Tectonic development, thermal regimes and hydrocarbon habitat of transform margins, and their differences from rifted margins – an introduction

Author:

Nemčok M.12ORCID,Doran H.3,Doré A. G.1,Ledvényiová L.12,Rybár S.24,Staniaszek S.5,Gontar T.5

Affiliation:

1. Energy and Geoscience Institute at University of Utah, 423 Wakara Way, Suite 300, Salt Lake City, UT 84108, USA

2. Faculty of Mining and Geology, VŠB-Technical University of Ostrava, 17. listopadu 15, Ostrava, Czech Republic

3. Ola Geoscience, 11 Castlevennon Road, Katesbridge, Banbridge BT325QA, Northern Ireland

4. Department of Geology and Paleontology, Comenius University, Ilkovičova 6, Bratislava, Slovakia

5. Faculty of Geology, University of Warszaw, Krakowskie Przedmieście 26/28, Warsaw, Poland

Abstract

AbstractDrilling, 3D seismic and deep seismic studies in recent years have significantly progressed our knowledge of continental margins. Some of the key studies are brought together in this volume, focusing on the evolution and architecture of transform faults and transform margins, giving special attention to the relationship, and differences, between transform and rift margins. Papers from a wide range of global settings consider thermal history, depositional regime, hydrocarbon prospectivity and (in a continental setting) geothermal potential. This scene-setting paper examines our current state of knowledge on transform and rift settings, and provides a brief introduction to the subject matter and context of the papers in the volume.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference232 articles.

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2. Addis, D., Brown, A., Grant, J., Kline, P., Layman, J. and Towle, P. 2013b. Influences of tectonics, drainage and sediment supply on Upper Cretaceous deepwater deposits in the Deep Ivorian Basin of Western Ghana and Cote d'Ivoire. The 12th PESGB/HGS Conference on African E&P, Wembley Stadium, London, 10–11 September, extended abstracts.

3. Anderson, E.M. 1951. The Dynamics of Faulting and Dyke Formation with Application to Britain. Oliver & Boyd, Edinburgh.

4. Rift–shear architecture and tectonic development of the Ghana margin deduced from multichannel seismic reflection and potential field data

5. Westward migration of extension in the northern Gulf of California, Mexico

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