Listar DMP - Artículos por financiación

Mostrando ítems 1-20 de 31

      Financiación
      TelluS Program of CNRS/INSU [1]
      The Andalusian Research Group RNM-179 [1]
      The authors would like to acknowledge the support given by the Institute of Water Research, the Department of Civil Engineering, the Department of Microbiology and the Department of Mineralogy and Petrology with all from the University of Granada. Additionally, they would like to acknowledge the economic support given by the Government of Spain and the Ministry of Economy and Competitivity under the funding project CTM2013-48154-P and grant BES-2014-067852. [1]
      The COST Action CA15224 Keel Bone Damage [1]
      The following funding is acknowledged: European Commission Seventh Framework Programme (grant No. 2012-328731 to HEK); Universidad de Granada (grant Nos. CGL2015- 64683-P and UCE PP 2016.05 to ABRN). [1]
      the MECRAS Project A-RNM-356-UGR20 “Proyectos de I+D+i en el marco del Programa Operativo FEDER Andalucía 2014-2020” defrayed by the “Junta de Andalucía” [1]
      The Spanish Ministry of Economy and Competitiveness (MINECO) IJCI-2017-3277 [1]
      The work was supported through an ERANET by the Biotechnology and Biological Sciences Research Council, UK grant ‘Better Bones’ BB/M028291/1, FORMAS 2014-01840, Investigación y Tecnología Agraria y Alimentaria 291815. The Roslin Institute is funded with a BBSRC Institute strategic programme grant BB/J004316/1. [1]
      This paper has been financed by the Spanish Grants CGL2013-40785-P and CGL2017-84469-P. [1]
      This research has also been funded by the Spanish Government (Grants CGL2015-70642-R, CGL2015-73103-EXP), the University of Granada (‘‘Unidad Científica de Excelencia’’ UCE-PP2016-05), the Junta de Andalucía (P11-RNM-7550), and the research group RNM-179 of the Junta de Andalucía. [1]
      This research was done within the grants MAT2012-37584, CGL2015-70642-R and P11-RNM-7550, funded by the Spanish Government, European Commission (ERDF funds) and the Junta de Andalucía. Additional funding was provided by the research group RNM-179 of the Junta de Andalucía and the Unidad Científica de Excelencia UCE-PP2016-05 of the University of Granada. Encarnacion Ruiz-Agudo acknowledges the receipt of a Ramón y Cajal grant from the Spanish Government (Ministerio de Economía y Competitividad) and CVP acknowledges funding from the EU Marie Curie initial training networks: Minsc, CO2 React and Flowtrans as well as an Australian Research Council (ARC) grant awarded to Julian Gale at Curtin University, Perth Australia. [1]
      This research was financially supported by the Spanish project CGL2007-61205 of the MEC, the CSICBAS collaborative project 2007BG0006, the research group (RNM 131) of the Junta de Andalucía, and an F.P.I grant BES-2005-8328 of the Spanish Ministry of Education and Sciences. [1]
      This research was financially supported by FEDER Funds, the Spanish Project CGL2015-65824 granted by the Spanish “Ministerio de Economía y Competitividad” to JAP, and the Ramón y Cajal Fellowship RYC-2015-17596 to JMGJ. This is also a contribution from the ARC National Key Centre for Geochemical Evolution and Metallogeny of Continents (www.es.mq.edu.au/GEMOC) and the ARC Centre of Excellence for Core to Crust Fluid Systems. Y.R-A acknowledges support by the Deutsche Forschungsgemeinschaft (DFG) grant RO4174/2-1. Supportwas also provided by the technical staff of the SHRIMP facility at Curtin University. [1]
      This research was financially supported by the Spanish Project CGL2015-65824 granted by the Spanish “Ministerio de Economía y Competitividad” to J.A.P., the Ramón y Cajal Fellowship RYC-2015-17596 to J.M.G.-J. and a FPU Ph.D grant to N.P.-S. by the Ministerio de Educación of the Spanish Government. [1]
      This research was funded by the Spanish Government (grants CGL2015-70642-R, CGL2015-73103-EXP, CTQ2017-84692-R), EU FEDER funding, the University of Granada (“Unidad Científica de Excelencia” UCE-PP2016-05) and the Junta de Andalucía (grant P11-RNM-7550 and Research Group RNM-179). We thank the personnel of the Centro de Instrumentación Científica (CIC) of the University of Granada for their help during TG-DSC, FESEM, -XRD, and ICP-OES analyses. [1]
      This research was funded by the Spanish Government FEDER project CGL 2015-65404-R/BTE, CGL2016-75679-P, by the Basque Government project IT930-16, Research Group RNM-179 of the Junta de Andalucía and the Aragon Government project E18_17R. [1]
      This research was supported by Spanish projects: RTI2018-099157-A-I00 and CGL2015-65824-P granted by the “Ministerio de Ciencia, Innovación y Universidades” and Ministerio de Economía y Competitividad” (MINECO) respectively. Additional funding was provided by the Ramón y Cajal Fellowship RYC-2015-17596 granted by the Spanish MINECO to JMGJ. A. Jiménez-Franco is supported with a postdoctoral grant (CVU 350809) from the National Council on Science and Technology (CONACYT) of Mexico. [1]
      This study has been financially supported by the Andalusian grant RNM1595, the Spanish grant CGL2008-02864, and a Masters grant awarded to AC by the Departamento de Mineralogía. y Petrología, Universidad de Granada, Spain. [1]
      This study was financially supported by Research Group RNM179 of the Junta de Andalucía and by Research Project MAT2016-75889-R. [1]
      This study was financially supported by the Spanish research group RNM179 of the Junta de Andalucía, by the research project MAT-2012-34473 and by the Institute of Conservation and Restoration of Cultural Heritage of the CICOP foundation (ICON-CICOP). [1]