| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Petrology of an Irregular-Nodule Bed, Lower Carboniferous, Anglesey, North Wales |
|---|
| Journal | Geological Magazine |
|---|
| Authors | Nichols, R. A. H. | Author |
|---|
| Year | 1966 (December) | Volume | 103 |
|---|
| Issue | 6 |
|---|
| Publisher | Cambridge University Press (CUP) |
|---|
| DOI | doi:10.1017/s0016756800054182Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 249697 | Long-form Identifier | mindat:1:5:249697:3 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Nichols, R. A. H. (1966) Petrology of an Irregular-Nodule Bed, Lower Carboniferous, Anglesey, North Wales. Geological Magazine, 103 (6) 477-486 doi:10.1017/s0016756800054182 |
|---|
| Plain Text | Nichols, R. A. H. (1966) Petrology of an Irregular-Nodule Bed, Lower Carboniferous, Anglesey, North Wales. Geological Magazine, 103 (6) 477-486 doi:10.1017/s0016756800054182 |
|---|
| In | (1966, December) Geological Magazine Vol. 103 (6) Cambridge University Press (CUP) |
|---|
| Abstract/Notes | AbstractSome of the nodules described are similar to trace-fossils described by Donaldson and Simpson and some ichnofossils described by Seilacher, but many appear to be structures produced by sedimentary boudinage. These do not seem to be a result of organic or concretionary action. It is suggested that currents deposited thin bioclastic calcarenites with interbeds of calcite silt, and that crinoids and coral patches developed only sporadically during deposition. A few scavengers reworked the bioclastic calcarenites and calcite silt layers thus forming the trace-fossils; many of the irregular-nodules, however, were probably formed by differential compaction and segregation in the calcite silt beds, and may represent sedimentary boudins, which are relicts of former layers. |
|---|
These are possibly similar items as determined by title/reference text matching only.
