Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin

.Khon Kaen’s petrified wood fossil sites in northeastern Thailand, though less studied, hold significant paleontological value. These sites offer crucial insights into the region’s geology. The Quaternary gravel beds, which contain a diverse array of petrified wood, were deposited on elevated terrac...

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Main Authors: Parisa Nimnate, Rungroj Arjwech, Pradit Nulay, Sutatcha Hongsresawat
Format: Article
Language:English
Published: Taylor & Francis Group 2025-05-01
Series:Geology, Ecology, and Landscapes
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Online Access:https://www.tandfonline.com/doi/10.1080/24749508.2025.2506851
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author Parisa Nimnate
Rungroj Arjwech
Pradit Nulay
Sutatcha Hongsresawat
author_facet Parisa Nimnate
Rungroj Arjwech
Pradit Nulay
Sutatcha Hongsresawat
author_sort Parisa Nimnate
collection DOAJ
description .Khon Kaen’s petrified wood fossil sites in northeastern Thailand, though less studied, hold significant paleontological value. These sites offer crucial insights into the region’s geology. The Quaternary gravel beds, which contain a diverse array of petrified wood, were deposited on elevated terraces along the western boundary of the Khon Kaen subbasin. Field investigations focused on collecting sedimentological data to analyze the stratigraphic sequence, identify lithofacies, and characterize architectural elements in the gravel pits. The unconsolidated units (Units I–IV) unconformably overlie the Khorat Group bedrock in the Ban Non Rang area (north) and the Ban Kean Phra Doo area (south). From bottom to top, these units are as follows: I) conglomeratic sand, II) lenticular gravel with sand, III) massive gravel, and IV) red sandy soil containing minor pebble clasts. The depositional environment is interpreted as a braided stream on an alluvial fan with some debris flow occurrences, influenced by medium- to high-energy gravity/debris flows (Units I–III). Unit IV is identified as having been influenced by bioturbation processes. The majority of clasts in Units II and III consist of quartz, likely originating from the mountain ranges to the north to northwest of the subbasin.
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spelling doaj-art-846e2fd7ec4b4995b6a90e9375cd8bc62025-08-20T03:09:42ZengTaylor & Francis GroupGeology, Ecology, and Landscapes2474-95082025-05-0111610.1080/24749508.2025.2506851Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasinParisa Nimnate0Rungroj Arjwech1Pradit Nulay2Sutatcha Hongsresawat3Division of Geoscience, Mahidol University Kanchanaburi Campus, Kanchanaburi, ThailandDepartment of Geotechnology, Faculty of Technology, Khon Kaen University, Khon Kaen, ThailandDepartment of Mineral Resources, Ministry of Natural Resources and Environment, Office of Mineral Resources Region 2, Khon Kaen, ThailandDivision of Geoscience, Mahidol University Kanchanaburi Campus, Kanchanaburi, Thailand.Khon Kaen’s petrified wood fossil sites in northeastern Thailand, though less studied, hold significant paleontological value. These sites offer crucial insights into the region’s geology. The Quaternary gravel beds, which contain a diverse array of petrified wood, were deposited on elevated terraces along the western boundary of the Khon Kaen subbasin. Field investigations focused on collecting sedimentological data to analyze the stratigraphic sequence, identify lithofacies, and characterize architectural elements in the gravel pits. The unconsolidated units (Units I–IV) unconformably overlie the Khorat Group bedrock in the Ban Non Rang area (north) and the Ban Kean Phra Doo area (south). From bottom to top, these units are as follows: I) conglomeratic sand, II) lenticular gravel with sand, III) massive gravel, and IV) red sandy soil containing minor pebble clasts. The depositional environment is interpreted as a braided stream on an alluvial fan with some debris flow occurrences, influenced by medium- to high-energy gravity/debris flows (Units I–III). Unit IV is identified as having been influenced by bioturbation processes. The majority of clasts in Units II and III consist of quartz, likely originating from the mountain ranges to the north to northwest of the subbasin.https://www.tandfonline.com/doi/10.1080/24749508.2025.2506851Petrified woodlithofaciesarchitectural elementdepositional environmentKhon Kaen subbasin
spellingShingle Parisa Nimnate
Rungroj Arjwech
Pradit Nulay
Sutatcha Hongsresawat
Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin
Geology, Ecology, and Landscapes
Petrified wood
lithofacies
architectural element
depositional environment
Khon Kaen subbasin
title Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin
title_full Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin
title_fullStr Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin
title_full_unstemmed Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin
title_short Lithostratigraphy of a high terrace with petrified wood fossils in Northeastern Thailand: implication for the depositional environment and geologic setting of the Khon Kaen subbasin
title_sort lithostratigraphy of a high terrace with petrified wood fossils in northeastern thailand implication for the depositional environment and geologic setting of the khon kaen subbasin
topic Petrified wood
lithofacies
architectural element
depositional environment
Khon Kaen subbasin
url https://www.tandfonline.com/doi/10.1080/24749508.2025.2506851
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