نتایج جستجو برای: marly

تعداد نتایج: 194  

2004
Crispin KATONGO Christian KOEBERL Brian J. WITZKE Richard H. HAMMOND Raymond R. ANDERSON

The Crow Creek Member is one of several marl units recognized within the Upper Cretaceous Pierre Shale Formation of eastern South Dakota and northeastern Nebraska, but it is the only unit that contains shock-metamorphosed minerals. The shocked minerals represent impact ejecta from the 74-Ma Manson impact structure (MIS). This study was aimed at determining the bulk chemical compositions and ana...

Journal: :Bulletin of the Geological Society of Greece 2007

2004
Fabio Berezowsky Rocha Marcello Zapparoli Marcia Lima de Oliveira Mugnaini Luiz Francisco Rodrigues José Rodrigues Parga Carlos Eduardo Rochitte

Fabio Berezowsky Rocha, MD, Marcello Zapparoli, MD, Marcia Lima de Oliveira Mugnaini, MD, Marly Maria Uellendahl, MD, Miguel Rosario, MD, Fátima Cristina Pedroti, MD, Luiz Francisco Rodrigues de Ávila, MD, PhD, Roberto Kalil-Filho, MD, PhD, Bernardo Léo Wajchenberg, MD, PhD, Cláudio Campi de Castro, MD, PhD, José Rodrigues Parga, MD, PhD, Carlos Eduardo Rochitte, MD, PhD. Cardiovascular Magneti...

Journal: :Annals of oncology : official journal of the European Society for Medical Oncology 2014
P Mohr M Harries F Grange R Ehness L Benjamin O Siakpere L McLeod S Wolowacz J A Kaye I Kontoudis

P. Mohr1, M. Harries2, F. Grange3, R. Ehness4, L. Benjamin5, O. Siakpere6, L. McLeod7, S. Wolowacz8, J.A. Kaye9, I. Kontoudis10 Clinic of Dermatology, Dermatologic Center Buxtehude, Buxtehude, GERMANY Department of Medical Oncology, Guys and St Thomas’s Hospitals NHS Foundation Trust, Guys Hospital, London, UK Dermatology, Reims University Hospital, Reims, FRANCE Medical Hematology/oncology, Gl...

Journal: :Bulletin du Centre de recherche du château de Versailles 2015

2012
Dietmar Adam Roman Markiewicz Markus Brunner

The city bypass tunnel of Waidhofen an der Ybbs (Austria) is situated in an intricate geological-geotechnical complex consisting of soil, hard soil, weak rock and solid rock. Marls and marly limestone (Waidhofener formation) predominate followed by tectonic breccia of the Alpine cliff zone, which is a tectonic melange zone. Materials of this kind universally have isolated interior blocks embedd...

Journal: :Bulletin du Centre de recherche du château de Versailles 2012

Journal: :Bulletin du Centre de recherche du château de Versailles 2012

Journal: :Journal of Architecture and Planning (Transactions of AIJ) 2001

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