Facies model for a coarse-grained, tide-influenced delta : Gule Horn Formation (Early Jurassic), Jameson Land, Greenland


Autoria(s): Eide, Christian Haug; Howell, John A; Buckley, Simon J.; Martinius, Allard W; Terje Oftedal, Bjørn; Henstra, Gijs A.
Contribuinte(s)

University of Aberdeen, Geosciences, Geology & Petroleum Geology

University of Aberdeen, Energy

Data(s)

15/09/2016

15/09/2016

26/05/2016

Resumo

Acknowledgements: Funding for this project was provided from the Research Council of Norway through the Petromaks project 193059 and the FORCE Safari Project. Arild Andresen (University of Oslo) and Aka Lynge (POLOG) are thanked for logistical support, Björn Nyberg (Uni Research CIPR and University of Bergen) for assistance in the field, Arve Næss (Statoil) for providing data and assistance during the planning phase, Julien Vallet and Huges Fournier (Helimap Systems SA) for data acquisition. Riegl LMS GmbH is acknowledged for software support. We thank Brian Willis and an anonymous reviewer for their insightful and thorough reviews and Mariano Marzo for editorial comments.

Peer reviewed

Publisher PDF

Identificador

Eide , C H , Howell , J A , Buckley , S J , Martinius , A W , Terje Oftedal , B & Henstra , G A 2016 , ' Facies model for a coarse-grained, tide-influenced delta : Gule Horn Formation (Early Jurassic), Jameson Land, Greenland ' Sedimentology . , 10.1111/sed.12270

0037-0746

PURE: 64679451

PURE UUID: 82d41e91-3416-45f4-a144-58411edc58e8

http://hdl.handle.net/2164/7479

http://dx.doi.org/10.1111/sed.12270

Idioma(s)

eng

Relação

Sedimentology

Direitos

© 2016 The Authors. Sedimentology © 2016 International Association of Sedimentologists This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

Palavras-Chave #delta #deltaic #Elis Bjerg #facies model #tidal bar #tidal delta #tide-dominated #Tilje Formation #QE Geology #QE
Tipo

Journal article