首页|期刊导航|极地科学进展(英文版)|Late Maastrichtian–Paleocene chronostratigraphy from Seymour Island, James Ross Basin, Antarctic Peninsula:Eustatic controls on sedimentation
极地科学进展(英文版)2019，Vol.30Issue(3)：303-327,25.DOI:10.13679/j.advps.2018.0045
Late Maastrichtian–Paleocene chronostratigraphy from Seymour Island, James Ross Basin, Antarctic Peninsula:Eustatic controls on sedimentation
Late Maastrichtian–Paleocene chronostratigraphy from Seymour Island, James Ross Basin, Antarctic Peninsula:Eustatic controls on sedimentation
摘要
关键词
Paleocene/magnetostratigraphy/Antarctic Peninsula/James Ross Basin/Seymour IslandKey words
Paleocene/magnetostratigraphy/Antarctic Peninsula/James Ross Basin/Seymour Island引用本文复制引用
Manuel MONTES,Elisabet BEAMUD,Francisco NOZAL,Sergio SANTILLANA..Late Maastrichtian–Paleocene chronostratigraphy from Seymour Island, James Ross Basin, Antarctic Peninsula:Eustatic controls on sedimentation[J].极地科学进展(英文版),2019,30(3):303-327,25.基金项目
The authors are most grateful to the DNA-Instituto Antártico Argentino for the scientific and logistic support during the Argentine Summer Antarctic Expeditions 2009–2011. This work was supported by the Instituto Geológico y Minero de España (IGME) and Dirección General de Investigación (DGI) from Spain by the projects CTM2011-30241-C02-02 and CTM2014-60451-C2-2-P. The authors want to thank the Geomodels Research Institute and the Grup de Recerca de Geodinàmica i Anàlisi de Conques (Grant no. 2017SGR596, supported by AGAUR). We thank the Paleomagnetic Laboratory of Barcelona (CCiTUB-ICTJA CSIC) where the palaeomagnetic analyses were carried out. （IGME）
