Physical models of normal-fault relays between variably offset grabens
Journal Article
·
· AAPG Bulletin
OSTI ID:127725
- Univ. of Texas, Austin, TX (United States)
- Universite de Nice (France)
We conducted a series of scaled models in which two grabens initially offset along the direction of regional extension subsequently propagated freely along strike while synkinematic sediments were added. Models comprised a thick layer of dry sand overlying a thin lubricating layer of viscous silicone. The experiments are applicable to both crustal scale and to the scale of a brittle sedimentary cover above a salt or shale decollement. Results show that fault orientation and linkage vary with graben offset ({Delta}L) and model thickness (h). Grabens with small offset (O < {Delta}L< h/2) propagated along strike while remaining perpendicular to the direction of regional extension; the grabens eventually linked. Fault traces were initially jagged but straightened after further extension and sedimentation. Grabens with moderate offsets (h/2 < {Delta}L < 2h) widened as they propagated toward each other. Soft fault linkage created ramps of strained overburden blocks between faults. Later, ramps were cut by hard-linked faults. Hour-glass structures formed where faults of opposite vergence intersected. Fault slip progressively decreased along strike. Where graben offset was large ({Delta}L > 2h), a transtensional graben was generated oblique to the direction of regional extension, providing hard linkage with each initial graben. Fault-slip gradients along fault strike remained low. We infer that formation of a new oblique graben reflects a size threshold above which the rock volume between the grabens (proportional to graben offset) cannot rotate or deform by soft linkage to accommodate deformation.
- OSTI ID:
- 127725
- Report Number(s):
- CONF-950995--
- Journal Information:
- AAPG Bulletin, Journal Name: AAPG Bulletin Journal Issue: 8 Vol. 79; ISSN 0149-1423; ISSN AABUD2
- Country of Publication:
- United States
- Language:
- English
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