Results 171 to 180 of about 3,184 (221)

Articulated specimens provide new insights into the iconic Mesozoic shark genus <i>Sphenodus</i>. [PDF]

open access: yesJ Syst Palaeontol
Villalobos-Segura E   +8 more
europepmc   +1 more source

Stop 3 : Gnieździska, Callovian-Oxfordian

open access: yes, 2008
Pieńkowski, Grzegorz   +2 more
openaire   +1 more source

Revisiting Hydrogen Sorption-Desorption in Natural Rocks. [PDF]

open access: yesInd Eng Chem Res
Masoudi M   +5 more
europepmc   +1 more source

HTO Diffusion in Oxfordian Limestone and Callovo-Oxfordian Argillite Formations

open access: yesMRS Proceedings, 2004
AbstractDiffusion coefficients and accessible porosities for HTO were measured on 30 samples from the Andra Underground Rock Laboratory in Meuse/Haute-Marne (France) using the through diffusion technique. Two distinct geological formations were studied: Oxfordian limestone and Callovo-oxfordian argillite between 166 and 477 m depth.
M. Descostes   +4 more
openaire   +2 more sources

The shifting biogeography of reef corals during the Oxfordian (Late Jurassic). A climatic control?

open access: yesPalaeogeography, Palaeoclimatology, Palaeoecology, 2012
International audienceUntil recently, the Jurassic was thought to have been a period characterised by a predominantly warm and equable climate. During the Oxfordian (a time span of six million years in the Late Jurassic) the distribution of tropical ...
Bertrand Martin-Garin   +1 more
exaly   +2 more sources

Dissolved helium distribution in the Oxfordian and Dogger deep aquifers of the Meuse/Haute-Marne area

open access: yesPhysics and Chemistry of the Earth, 2011
The 140-m-thick, clay-rich Callovo-Oxfordian (COX) layer of the eastern Paris Basin, France, is being considered by the French Nuclear Waste Agency (Andra) as a long-term underground nuclear waste repository.
E Fourre, P Jean-Baptiste, A Dapoigny
exaly   +2 more sources

A new sedimentary and biostratigraphic framework for the Callovian-Oxfordian transition on the Atlantic margin of Morocco [PDF]

open access: yesJournal of African Earth Sciences
A major global marine transgression occurred during the Callovian to Early Kimmeridgian, which was interrupted locally by a hiatus during the Late Callovian to Early Oxfordian.
Aude Duval-Arnould, Luc G Bulot
exaly   +2 more sources

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