Silica gel in a fault slip surface: Field evidence for palaeo-earthquakes?

Faber, Carly, Rowe, Christie D., Miller, Jodie A., Fagereng, Ake ORCID: https://orcid.org/0000-0001-6335-8534 and Neethling, Jan H. 2014. Silica gel in a fault slip surface: Field evidence for palaeo-earthquakes? Journal of Structural Geology 69 (A) , pp. 108-121. 10.1016/j.jsg.2014.09.021

Full text not available from this repository.

Abstract

High-velocity friction experiments have shown an almost complete loss of strength associated with silica gel formation on slip surfaces. The identification of frictional silica gel products in palaeo-seismic faults is, however, problematic, because there are multiple natural sources of silica gel and recrystallization of gel to quartz complicates preservation. The importance of gel formation on natural faults is therefore unknown. Here, we report a structurally distinct and semi-continuous, 0.5 – 10 mm thick layer of microcrystalline quartz along a major carbonate-hosted fault, the Olive fault, in the Naukluft Nappe Complex, Namibia. The quartz layer is distinguished by flow banding-like textures and unusual cathodoluminescence characteristics. The layer consists of ∼2-20 μm hexagonal quartz crystals, which include distinct, crystalline, pore-bearing micro-to nano-spheres, separated by pore geometries indicative of volumetric contraction, and with grain boundaries enriched in aluminium. We interpret these features to indicate that the quartz crystals formed from recrystallization and dehydration of a silica gel. Because it is found in a carbonate-hosted fault and crosscuts lithological layering, the silica source is not from comminution of local wall rocks. Rather, the gel likely formed from reshear of a quartz-coated fault surface, or incremental shear slip associated with precipitation of silica driven by co-seismic pressure drops. This example of fault-related silica gel may have formed by a different mechanism than the gels produced in high-velocity friction experiments, but once formed, may have comparable rheological effects.

Item Type:	Article
Date Type:	Publication
Status:	Published
Schools:	Earth and Environmental Sciences
Subjects:	Q Science > QE Geology
Uncontrolled Keywords:	silica gel; palaeo-earthquakes; velocity weakening; fault vein
Additional Information:	Available online 16 Oct 2014
Publisher:	Elsevier
ISSN:	0191-8141
Date of Acceptance:	14 September 2014
Last Modified:	27 Oct 2022 09:28
URI:	https://orca.cardiff.ac.uk/id/eprint/66020

Citation Data

Cited 24 times in Scopus. View in Scopus. Powered By Scopus® Data

Actions (repository staff only)

Edit Item