Microfacies and microfossils of the edge Cretaceous carbonate platform (figs

The phosphatic peloids may have different sizes and origins, the main mechanisms of their formation are growth around foreign grains (as coated grains), phospho-micritization of

Organocatalysis Organocatalysis 2.2 2.2 Transesterification Transesterification Alessio Caretto Jess Stanley Transesterification. Transesterification of organic of organic

2-7, provengono dalla sezione stratigrafica del Monte Meta, Gran Sasso d’Italia (Abruzzo) e Monte Cefalo, Monti Aurunci (Lazio meridionale).. RETICO – The microfacies of

2-4, provengono dalle sezioni stratigrafiche della Grotta dei Serpenti e del Monte Sorgenza, Monti Aurunci (Lazio meridionale).. Parte inferiore-media della Biozona a

2-7, provengono dalla sezione stratigrafica del Canale Bocca di Rio e Monte Vate Rutto, Monti Aurunci (Lazio meridionale).. Biozona a

BAJOCIANO SUPERIORE – BATHONIANO INFERIORE – Dorsale di Monte Bolza stratigraphic section, Gran Sasso d’Italia (Abruzzi).. Lower part of the Protopeneroplis

If G = (V, E) is a d-regular graph such that every edge has effective resistance O(1/d), the Marcus-Spielman-Srivastava [10] proof of the Kadison-Singer conjecture (henceforth, we

In particular, 1 H spin-lattice and spin-spin relaxation times allowed us to get insights into the dynamic properties of both the polymer bulk and the bound rubber, and to obtain