Perspectives for Geological Surveying in the Netherlands
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EBN Internship Report Confidential
EBN Internship Report Confidential Anja Dijkhuizen 3026051 Part I: Basin analysis of Tertiary deposits in the Gorredijk concession using 3D seismics and well data Part II: Extra Work Supervision: Maarten-Jan Brolsma, Guido Hoetz, Fokko van Hulten; EBN Prof. Dr. Chris Spiers; UU EBN September – November 2011 Part I: Basin analysis of Tertiary deposits in the Gorredijk concession using 3D seismics and well data 2 Basin analysis of Tertiary deposits in the Gorredijk concession using 3D seismics and well-data EBN-Internship Anja Dijkhuizen The 1000m thick Tertiary sequence present in the Dutch onshore subsurface can hold prospective reservoirs of shallow gas. In this report, an inventory of Tertiary reservoirs is made for the Gorredijk concession (Friesland, northern Netherlands). By using well, log and seismic data, the structural elements of the studied area are investigated. Thickness maps of the three Tertiary groups show a thickening trend towards the west. However, individual differences exist within the groups, implying basin shifts through the Tertiary Period. Gas migration would therefore be to the east, but timing is important due to the differences within each group. Indications of an erosive surface in the lower Tertiary Brussels Sand Member give more insight in the different Alpine phase pulses during the Tertiary. A large erosive event during the Miocene has eroded parts of the Upper Tertiary deposits. The associated angular unconformity, the ‘Mid Miocene Unconformity’, is shown not to be of tectonic but of sedimentary origin. Large Neogene delta foresets from the Eridanos deltaic system onlap on the Mid Miocene Unconformity. These delta deposits are so far only described to be found offshore. -
Handbook of Dutch Church History
Herman J. Selderhuis, Handbook of Dutch Church History © 2014, Vandenhoeck & Ruprecht GmbH & Co. KG, Göttingen ISBN Print: 9783525557877 — ISBN E-Book: 9783647557878 Herman J. Selderhuis, Handbook of Dutch Church History © 2014, Vandenhoeck & Ruprecht GmbH & Co. KG, Göttingen ISBN Print: 9783525557877 — ISBN E-Book: 9783647557878 Herman J. Selderhuis, Handbook of Dutch Church History Handbook of Dutch Church History edited by Herman J. Selderhuis Vandenhoeck & Ruprecht © 2014, Vandenhoeck & Ruprecht GmbH & Co. KG, Göttingen ISBN Print: 9783525557877 — ISBN E-Book: 9783647557878 Herman J. Selderhuis, Handbook of Dutch Church History Originally published in Dutch language as “Handboek Nederlandse Kerkgeschiedenis”, edited by Herman J. Selderhuis (© VBK|media B.V. on behalf of Uitgeverij Kok, Utrecht 2010). With 4 figures. Bibliographic information published by the Deutsche Nationalbibliothek The Deutsche Nationalbibliothek lists this publication in the Deutsche Nationalbibliografie; detailed bibliographic data available online: http://dnb.d-nb.de. ISBN 978-3-647-55787-8 You can find alternative editions of this book and additional material on our website: www.v-r.de Cover: Stichting Goudse Sint-Jan, Gouda, Netherlands © 2015, Vandenhoeck & Ruprecht GmbH & Co. KG, Göttingen/ Vandenhoeck & Ruprecht LLC, Bristol, CT, U.S.A. www.v-r.de All rights reserved. No part of this work may be reproduced or utilized in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without prior written permission from the publisher. 1SJOUFEJO(FSNBOZ Typesetting by Konrad Triltsch, Ochsenfurt 1SJOUFEBOECPVOECZ)VCFSU$P (ÚUUJOHFO 1SJOUFEPOOPOBHJOHQBQFS © 2014, Vandenhoeck & Ruprecht GmbH & Co. KG, Göttingen ISBN Print: 9783525557877 — ISBN E-Book: 9783647557878 Herman J. Selderhuis, Handbook of Dutch Church History Contents Acknowledgements . -
A Geological History of Groningen's Subsurface
A geological history of Groningen’s subsurface Erik Meijles, University of Groningen Date June 2015 Editors Jan van Elk & Dirk Doornhof Translated by E.L. Howard General introduction Ground acceleration caused by an induced earthquake is strongly dependent on the composition of local shallow soils. NAM commissioned Deltares to conduct a detailed survey of the shallow subsurface above the Groningen gas field. The survey focuses on Quaternary geology with an emphasis on the upper 50 metres. This report provides an introduction to Groningen’s Quaternary geology as a background to the comprehensive Deltares report, which has culminated in a detailed model of Groningen’s shallow subsurface. This report was written by Dr ir Erik Meijles, Assistant Professor of Physical Geography at the University of Groningen. Wim Dubelaar, Dr Jan Stafleu and Dr Wim Westerhoff of TNO Geological Survey of the Netherlands (TNO- NITG) in Utrecht assisted with editing this report and provided a number of key diagrams. Title A geological history of Groningen’s subsurface Date June 2015 Client NAM Author Erik Meijles, Assistant Professor Edited by Jan van Elk of Physical Geography and Dirk Doornhof Organization University of Groningen Organization NAM Significance for Research theme: earthquake Predicting ground acceleration research Explanation: Ground acceleration caused by an induced earthquake is strongly dependent on the composition of local shallow soils. NAM commissioned Deltares to conduct a detailed survey of the shallow subsurface above the Groningen gas field. This survey focuses on the Quaternary geology of Groningen with an emphasis on the upper 50 metres. Directly This research serves as background to the report entitled ‘Geological schematisation of related the shallow subsurface of Groningen’ written by various Deltares staff members. -
A Reappraisal of the Stratigraphy of the Upper Miocene Unit X in The
GEOLOGICA BELGICA (2020) 23/3-4: xxx-xxx A reappraisal of the stratigraphy of the upper Miocene unit X in the Maaseik core, eastern Campine area (northern Belgium) Stephen LOUWYE1* & Noël VANDENBERGHE2 1 Paleontology and paleoenvironments, Department of Geology, Ghent University, Belgium; [email protected]. 2 Department Earth and Environmental Sciences, KU Leuven, Belgium; [email protected]. * corresponding author ABSTRACT. The stratigraphy of the Tortonian-Messinian sequence from the Maaseik core, located on the shoulder of the Roer Valley Graben (RVG) in the eastern Campine area in northern Belgium, was improved. The analysis of the marine palynomorphs (dinoflagellate cysts and acritarchs) from the uppermost part of the Breda Formation, the unnamed unit X and the basal part of the Lower Waubach Member led to the recognition of the mid to upper Tortonian Hystrichosphaeropsis obscura biozone. Therefore deposition of this entire analyzed sequence took place sometime between 8.8 to 7.6 Ma. Paleoenvironmental interpretation of the palynomorphs points to shallow marine conditions and most probably a stressed environment during the deposition of unit X. A comparison with the time equivalent stratigraphy in the nearby Belgian Campine, the Dutch RVG and the German Lower Rhine Basin allowed the identification of the Inden Formation and required a shift in the base of the Kieseloolite Formation compared to the earlier lithostratigraphic interpretation of the Maaseik core. The regional stratigraphic scheme shows the progressive -
Neogene Stratigraphy of the Langenboom Locality (Noord-Brabant, the Netherlands)
Netherlands Journal of Geosciences — Geologie en Mijnbouw | 87 - 2 | 165 - 180 | 2008 Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands) E. Wijnker1'*, T.J. Bor2, F.P. Wesselingh3, D.K. Munsterman4, H. Brinkhiris5, A.W. Burger6, H.B. Vonhof7, K. Post8, K. Hoedemakers9, A.C. Janse10 & N. Taverne11 1 Laboratory of Genetics, Wageningen University, Arboretumlaan 4, 6703 BD Wageningen, the Netherlands. 2 Prinsenweer 54, 3363 JK Sliedrecht, the Netherlands. 3 Naturalis, P.O. Box 9517, 2300 RA Leiden, the Netherlands. 4 TN0 B&0 - National Geological Survey, P.O. Box 80015, 3508 TA Utrecht, the Netherlands. 5 Palaeocecology, Inst. Environmental Biology, Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, the Netherlands. 6 P. Soutmanlaan 18, 1701 MC Heerhugowaard, the Netherlands. 7 Faculty Earth and Life Sciences, Vrije Universiteit, de Boelelaan 1085, 1081 EH Amsterdam, the Netherlands. 8 Natuurmuseum Rotterdam, P.O. Box 23452, 3001 KL Rotterdam, the Netherlands. 9 Minervastraat 23, B 2640 Mortsel, Belgium. 10 Gerard van Voornestraat 165, 3232 BE Brielle, the Netherlands. 11 Snipweg 14, 5451 VP Mill, the Netherlands. * corresponding author. Email: [email protected] Manuscript received: February 2007; accepted: March 2008 Abstract The locality of Langenboom (eastern Noord-Brabant, the Netherlands), also known as Mill, is famous for its Neogene molluscs, shark teeth, teleost remains, birds and marine mammals. The stratigraphic context of the fossils, which have been collected from sand suppletions, was hitherto poorly understood. Here we report on a section which has been sampled by divers in the adjacent flooded sandpit 'De Kuilen' from which the Langenboom sands have been extracted. -
Zwolle, Leeuwarden/Groningen
richting/direction Zwolle, Leeuwarden/Groningen SteenwijkHeerenveenLeeuwarden AmersfoortAmersfoortAmersfoort CentraalNijkerk SchothorstPutten VathorstErmeloHarderwijkNunspeet't HardeWezepZwolleMeppel _` _` _` _` ` ` ` _` ` AssenGroningen _` _` De informatie op deze vertrekstaat kan zijn gewijzigd. Plan uw reis op ns.nl, in de app of raadpleeg de schermen met actuele vertrekinformatie op dit station. The information on this board may be subject to changes. Check your journey plan on ns.nl or consult the displays with real-time travel information at this station. Vertrektijd/ Treinen rijden op/ Spoor/ Soort trein/ Eindbestemming/ Vertrektijd/ Treinen rijden op/ Spoor/ Soort trein/ Eindbestemming/ Departure Trains run on Platf. Transportation Destination Departure Trains run on Platf. Transportation Destination 12 ma di wo 1 Sprinter Zwolle via Harderwijk 04 ma di wo do vr za zo 2 Intercity Groningen via Zwolle-Assen 6 12 do vr za 2 Sprinter Zwolle via Harderwijk 16 12 ma di wo do vr za zo 2 Sprinter Zwolle via Harderwijk 34 ma di wo do vr 2 Intercity Leeuwarden via Zwolle-Steenwijk-Heerenveen, stopt ook in/also calls 22 ma di wo do vr za zo 2 Intercity Amersfoort Schothorst at Meppel 29 ma di wo do vr za zo 1 Sprinter Amersfoort Vathorst 42 ma di wo do vr za 2 Sprinter Zwolle via Harderwijk 34 ma di wo do vr za zo 2 Intercity Leeuwarden via Zwolle-Steenwijk-Heerenveen, stopt ook in/also calls 49 ma di wo do vr 1 Intercity Amersfoort Schothorst at Meppel 59 ma di wo do vr 1 Sprinter Amersfoort Vathorst 39 ma di wo do vr 5b Sprinter Harderwijk, -
Closer Ties: the Dutch Caribbean and the Aftermath of Empire, 1942-2012
City University of New York (CUNY) CUNY Academic Works All Dissertations, Theses, and Capstone Projects Dissertations, Theses, and Capstone Projects 6-2017 Closer Ties: The Dutch Caribbean and the Aftermath of Empire, 1942-2012 Chelsea Schields The Graduate Center, City University of New York How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/gc_etds/1993 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] CLOSER TIES: THE DUTCH CARIBBEAN AND THE AFTERMATH OF EMPIRE, 1942-2012 by CHELSEA SCHIELDS A dissertation submitted to the Graduate Faculty in History in partial fulfillment of the requirements for the degree of Doctor of Philosophy, The City University of New York 2017 © 2017 CHELSEA SCHIELDS All Rights Reserved ii Closer Ties: The Dutch Caribbean and the Aftermath of Empire, 1942-2012 by Chelsea Schields This manuscript has been read and accepted for the Graduate Faculty in History in satisfaction of the dissertation requirement for the degree of Doctor of Philosophy. Professor Dagmar Herzog ______________________ _________________________________________ Date Chair of Examining Committee Professor Helena Rosenblatt ______________________ _________________________________________ Date Executive Officer Professor Mary Roldán Professor Joan Scott Professor Todd Shepard Professor Gary Wilder Supervisory Committee THE CITY UNIVERSITY OF NEW YORK iii Abstract Closer Ties: The Dutch Caribbean and the Aftermath of Empire, 1942-2012 by Chelsea Schields Advisor: Professor Dagmar Herzog This dissertation examines the unique trajectory of decolonization in the Netherlands and its former Caribbean colonies and argues that sexual and reproductive politics have played a pivotal role in forging a postcolonial commonwealth state. -
An Updated and Revised Stratigraphic Framework for the Miocene And
Netherlands Journal of An updated and revised stratigraphic Geosciences framework for the Miocene and earliest www.cambridge.org/njg Pliocene strata of the Roer Valley Graben and adjacent blocks Original Article Dirk K. Munsterman1 , Johan H. ten Veen1 , Armin Menkovic1, Jef Deckers2, 1 3 1 Cite this article: Munsterman DK, ten Veen JH, Nora Witmans , Jasper Verhaegen , Susan J. Kerstholt-Boegehold , Menkovic A, Deckers J, Witmans N, 1 1 Verhaegen J, Kerstholt-Boegehold SJ, van de Tamara van de Ven and Freek S. Busschers Ven T, and Busschers FS. An updated and revised stratigraphic framework for the 1TNO – Geological Survey of the Netherlands, P.O. Box 80015, 3508 TA Utrecht, the Netherlands; 2VITO, Flemish Miocene and earliest Pliocene strata of the Roer Institute for Technological Research, Boeretang 200, 2400 Mol, Belgium and 3Department of Earth and Valley Graben and adjacent blocks. Netherlands Environmental Sciences, KU Leuven, Celestijnenlaan 200E, 3001 Heverlee, Belgium Journal of Geosciences, Volume 98, e8. https:// doi.org/10.1017/njg.2019.10 Abstract Received: 23 January 2019 In the Netherlands, the bulk of the Miocene to lowest Pliocene sedimentary succession is cur- Revised: 1 November 2019 Accepted: 8 November 2019 rently assigned to a single lithostratigraphical unit, the Breda Formation. Although the forma- tion was introduced over 40 years ago, the definition of its lower and upper boundaries is still Keywords: problematic. Well-log correlations show that the improved lecto-stratotype for the Breda dinoflagellate cysts; lithostratigraphy; Formation in well Groote Heide partly overlaps with the additional reference section of the Neogene; seismic; southern North Sea Basin; well-log correlation older Veldhoven Formation in the nearby well Broekhuizenvorst. -
A Partial Rostrum of the Porbeagle Shark
GEOLOGICA BELGICA (2010) 13/1-2: 61-76 A PARTIAL ROSTRUM OF THE PORBEAGLE SHARK LAMNA NASUS (LAMNIFORMES, LAMNIDAE) FROM THE MIOCENE OF THE NORTH SEA BASIN AND THE TAXONOMIC IMPORTANCE OF ROSTRAL MORPHOLOGY IN EXTINCT SHARKS Frederik H. MOLLEN (4 figures, 3 plates) Elasmobranch Research, Meistraat 16, B-2590 Berlaar, Belgium; E-mail: [email protected] ABSTRACT. A fragmentary rostrum of a lamnid shark is recorded from the upper Miocene Breda Formation at Liessel (Noord-Brabant, The Netherlands); it constitutes the first elasmobranch rostral process to be described from Neogene strata in the North Sea Basin. Based on key features of extant lamniform rostra and CT scans of chondrocrania of modern Lamnidae, the Liessel specimen is assigned to the porbeagle shark, Lamna nasus (Bonnaterre, 1788). In addition, the taxonomic significance of rostral morphology in extinct sharks is discussed and a preliminary list of elasmobranch taxa from Liessel is presented. KEYWORDS. Lamniformes, Lamnidae, Lamna, rostrum, shark, rostral node, rostral cartilages, CT scans. 1. Introduction Pliocene) of North Carolina (USA), detailed descriptions and discussions were not presented, unfortunately. Only In general, chondrichthyan fish fossilise only under recently has Jerve (2006) reported on an ongoing study of exceptional conditions and (partial) skeletons of especially two Miocene otic capsules from the Calvert Formation large species are extremely rare (Cappetta, 1987). (lower-middle Miocene) of Maryland (USA); this will Therefore, the fossil record of Lamniformes primarily yield additional data to the often ambiguous dental studies. comprises only teeth (see e.g. Agassiz, 1833-1844; These well-preserved cranial structures were stated to be Leriche, 1902, 1905, 1910, 1926), which occasionally are homologous to those seen in extant lamnids and thus available as artificial, associated or natural tooth sets useful for future phylogenetic studies of this group. -
Impact of an Historic Underground Gas Well Blowout on the Current Methane Chemistry in a Shallow Groundwater System
Impact of an historic underground gas well blowout on the current methane chemistry in a shallow groundwater system Gilian Schouta,b,c,1, Niels Hartogb,c, S. Majid Hassanizadehb, and Jasper Griffioena,d aCopernicus Institute of Sustainable Development, Utrecht University, 3584 CS Utrecht, The Netherlands; bEarth Sciences Department, Utrecht University, 3584 CD Utrecht, The Netherlands; cGeohydrology Unit, KWR Water Cycle Research Institute, 3433 PE Nieuwegein, The Netherlands; and dGeological Survey of the Netherlands, Nederlandse Organisatie voor Toegepast Natuurwetenschappelijk Onderzoek (TNO), 3584 CB Utrecht, The Netherlands Edited by Susan L. Brantley, Pennsylvania State University, University Park, PA, and approved November 27, 2017 (received for review June 27, 2017) Blowouts present a small but genuine risk when drilling into the deep (15) and Aliso Canyon (16) blowouts. In some cases, the pres- subsurface and can have an immediate and significant impact on the sures generated during a blowout do not escape at the surface surrounding environment. Nevertheless, studies that document their but form a fracture network that allows the well to blow out long-term impact are scarce. In 1965, a catastrophic underground underground (17). When these fractures reach the surface, they blowout occurred during the drilling of a gas well in The Netherlands, may negatively impact the chemistry of shallow groundwater by which led to the uncontrolled release of large amounts of natural gas the massive introduction of methane (18). from the reservoir to the surface. In this study, the remaining impact In this study, we investigated the long-term effect of an un- on methane chemistry in the overlying aquifers was investigated. -
C:\Myfiles\Genealogy & Family\Family Books\WW2 Timeline
A World War II Timeline A Perspective from within The Netherlands Compiled by Jo Kruithof - December 2004 01 12 April 1945 Canadian troops liberate the town of Steenwijk, where I was staying with my family at the time I was six years old then. A World War II Timeline a Perspective from within The Netherlands INTRODUCTION This document is based entirely on information and pictures found on the Internet. It is a brief illustrated timeline of the events of World War 2, as seen from within the Netherlands. When I first came across a basic timeline on the (Dutch) web site http://hetillegaleparool.nl, it occurred to me that, if I ever got around to writing up my life’s story, this would paint a good picture of the background against which I lived my first six years. However, before it would be any use to my descendants, I would either have to translate it, or find an alternative in the English language. Any writings presenting the unique view of the war by Dutch people living in the Netherlands is much more likely to be in Dutch than in English (and a quick scan of the Net supported this notion), so I decided on the translation option. In the process of checking out a few facts, events and names, I came across large amounts of other material, but I have only used those bits and pieces that helped to flesh out my timeline into a record that can be read and understood by those who weren’t there or who haven’t heard the stories from parents or older relatives. -
Discord & Consensus
c Discor Global Dutch: Studies in Low Countries Culture and History onsensus Series Editor: ulrich tiedau DiscorD & Discord and Consensus in the Low Countries, 1700–2000 explores the themes D & of discord and consensus in the Low Countries in the last three centuries. consensus All countries, regions and institutions are ultimately built on a degree of consensus, on a collective commitment to a concept, belief or value system, 1700–2000 TH IN IN THE LOW COUNTRIES, 1700–2000 which is continuously rephrased and reinvented through a narrative of cohesion, and challenged by expressions of discontent and discord. The E history of the Low Countries is characterised by both a striving for consensus L and eruptions of discord, both internally and from external challenges. This OW volume studies the dynamics of this tension through various genres. Based C th on selected papers from the 10 Biennial Conference of the Association OUNTRI for Low Countries Studies at UCL, this interdisciplinary work traces the themes of discord and consensus along broad cultural, linguistic, political and historical lines. This is an expansive collection written by experts from E a range of disciplines including early-modern and contemporary history, art S, history, film, literature and translation from the Low Countries. U G EDIT E JANE FENOULHET LRICH is Professor of Dutch Studies at UCL. Her research RDI QUIST AND QUIST RDI E interests include women’s writing, literary history and disciplinary history. BY D JAN T I GERDI QUIST E is Lecturer in Dutch and Head of Department at UCL’s E DAU F Department of Dutch.