• Aucun résultat trouvé

A whole-genome sequence and transcriptome perspective on HER2-positive breast cancers

N/A
N/A
Protected

Academic year: 2021

Partager "A whole-genome sequence and transcriptome perspective on HER2-positive breast cancers"

Copied!
10
0
0

Texte intégral

Loading

Figure

Table 1 | Associations between RNA expression groups and biological characteristics for the 99 samples of the INCa-HER2 þ data set.
Figure 1 | Summary of biological and genomic features of the 64 sequenced HER2 þ tumours
Figure 2 | Examples of CNV patterns in the ERBB2 amplicon. X axis: position on chromosome 17, the minimal region defining the ERBB2 amplicon is indicated by the blue shaded box
Figure 3 | Multiple correspondence analysis of selected biological and genomic variables

Références

Documents relatifs

L’accès à ce site Web et l’utilisation de son contenu sont assujettis aux conditions présentées dans le site LISEZ CES CONDITIONS ATTENTIVEMENT AVANT D’UTILISER CE SITE WEB.

For a special case of pair-wise mobility model in which the origin and destination of vehicles are in the coverage range of adjacent base stations, we first present a static offline

In order to identify the role of PI3K, Src and JAK2 path- ways in the proliferation of human colonic tumour cells induced by G-gly, we measured HCT116 proliferation in the

This learning system was achieved by developing a feedback loop between a supply chain network simulation and an artificial intelligence model to predict the patterns of

Index Terms—Silicon photonics, process variations, line edge roughness, adjoint method, DFM, Y-branch, sensitivity analysis..

RÉSUMÉ – Cet article présente les résultats d’une étude expérimentale dont l’objectif est d’évaluer le comportement de deux familles chimiques de géomembranes

Phase equilibria constraints, i.e., the necessity of preserving the mantle signature seen in high-MgO and picritic arc basalts, and glass inclusion data suggest that STV301

er precipitation in between the convective and stratiform parts, 2) the rearward evacuation of ice precipitation by a front to rear updraft, which generates the stratiform part