Illtyd Formation
| Illtyd Formation | |
|---|---|
| Stratigraphic range: Cambrian | |
| Type | Formation |
| Underlies | Slats Creek Fm |
| Location | |
| Region | Yukon |
| Country | Canada |
The Illtyd Formation is an up to 1000-m thick geologic formation in Yukon. It preserves fossils dating back to the Dyerian subdivision of the Cambrian period, which spans the Stage 3 / Stage 4 boundary; it's considered to belong to the mid-upper Bonnia-Olenellus trilobite Zone. Top of the unit corresponds, more or less, to the top of Stage 4.[1][2] These fossils include Lower Cambrian trilobites'.[3]
The type section is in the Wernecke Mtns; it corps out also in and to the S/SW of the Rochardson Moutnars. It possibly corresponds to the Sekwi Fm in the Macxkenzie mtns.[1]
Lowermost of the Palaeozoic strata west of the Richardson Mountains, angular unconformity at base, overlying various Precambrian strata. Silty limestones and massive dolomites. In places rhythmically bedded. Colour: Tan, brownish grey muds; sandier layers orange. Upper layers include oolites and oncolites. Trace fossils include burrows and 'worm trails'. In some places unit is massively faulted and altered / weathered, approaching marble grade metamorphism near faults.[1]
See also[edit]
References[edit]
- ^ a b c Morrow, D. W. (1999). Lower Paleozoic stratigraphy of northern Yukon Territory and northwestern District of Mackenzie. Bulletin 538. Geological Survey of Canada. ISBN 0-660-17808-7.
- ^ Foster, John R. (2011). "sp.(Trilobita; Corynexochida) from the Chambless Limestone (Lower Cambrian) of the Marble Mountains, California: First Dorypygidae in a cratonic region of the southern Cordillera". PaleoBios. 30 (2).
- ^ Fritz, W. H. (1991). Lower Cambrian trilobites from the Illtyd Formation, Wernecke Mountains, Yukon Territory. Bulletin. Geological Survey of Canada. ISBN 0-660-13836-0. ISSN 0068-7626.
External links[edit]
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