sandstone, cherty limestone bearing abundant crinoids, brachiopods, ammonoids, trilobites, plants of the Viséan age. The Muong Long Formation is composed of thick-bedded limestone over 1000m thick, containig foraminifers Millerella, Eostafella, Quydatella, Fusulinella, Obsoletes, Triticites, Schwagerina, Robustoschwagerina, Misellina, Neoschwagerina; and brachiopod Phricodothyris asiatica of the Carboniferous-Middle Permian age. An abundant fossil assemblage of plants Archaeocalamites sp., Sigillaria sp., Lepidodendron sp. associated with brachiopods Plicatifera sp., Chonetes sp., Lingula sp.; bivalve Mytilarca sp.; ammonoids Sulcogirtyoceras cf. limatum, Neoglyphioceras sp.; trilobites Linguaphillipsia cf. subconical, Phillipsia propiqua of nearshore facies has been found in the upper part of the La Khe Formation by the Hanoi Fossil Museum in 2022.},
     year = {2022}
    }
    

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    T1  - Stratigraphic Order in the Sung Village-Len Bac Mountain Section, Yen Hoa Commune, Minh Hoa District, Quang Binh Province, North-Central Vietnam
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    AB  - The Sung-Len Bac Mountain Section is one of the best section to study stratigraphy and paleontology of the Middle-Upper Devonian, Lower Carboniferous to Middle Permian sediments in North-central Vietnam, including formations in the ascending order: The Dong Tho Formation (D2-3 dt) is composed of silstone and quartz sandstone, 250m thick containing fish Bothiolepis sp, brachiopod? Holynetes caurongensis, tentaculite Homoctenus sp, plant Lepidodendropsis sp. of the Late Givetian-Early Frasnian. The Xom Nha Formation is composed of stylolitic limestone, 20m thick containing conodonts of the Palmatolepis glabra Zone of the Famennian age. The La Khe Formation is composed of silstone, shale, sandstone, cherty limestone bearing abundant crinoids, brachiopods, ammonoids, trilobites, plants of the Viséan age. The Muong Long Formation is composed of thick-bedded limestone over 1000m thick, containig foraminifers Millerella, Eostafella, Quydatella, Fusulinella, Obsoletes, Triticites, Schwagerina, Robustoschwagerina, Misellina, Neoschwagerina; and brachiopod Phricodothyris asiatica of the Carboniferous-Middle Permian age. An abundant fossil assemblage of plants Archaeocalamites sp., Sigillaria sp., Lepidodendron sp. associated with brachiopods Plicatifera sp., Chonetes sp., Lingula sp.; bivalve Mytilarca sp.; ammonoids Sulcogirtyoceras cf. limatum, Neoglyphioceras sp.; trilobites Linguaphillipsia cf. subconical, Phillipsia propiqua of nearshore facies has been found in the upper part of the La Khe Formation by the Hanoi Fossil Museum in 2022.
    VL  - 11
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Author Information
  • Paleontological Department, Hanoi Fossil Museum (HFM), Hanoi City, Vietnam

  • Geological Department, Vietnam National Museum of Nature, Hanoi City, Vietnam

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