Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Devonian conodont biostratigraphy of the Mackenzie Mountains, western part of the Northwest Territories

View through CrossRef
In this paper, a review of the current understanding of Devonian conodont biostratigraphy in the Mackenzie Mountains in the Northwest Territories is presented. The Devonian stratigraphy of the northern and southern Mackenzie Mountains is presented on two chronostratigraphic charts, from the first deposits on top of the sub-Devonian unconformity to the lower part of the Imperial and Fort Simpson formations. Schematic maps give an overview of the regional distribution of the formations in the Mackenzie Mountains. This update revealed that several of the assemblage and formation contacts are younger than presumed in an earlier time-stratigraphic chart; several formations and members are now better constrained in the updated charts. The update also pointed out intervals in the charts for which no data were available and for which more research is needed to constrain formations in the Devonian conodont biozonation.
Natural Resources Canada/CMSS/Information Management
Title: Devonian conodont biostratigraphy of the Mackenzie Mountains, western part of the Northwest Territories
Description:
In this paper, a review of the current understanding of Devonian conodont biostratigraphy in the Mackenzie Mountains in the Northwest Territories is presented.
The Devonian stratigraphy of the northern and southern Mackenzie Mountains is presented on two chronostratigraphic charts, from the first deposits on top of the sub-Devonian unconformity to the lower part of the Imperial and Fort Simpson formations.
Schematic maps give an overview of the regional distribution of the formations in the Mackenzie Mountains.
This update revealed that several of the assemblage and formation contacts are younger than presumed in an earlier time-stratigraphic chart; several formations and members are now better constrained in the updated charts.
The update also pointed out intervals in the charts for which no data were available and for which more research is needed to constrain formations in the Devonian conodont biozonation.

Related Results

Region czy regiony? Ziemie Zachodnie i Północne 1945−1989
Region czy regiony? Ziemie Zachodnie i Północne 1945−1989
This book is not a publication with a thesis and – as it turned out during its preparation – it does not give a final answer to the titular question. Rather, it is an attempt to de...
Norian conodont biostratigraphy and carbon isotopic perturbations in the Lanping-Simao terrane, Eastern Tethy
Norian conodont biostratigraphy and carbon isotopic perturbations in the Lanping-Simao terrane, Eastern Tethy
Norian time interval is a crucial period in Earth’s evolutionary history, characterized by several organic carbon-isotope perturbations in the carbon cycle that are close...
Recent progress in Cambrian and Ordovician conodont biostratigraphy of China
Recent progress in Cambrian and Ordovician conodont biostratigraphy of China
Study of the Cambrian and Ordovician conodont biostratigraphy of China is mainly confined to the eastern parts of China, where the conodont faunas are very rich and varied. There a...
Zero to hero
Zero to hero
Western images of Japan tell a seemingly incongruous story of love, sex and marriage – one full of contradictions and conflicting moral codes. We sometimes hear intriguing stories ...
Devonian
Devonian
During Early and Middle Devonian time, carbonate successions were deposited on the Mackenzie Platform in the east, on the Yukon Stable Block in the west, and on two small isolated ...
Biostratigraphy and trilobite fauna of the lower silurian Tegart formation, southeastern British Columbia
Biostratigraphy and trilobite fauna of the lower silurian Tegart formation, southeastern British Columbia
In the Western Ranges of the Rocky Mountains, the Tegart Formation is preserved locally beneath the sub-Devonian unconformity, with a maximum thickness of 66 m. Argillaceous limest...
Thermophysical Properties Of Devonian Shales
Thermophysical Properties Of Devonian Shales
Abstract A detailed study of the thermophysical properties of Devonian shales from the central and eastern United States has been carried out. The properties enco...
Upper Ordovician (Sandbian–Katian) graptolite and conodont zonation in the Yangtze region, China
Upper Ordovician (Sandbian–Katian) graptolite and conodont zonation in the Yangtze region, China
ABSTRACTThe graptolite and conodont biostratigraphy of the latest Darriwilian, Sandbian and early and middle Katian succession on the Yangtze Platform is reassessed based on numero...

Back to Top