TY - JOUR
T1 - Application of geometric models to inverted listric fault systems in sandbox experiments. Paper 1
T2 - 2D hanging wall deformation and section restoration
AU - Yamada, Yasuhiro
AU - McClay, Ken
N1 - Funding Information:
This work is based on YY's PhD research at Royal Holloway University of London, and further developed at JAPEX Research Centre. The analogue modelling was supported by the Fault Dynamics Project, sponsored by ARCO British Ltd, PETROBRAS UK Ltd, BP Exploration, Conoco (UK) Ltd, Mobil North Sea Ltd, and Sun Oil Britain. JNOC and JAPEX are thanked for their financial support during YY's stay at Royal Holloway (1994–1996). The earlier version of the manuscript was greatly improved after constructive comments by Takashi Tsuji at JAPEX. Rasoul Sorkhabi and Fumio Akiba carefully reviewed the manuscript. Journal reviews by Fabrizio Storti and Steve Wojtal are also acknowledged for their constructive criticism.
PY - 2003/9
Y1 - 2003/9
N2 - Fault geometry is a primary control on hanging wall deformation. In order to examine their geometrical relationships, a positive inversion analogue experiment was conducted using a rigid fault surface of listric geometry. The hanging wall deformation observed on a representative vertical section was examined with conventional 2D geometric models, and was restored to its pre-inversion phase with two techniques. These results suggest that the deformation can be best approximated by inclined simple shearing (ISS). The ISS model can determine the inclination of the apparent shear plane and the amount of apparent horizontal shortening, which is equivalent to that calculated with the conventional depth-to-detachment method. This estimated apparent shortening was generally smaller than the actual amount of the experiments, probably due to tectonic compaction.
AB - Fault geometry is a primary control on hanging wall deformation. In order to examine their geometrical relationships, a positive inversion analogue experiment was conducted using a rigid fault surface of listric geometry. The hanging wall deformation observed on a representative vertical section was examined with conventional 2D geometric models, and was restored to its pre-inversion phase with two techniques. These results suggest that the deformation can be best approximated by inclined simple shearing (ISS). The ISS model can determine the inclination of the apparent shear plane and the amount of apparent horizontal shortening, which is equivalent to that calculated with the conventional depth-to-detachment method. This estimated apparent shortening was generally smaller than the actual amount of the experiments, probably due to tectonic compaction.
UR - http://www.scopus.com/inward/record.url?scp=0038344169&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0038344169&partnerID=8YFLogxK
U2 - 10.1016/S0191-8141(02)00181-5
DO - 10.1016/S0191-8141(02)00181-5
M3 - Article
AN - SCOPUS:0038344169
SN - 0191-8141
VL - 25
SP - 1551
EP - 1560
JO - Journal of Structural Geology
JF - Journal of Structural Geology
IS - 9
ER -