Chromatin and cytoskeletal tethering determine nuclear morphology in progerin expressing cells

Autor: Lionetti, M. C., Bonfanti, S., Fumagalli, M. R., Budrikis, Z., Clos, F. Font, Costantini, G., Chepizhko, O., Zapperi, S., La Porta, C. A. M.

The nuclear morphology of eukaryotic cells is determined by the interplay between the lamina forming the nuclear skeleton, the chromatin inside the nucleus and the coupling with the cytoskeleton. Nuclear alterations are often associated with patholog

Externí odkaz: http://arxiv.org/abs/2003.08232

When crust comes of age : on the chemical evolution of Archaean, felsic continental crust by crustal drip tectonics

Autor: Nebel, O., Capitanio, F. A., Moyen, J.-F., Weinberg, R. F., Clos, F., Nebel-Jacobsen, Y. J., Cawood, P. A.

Publikováno v: Philosophical Transactions: Mathematical, Physical and Engineering Sciences, 2018 Nov . 376(2132), 1-21.

Externí odkaz: https://www.jstor.org/stable/26601831

Exact Derivation of a Finite-Size Scaling Law and Corrections to Scaling in the Geometric Galton-Watson Process

Autor: Garcia-Millan, R., Font-Clos, F.

Publikováno v: RECERCAT (Dipòsit de la Recerca de Catalunya)
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Recercat. Dipósit de la Recerca de Catalunya
instname

The theory of finite-size scaling explains how the singular behavior of thermodynamic quantities in the critical point of a phase transition emerges when the size of the system becomes infinite. Usually, this theory is presented in a phenomenological

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::5d5f2379d8b2e4836da377afd3b5f4ee
http://hdl.handle.net/2072/377764

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Fragments of deeper parts of the hanging wall mantle preserved as orogenic peridotites in the central belt of the Seve Nappe Complex, Sweden

Autor: Clos, F., Gilio, M., van Roermund, H.L.M., Structural geology & tectonics, Structural geology and EM

Publikováno v: Lithos, 192-195, 8. Elsevier

Formation conditions of olivine microstructures are investigated in the Kittelfjäll spinel peridotite (KSP), a fragment of lithospheric mantle which occurs as an isolated body within high grade metamorphic crustal rocks of the Seve Nappe Complex (SN

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::66632fad7f59f13f3d7186b50960ae70
https://dspace.library.uu.nl/handle/1874/306835