Devonian lacustrine shore zone architecture

giving perspective to cliff exposures with ground penetrating radar

Steven David Andrews, Julien Moreau, Stuart Archer

Research output: Contribution to conferenceAbstract

Abstract

Lake margin sedimentary systems have been the subject of only limited study. The orbitally controlled cyclic lacustrine successions of the Middle Old Red Sandstone of Northern Scotland contains repeated developments of shore zone sandstones and thus provides an ideal location for the study of these units. The cycles are on average 16 m thick and comprise deep lake, perennial lake and playa facies. The shore zone facies reaches 2 to 3.5 m in thickness and is found within the playa facies. Detailed field observations are presented alongside ground penetrating radar data which has aided the three dimensional characterisation of these sand bodies.
Loading and discrete channel forms are recognised in thin-bedded sandstones within the lower portion of the lake shore zone successions. Radar profiles provide evidence for an extensively developed sharp base to these units with some erosional features also recognised. Up-section the sandstone beds appear to become amalgamated forming subtle low angle accretionary bar complexes. These features are imaged well on the radar profiles where successive erosion/accretion can be recognised and their three dimensional form and distribution mapped. The orientation of these features is consistent with extensive palaeocurrent measurements from oscillation ripples. Further loaded sandstone beds and sand-filled shallow channel features overlie the bar forms. The channels are well imaged in the radar scans where their wider context can be gained.
The shore zone sandstones overlie playa facies which contains abundant desiccation horizons, reflecting the most arid phase in the climatically controlled lacustrine cycle. As climatic conditions ameliorated the rejuvenation of fluvial systems resulted in the transport of sand out into the basin. Initial deposition was limited to intermittent events where sediment was laid down on a water saturated substrate. Some of these may have occurr¬¬¬ed subaqueously as small scale turbidity flows. High resolution fluctuations in lake level resulted in periodic short lived reworking events along the lake margin which produced amalgamated sands which formed low relief bars. Shore zone reworking is likely to have occurred over a wide area as the lake margin migrated back and forth, and gradually transgressed. Continued transgression forced fluvial systems back towards the basin margin.
Original languageEnglish
Publication statusPublished - 2014
EventInternational Sedimentological Congress - Switzeland, Geneva, United Kingdom
Duration: 18 Aug 201422 Aug 2014

Conference

ConferenceInternational Sedimentological Congress
CountryUnited Kingdom
CityGeneva
Period18/08/1422/08/14

Fingerprint

ground penetrating radar
cliff
sandstone
playa
lake
sand
radar
reworking
shore (nonmarine)
Old Red Sandstone
ripple
lake level
desiccation
basin
transgression
turbidity
relief
oscillation
accretion
exposure

Cite this

Andrews, S. D., Moreau, J., & Archer, S. (2014). Devonian lacustrine shore zone architecture: giving perspective to cliff exposures with ground penetrating radar. Abstract from International Sedimentological Congress, Geneva, United Kingdom.

Devonian lacustrine shore zone architecture : giving perspective to cliff exposures with ground penetrating radar. / Andrews, Steven David; Moreau, Julien; Archer, Stuart.

2014. Abstract from International Sedimentological Congress, Geneva, United Kingdom.

Research output: Contribution to conferenceAbstract

Andrews, SD, Moreau, J & Archer, S 2014, 'Devonian lacustrine shore zone architecture: giving perspective to cliff exposures with ground penetrating radar' International Sedimentological Congress, Geneva, United Kingdom, 18/08/14 - 22/08/14, .
Andrews SD, Moreau J, Archer S. Devonian lacustrine shore zone architecture: giving perspective to cliff exposures with ground penetrating radar. 2014. Abstract from International Sedimentological Congress, Geneva, United Kingdom.
Andrews, Steven David ; Moreau, Julien ; Archer, Stuart. / Devonian lacustrine shore zone architecture : giving perspective to cliff exposures with ground penetrating radar. Abstract from International Sedimentological Congress, Geneva, United Kingdom.
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abstract = "Lake margin sedimentary systems have been the subject of only limited study. The orbitally controlled cyclic lacustrine successions of the Middle Old Red Sandstone of Northern Scotland contains repeated developments of shore zone sandstones and thus provides an ideal location for the study of these units. The cycles are on average 16 m thick and comprise deep lake, perennial lake and playa facies. The shore zone facies reaches 2 to 3.5 m in thickness and is found within the playa facies. Detailed field observations are presented alongside ground penetrating radar data which has aided the three dimensional characterisation of these sand bodies.Loading and discrete channel forms are recognised in thin-bedded sandstones within the lower portion of the lake shore zone successions. Radar profiles provide evidence for an extensively developed sharp base to these units with some erosional features also recognised. Up-section the sandstone beds appear to become amalgamated forming subtle low angle accretionary bar complexes. These features are imaged well on the radar profiles where successive erosion/accretion can be recognised and their three dimensional form and distribution mapped. The orientation of these features is consistent with extensive palaeocurrent measurements from oscillation ripples. Further loaded sandstone beds and sand-filled shallow channel features overlie the bar forms. The channels are well imaged in the radar scans where their wider context can be gained.The shore zone sandstones overlie playa facies which contains abundant desiccation horizons, reflecting the most arid phase in the climatically controlled lacustrine cycle. As climatic conditions ameliorated the rejuvenation of fluvial systems resulted in the transport of sand out into the basin. Initial deposition was limited to intermittent events where sediment was laid down on a water saturated substrate. Some of these may have occurr¬¬¬ed subaqueously as small scale turbidity flows. High resolution fluctuations in lake level resulted in periodic short lived reworking events along the lake margin which produced amalgamated sands which formed low relief bars. Shore zone reworking is likely to have occurred over a wide area as the lake margin migrated back and forth, and gradually transgressed. Continued transgression forced fluvial systems back towards the basin margin.",
author = "Andrews, {Steven David} and Julien Moreau and Stuart Archer",
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T2 - giving perspective to cliff exposures with ground penetrating radar

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N2 - Lake margin sedimentary systems have been the subject of only limited study. The orbitally controlled cyclic lacustrine successions of the Middle Old Red Sandstone of Northern Scotland contains repeated developments of shore zone sandstones and thus provides an ideal location for the study of these units. The cycles are on average 16 m thick and comprise deep lake, perennial lake and playa facies. The shore zone facies reaches 2 to 3.5 m in thickness and is found within the playa facies. Detailed field observations are presented alongside ground penetrating radar data which has aided the three dimensional characterisation of these sand bodies.Loading and discrete channel forms are recognised in thin-bedded sandstones within the lower portion of the lake shore zone successions. Radar profiles provide evidence for an extensively developed sharp base to these units with some erosional features also recognised. Up-section the sandstone beds appear to become amalgamated forming subtle low angle accretionary bar complexes. These features are imaged well on the radar profiles where successive erosion/accretion can be recognised and their three dimensional form and distribution mapped. The orientation of these features is consistent with extensive palaeocurrent measurements from oscillation ripples. Further loaded sandstone beds and sand-filled shallow channel features overlie the bar forms. The channels are well imaged in the radar scans where their wider context can be gained.The shore zone sandstones overlie playa facies which contains abundant desiccation horizons, reflecting the most arid phase in the climatically controlled lacustrine cycle. As climatic conditions ameliorated the rejuvenation of fluvial systems resulted in the transport of sand out into the basin. Initial deposition was limited to intermittent events where sediment was laid down on a water saturated substrate. Some of these may have occurr¬¬¬ed subaqueously as small scale turbidity flows. High resolution fluctuations in lake level resulted in periodic short lived reworking events along the lake margin which produced amalgamated sands which formed low relief bars. Shore zone reworking is likely to have occurred over a wide area as the lake margin migrated back and forth, and gradually transgressed. Continued transgression forced fluvial systems back towards the basin margin.

AB - Lake margin sedimentary systems have been the subject of only limited study. The orbitally controlled cyclic lacustrine successions of the Middle Old Red Sandstone of Northern Scotland contains repeated developments of shore zone sandstones and thus provides an ideal location for the study of these units. The cycles are on average 16 m thick and comprise deep lake, perennial lake and playa facies. The shore zone facies reaches 2 to 3.5 m in thickness and is found within the playa facies. Detailed field observations are presented alongside ground penetrating radar data which has aided the three dimensional characterisation of these sand bodies.Loading and discrete channel forms are recognised in thin-bedded sandstones within the lower portion of the lake shore zone successions. Radar profiles provide evidence for an extensively developed sharp base to these units with some erosional features also recognised. Up-section the sandstone beds appear to become amalgamated forming subtle low angle accretionary bar complexes. These features are imaged well on the radar profiles where successive erosion/accretion can be recognised and their three dimensional form and distribution mapped. The orientation of these features is consistent with extensive palaeocurrent measurements from oscillation ripples. Further loaded sandstone beds and sand-filled shallow channel features overlie the bar forms. The channels are well imaged in the radar scans where their wider context can be gained.The shore zone sandstones overlie playa facies which contains abundant desiccation horizons, reflecting the most arid phase in the climatically controlled lacustrine cycle. As climatic conditions ameliorated the rejuvenation of fluvial systems resulted in the transport of sand out into the basin. Initial deposition was limited to intermittent events where sediment was laid down on a water saturated substrate. Some of these may have occurr¬¬¬ed subaqueously as small scale turbidity flows. High resolution fluctuations in lake level resulted in periodic short lived reworking events along the lake margin which produced amalgamated sands which formed low relief bars. Shore zone reworking is likely to have occurred over a wide area as the lake margin migrated back and forth, and gradually transgressed. Continued transgression forced fluvial systems back towards the basin margin.

M3 - Abstract

ER -