TY - CONF
T1 - Hangingwall deformation above inverted 3D listric fault systems - Insights from experiments and section-balancing techniques
AU - Yamada, Yasuhiro
AU - McClay, Ken
N1 - Funding Information:
This work is based on YY s Ph.D. research at Geology Department, Royal Holloway University of London, and further developed at JAPEX Research Center. The analogue modelling was supported by the Fault Dynamics Project. JNOC and JAPEX are thanked for their financial support during YY s stay at Royal Holloway (1994-1996).
Publisher Copyright:
© 2001 Society of Exploration Geophysicists. All rights reserved.
PY - 2001
Y1 - 2001
N2 - Fault geometry is a primary control on hangingwall deformation. In this study, a series of inversion analogue experiments was conducted by using rigid fault surfaces of spoon-like true 3D geometries. The hangingwall geometry on serial sections of the experiments was then examined with conventional 2D geometric models. The deformation geometry of the hangingwall has an along-strike variation corresponding to the 3D geometry of the underlying detachment. The apparent shear plane inclination and the estimated shortening also show a systematic change along strike. These changes suggest that the hangingwall displacement had an along-strike element during deformation; the hangingwall material moves from the regions above salients to those above embayments in the detachment surface during contraction. The data presented in this paper help us understand 3D geometric relations between the hangingwall deformation and the underlying detachment surfaces.
AB - Fault geometry is a primary control on hangingwall deformation. In this study, a series of inversion analogue experiments was conducted by using rigid fault surfaces of spoon-like true 3D geometries. The hangingwall geometry on serial sections of the experiments was then examined with conventional 2D geometric models. The deformation geometry of the hangingwall has an along-strike variation corresponding to the 3D geometry of the underlying detachment. The apparent shear plane inclination and the estimated shortening also show a systematic change along strike. These changes suggest that the hangingwall displacement had an along-strike element during deformation; the hangingwall material moves from the regions above salients to those above embayments in the detachment surface during contraction. The data presented in this paper help us understand 3D geometric relations between the hangingwall deformation and the underlying detachment surfaces.
UR - http://www.scopus.com/inward/record.url?scp=85054083358&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85054083358&partnerID=8YFLogxK
M3 - Paper
AN - SCOPUS:85054083358
T2 - 2001 Society of Exploration Geophysicists Annual Meeting, SEG 2001
Y2 - 9 September 2001 through 14 September 2001
ER -