R
Robert Hall
Researcher at Wageningen University and Research Centre
Publications - 561
Citations - 32813
Robert Hall is an academic researcher from Wageningen University and Research Centre. The author has contributed to research in topics: Provenance & Basement (geology). The author has an hindex of 81, co-authored 525 publications receiving 28159 citations. Previous affiliations of Robert Hall include Rice University & University College London.
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Journal Article
Pertussis in South Australia 1893 to 1996.
TL;DR: Despite no substantial increase in mortality nor hospitalisation for pertussis in South Australia, the notification rate has remained high since 1993, and this increase may be attributable to the use of more sensitive tests for pertussedis, such as serology.
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Spontaneous closure of a ventricular septal defect after banding of the pulmonary artery.
TL;DR: Mechanisms of spontaneous closure of ventricular septal defects have been reviewed and speculations offered regarding the relation of pulmonary arterial banding to this process.
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Maltodextrin improves physical properties and volatile compound retention of spray-dried asparagus concentrate
Joanne W. Siccama,Eirini Pegiou,Lu Zhang,Roland Mumm,Robert Hall,Remko M. Boom,Maarten A.I. Schutyser +6 more
TL;DR: In this paper, asparagus juice is concentrated into a powder with a poor aroma profile and spray-dried with maltodextrin DE12 as a carrier agent to improve the volatile profiles of aspagus powder.
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Gravity fields in eastern Halmahera and the Bonin Arc: Implications for ophiolite origin and emplacement
TL;DR: A Mesozoic ophiolitic basement is overlain by, and imbricated with, Upper Cretaceous and Paleogene arc volcanic and sedimentary rocks in Halmahera as mentioned in this paper.
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Oligocene-Miocene drainage evolution of NW Borneo: Stratigraphy, sedimentology and provenance of Tatau-Nyalau province sediments
H. Tim Breitfeld,Juliane Hennig-Breitfeld,Marcelle K. BouDagher-Fadel,Robert Hall,Thomson Galin +4 more
TL;DR: In this article, the Nyalau Formation (Biban sandstone Member and Upper Nyalua Member), Kakus Unit, and Merit-Pila Formation are divided into Oligocene to Lower Miocene sequences.