Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Leonardo Pasqualetto"'
Autor:
Larry Falvello, Paolo Lotti, Chiara Massera, Serena C. Tarantino, Michele Zema, Horst Puschmann, Marielle Y. Agbahoungbata, Jacopo Andreo, Suchithra Ashoka Sahadevan, Alessandro Bismuto, Giulia Bonfant, Sourou A. S. Bonou, Claudia Carraro, Marta De Zotti, Armando di Biase, Riccardo Fantini, Ilaria Ferraboschi, Jean Marcos Ferreira Custodio, Matteo Frigerio, Gianpiero Gallo, Silvana Gjyli, Meriem Goudjil, Fernando Igoa, Enver Kahveci, Maksim Kalienko, Sofia Lorenzon, Ludovico Macera, Joaqun Joaqun Manrique Fajardo, Enida Nushi, Said Ouaatta, Emmanuele Parisi, Leonardo Pasqualetto, Edyta Pesko, Giovanni Pierri, Roberta Pinalli, Romy Poppe, Antonio Santoro, Ekaterina Smirnova, Simona Sorbara, Leonardo Tensi, Gers Tusha
Publikováno v:
IUCrData, Vol 4, Iss 9, p x191222 (2019)
The title two-dimensional coordination polymer, [Zn(C6H5PO3)]n, was synthesized serendipitously by reacting a tetraphosphonate cavitand Tiiii[C3H7, CH3, C6H5] and Zn(CH3COO)2·2H2O in a DMF/H2O mixture. The basic conditions of the reaction cleaved th
Externí odkaz:
https://doaj.org/article/7ffd732a6c9d4e22b63d2e900d0b37ae
Publikováno v:
American Mineralogist. 106:301-308
Crowningshieldite is the natural analog of the synthetic compound α-NiS. It has a NiAs-type structure and is the high-temperature polymorph relative to millerite (β-NiS), with an inversion temperature of 379 °C. Crowningshieldite is hexagonal, spa
Autor:
Leonardo Pasqualetto
Data for the reciprocal orientations between diamonds/clinopyroxene (cpx) and the Sm diffusion model.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::388a77c91b9edba88b3f2fd773bfdbf8
https://doi.org/10.1130/geol.s.19783150.v1
https://doi.org/10.1130/geol.s.19783150.v1
Autor:
Luca Faccincani, Valerio Cerantola, Fabrizio Nestola, Paolo Nimis, Luca Ziberna, Leonardo Pasqualetto, Aleksandr I. Chumakov, Jeffrey W. Harris, Massimo Coltorti
Thanks to the physical strength of diamonds and their relatively unreactive chemical nature, their mineral inclusions may remain exceptionally preserved from alteration processes and chemical exchanges with surrounding minerals, fluids and/or melts f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::740c9d24a870afca580d3842f453c3d7
https://hdl.handle.net/11368/3045839
https://hdl.handle.net/11368/3045839
Publikováno v:
Geological Society of America Abstracts with Programs.