Lower Greensand Fossils in Kent
نویسندگان
چکیده
منابع مشابه
Enigmatic Fossils from the Lower Carboniferous Shrimp Bed, Granton, Scotland
The Lower Carboniferous (Visean) Granton Lagerstätte (Edinburgh, Scotland) is principally known for the discovery of the conodont animal, but has also yielded numerous crustaceans and other faunas. Here we report on small branching colonies, reaching 10 mm in length. They are small, erect, arborescent, and irregularly branched with predominant monopodial and dichotomous growth. They bud in a si...
متن کاملClement Kent
report, was the deep divergence of the rosada lineage at the base of the Conolophus clade. “The species alters the current thinking about the timing of diversification of land iguanas, which was previously supposed to have occurred in the Pleistocene era,” the researchers write. “In addition to the taxonomic implications, this form, which we recognise as a good species, is very important becaus...
متن کاملComputer Science at Kent
This talk sets out the problem domain for model transformation and introduces a set of use cases for transformation including model differencing, pattern expansion, model merging and weaving, alternate views and generation of platform specific artifacts from a platform independent model. The talk also discusses where model transformation fits into the development process and who we can expect t...
متن کاملRock physics model of glauconitic greensand from the North Sea
The objective of this study was to establish a rock physics model of North Sea Paleogene greensand. The Hertz-Mindlin contact model is widely used to calculate elastic velocities of sandstone as well as to calculate the initial sand-pack modulus of the soft-sand, stiff-sand, and intermediate-stiff-sand models. When mixed minerals in rock are quite different, e.g., mixtures of quartz and glaucon...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Geological Magazine
سال: 1895
ISSN: 0016-7568,1469-5081
DOI: 10.1017/s0016756800129693