▪ Abstract Rift basins of the Central Atlantic Margins (CAM) of North America and Morocco
preserve largely continental sequences of sedimentary strata and less important minor …

The extension-driven break-up of the Pangean Supercontinent in the present-day Central
and North Atlantic domains commenced during Permo-Triassic times. Permian rift processes …

Abstract Although the Late Triassic was a time of widespread aridity, evidence exists for a
significant increase in rainfall during the middle to late Carnian. Upper Triassic playa-lake …

The thickest part of asymmetric rift, pull-apart, and foreland basin fills commonly consists of
large-scale (hundreds to thousands of metres thick), tectonically generated cyclothems of …

Generally arid conditions that pervaded much of Europe and North America during the late
Triassic were interrupted by a wet monsoonal climatic phase during Middle and Late …

At the beginning of the Late Triassic, a period of increased precipitation occurred over large
tracts of Central Pangea, the “Carnian Pluvial Event”. It was a short-lived event (> 1 Ma) …

The palynological analysis on a continuous shallow-marine succession of the western
Tethys realm allows a better characterization of the Carnian (late Triassic) paleofloristic and …

Geological relationships preserved in the New Brunswick segment of the Appalachian
orogen are key to deciphering the complex tectonic events that occurred during the closing …

1. Acquisition of new data. Over the past two decades, regional and local geologic map**,
drilling and coring, and seismic-reflection profiling have increased vastly our structural and …

Alluvial fan and braided fluvial redbeds of the Triassic Lepreau Formation of southern New
Brunswick, eastern Canada, contain a moderately diverse and abundant invertebrate …