Cretaceous owing: sequencing laissez

PDF Alluvial Facies and Paleosols in The Cretaceous Nanushuk. – (sequence boundaries) and Cretaceous high latitude paleoenvironmental conditions. Introduction The purpose of this paper is to document the characteristics of cretaceous alluvial facies and paleosols in the Nanushuk Formation (Mull et al., in prep.) exposed in outcrop in the brooks range foothills along the Kanayut River south of the National

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Predation upon Hatchling Dinosaurs by a New Snake from. – Predation upon Hatchling Dinosaurs by a New Snake from the Late Cretaceous of India Jeffrey A. Wilson1*, Dhananjay M. Mohabey2, Shanan E. Peters3, Jason J. Head4 1Museum of Paleontology and Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan, United States of America, 2Geological Survey of India

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Towards a sequence stratigraphic solution set for autogenic processes and allogenic controls: upper cretaceous strata, Book Cliffs, Utah, USA Gary J. Hampson Department of Earth Science and Engineering, Imperial College London, south kensington campus, London SW7 2AZ, UK g.j.hampson@imperial.ac.uk

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CRETACEOUS AQUIFERS. The aquifer overlies and in places is hydraulically interconnected with water-yielding sands of the Trinity aquifer. The upper part of the Tokio-Woodbine aquifer consists of the Tokio Formation, which is a sequence of cross-bedded sand, gravel, and lignitic clay that grades downdip to sand and shale.

PDF Shelf stability and mantle convection on Africa's passive. – the Cretaceous, followed by a variable but generally unstable Tertiary. As in Namibia, the shelf stability is a reflection of the steepness of the gradient from shelf to basin floor, and changes in this slope gradient owing to basin uplift or subsidence would be the main drivers of structuration, assisted by organic-rich dcollement surfaces.

PDF Mid Cretaceous orbitolinid (Foraminiferida) record from the. – Mid Cretaceous orbitolinid (Foraminiferida) record from the islands of Cres and Losinj (Croatia) and its regional stratigraphic. Owing to synsedimen-. dierentiation during the early Aptian is the sequence of strata on Losinj (Figure 4). Unlike the situation in

Geological Magazine – If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. conglomerate in the eastern segment of the basin. The Lower Cretaceous.

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