Provenance and tectonic evolution of Lower Paleozoic–Upper Mesozoic strata from Sibumasu terrane, Myanmar

Lower Paleozoic stratigraphic and biostratigraphic correlations in the Canadian Cordillera: implications for the tectonic evolution of the Laurentian margin

Canadian Journal of Earth Sciences ◽

10.1139/e03-049 ◽

2003 ◽

Vol 40 (12) ◽

pp. 1739-1753 ◽

Cited By ~ 16

Author(s):

Leanne J Pyle ◽

Christopher R Barnes

Keyword(s):

Tectonic Evolution ◽

Passive Margin ◽

Lower Paleozoic ◽

Early Devonian ◽

Southern Rocky Mountains ◽

Peace River ◽

Regional Correlation ◽

Laurentian Margin ◽

Peace River Arch ◽

Early Late

The ancient Laurentian margin rifted in the latest Neoproterozoic to early Cambrian but appears not to have developed as a simple passive margin through a long, post-rift, drift phase. Stratigraphic and conodont biostratigraphic information from four platform-to-basin transects across the margin has advanced our knowledge of the early Paleozoic evolution of the margin. In northeastern British Columbia, two northern transects span the Macdonald Platform to Kechika Trough and Ospika Embayment, and a third transect spans the parautochthonous Cassiar Terrane. In the southern Rocky Mountains, new conodont biostratigraphic data for the Ordovician succession of the Bow Platform is correlated to coeval basinal facies of the White River Trough. In total, from 26 stratigraphic sections, over 25 km of strata were measured and > 1200 conodont samples were collected that yielded over 100 000 conodont elements. Key zonal species were used for regional correlation of uppermost Cambrian to Middle Devonian strata along the Cordillera. The biostratigraphy temporally constrains at least two periods of renewed extension along the margin, in the latest Cambrian and late Early Ordovician. Alkalic volcanics associated with abrupt facies changes across the ancient shelf break, intervals of slope debris breccia deposits, and distal turbidite flows suggest the margin was characterized by intervals of volcanism, basin foundering, and platform flooding. Siliciclastics in the succession were sourced by a reactivation of tectonic highs, such as the Peace River Arch. Prominent hiatuses punctuate the succession, including unconformities of early Late Ordovician, sub-Llandovery, possibly Early to Middle Silurian and Early Devonian ages.

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Les contraintes phanérozoïques dans la plate-forme du Saint-Laurent, région de Montréal, Québec

Canadian Journal of Earth Sciences ◽

10.1139/e92-043 ◽

1992 ◽

Vol 29 (3) ◽

pp. 499-505 ◽

Cited By ~ 3

Author(s):

Jean-Pierre Gélard ◽

Michel Jébrak ◽

Gilbert Prichonnet

Keyword(s):

North America ◽

Tectonic Evolution ◽

Lower Paleozoic ◽

Its Analysis ◽

History Of

The tectonic evolution of the Appalachian platform is still not well understood. The Montréal area, however, shows evidence of major fracturing events, some of which cut the Cretaceous intrusions. The history of the different stress events recorded in the platform was studied by the analysis of brittle faults and dykes, followed by the calculation, by way inversion of tensors, of the corresponding stresses. The tectonics represented is polyphased and its analysis allows a historical reconstitution of the carbonate and flyschoid platform since the Lower Paleozoic. Five tectonic stages are recognized, corresponding to the major geodynamic events characteristics of northeast North America: (i) early north–south distensional events; (ii) Appalachian compression in a west-northwest–east-southeast direction; (iii) terminal Appalachian compression oriented north-northeast–south-southwest; (iv) Cretaceous north–south distension; (v) a Cenozoic to Recent compression in a northwest–southeast direction. [Journal Translation]

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