| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Relative sea-level changes and the development of a Cambrian transgression |
|---|
| Journal | Geological Magazine |
|---|
| Authors | McKie, T. | Author |
|---|
| Year | 1993 (March) | Volume | 130 |
|---|
| Issue | 2 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800009894Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 255703 | Long-form Identifier | mindat:1:5:255703:2 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | McKie, T. (1993) Relative sea-level changes and the development of a Cambrian transgression. Geological Magazine, 130 (2) 245-256 doi:10.1017/s0016756800009894 |
|---|
| Plain Text | McKie, T. (1993) Relative sea-level changes and the development of a Cambrian transgression. Geological Magazine, 130 (2) 245-256 doi:10.1017/s0016756800009894 |
|---|
| In | (1993, March) Geological Magazine Vol. 130 (2) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | AbstractThe Lower Cambrian in northwest Scotland is one example of a Lower Palaeozoic ‘orthoquartzite-carbonate’ succession deposited on a slowly subsiding, peneplained Precambrian basement during a period of relative sea-level rise. This particular setting led to the development of a very wide, low gradient shelf which was extremely sensitive to minor sea-level changes. The basal quartz arenite section (Lower Member-Pipe Rock) is a transgressive, tide-dominated systems tract, but lacks a systematic parasequence architecture because of three factors: a fluvial sediment flux was insufficient to induce shoreline progradation, accommodation space was limited during sea-level falls (which are commonly expressed by widespread erosional surfaces), and sediment yield to the shelf by transgressive reworking was a major contributor towards the preserved stratigraphy. The storm-dominated Fucoid Beds represent a condensed section and also show the effects of rapid and widespread facies belt oscillations because of the low shelf gradient. An overlying highstand systems tract is also lacking, partly due to the absence of a large fluvial sediment yield and also due to lowstand and transgressive reworking. An erosively based tidal sandsheet at the top of the Fucoid Beds, interpreted to be a lowstand systems tract, therefore rests directly on the condensed section of the underlying sequence. This was in turn reworked into linear tidal sandbanks (Salterella Grit) during slow sea-level rise, prior to the next major transgression. The limited accommodation space therefore introduced a preservational bias towards deepening-upward trends on a parasequence and sequence scale. The oscillations in facies belts, episodic subareal exposure and the potential to remove substantial portions of systems tracts suggests that Lower Palaeozoic ‘orthoquartzite’ successions may exhibit regular and abrupt vertical shifts in depositional environment which, given their subtle lithological character, may require detailed analysis to identify. Such successions may also display incomplete development of several components of transgressive-regressive sequence architecture. |
|---|
These are possibly similar items as determined by title/reference text matching only.
